Alabama: Denial of State Coal Combustion Residuals Permit Program, 55220-55274 [2023-17023]
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ENVIRONMENTAL PROTECTION
AGENCY
40 CFR Part 257
[EPA–HQ–OLEM–2022–0903; FRL 11262–
01–OLEM]
Alabama: Denial of State Coal
Combustion Residuals Permit Program
Environmental Protection
Agency (EPA).
ACTION: Notice of availability; request
for comment.
AGENCY:
Pursuant to section 4005(d) of
the Resource Conservation and
Recovery Act (RCRA), the
Environmental Protection Agency (EPA
or the Agency) is proposing to deny the
Alabama Department of Environmental
Management’s (ADEM or Department)
Application for approval of the Alabama
coal combustion residuals (CCR) permit
program (Application). After reviewing
the State CCR permit program
Application submitted by ADEM on
December 29, 2021, and additional
relevant materials, and based on
extensive discussions with ADEM
regarding its Application, EPA has
preliminarily determined that
Alabama’s CCR permit program does not
meet the standard for approval under
RCRA. This document announces that
EPA is seeking comment on this
proposal during a 60-day public
comment period and will be holding an
in-person public hearing on EPA’s
proposed denial of Alabama’s CCR
permit program.
DATES:
Comments due. Comments must be
received on or before October 13, 2023.
Public Hearing: EPA will hold an inperson public hearing on September 20,
2023, and a virtual public hearing on
September 27, 2023. Please refer to the
SUPPLEMENTARY INFORMATION section for
additional information on the public
hearing.
SUMMARY:
You may send comments,
identified by Docket ID No. EPA–HQ–
OLEM–OLEM–2022–0903, by any of the
following methods:
• Federal eRulemaking Portal:
https://www.regulations.gov/ (our
preferred method). Follow the online
instructions for submitting comments.
• Mail: U.S. Environmental
Protection Agency, EPA Docket Center,
Office of Land and Emergency
Management (OLEM) Docket, Mail Code
28221T, 1200 Pennsylvania Ave. NW,
Washington, DC 20460.
• Hand Delivery or Courier (by
scheduled appointment only): EPA
Docket Center, WJC West Building,
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ADDRESSES:
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Room 3334, 1301 Constitution Avenue
NW, Washington, DC 20004. The Docket
Center’s hours of operations are 8:30
a.m.–4:30 p.m., Monday–Friday (except
Federal holidays).
Instructions: All submissions received
must include the Docket ID No. for this
rulemaking. Comments received may be
posted without change to https://
www.regulations.gov/, including any
personal information provided. For
detailed instructions on sending
comments and additional information
on the rulemaking process, see the
‘‘Public Participation’’ heading of the
SUPPLEMENTARY INFORMATION section of
this document.
FOR FURTHER INFORMATION CONTACT:
Michelle Lloyd, Office of Resource
Conservation and Recovery, Materials
Recovery and Waste Management
Division, U.S. Environmental Protection
Agency, 1200 Pennsylvania Avenue
NW, MC: 5304T, Washington, DC
20460; telephone number: (202) 566–
0560; email address: lloyd.michelle@
epa.gov. For more information on this
notice please visit https://www.epa.gov/
coalash.
SUPPLEMENTARY INFORMATION:
Table of Contents
I. Public Participation
A. Written Comments
B. Participation in In-Person Public
Hearing
C. Participation in Virtual Public Hearing
II. General Information
A. Overview of Proposed Action
B. Background
C. Statutory Authority
III. The Alabama CCR Permit Program
Application
A. Alabama CCR Units and Resources
B. Alabama CCR Regulations
C. Alabama Authority To Regulate CCR
D. Alabama Permits
E. Summary of EPA Communications With
Alabama
IV. EPA Analysis of the Alabama Application
and Basis for Denial
A. Legal Authority To Evaluate State CCR
Program Submittals
1. The Statute Requires EPA To Consider
a State’s CCR Permits When Determining
Whether To Approve the Program if the
Information Is Available
2. EPA Is Not Required To Approve a
Deficient State Program and Then
Redress the Deficiencies Through
RCRA’s Program Review Provisions
B. EPA’s Analysis of the Alabama CCR
Regulations
1. Adequacy of Technical Criteria
2. Review of Generally Applicable
Alabama CCR Permit Program Statutes
and Regulations
C. EPA’s Analysis of Alabama’s Permits
Issued Under the State CCR Regulations
1. Colbert Fossil Plant
2. Plant Gadsden
3. Plant Gorgas
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4. Plant Greene County
5. EPA conclusion About Alabama’s
Implementation of the CCR Regulations
V. Proposed Action
List of Acronyms
ACM Assessment of Corrective Measures
ADEM Alabama Department of
Environmental Management
ASD alternative source demonstration
BGS below ground surface
CBI Confidential Business Information
CCP coal combustion product
CCR coal combustion residuals
CD Consent Decree
CFR Code of Federal Regulations
CY cubic yards
eFile electronic filing system
EPA Environmental Protection Agency
EPRI Electric Power Research Institute
FR Federal Register
GWMCA groundwater monitoring and
corrective action
GWMP Groundwater Monitoring Plan
GWPS groundwater protection standard
HSWA Hazardous and Solid Waste
Amendments
ICR Information Collection Request
MCL maximum contaminant level
MNA Monitored Natural Attenuation
MSL mean sea level
NOPV Notice of Potential Violation
NPDES National Pollutant Discharge
Elimination System
RCRA Resource Conservation and Recovery
Act
RTC Response to Comments
SSI statistically significant increase
SSL statistically significant level
TSD Technical Support Document
TVA Tennessee Valley Authority
USGS U.S. Geological Survey
USWAG Utility Solid Waste Activities
Group
WBWT waste below the water table
WIIN Water Infrastructure Improvements
for the Nation
I. Public Participation
A. Written Comments
Submit your comments, identified by
Docket ID No. EPA–HQ–OLEM–OLEM–
2022–0903, at https://
www.regulations.gov (our preferred
method), or the other methods
identified in the ADDRESSES section.
Once submitted, comments cannot be
edited or removed from the docket. EPA
may publish any comment received to
its public docket. Do not submit to
EPA’s docket at https://
www.regulations.gov any information
you consider to be Confidential
Business Information (CBI) or other
information whose disclosure is
restricted by statute. Multimedia
submissions (audio, video, etc.) must be
accompanied by a written comment.
The written comment is considered the
official comment and should include
discussion of all points you wish to
make. EPA will generally not consider
comments or comment contents located
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outside of the primary submission (i.e.,
on the web, cloud, or other file sharing
system). For additional submission
methods, the full EPA public comment
policy, information about CBI or
multimedia submissions, and general
guidance on making effective
comments, please visit https://
www.epa.gov/dockets/commenting-epadockets.
B. Participation in In-Person Public
Hearing
EPA will begin pre-registering
speakers for the hearing upon
publication of this document in the
Federal Register. To register to speak at
the hearing, please use the online
registration form available on EPA’s
CCR website (https://www.epa.gov/
coalash) or contact the person listed in
the FOR FURTHER INFORMATION CONTACT
section to register to speak at the
hearing. The last day to pre-register to
speak at the hearing will be September
18, 2023.
EPA will make every effort to follow
the schedule as closely as possible on
the day of the hearing; however, please
plan for the hearings to run either ahead
of schedule or behind schedule.
Additionally, requests to speak will be
taken the day of the hearing at the
hearing registration desk. EPA will
make every effort to accommodate all
speakers who arrive and register,
although preferences on speaking times
may not be able to be fulfilled.
Each commenter will have five (5)
minutes to provide oral testimony. EPA
encourages commenters to provide EPA
with a copy of their oral testimony
electronically by emailing it to the
person listed in the FOR FURTHER
INFORMATION CONTACT section. EPA also
recommends submitting the text of your
oral comments as written comments to
the rulemaking docket. If EPA is
anticipating a high attendance, the time
allotment per testimony may be
shortened to no shorter than three (3)
minutes per person to accommodate all
those wishing to provide testimony and
who have pre-registered. While EPA
will make every effort to accommodate
all speakers who do not pre-register,
opportunities to speak may be limited
based upon the number of pre-registered
speakers. Therefore, EPA strongly
encourages anyone wishing to speak to
pre-register. Participation in the public
hearing does not preclude any entity or
individual from submitting a written
comment.
EPA may ask clarifying questions
during the oral presentations but will
not respond to the presentations at that
time. Written statements and supporting
information submitted during the
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comment period will be considered
with the same weight as oral comments
and supporting information presented at
the public hearing.
Please note that any updates made to
any aspect of the hearing are posted
online at EPA’s CCR website at https://
www.epa.gov/coalash. While EPA
expects the hearing to go forward as set
forth above, please monitor our website
or contact the person listed in the FOR
FURTHER INFORMATION CONTACT section to
determine if there are any updates. EPA
does not intend to publish a document
in the Federal Register announcing
updates.
If you require the services of an
interpreter or special accommodations
such as audio description, please preregister for the hearing with the person
listed in the FOR FURTHER INFORMATION
CONTACT section and describe your
needs by September 6, 2023. EPA may
not be able to arrange accommodations
without advance notice.
C. Participation in Virtual Public
Hearing
EPA will begin pre-registering
speakers for the hearing upon
publication of this document in the
Federal Register. To register to speak at
the virtual hearing, please use the
online registration form available on
EPA’s CCR website (https://
www.epa.gov/coalash) or contact the
person listed in the FOR FURTHER
INFORMATION CONTACT section to register
to speak at the hearing. The last day to
pre-register to speak at the hearing will
be September 25, 2023.
EPA will make every effort to follow
the schedule as closely as possible on
the day of the hearing; however, please
plan for the hearing to run either ahead
of schedule or behind schedule.
Additionally, requests to speak will be
taken the day of the hearing according
to the procedures specified on EPA’s
CCR website (https://www.epa.gov/
coalash) for this hearing. The Agency
will make every effort to accommodate
all speakers who arrive and register,
although preferences on speaking times
may not be able to be fulfilled.
Each commenter will have five (5)
minutes to provide oral testimony. EPA
encourages commenters to provide EPA
with a copy of their oral testimony
electronically (via email) to the person
listed in the FOR FURTHER INFORMATION
CONTACT section. If EPA is anticipating
a high attendance, the time allotment
per testimony may be shortened to no
shorter than three (3) minutes per
person to accommodate all those
wishing to provide testimony and who
have pre-registered. While EPA will
make every effort to accommodate all
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speakers who do not pre-register,
opportunities to speak may be limited
based upon the number of pre-registered
speakers. Therefore, EPA strongly
encourages anyone wishing to speak to
pre-register. Participation in the virtual
public hearing does not preclude any
entity or individual from submitting a
written comment.
EPA may ask clarifying questions
during the oral presentations but will
not respond to the presentations at that
time. Written statements and supporting
information submitted during the
comment period will be considered
with the same weight as oral comments
and supporting information presented at
the public hearing. Verbatim transcripts
of the hearings and written statements
will be included in the docket for this
action.
Please note that any updates made to
any aspect of the hearing will be posted
online on EPA’s CCR website at https://
www.epa.gov/coalash. While EPA
expects the hearing to go forward as set
forth above, please monitor our website
or contact the person listed in the FOR
FURTHER INFORMATION CONTACT section to
determine if there are any updates. EPA
does not intend to publish a document
in the Federal Register announcing
updates.
If you require the service of a
translator, please pre-register for the
hearing and describe your needs on the
registration form by September 13, 2023.
If you require special accommodations
such as audio description or closed
captioning, please pre-register for the
hearing and describe your needs on the
registration form by September 13, 2023.
Alternatively, registrants may notify the
person listed in the FOR FURTHER
INFORMATION CONTACT section of any
special needs. We may not be able to
arrange accommodations without
advanced notice.
II. General Information
A. Overview of Proposed Action
On April 17, 2015, EPA published a
final rule, creating 40 CFR part 257,
subpart D,1 that established a
comprehensive set of minimum Federal
requirements for the disposal of CCR in
landfills and surface impoundments (80
FR 21302) (‘‘Federal CCR regulations’’).
Section 2301 of the 2016 Water
Infrastructure Improvements for the
Nation (WIIN) Act amended section
4005 of RCRA, creating a new
subsection (d) that establishes a Federal
CCR permit program that is similar to
the permit programs under RCRA
1 Unless otherwise specified, all references to part
257 and part 239 in this notice are to title 40 of the
Code of Federal Regulations (CFR).
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subtitle C and other environmental
statutes. See 42 U.S.C. 6945(d).
RCRA section 4005(d) also allows
states to seek approval for a State CCR
permit program that will operate in lieu
of a Federal CCR permit program in the
State. The statute provides that within
180 days after a State submits an
application to the Administrator for
approval, EPA shall approve the State
permit program if the Administrator
determines that the State program
requires each CCR unit located in the
State to achieve compliance with either
the Federal requirements or other State
requirements that EPA determines, after
consultation with the State, are at least
as protective as those included in the
Federal CCR regulations. See, 42 U.S.C.
6945(d)(1)(B).
On December 29, 2021, ADEM
submitted its State CCR permit program
Application to EPA Region 4 requesting
approval of the State’s partial CCR
permit program.2 3 ADEM established
State CCR regulations that mirrored the
provisions in the Federal CCR
regulations with additional Statespecific provisions and clarifications.
Though ADEM primarily adopted the
language in the Federal CCR regulations,
EPA reviewed both proposed and final
permits Alabama issued under its CCR
program and concluded that ADEM was
interpreting its State regulations in a
manner inconsistent with the plain
language of the Federal requirements,
and that, as a result, the permits for CCR
units in the State contain permit terms
that are neither the same as, nor as
protective as, the Federal CCR
regulations. Specifically, EPA identified
deficiencies in ADEM’s permits with
respect to the closure requirements for
unlined surface impoundments and the
associated groundwater monitoring
network and corrective action
requirements. EPA discussed these
issues with ADEM, and, despite EPA’s
concerns, the State declined to modify
the existing permits and proceeded to
issue another CCR permit with the same
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2 Alabama
Department of Environmental
Management. Application For CCR Permit Program
Approval. December 2021.
3 In the December 29, 2021 Application, Alabama
sought a partial program approval (rather than full
program approval) of the State’s CCR permit
program because it is not seeking approval for some
of its CCR regulations. Specifically, ADEM is not
seeking approval for six items that are listed in Unit
IV.B.1.b of this preamble and in the Technical
Support Document Volume III. See Volume III:
Technical Support Document for the Proposed
Notice to Deny Alabama’s Coal Combustion
Residuals Permit Program, EPA Analysis of
Alabama CCR Permitting and Technical
Regulations. U.S. Environmental Protection Agency,
Office of Land and Emergency Management
(5304T), 1200 Pennsylvania Avenue NW,
Washington, DC 20460. August 2023.
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deficient provisions. Further, ADEM
failed to adequately explain how the
permits ensured that each CCR unit
would achieve compliance with either
the Federal requirements or other State
requirements that are at least as
protective as the requirements in the
Federal CCR regulations.
EPA is proposing to deny Alabama’s
request for approval of its CCR permit
program Application pursuant to RCRA
section 4005(d)(1)(B), because the
State’s program does not meet either
standard for approval. 42 U.S.C.
6945(d)(1)(B).
B. Background
CCR are generated from the
combustion of coal, including solid
fuels classified as anthracite,
bituminous coal, subbituminous coal,
and lignite, for the purpose of
generating steam to power a generator to
produce electricity or electricity and
other thermal energy by electric utilities
and independent power producers.
CCR, commonly known as coal ash,
include fly ash, bottom ash, boiler slag,
and flue gas desulfurization materials.
As noted above, on April 17, 2015,
EPA published a final rule that
established a comprehensive set of
minimum Federal requirements in 40
CFR part 257, subpart D for the disposal
of CCR in landfills and surface
impoundments. The rule created a selfimplementing program that regulates
the location, design, operating criteria,
and groundwater monitoring and
corrective action for CCR units, as well
as the closure and post-closure care of
CCR units. The rule also includes
requirements for recordkeeping and
notifications for CCR units. EPA has
since amended 40 CFR part 257, subpart
D (81 FR 51802, August 5, 2016), (83 FR
36435, July 30, 2018), (85 FR 53516,
August 28, 2020), (85 FR 72506,
November 12, 2020). More information
on these rules is provided in the
Technical Support Document (TSD)
Volume III.
C. Statutory Authority
EPA is issuing this proposed action
pursuant to sections 4005(d) and
7004(b)(1) of RCRA. See 42 U.S.C.
6945(d) and 6974(b)(1). As stated above,
section 2301 of the WIIN Act amended
section 4005 of RCRA, creating a new
subsection (d) that establishes a Federal
CCR permitting program similar to
permit programs under RCRA subtitle C
and other environmental statutes. See
42 U.S.C. 6945(d).
Under RCRA section 4005(d)(1)(A), 42
U.S.C. 6945(d)(1)(A), states seeking
approval of a permit program must
submit to the Administrator, ‘‘in such
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form as the Administrator may
establish, evidence of a permit program
or other system of prior approval and
conditions under [S]tate law for
regulation by the State of coal
combustion residuals units that are
located in the State.’’ EPA shall approve
a State permit program if the
Administrator determines that the State
program requires each CCR unit located
in the State to achieve compliance with
either: (1) The Federal CCR
requirements at 40 CFR part 257,
subpart D; or (2) Other State criteria that
the Administrator, after consultation
with the State, determines to be ‘‘at least
as protective as’’ the Federal
requirements. See 42 U.S.C.
6945(d)(1)(B). The Administrator must
make a final determination, after
providing for public notice and an
opportunity for public comment, within
180 days of determining that the State
has submitted a complete application
consistent with RCRA section
4005(d)(1)(A).4 See 42 U.S.C.
6945(d)(1)(B). EPA may approve a State
CCR permit program in whole or in part.
Id. Once approved, the State permit
program operates in lieu of the Federal
requirements. See 42 U.S.C.
6945(d)(1)(A). In a State with a partial
permit program, only the State
requirements that have been approved
operate in lieu of the Federal
requirements, and facilities remain
responsible for compliance with all
remaining non-State approved
requirements in 40 CFR part 257,
subpart D.
As noted above, the Federal CCR
regulations are self-implementing and
that means that CCR landfills and
surface impoundments must comply
with the terms of the rule even prior to
obtaining a Federal permit or permit
issued by an approved State, and
noncompliance with any requirement of
the Federal CCR regulations can be
directly enforced against the facility.
Once a final CCR permit is issued by an
approved State or pursuant to a Federal
CCR permit program, however, the
terms of the permit apply in lieu of the
terms of the Federal CCR regulations
and/or requirements in an approved
State program, and RCRA section
4005(d)(3) provides a permit shield
against direct enforcement of the
applicable Federal or State CCR
regulations (meaning the permits terms
4 See U.S. Environmental Protection Agency. Coal
Combustion Residuals State Permit Program
Guidance Document; Interim Final, August 2017,
Office of Land and Emergency Management,
Washington, DC 20460 (providing that the 180-day
deadline does not start until EPA determines the
application is complete).
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become the enforceable requirements for
the permittee).
In addition, RCRA section 7004(b)
applies to all RCRA programs, directing
that ‘‘public participation in the
development, revision, implementation,
and enforcement of any. . .program
under this chapter shall be provided for,
encouraged, and assisted by the
Administrator and the States.’’ 42 U.S.C.
6974(b)(1).
III. The Alabama CCR Permit Program
Application
On December 29, 2021, ADEM
submitted its revised CCR permit
program Application to EPA Region 4.5
The Application requested approval of
the State’s partial CCR permit program.6
Alabama’s first CCR regulations were
promulgated in 2018 and continued to
be revised over the next several years in
response to public comment,
discussions between ADEM and EPA,
and changes to the Federal CCR
regulations in 40 CFR part 257, subpart
D.
EPA conducted an analysis of the
Alabama CCR permit program
Application, including a thorough
analysis of ADEM’s statutory authorities
for the CCR program, as well as
regulations at Alabama Administrative
Code Chapter. 335–13–15, Standards for
the Disposal of Coal Combustion
Residuals in Landfills and
Impoundments. This analysis is
discussed in Unit IV.B.2.b of this
preamble and in the TSD Volume III.
EPA also reviewed Alabama’s
permitting regulations, as well as recent
and ongoing permit decisions ADEM
was making under its CCR regulations.
A. Alabama CCR Units and Resources
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In the Program Narrative in the
Application, ADEM identified 16 units
that are currently, or have been, used for
disposal of CCR (3 landfills and 13
surface impoundments) in Alabama.
ADEM stated that it has the personnel
and funding to administer a CCR permit
program. The State also indicated that
its program is funded from three
sources: tipping fees collected for the
disposal of solid waste, permitting fees,
and civil penalties from enforcement
orders.
5 Application
to USEPA Region IV for CCCR
Permit Program Approval in Accordance with
Section 4005 of the Resource Conservation and
Recovery Act (RCRA) Alabama Department of
Environmental Management Land Division-Solid
Waste Branch. December 2021.
6 ADEM previously submitted CCR permit
program applications on July 12, 2018, and
February 26, 2021. For purposes of this proposed
action, EPA reviewed the most recent Application
submitted on December 29, 2021.
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B. Alabama CCR Regulations
ADEM Administrative Code Chapter
335–13–15 largely replicates the
requirements of 40 CFR part 257,
subpart D, for the portions of those
regulations for which the State is
seeking approval. In addition to the
technical criteria at ADEM Chapter 335–
13–15, ADEM has adopted State-specific
permitting requirements, including
public participation requirements, at
ADEM Administrative Code Chapter.
335–13–05. ADEM also has additional
reporting and approval requirements for
CCR units, as described in the TSD
Volume III.
C. Alabama Authority To Regulate CCR
ADEM derives its authority to operate
the Solid Waste Program, which
includes CCR, in Alabama pursuant to
the following statutory provisions of the
Code of Alabama, 1975: (1) Section 22–
22A–5 provides the Department with
the authority to administer and enforce
the State’s Solid Wastes and Recyclable
Materials Management Act, to adopt and
promulgate rules, regulations, and
standards through the Environmental
Management Commission, and to
develop environmental policy for the
State; and to serve as the State Agency
responsible for administering federallyapproved or federally-delegated
environmental programs; (2) Section
22–27–9 provides ADEM with authority
over the management of solid waste in
the State (except for the collection and
transportation of nonhazardous and
nonmedical solid waste) and the
permitting and operation of solid waste
management facilities; and (3) Section
22–27–12 provides ADEM with the
authority to promulgate and adopt rules
establishing requirements for the
management of solid waste and to issue
permits with conditions regarding the
management of such solid waste.
D. Alabama Permits
Unlike Georgia, Texas, and Oklahoma
(currently the only three States with
EPA approval for State CCR permit
programs), Alabama had already begun
implementing its State CCR permit
program and issuing permits prior to its
submittal of an Application for EPA
approval of the State’s CCR permit
program. At the time of submission of
ADEM’s December 29, 2021
Application, ADEM had issued permits
for the following CCR facilities: (1) the
James H. Miller Electric Generating
Plant (Permit #37–51; issued December
18, 2020); (2) Greene County Electric
Generating Plant (Permit #32–03: issued
December 18, 2020); (3) Gadsden Steam
Plant (Permit #28–09, issued December
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18, 2020); (4) James M. Barry Electric
Generating Plant (Permit #49–35, issued
July 1, 2021); (5) E.C. Gaston Electric
Generating Plant (Permit #59–16, issued
May 25, 2021); and (6) Charles R.
Lowman Power Plant (Permit #65–06,
issued August 30, 2021). At the time of
submission of the December 29, 2021
Application, permits were under
development by ADEM at two other
facilities: the William C. Gorgas Electric
Generating Plant and Tennessee Valley
Authority (TVA) Plant Colbert. Since
the submission of ADEM’s Application,
ADEM has proceeded to issue both the
Plant Gorgas Permit (Permit #64–12
issued February 28, 2022) and the TVA
Colbert Permit (Permit #17–11, issued
October 25, 2022).
E. Summary of EPA Communications
With Alabama
As part of EPA’s review of State CCR
permit programs, the Agency engages
the State both before and after submittal
of a State CCR permit program
application. These discussions serve a
number of purposes; for example, EPA
engages in these discussions to help the
State determine the scope of the CCR
permit program it wants to adopt (e.g.,
full or partial program) and to ensure
the State establishes the necessary State
CCR regulations prior to submitting the
request for program approval. EPA also
assists the State in determining what to
include in the Narrative Statement
component of its permit program
application, which serves as a roadmap
to the State’s CCR permit program. EPA
also uses these discussions to clarify
questions raised during the public
comment period about the State
program. To the extent the State
implements its CCR regulations prior to
EPA’s determination of State program
adequacy, EPA will also discuss the
State’s interpretation and
implementation of its program to ensure
that EPA fully understands the program
and to determine which of the two
statutory standards EPA will use to
evaluate the State program. EPA took
the same approach with Alabama as
with other states seeking approval, and,
as detailed below, EPA and ADEM have
had extensive discussions about the
State’s CCR permit program.7
7 EPA has attempted to identify all the
interactions between EPA and ADEM with respect
to the State’s CCR permit program. A summary of
the interactions between EPA and ADEM is
included in the docket to this notice in Volume II:
Technical Support Document for the Proposed
Notice to Deny Alabama’s Coal Combustion
Residuals Permit Program, Communication
Between EPA and ADEM. U.S. Environmental
Protection Agency Office of Land and Emergency
Management (5304T). August 2023. In addition,
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EPA began telephone calls and
meetings with ADEM about its
development of an Application for a
CCR permit program in January 2018
and continued them through July 2022.
In the early calls, EPA and ADEM
discussed the process for EPA to review
and approve State CCR permit
programs, ADEM’s plans for formally
adopting CCR regulations, its
anticipated timeline for submitting a
CCR permit program Application to
EPA, and ADEM’s permit requirements.
During these calls, EPA reviewed
ADEM’s submission and sent comments
to ADEM on those documents. The
frequency of calls between EPA and
ADEM varied depending on the stage of
ADEM’s efforts to develop and submit
(or re-submit) its CCR permit program
Application. For example, during
ADEM’s public comment periods
associated with State rulemaking, or
during periods of re-working regulations
or documents, calls were held less
frequently. When ADEM had questions
or requested EPA input, calls were held
more often.
After ADEM’s initial CCR regulations
became effective in 2018, the State
began to issue permits. Calls were then
held on specific facilities and technical
issues that ADEM sought EPA’s input
on, such as specific corrective action
proposed remedies or closure methods.
In addition, consistent with RCRA
section 4005(d), EPA began discussions
with ADEM on specific facilities and
permits to evaluate whether ADEM was
requiring, as part of its permit process,
each CCR unit in the State ‘‘to achieve
compliance with’’ the Federal part 257
standards or ‘‘other State criteria that
the Administrator, after consultation
with the State, determines to be at least
as protective as’’ the Federal criteria.
Of particular concern to the Agency
were facilities that were closing (or had
already closed) unlined CCR surface
impoundments while leaving waste (i.e.,
CCR) below the water table (WBWT). On
March 15, 2022, EPA shared a list of
such facilities in Alabama with ADEM
and scheduled discussions regarding the
closures and groundwater monitoring
activities at the Greene County Electric
Generating Plant and the Gadsden
Steam Plant. Discussions also focused
on the William C. Gorgas Electric
Generating Plant. ADEM had issued
permits at all three of these facilities.
During these discussions and written
communication, EPA expressed concern
that Alabama’s permit program
appeared to differ from the Federal
program, and that these differences
copies of emails and letters between EPA and
ADEM can be found in the docket.
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appeared to make the State’s program
less protective than the Federal
program. The Agency specifically
identified problems with the State’s
permit requirements covering closure of
unlined surface impoundments,
groundwater monitoring networks, and
corrective action. See also Unit IV.C of
this preamble below and the TSD
Volume I for a detailed discussion of the
deficiencies in ADEM’s CCR permits. In
addition to the concerns raised with
respect to Plants Greene, Gorgas, and
Gadsden, EPA has also raised concerns
with respect to the TVA Plant Colbert
permit. On June 29, 2022, ADEM posted
public notice of the draft permit for
Plant Colbert. Because the proposed
permit for Plant Colbert raised many of
the same issues already being discussed
with respect to Plants Greene, Gorgas,
and Gadsden, EPA submitted a letter to
ADEM outlining specific concerns with
respect to the proposed permit.8
As a result of these discussions, on
July 7, 2022, EPA informed ADEM via
telephone that the Agency was putting
on hold its completeness review of
ADEM’s CCR permit program
Application until Alabama
demonstrated to EPA that the State was
implementing its program consistent
with the Federal CCR regulations.
Further, EPA explained to ADEM that it
was exploring options for actions to take
at the Federal level with respect to both
the CCR permit program Application,
and at specific facilities where there are
outstanding concerns.
On October 25, 2022, ADEM
proceeded to issue a CCR permit to
Plant Colbert without revising the
proposed permit to address EPA’s
concerns. In a letter dated October 27,
2022, ADEM responded to EPA’s letter
regarding Plant Colbert, presenting an
interpretation of the requirements
applicable to closing CCR
impoundments that EPA had previously
rejected in the discussions about the
interpretation of the Federal CCR
regulations with ADEM described above
and in EPA’s Part A proposed and final
decisions. See discussion of Part A
proposals in Unit IV.C. of this preamble.
To date, the State has not taken action
to revise the permits issued to Plants
Colbert, Green, Gorgas, or Gadsden to
address the deficiencies EPA noted to
ADEM.
8 Letter from Carolyn Hoskinson, Director, Office
of Resource Conservation and Recovery, to Mr.
Russell A. Kelly, Chief, Permits and Services
Division, and Mr. Steve Cobb, Chief, Land Division.
EPA Comments on Proposed Permit, Tennessee
Valley Authority Colbert Fossil Plant, Alabama
Department of Environmental Management, Permit
No. 17–11. September 15, 2022.
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On December 9, 2022, ADEM gave
EPA notice of its intent to sue EPA
under section 7002(a)(1)(A) and (1)(B) of
RCRA, alleging EPA failed to perform a
nondiscretionary duty to approve the
State’s CCR permit program.9 Among
other things, ADEM asserted that EPA
failed to comply with the statutory
requirement to approve the State’s CCR
permit program within 180 days of the
State’s submittal of the permit program
Application on December 29, 2021. On
February 1, 2023, EPA responded to
ADEM’s Notice of Intent to Sue letter
and informed the State that the 180-day
timeframe does not start until EPA
determines that a State’s Application is
administratively complete and that, in
this case, EPA did not start the clock
because EPA’s concerns with ADEM’s
interpretation of the minimum
requirements of the Federal CCR
regulations had yet to be resolved and
EPA was providing an opportunity for
ADEM to submit further Application
information.10 EPA further stated that
the Agency could evaluate the State’s
program on the current record if ADEM
decided not to supplement its
Application with an explanation of how
the State’s interpretation of its
regulations is at least as protective as
the Federal CCR regulations, but EPA
expressed concern that the current
record would not support a proposal to
approve the State’s partial CCR permit
program. Id. On February 17, 2023,
ADEM responded to EPA that it did not
intend to supplement the record and
that EPA should evaluate its program
accordingly.11 EPA thereafter continued
to review the Application based on the
information submitted to date, and this
notice reflects EPA’s proposed
conclusions from that review.
IV. EPA Analysis of the Alabama
Application and Basis for Denial
As stated above, a State seeking
approval of a CCR permit program can
either adopt the Federal CCR
requirements or establish State-specific
criteria that are at least as protective as
the Federal CCR requirements. See 42
U.S.C. 6945(d)(1)(B). After a State
submits a complete application, EPA
evaluates the State program to
determine whether it ‘‘requires each
9 Letter from Alabama Attorney General Steve
Marshall to EPA Administrator Michael Regan,
Notice of Endangerment and Intent to Sue under
Section 7002(a)(1)(A) and (1)(B) of the Resource
Conservation and Recovery Act. December 9, 2022.
10 Letter from Barry Breen, Acting Assistant
Administrator, OLEM, to Lance LeFleur, Director,
ADEM, February 1, 2023. Email sent February 2,
2023.
11 Letter from Lance LeFleur, Director, ADEM, to
Barry Breen, Acting Assistant Administrator,
OLEM, February 17, 2023.
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coal combustion residuals unit located
in the state to achieve compliance with
the applicable [Federal or other equally
protective State] criteria.’’ Id.
Specifically, EPA evaluates the terms of
the permit program or other system of
prior approval and conditions and the
Narrative Statement, to determine
whether by its terms the State program
meets either of these standards for each
CCR unit regulated by the State. As
discussed in more detail below and in
the TSD Volume III, to make this
determination EPA evaluates not only
the CCR specific requirements but also
the State’s general authority to issue
permits and impose conditions in those
permits, as well as the State’s authority
for compliance monitoring and
enforcement.12 Thus, collectively, the
CCR specific and general permit
requirements must provide the State
with sufficient authority to require
compliance from all CCR units located
within the State. In addition, if the State
begins issuing CCR permits and
overseeing compliance with the permits
prior to EPA’s State program approval
decision, the Agency must also consider
whether the State in fact ‘‘requires each
CCR unit located in the state to achieve
compliance with’’ either the Federal
criteria in part 257 or other State criteria
that ‘‘are at least as protective as’’ the
Federal regulations. 42 U.S.C.
6945(d)(1)(B) (emphasis added). See
Unit IV.A of this preamble (discussing
the Agency interpretation of RCRA
section 4005(d)).
ADEM adopted regulations that
largely mirror the Federal CCR
regulations, but in some places ADEM
also added additional or different
criteria to be consistent with its existing
solid waste regulations. When a State
adopts the language in the Federal CCR
regulations, EPA’s review of the terms of
the permit program is generally
straightforward, and, in this case, EPA’s
review of the express terms of ADEM’s
CCR permit program demonstrates that
the State program includes all
regulatory provisions required for
approval of a partial program.13 Thus,
12 State permit program regulations usually
include general requirements that apply across
multiple permit programs (e.g., procedures for
issuing permits). When new performance standards
are issued for a type of facility or unit (for example,
CCR regulations), states include both general and
facility/unit specific requirements in the State
permit program as necessary to develop a program
that satisfies the Federal requirements to support
approval of a State program.
13 EPA conducted a thorough review of the terms
of Alabama’s CCR permit program submittal,
consistent with review of submittals by states that
were granted approval, and that review can be
found in the Volume III: Technical Support
Document for the Proposed Notice to Deny
Alabama’s Coal Combustion Residuals Permit
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the terms of the permit program provide
ADEM with the authority necessary to
issue permits that will ensure each CCR
unit in the State achieves the minimum
required level of control (i.e., the State
has the authority to issue permits that
require compliance with standards that
are at least as protective as those in the
Federal CCR regulations).
While the statutes and regulations of
the Alabama CCR permit program
provide the State with sufficient
authority to require compliance with the
Federal requirements or equivalent State
requirements, EPA is proposing to
determine that permits issued by ADEM
allow CCR units in the State to comply
with alternative requirements that are
less protective than the requirements in
the Federal CCR regulations with
respect to groundwater monitoring,
corrective action, and closure. For
example, as discussed in more detail in
subsequent sections, ADEM has issued
multiple permits allowing CCR in
closed units to remain saturated by
groundwater, without requiring any
engineering measures to control the
groundwater flowing into and out of the
closed unit. ADEM has also approved
groundwater monitoring systems that
contain an inadequate number of wells,
and in incorrect locations, to detect
groundwater contamination from the
CCR units. Finally, ADEM has issued
multiple permits that effectively allow
the permittee to delay implementation
of effective measures to remediate
groundwater contamination both onand off-site of the facility. Overall,
EPA’s review of the permit records
demonstrates a consistent pattern of
deficiencies in the permits and a lack of
oversight and independent evaluation of
facilities’ proposed permit terms on the
part of ADEM. In each case, EPA was
unable to locate any evaluation or
record of decision documenting that
ADEM had critically evaluated the
materials submitted as part of the permit
applications, or otherwise documented
its rationale for adopting those proposed
permit terms prior to approving the
application. As a consequence, EPA
cannot conclude that the permits are as
protective as the Federal CCR
regulations.
As noted above, EPA discussed many
of these issues with ADEM and the State
declined to revise the permits to be
consistent with the Federal CCR
regulations. ADEM also declined to
demonstrate that its alternative
requirements satisfy the requirement in
Program, EPA Analysis of Alabama CCR Permitting
and Technical Regulations. U.S. Environmental
Protection Agency, Office of Land and Emergency
Management (5304T), 1200 Pennsylvania Avenue
NW, Washington, DC 20460. August 2023.
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55225
RCRA section 4005(d)(1)(B). Instead, the
Alabama Attorney General, on behalf of
ADEM, asserted in the Notice of Intent
to Sue that EPA does not have the
authority to consider implementation of
the State program when determining
whether a State program is sufficient,
and that the Agency may only look to
the ‘‘four corners’’ of the State program
submission when evaluating the
program for approval. In the Notice of
Intent to Sue, the ‘‘four corners’’ of the
application are described as being
public participation, guidelines for
compliance, guidelines for enforcement
authority, and intervention in civil
enforcement proceedings. Regarding
deficiencies in implementation of a
State CCR permit program, the State of
Alabama’s position must, therefore, be
that EPA first approve a State CCR
permit program even if the Agency
knows the State’s implementation is
deficient prior to approval, and the
Agency must then follow the process for
withdrawal of the program through the
program review and withdrawal
provisions in RCRA sections
4005(d)(1)(D) and (E), respectively. Id.
EPA does not agree with ADEM’s
interpretation of the Agency’s authority
under RCRA, and the Agency is
proposing to deny the program under
RCRA section 4005(d)(1)(B). Though the
statute authorizes EPA to approve a
State CCR permit program in whole or
in part, implementation of the
groundwater monitoring, corrective
action, and closure regulations are
fundamental to an adequate CCR State
permit program. EPA does not see any
meaningful way for a State to
implement a partial CCR permit
program without the authority to
oversee these three major elements of
the CCR program. Thus, EPA is
proposing to deny the entire Alabama
CCR State permit program that ADEM
submitted for approval.
In Unit IV.A of this preamble, EPA
responds to ADEM’s position that RCRA
section 4005(d) prohibits EPA from
considering the permits issued under
the State CCR permit program when
determining whether to approve the
program and that EPA may only address
such issues after the State program is
approved. In Unit IV.B of this preamble,
the Agency provides a short summary of
EPA’s conclusions after review of the
express terms of the ADEM statutes and
regulations. In Unit IV.C of this
preamble, EPA identifies specific
permits that the Agency believes are
deficient and explains the bases for
EPA’s proposed determination that they
are inconsistent with the standard for
approval in RCRA section 4005(d)(1)(B).
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A. Legal Authority To Evaluate State
CCR Program Submittals
For the reasons set forth below, EPA
does not agree with ADEM’s assertion
that EPA may not consider the State’s
CCR permit history when determining
whether to approve its permit program.
In short, the Agency interprets the
statute to require EPA to consider the
CCR permits a State has issued under its
CCR program when determining
whether the State program can be
approved, where such information is
available prior to approval.
1. The Statute Requires EPA To
Consider a State’s CCR Permits When
Determining Whether To Approve the
Program if the Information Is Available
Section 4005(d)(1)(B) of RCRA
provides in part that the Administrator
‘‘shall approve, in whole or in part, a
permit program or other system of prior
approval and conditions submitted
under subparagraph (A) if the
Administrator determines that the
program or other system requires each
coal combustion residuals unit located
in the State to achieve compliance with’’
either: (1) The Federal CCR
requirements at 40 CFR part 257 (i.e.,
the Federal CCR regulations); or (2)
Other State criteria that the
Administrator, after consultation with
the State, determines to be at least as
protective as the Federal requirements.
42 U.S.C. 6945(d)(1)(B) (emphasis
added). The statute directs the
Administrator to determine whether the
State program ‘‘requires each’’ CCR unit
in the State ‘‘to achieve compliance’’
with either the Federal standard or an
alternative State standard at least as
protective as the Federal CCR
regulations. This necessarily includes
Agency consideration of both a State’s
statute and regulations and what the
State actually requires individual CCR
units to do, such as in permits or orders,
when such information is available
prior to approval of the State program.
By specifying that EPA is to determine
that the State program requires each
unit ‘‘to achieve compliance,’’ rather
than merely that the State requires
compliance or has the authority to
require compliance, Congress indicated
that EPA is not restricted to evaluating
the letter of the State’s regulations.
Moreover, the statute makes clear that
once a permit goes into effect, those are
the relevant requirements applicable to
the CCR unit rather than the regulations.
See 42 U.S.C. 6945(d)(3) (specifying that
the applicable criteria for CCR units in
an approved State are those contained
in the State permit, rather than the
Federal or State regulations). Whether
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issued permits comply with Federal
requirements or a State program that is
at least as protective is directly relevant
to whether the State program ‘‘requires
each CCR unit in the State to achieve
compliance.’’ If issued permits do not
comply, the State program does not
require compliance. EPA cannot
reasonably ignore such information,
when available, as it falls squarely
within the ordinary meaning of what the
statute expressly directs EPA to
consider. This is particularly true,
where, as here, the Agency knows
ADEM is issuing permits to CCR units
that do not require compliance with the
Federal CCR regulations, and the State
has not demonstrated that its alternative
approach is as protective as the Federal
CCR regulations.
In this case, ADEM adopted into its
State regulations the provisions of the
Federal CCR regulations. For this
reason, ADEM believes that EPA must
approve the State’s CCR program
because it in large part mirrors to the
Federal CCR regulations, thus,
according to ADEM, the State program
satisfies the requirements for an
approvable program pursuant to RCRA
section 4005(d)(1)(B)(i). ADEM is
correct that EPA may approve a State
program under this provision based on
the fact that the State’s regulations are
identical to those in the Federal CCR
regulations, but not where the State
interprets the State regulations to
impose significantly different
requirements than the Federal CCR
regulations, and the State has issued
permits authorizing actions that the
Federal regulations prohibit. Here,
despite adopting the language in the
Federal CCR regulations, ADEM has
affirmatively stated that it interprets the
State regulations differently than the
identically worded Federal provisions
and has issued permits on that basis,
even though the Agency has informed
the State on multiple occasions that its
interpretation and implementation of
the regulations are not consistent with
the Federal CCR regulations. See Units
III.E and IV.C of this preamble
(discussing Alabama’s interpretation of
‘‘infiltration’’ under § 257.102(d)(1)(i),
among other examples). Based on all of
the information in the record, EPA
cannot conclude that Alabama’s
program ‘‘requires each’’ CCR unit in
the State ‘‘to achieve compliance with’’
the Federal CCR regulations as required
by RCRA section 4005(d)(1)(B)(i).
Further, because Alabama is
interpreting the language in the Federal
CCR regulations differently than the
Agency, Alabama is essentially
submitting ‘‘other State criteria,’’ and in
order for EPA to approve such a
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program, Alabama must provide
information to support a determination
that the State criteria are ‘‘at least as
protective as the [Federal CCR
regulations]’’ consistent with RCRA
section 4005(d)(1)(B)(ii). EPA has
explained its position to Alabama, most
recently by letter dated February 1,
2023, and Alabama has declined to
provide any explanation, much less an
adequate one, of how its program will
require each CCR unit to achieve
compliance with standards at least as
protective as the Federal CCR
regulations. Accordingly, the Agency is
proposing to deny Alabama’s request for
approval of its CCR permit program.
This proposed denial is based on all the
available information in the record, and
as discussed in Unit IV.C of this
preamble, it demonstrates that the
Alabama CCR permits do not require
each CCR unit in the State to achieve
compliance with requirements at least
as protective as those contained in the
Federal CCR regulations.
2. EPA Is Not Required To Approve a
Deficient State Program and Then
Redress the Deficiencies Through
RCRA’s Program Review Provisions
In addition to the express terms of
RCRA section 4005(d)(1)(B), as
explained below, the overall context of
RCRA section 4005(d) supports
consideration of State CCR permits
when they have been issued prior to
approval of the State program. Even
were that not the case, it would be
unreasonable to interpret the statute to
require that EPA must approve a State
program based on the four corners of the
submission and then use the program
review provisions of RCRA section
4005(d)(1)(D) to address pre-existing
deficiencies in the program. As an
initial matter, EPA questions how it
would be reasonable to ignore directly
relevant and readily available
information in review of a State program
that will stand in for a Federal program,
because once EPA approves a State
program, the requirements of the State
program apply instead of the Federal
rules. Further, once a State permit is
issued, facilities are shielded from
enforcement of anything other than the
provisions of the State permit.
Compounding the problem is the time it
would take to go through the statutorily
mandated process to withdraw a
deficient program and the fact that prior
noncompliance would be arguably
sanctioned by approval of a State
program that is being implemented
improperly.
In this case, all the potential problems
that can arise by approving a State CCR
program based solely on the ‘‘four
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corners’’ of the State application are in
play. Specifically, the State is
interpreting the terms of the State
program (i.e., the terms of the Federal
CCR regulations) in a manner that is less
protective than the Federal CCR
regulations, the State is issuing permits
based on its flawed interpretation, EPA
approval of the State program would be
the equivalent of approving the
deficient permits, it would take
considerable time to withdraw the State
program after approval, and, in the
interim, facilities would be able to
operate under permits that are less
protective than required. Furthermore,
the Agency is proposing to determine,
based on the available information, that
Alabama’s CCR permit program is
deficient under two of the bases
provided in RCRA section
4005(d)(1)(D)(ii), EPA has notified
Alabama of the deficiencies, and the
State has declined to address them. See
Unit IV.C of this preamble (discussing
the deficiencies in Alabama’s CCR
program).
The statute requires EPA to
periodically review approved State
programs and provides a process by
which EPA can address identified
deficiencies. RCRA sections
4005(d)(1)(D)(i) and 4005(d)(1)(D)(ii),
respectively. The review provisions in
RCRA section 4005(d)(1)(D)(i) require
review:
• from time to time, as the
Administrator determines necessary, but
not less frequently than once every 12
years;
• not later than 3 years after the date
on which the Administrator revises the
applicable criteria for coal combustion
residuals units under part 257 of title
40, Code of Federal Regulations (or
successor regulations promulgated
pursuant to sections 6907(a)(3) and
6944(a) of this title);
• not later than 1 year after the date
of a significant release (as defined by the
Administrator), that was not authorized
at the time the release occurred, from a
coal combustion residuals unit located
in the State; and
• on request of any other State that
asserts that the soil, groundwater, or
surface water of the State is or is likely
to be adversely affected by a release or
potential release from a coal combustion
residuals unit located in the State for
which the program or other system was
approved.
The statute clearly provides for
review of State programs whenever ‘‘the
Administrator determines necessary,’’ in
addition to the situations that mandate
EPA review of a State program (e.g.,
RCRA section 4005(d)(1)(D)(i)(I)
requiring review periodically and at
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least every 12 years). Under Alabama’s
reading of the statute, EPA must
approve a knowingly deficient State
program and then undertake a program
review, either mandatory or
discretionary, to address the
deficiencies in that same program.
Under such circumstances, CCR units in
the State would potentially be allowed
to operate in a manner that is not
consistent with the Federal CCR
regulations for many years unless EPA
were to undertake a voluntary program
review immediately after approving the
program.
An additional factor that argues
against Alabama’s interpretation is the
fact that RCRA section 4005(d)(1)(D)(ii)
provides a process that EPA must follow
to address identified deficiencies in a
State CCR permit program before EPA
may withdraw the program, and, during
that time, ADEM could continue to
issue permits that are not as protective
as the statute requires. See also 42
U.S.C. 6945(d)(1)(E)(i) (allowing
withdrawal of a State program only after
notice to the State and an opportunity
for a hearing). Specifically, under RCRA
section 4005(d)(1)(D)(ii), EPA must
provide the State with notice of
deficiencies in the State program and an
opportunity for a hearing if the
Administrator determines that:
• a revision or correction to the
permit program or other system of prior
approval and conditions of the State is
necessary to ensure that the permit
program or other system of prior
approval and conditions continues to
ensure that each coal combustion
residuals unit located in the State
achieves compliance with the criteria
described in clauses (i) and (ii) of
subparagraph (B);
• the State has not implemented an
adequate permit program or other
system of prior approval and conditions
that requires each coal combustion
residuals unit located in the State to
achieve compliance with the criteria
described in subparagraph (B); or
• the State has, at any time, approved
or failed to revoke a permit for a coal
combustion residuals unit, a release
from which adversely affects or is likely
to adversely affect the soil, groundwater,
or surface water of another State.
The information currently available to
EPA already indicates that Alabama’s
program is deficient under the first two
provisions of RCRA section
4005(d)(1)(D)(ii). First, a revision to
Alabama’s CCR permit program is
necessary to ensure that each CCR unit
located in the State achieves compliance
with State standards that are ‘‘at least as
protective as’’ the Federal CCR
regulations because Alabama has never
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55227
adequately explained how its alternative
requirements achieve that standard. 42
U.S.C. 6945(d)(1)(D)(ii)(I). Second, as
explained further in Unit IV.C. of this
preamble, ADEM has not implemented
its permit program in a manner that
‘‘ensures each CCR unit located in the
State achieves compliance with the
criteria described in subparagraph (B).’’
42 U.S.C. 6945(d)(1)(D)(ii)(II). In
addition, EPA has notified Alabama of
these deficiencies on multiple
occasions, and the State has not
provided an adequate justification for
the position that its interpretation of the
Federal CCR regulations should govern
over EPA’s interpretation.
Given Alabama’s continued failure to
adequately address EPA’s concerns with
its CCR program, EPA has no reason to
believe that Alabama will change its
interpretation and implementation of its
program if EPA were to approve
Alabama’s CCR program and then
subsequently proceed with the RCRA
section 4005(d)(1)(D)(ii) process to
attempt to resolve the program
deficiencies. EPA would then have to go
through the RCRA section 4005(d)(1)(E)
process to withdraw the Alabama
program. In that case, EPA would then
be back at the point where Alabama
would have to either adopt EPA’s
interpretation of the Federal CCR
regulations or explain how its
alternative interpretation ensures that
the State’s program is as least as
protective as the Federal CCR
regulations.
The statutory language is clear, and it
does not support Alabama’s
interpretation. In addition, the Agency
believes Alabama’s interpretation could,
as in this case, lead to the illogical result
that EPA must approve a State CCR
permit program that it believes it likely
will eventually have to withdraw. EPA
also declines to adopt Alabama’s
suggested approach because the process
to withdraw takes significant time and
in the interim Alabama would likely
continue to issue permits that allow
CCR units in the State to operate under
conditions that are less protective than
those required in the Federal CCR
regulations. Finally, EPA is aware of
several CCR permits that allow units to
operate less protectively than required
by Federal CCR regulations and
approving Alabama’s program would
mean that these units would no longer
be subject to the Federal CCR
regulations. Thus, if EPA were to
approve Alabama’s program now (i.e.,
after the deficient CCR permits were
issued), the Alabama CCR program,
including the facility-specific permits,
would apply in lieu of the Federal CCR
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regulations pursuant to RCRA section
4005(d)(1)(A) and (3).
For all these reasons, EPA does not
believe the statute must be interpreted
as Alabama suggests and EPA declines
to adopt the State’s interpretation.
B. EPA’s Analysis of the Alabama CCR
Regulations
Section 4005(d)(1)(A) of RCRA, 42
U.S.C. 6945(d)(1)(A), requires a State
seeking CCR permit program approval to
submit to EPA, ‘‘in such form as the
Administrator may establish, evidence
of a permit program or other system of
prior approval and conditions under
State law for regulation by the State of
coal combustion residuals units that are
located in the State.’’ Although the
statute directs EPA to establish the form
of such evidence, the statute does not
require EPA to promulgate regulations
governing the process or standard for
determining the adequacy of such State
programs. EPA, therefore, developed the
Coal Combustion Residuals State Permit
Program Guidance Document; Interim
Final (82 FR 38685, August 15, 2017)
(the ‘‘Guidance Document’’). The
Guidance Document provides
recommendations on a process and
standards that states may choose to use
to apply for EPA approval of a State
CCR permit program, based on the
standards in RCRA section 4005(d),
existing regulations at 40 CFR part 239,
and the Agency’s experience in
reviewing and approving State
programs.
As stated above, State permit
programs under RCRA generally include
both sector specific technical
regulations (e.g., performance standards
for CCR units) and general State
permitting and enforcement provisions
that apply to all the different State
RCRA permitting programs. In this case,
Alabama is seeking approval of a partial
State CCR permit program and it
established State regulations that are
almost the same as the Federal CCR
regulations for the portions of the
Federal program for which the State is
seeking approval. To the extent the
Federal and State provisions are
different, the differences do not on their
face substantively make the State
regulations less protective than the
Federal CCR regulations. EPA reviewed
ADEM’s CCR regulations and, based on
that review, EPA proposes to find that
the express terms of the regulations
provide ADEM with sufficient authority
to issue permits that are at least as
protective as those required under the
Federal CCR regulations. See the TSD
Volume III (providing a detailed
analysis of the regulatory terms of
Alabama’s CCR regulations). EPA is
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proposing to determine that the terms of
the regulations provide the State with
sufficient authority to implement an
adequate CCR permit program despite
the fact that the Agency is also
proposing to deny the Application for
Alabama CCR permit program based on
the State’s issuance of permits under
those same regulations. Therefore, the
Agency believes the record would
support approval of Alabama’s program
if the State either modified its permits
to be consistent with the Federal
requirements or demonstrated that its
alternative requirements are at least as
protective as the Federal CCR
regulations.
EPA briefly discusses its evaluation of
the State’s regulations below. A
comprehensive evaluation is included
in the TSD Volume III in the docket for
this proposed action.
1. Adequacy of Technical Criteria
a. Alabama CCR Regulations
EPA first evaluates the technical
criteria that will be included in each
permit the State issues to determine
whether they are the same as the
Federal criteria, or to the extent they
differ, whether the modified criteria are
‘‘at least as protective as’’ the Federal
requirements. See 42 U.S.C.
6945(d)(1)(B).
On April 20, 2018, ADEM, by and
through the Alabama Environmental
Management Commission (EMC),
amended ADEM Admin. Code div. 335–
13 to: (1) Modify Chapters 1, 4, and 5
and (2) Add a new Chapter 15:
Standards for the Disposal of Coal
Combustion Residuals in Landfills and
Surface Impoundments. These rules
became effective on June 8, 2018. In
response to EPA comments and changes
to the Federal CCR regulations, ADEM
proposed and finalized several
amendments to its CCR rules with the
first revisions becoming effective
February 15, 2021. The most recent
revisions became effective December 13,
2021.
ADEM’s regulations adopt the Federal
CCR regulations amended through
August 28, 2020, and include the
corrections EPA made at
§§ 257.102(d)(3)(ii) and 257.103(f)(1)(vi)
(85 FR 72506, November 12, 2020)
(except for certain provisions outlined
below).
EPA has preliminarily determined
that the Alabama CCR permit program
contains all the technical criteria in 40
CFR part 257, subpart D, except for the
provisions specifically discussed below.
EPA’s full analysis of the terms of the
Alabama CCR permit program and how
the Alabama regulations differ from the
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Federal requirements can be found in
the TSD Volume III.
b. Federal Rule Provisions Excluded
From Alabama’s Request for Approval
of a Partial Program
Alabama is requesting approval for a
partial State CCR program, rather than a
full CCR program that includes all the
requirements of the Federal CCR
regulations. ADEM is not seeking
approval for the following six
provisions:
1. ADEM Administrative Code r. 335–
13–15–.01(1)(d); this State provision is
the analog to the Federal exclusion of
inactive surface impoundments at
inactive facilities, found at § 257.50(e),
that was vacated in Utility Solid Waste
Activities Group v. EPA, 901 F.3d 414
(per curiam) (USWAG);
2. ADEM Admin. Code r. 335–13–15–
.07(4)(f); this State provision is the
analog to the Federal requirement for
alternative closure deadlines, found at
40 CFR 257.103(f);
3. EPA has revised the Federal
regulations to granting Participating
State Directors authority to issue
certifications in lieu of requiring a
professional engineer (PE) certification.
ADEM did not adopt these provisions;
therefore, an owner or operator of a CCR
unit must submit certifications from a
PE, as appropriate, as required by
ADEM Admin. Code chapter 335–13–
15;
4. The Federal regulations include a
provision that authorizes the suspension
of groundwater monitoring
requirements under certain
circumstances, found at § 257.90(g),
which the State has not adopted;
5. The Federal regulations include a
provision for an alternate liner
demonstration found at § 257.71(d), and
the State has not adopted this Federal
provision; and,
6. ADEM Admin. Code r. 335–13–15–
.06(6)(h)2.: The State has adopted the
groundwater protection standards for
cobalt, lead, lithium, and molybdenum
found at § 257.95(h)(2) but is not
seeking approval because the Federal
provision has been challenged and is
under reconsideration.
More detail on the elements of the
partial program and EPA’s analysis of
the program can be found in the TSD
Volume III. With the exception of
specific provisions spelled out in the
TSD Volume III, EPA has preliminarily
determined that the Alabama CCR
regulations contain all the technical
elements of the portions of the Federal
CCR regulations for which the State is
seeking approval.
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2. Review of Generally Applicable
Alabama CCR Permit Program Statutes
and Regulations
As explained above, supra note 12,
Alabama’s CCR permit program
regulations include general
requirements that apply across multiple
permit programs, and its Application for
approval of a CCR permit program thus
includes both general and facility/unitspecific requirements in the State CCR
permit program. EPA therefore also
evaluated the Alabama CCR permit
program as modified to address CCR
units using the process discussed in
Units II.C and IV.A of this preamble.
EPA’s findings are summarized below
and provided in more detail in in the
TSD Volume III for this notice.
In evaluating Alabama’s CCR
permitting requirements, EPA reviewed
the State’s permit requirements for CCR
units including applicability, duration,
application process, denial process, and
the process for draft and final permit
determinations. EPA also reviewed
Alabama’s requirements that apply to
modification, suspension, and
revocation of permits. For permit
modifications, EPA specifically looked
at major and minor modifications to
determine which modifications would
require public participation. After
conducting this review, EPA has
preliminarily determined that the
Alabama regulations concerning CCR
permit applications and approvals is
adequate, and that this aspect of the
Alabama CCR permit program meets the
standard for program approval.
Based on RCRA section 7004, 42
U.S.C. 6974, it is EPA’s judgment that
an adequate State CCR permit program
will ensure that: (1) Documents for
permit determinations are made
available for public review and
comment; (2) Final determinations on
permit applications are made known to
the public; and (3) Public comments on
permit determinations are considered.
Alabama has adopted public
participation opportunities for the CCR
program that can provide an inclusive
dialogue, allowing interested parties to
talk openly and frankly about issues
within the CCR program and search for
mutually agreeable solutions to
differences. EPA reviewed Alabama’s
public participation requirements,
processes, and procedures including
public notices, public comment periods
(including consideration of public
comments), public hearings, and public
availability of final determinations. An
overview of the Alabama public
participation provisions is provided in
the TSD Volume III. After conducting
this review, EPA has preliminarily
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determined that the Alabama approach
to public participation requirements
provides adequate opportunities for
public participation in the permitting
process sufficient to meet the standard
for program approval.
EPA also reviewed Alabama’s
compliance monitoring authority,
enforcement authority, and the
procedures for intervention in civil
enforcement proceedings. It is EPA’s
judgment that an adequate permit
program should provide the State with
the authority to gather information
about compliance, perform inspections,
and ensure that information it gathers
provides an adequate basis for
enforcement. ADEM’s statutory
authority for compliance monitoring for
its Solid Waste Program is set forth in
sections 22–27–7, 22–27–9, 22–27–12,
22–22A–5 and 22–22A–8 of the Code of
Alabama, 1975. These portions of the
statute, as well as ADEM Admin. Code
rules 335–13–1–.11(2) and 335–13–6.01(2) give the Department authority
during an inspection to obtain all
information necessary to determine
whether the owner/operator is in
compliance with State CCR
requirements. This includes authority to
conduct monitoring and testing when
necessary.
Based on the information Alabama
has submitted on the State’s permitting
requirements, EPA has preliminarily
determined these aspects of the
Alabama CCR permit program provide
the State with the necessary authority to
implement an adequate State program.
More detail on the review and analysis
of Alabama’s CCR permit program can
be found in the TSD Volume III.
C. EPA’s Analysis of Alabama’s Permits
Issued Under the State CCR Regulations
EPA conducted a review of Alabama’s
permitting decisions as part of the
Agency’s evaluation of whether ADEM’s
CCR permit program requires each coal
combustion residual unit located in the
State to achieve compliance with
standards at least as protective as the
Federal CCR regulations. 42 U.S.C.
6945(d)(1)(B). Alabama’s permitting
decisions issued under its CCR
regulations are directly relevant to
determining whether the State’s
program satisfies this statutory
requirement, and EPA considers such
information to be appropriately part of
the record for a decision on the permit
program when permit issuance begins
prior to approval of the State program
and the Agency has information that the
State’s implementation is not
sufficiently protective.
ADEM submitted its revised State
CCR permit program Application on
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December 29, 2021. Less than a month
later, on January 11, 2022, EPA
published several proposed decisions
responding to requests from owners and
operators of CCR units nationwide for
extensions of the April 11, 2021,
deadline to cease sending waste to
unlined CCR surface impoundments
(Part A proposals). EPA proposed to
deny several of the extension requests
because facilities were planning to close
unlined CCR surface impoundments
with, among other things, waste
remaining in groundwater without
adopting engineering measures to limit
the flow of groundwater into and out of
the unit. Soon after issuing the Part A
proposals, several states, utility facilities
that own unlined surface
impoundments, and trade groups
contacted EPA to object to the Agency’s
application of the closure requirements
to the unlined surface impoundments in
those proposed decisions. Based on
these objections, EPA was concerned
that Alabama’s and other states’ CCR
permit programs were being interpreted
and implemented to allow facilities to
close unlined surface impoundments
without complying with all the
necessary requirements in the Federal
regulations.
Because of these concerns, on March
15, 2022, EPA sent a list to ADEM of
CCR surface impoundments in Alabama
that, based on the information available
to EPA, appear to be inundated by
groundwater.14 Over the next several
months, EPA and ADEM met several
times to discuss the application of the
Federal closure performance standards
to such impoundments, and to better
understand how the State interpreted its
own requirements.15
EPA also started reviewing permits for
unlined surface impoundments in
Alabama as part of EPA’s review of the
State CCR permit program. As a
consequence, in meetings and in
correspondence with ADEM, EPA
14 The CCR surface impoundments with
insufficient permits that are discussed in this Unit
of the preamble are all surface impoundments with
WBWT. For a list of all the CCR surface
impoundments EPA identified in Alabama with
WBWT, see Email from Meredith Anderson to Scott
Story. CCR units in AL. March 15, 2022.
15 Interactions between EPA and Alabama about
implementation of the State program include: April
13, 2022, meeting to discuss the Federal closure
performance standards; three separate meetings to
discuss the proposed closure requirements for Plant
Gorgas, Plant Greene County, and Plant Gadsden;
May 10, 2022, meeting to further discuss the closure
performance standard and specifically how ADEM
was interpreting and applying the closure and
groundwater monitoring performance standards at
the Ash Pond at Plant Gadsden; and May 28, 2022,
meeting to discuss the status of closure activities at
Plant Greene County and Plant Gadsden. A list of
EPA/Alabama interactions is in the Technical
Support Document Volume II.
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expressed concern that Alabama’s
permit program appeared to differ from
the Federal program, and that these
differences appeared to make the State’s
program less protective than the Federal
program. As a result of these
discussions, on July 7, 2022, EPA
informed ADEM via telephone that EPA
would be unable to approve ADEM’s
CCR permit program Application until
Alabama demonstrated to EPA that the
State is implementing its program to be
as protective as the Federal CCR
regulations.16 Further, EPA explained to
ADEM that it was exploring options for
actions to take at the Federal level with
respect to both the CCR permit program
Application and at specific facilities
where there are outstanding concerns.
Throughout the course of these
discussions, and in EPA’s nationwide
Part A determinations, EPA explained
the existing requirements under the
Federal regulations; in response, ADEM
offered notably different interpretations
of some of the obligations under the
State’s current closure requirements.
Despite the Agency’s concerns, the State
continues to implement its CCR
program in a manner that is less
protective than the Federal CCR
regulations, and Alabama has not
adequately explained how its alternative
State program satisfies the statutory
requirement to require each CCR unit in
the State to achieve compliance with
either the Federal requirements or with
State standards that are at least as
protective as the Federal requirements.
As part of the evaluation of Alabama’s
CCR program submittal, EPA reviewed
four final State CCR permits issued by
ADEM for the following facilities: Plants
Colbert, Gadsden, Greene County, and
Gorgas. EPA’s review focused
specifically on permits issued to
unlined surface impoundments that
have closed or are closing with waste
that will remain in place below the
water table, because these units have the
greatest potential to cause significant
environmental and human health effects
if mismanaged. EPA limited its review
to information in the permit record (e.g.,
the Permit Application or information
on ADEM’s e-File site) and to
information publicly available on each
facility’s CCR website, even though the
permit record alone should contain all
the information necessary to determine
whether the permit is as protective as
the Federal CCR regulations. EPA also
did not attempt to catalog every
potential inconsistency between the
16 July 7, 2022– Telephone call between Carolyn
Hoskinson, Director of EPA’s Office of Resource
Conservation and Recovery, and Stephen Cobb,
Chief of the Land Division at the Alabama
Department of Environmental Management.
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permits and the Federal CCR
regulations. Instead, EPA concentrated
on the permits’ consistency with
fundamental aspects of the closure,
groundwater monitoring, and corrective
action requirements. EPA took this
approach because the purpose of this
review is to determine whether
Alabama’s program meets the statutory
standard for approval, not to reach final
conclusions about an individual
facility’s compliance with the CCR
regulations.
During its review, EPA identified a
consistent pattern of ADEM issuing
permits to CCR units that fail to
demonstrate compliance with
fundamental requirements in part 257,
without requiring the permittees to take
specific actions to bring the units into
compliance. EPA also identified a
consistent pattern of ADEM approving
documents submitted by the facilities,
such as closure plans, groundwater
monitoring plans, and assessments of
corrective measures, even though the
submissions lacked critical information
or are otherwise deficient. ADEM also
did not require the permittees to take
any action to cure deficiencies in the
permits even where ADEM previously
identified the deficiencies and
requested further information prior to
issuing the final permits. Specifically,
EPA is proposing to determine that
ADEM issued multiple permits allowing
CCR in closed units to remain saturated
by groundwater, without requiring
engineering measures that will control
the groundwater flowing into and out of
the closed unit. See, 40 CFR 257.102(d).
EPA is also proposing to determine that
ADEM approved groundwater
monitoring systems that contain an
inadequate number of wells, and in
incorrect locations, to monitor all
potential contaminant pathways and to
detect groundwater contamination from
the CCR units in the uppermost aquifer.
See, 40 CFR 257.91. Finally, EPA is
proposing to determine that ADEM
issued multiple permits that effectively
allow the permittee to delay
implementation of effective measures to
remediate groundwater contamination
both on- and off-site of the facility. See,
40 CFR 257.96–257.97. Overall, EPA’s
review of the permit records and other
readily available information documents
a consistent pattern of deficient permits
and a lack of oversight and independent
evaluation of facilities’ proposed permit
terms. In each case, EPA was unable to
locate any evaluation or record of
decision documenting that ADEM
critically evaluated the materials
submitted as part of the permit
application, or otherwise documented
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its rationale for adopting them. For all
these reasons, EPA is proposing to
conclude that the ADEM permits
discussed below are not as protective as
the Federal CCR regulations.
In the next several sections, EPA
discusses specific issues identified
during the review of ADEM’s final
permits for Plants Colbert, Gadsden,
Greene County, and Gorgas.17 Based on
EPA’s review, the Agency is proposing
to deny Alabama’s Application because
the State’s CCR permit program does not
require each CCR unit in the State to
achieve compliance with either the
minimum requirements in the Federal
CCR regulations or with alternative
requirements that EPA has determined
to be at least as protective as the Federal
provisions.
1. Colbert Fossil Plant
TVA owns and operates the Colbert
Fossil Plant (Colbert or Colbert Plant)
located in Colbert County, Alabama, and
it submitted a permit application for the
facility dated December 10, 2021.18 The
plant property is on the south bank of
the Tennessee River, approximately 8
miles west of Tuscumbia, Alabama. The
Colbert Fossil Plant was fully idled and
stopped generating electricity in March
2016. The plant had five generating
units with a combined generating
capacity of 1,204 megawatts. In
accordance with the ADEM Land
Division, Solid Waste Program,
Standards for Disposal of Coal
Combustion Residuals in Landfills and
Surface Impoundments, Chapter 335–
13–15–.02, Ash Disposal Area 4 (also
called Ash Pond 4) is classified as an
existing CCR surface impoundment. Ash
Disposal Area 4 is located on the
southern portion of the plant property,
approximately 3,000 feet south of the
powerhouse. The CCR surface
impoundment is bounded to the west by
Colbert Steam Plant Road, to the east by
Cane Creek, and to the south by Lee
Highway. EPA reviewed TVA’s permit
application and draft and final permits
17 On January 31, 2023, EPA Region 4 sent a
Notice of Potential Violations (NOPV) and
Opportunity to Confer to Alabama Power Company.
The NOPV addressed concerns with compliance of
Alabama Power Company’s Plant Barry Ash Pond.
The NOPV addressed the following potential
violations: failure to meet the criteria for
conducting the closure of the Plant Barry Ash Pond,
failure to establish an adequate groundwater
monitoring system, and failure to address certain
site-specific criteria in the Emergency Action Plan.
Although the permit and record for Plant Barry
share many of the flaws in the CCR permits for
other unlined surface impoundments in Alabama,
EPA will not address the Plant Barry permit as part
of this action because the enforcement process with
the facility is ongoing.
18 Tennessee Valley Authority Colbert Fossil
Plant (COF) Ash Pond 4 Permit Application.
Submitted to ADEM. December 10, 2021.
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for the Colbert Plant along with
associated documents. Issues with
closure, groundwater monitoring
networks, and corrective action at the
Colbert Plant are discussed below.
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a. TVA Colbert Closure Issues
The Federal CCR regulations provide
two options for closing a CCR unit:
closure by removal and closure with
waste in place. 40 CFR 257.102(a). Both
options establish specific performance
standards. 40 CFR 257.102(c) and (d).
TVA closed Ash Pond 4 at Colbert by
leaving the CCR in the unit in place;
but, as explained below, the TVA
application for Ash Pond 4 did not
comply with the Federal closure
standards for closure with waste in
place for unlined surface
impoundments and ADEM issued the
permit without addressing the
deficiencies.
TVA’s Permit Application for the
Colbert Plant explains that Ash Pond 4
was built in 1972 and TVA completed
its closure in early 2018, prior to its
application for a permit under the
ADEM CCR rules in Chapter 335–13–
15.19 TVA elected to close Ash Pond 4
by leaving CCR in place and
constructing a final cover system over
the waste, which is estimated to be 2.6
million cubic yards (CY) of waste.20
Closure of Ash Pond 4 was completed
in accordance with a closure and postclosure care plan dated February 2017,
which was approved by ADEM on
August 22, 2017.21 Closure activities
were deemed complete in March 2018
and a certification report dated
September 18, 2018, documenting
closure of Ash Disposal Area 4, was
submitted to ADEM.
ADEM’s Final Permit, issued in
October 2022, provides the following
terms and conditions:
Closure Timeframe and Notifications.
The Permittee shall close their CCR
19 The terms ‘‘Ash Pond 4’’ and ‘‘Ash Pond Area
4’’ are both used in the Colbert Plant Permit
Application to refer to the impoundment in
question. For purposes of this proposal, EPA is
referring to the impoundment as Ash Pond 4.
20 The Permit Application states that the ‘‘total
capacity of Ash Disposal Area 4 is approximately
2.6 million CY, covering approximately 52 acres.’’
EPA is aware that other reports State that the
‘‘approximate volume of CCR material at the time
of the inspection’’ is 3.29 million CY. See, e.g.,
FY2021 Intermediate Inspection of CCR Facilities
dated May 6, 2021. For purposes of estimating
volumes of saturated CCR in this proposal, EPA is
taking an approach that provides a minimum
estimate, relying on the value presented in the
Permit Application to represent the volume of CCR
in the impoundment, instead of relying on the
larger estimates established based on the inspection
of the unit.
21 Tennessee Valley Authority. Permit
Application for CCR Surface Impoundment, TVA
Colbert Fossil Plant Ash Disposal Area 4. December
10, 2021. Attachment I.
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units as specified in 335–13–15–.07(2),
this permit and the Application.
B. Criteria for Closure.
1. Cover. Closure of a CCR landfill,
surface impoundment, or any lateral
expansion of a CCR unit must be
completed by either leaving the CCR in
place and installing a final cover system
or through removal of the CCR and
decontamination of the CCR unit, as
described in 335–13–15–.07(3)(b)
through (j). The minimum and
maximum final grade of the final cover
system may be less than 5 percent and
greater than 25 percent, as specified in
the Permit Application, for the Colbert
Fossil Plant Ash Disposal Area 4. Ash
Disposal Area 4 may utilize erosion
control measures, as specified in the
Permit Application, other than
horizontal terraces. (See Section IX.A.
and B.)
2. Written Closure Plan. The written
closure plan, as part of the Application,
must include, at a minimum, the
information specified in 335–13–15–
.07(3)(b)1.(i) through (vi).
According to ADEM, ‘‘[t]he
Department adopted the terms of the
closure plan as part of the permit as the
Department has previously approved
the plan and determined it meets both
State and Federal regulations for closure
of a CCR unit.’’ 22 Once ADEM approved
and adopted TVA’s Closure Plan into
the permit, the Closure Plan, rather than
the referenced State regulations, became
the State requirements with which TVA
is required to comply. See, 42 U.S.C.
6945(d)(3)(A). As discussed in detail in
the next section and summarized in
Table II, between 2019 and 2021,
approximately 6 to 13 feet of ash (on
average)– or 13 to 35 percent of the CCR
in the closed Ash Pond remains
saturated by groundwater.
i. The CCR in the Closed Ash Pond 4
Remains Saturated by Groundwater
Neither TVA’s Closure Plan, the
Permit Application, ADEM’s Final
Permit, or any other document in the
permitting record specifically discuss
how the closure of Ash Pond 4 would
meet the closure performance standards
given the measured groundwater
elevations and hydrogeology of the site.
Accordingly, EPA reviewed information
in the Permit Application as well as
other publicly available information
available on TVA’s CCR website to
determine whether groundwater
remains in contact with the CCR in Ash
Pond 4 since closure was completed in
22 Letter from Stephen Cobb to Carolyn
Hoskinson, Responding to EPA Comments on
Proposed Permit for the
Tennessee Valley Authority Colbert Fossil Plant,
October 27, 2022, Enclosure 1, page 6.
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55231
March 2018. As described below,
available groundwater measurements
recorded between 2018 and 2021 show
that, even after closure, groundwater
levels at Ash Pond 4 continue to be
present above the base of the unlined
impoundment, saturating a portion of
the CCR in the closed unit. EPA’s basis
for these findings is described in the
succeeding paragraphs, which
summarize EPA’s understanding of the
base elevation of Ash Pond 4 (e.g., the
lowest extent of CCR in the unit), the
groundwater levels since closure was
completed in 2018, and EPA’s estimate
of the volume of CCR that remains
saturated with liquid (groundwater).
More details on EPA’s analyses can be
found in TSD Volume I.23
(1) Base of the Impoundment
Ash Pond 4 is a 52-acre CCR surface
impoundment that was created by
constructing a single dike around the
perimeter of the impoundment and two
internal divider dikes. EPA was unable
to locate information in the Permit
Application or other publicly available
documents that fully describes the asconstructed configuration of the bottom
of Ash Pond 4 across its entire footprint
prior to the initial receipt of waste.
However, based on information in the
Permit Application and documents
referenced in the Permit Application,
the lowermost documented elevations at
which CCR occurs within the
impoundment varies depending on the
location, ranging from approximately
413.5 to 427.1 ft above mean sea level
(MSL). See TSD Volume I, Section II.a.
EPA also relied on an average
elevation to estimate the volume of CCR
in the impoundment remaining in
contact with groundwater, rather than
trying to account for what may be as
much as a 14-foot difference across the
52-acre impoundment. Specifically,
EPA relied on an average bottom
elevation of 422 ft above MSL, which is
the average of elevation measurements
taken at 18 locations within the
footprint of the impoundment based on
borings for piezometers and wells.
Information on these borings is found
on construction drawings 10W395–7
through 9 and a report from 2010. See
TSD Volume I, Section II.a. This average
is also consistent with several
documents in the Permit Application
and other documents that depict the
23 Volume I: Technical Support Document for the
Proposed Notice to Deny Alabama’s Coal
Combustion Residuals Permit Program,
Supplemental Analyses of Technical Issues with
ADEM Permits. U.S. Environmental Protection
Agency, Office of Land and Emergency
Management (5304T), 1200 Pennsylvania Avenue
NW, Washington, DC 20460. August 2023.
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base of the impoundment at 422 ft above
MSL. For example, Section A–A of
construction drawing 10N292R3 shows
a bottom elevation of approximately 422
ft above MSL in the vicinity of the
northern perimeter dike where the
spillways were constructed. Id. at
Volume I, Section II.a.i.3. Another
example is a slope stability section
supporting a steady-state seepage
analysis that shows a portion of the base
of the impoundment to be at an
elevation of 422 ft above MSL. Id. at
Section II.a.i.2. Similarly, design
drawings from 2010 for a temporary
rock buttress and sheet pile wall
constructed in a portion of an internal
divider dike show the bottom of the
impoundment to be 422 ft above MSL at
this location. Id. at Section II.a.i.3. A
final example is the liner design
demonstration prepared by TVA to
comply with § 257.71 that states ‘‘[f]rom
information contained in drawing
10N290, it was assumed the base of the
pond is at elevation 422 ft.’’ Id. at
Section II.a.iv. However, it is important
to note that the use of the 422 ft
elevation mark to represent the base of
the unit was an effort to represent
average conditions. As noted earlier, the
preponderance of the evidence suggests
that base of the impoundment varies
depending on the location, ranging from
approximately 413.5 to 427.1 ft above
MSL, but an average value of 422 ft
above MSL is technically defensible and
conservatively high. See TSD Volume I,
Section II.a. Volumes during worst case
conditions (i.e., when river stages and
water tables are higher than reported
values) would be greater, and actual
saturated CCR volumes could be higher
than estimated if portions of the unit
with lower documented waste bottom
elevations (less than 422 ft above MSL)
were considered. The estimates
provided by EPA below and in the TSD
Volume I are reasonable based on the
available information provided in the
Permit Application regarding the waste
bottom elevations.
ddrumheller on DSK120RN23PROD with PROPOSALS3
ii. Characterization of Groundwater
Elevations
Information from TVA’s Permit
Application clearly supports a
conclusion that at least some portion of
the CCR in Ash Pond 4 remains
saturated by continued infiltration of
groundwater. The groundwater
elevation maps for 2020 and 2021
provided in the Permit Application
reveal that the lowest measured
groundwater elevations range between
just over 414 to just over 416 ft above
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MSL.24 These levels are found in
groundwater monitoring wells COF–105
and CA31A, which are screened in the
residuum/alluvium layer, and
consistently measure the lowest
groundwater elevations of any of the
wells immediately surrounding Ash
Pond 4. In every measurement reported
in the Permit Application, the
groundwater elevations measured in
these wells are 0.86 to 2.7 feet above the
lowest documented elevation of CCR
within the unit (413.5 ft above MSL).
Furthermore, COF–105 is located
approximately 150 feet east of the unit
boundary in the downgradient direction
and CA31A is located approximately
400 feet northeast of the unit boundary
in the downgradient direction. As
corroborated by monitoring well and
piezometer data from within the unit,
the actual groundwater elevations
directly beneath the unit are generally
higher than these minimum recorded
values, which are well beyond the unit
boundary in downgradient directions.
This basic information clearly supports
a conclusion that at least some portion
of the waste in Ash Pond 4 is wet under
typical conditions.
A closer examination of available data
from the Permit Application further
supports this conclusion. Assuming that
the base of the CCR is uniformly at 422
ft above MSL, based on the contour
intervals depicted on the groundwater
elevation map for February 27, 2020
(Figure A–1), groundwater elevations
range from 414.36 to 437.46 ft above
MSL, and exceed 422 ft above MSL at
over fifty percent of the entire Ash Pond
4 footprint. Similarly, the groundwater
elevation contours depicting the
February 22, 2021 (Figure A–3),
groundwater elevation data documents
water levels ranging from 415.14 to
436.54 ft above MSL, indicating that
water levels greater than 422 ft above
MSL are present at one-third or more of
the area within the impoundment.
Even though data from summer
monitoring events show that summer
groundwater levels are considerably
lower than the data reported for
February 2020 and 2021, there still
appears to be a considerable footprint of
wet waste under all reported conditions,
and conditions indicative of
groundwater saturation or infiltration
into the closed unit appear to be
sustained without interruption in some
regions of the unit. On August 10, 2020
(Figure A–2), groundwater levels ranged
from 414.38 to 422.58 ft above MSL and
24 Tennessee Valley Authority. Permit
Application for CCR Surface Impoundment, TVA
Colbert Fossil Plant Ash Disposal Area 4. December
10, 2021. Attachment H, Appendix A, Figures A–
1 through A–4.
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are mapped between 415 and 420 ft over
most of the unit’s footprint, with a small
portion in the extreme southwest corner
of the mapped area showing higher
groundwater levels of greater than 420
ft. On August 23, 2021 (Figure A–4),
groundwater elevations ranged from
414.79 to 429.00 ft above MSL and are
mapped as being greater than 422 ft
above MSL beneath a somewhat larger
portion of the impoundment’s surface
area in the southwestern corner, with
the remainder of groundwater elevations
in the unit mapped between 415 and
420 ft above MSL.
The Permit Application also presents
groundwater elevation contour maps for
the Tuscumbia limestone bedrock
aquifer for 2020 and 2021. This is
appropriate as there is an abundance of
information contained in the materials
presented for the Permit Application,
the annual groundwater monitoring
reports, and the 2019 Comprehensive
Groundwater Investigation Report that
indicates that the Tuscumbia limestone
aquifer is in direct contact and is in
direct hydraulic communication with
the overlying residuum/alluvium
aquifer.25 In this respect, EPA interprets
the Tuscumbia limestone aquifer to be
part of the uppermost aquifer system for
the unit. EPA’s analysis in this regard is
included in Section II.b of the TSD
Volume I.
For the Tuscumbia limestone, the
Permit Application included four
contour maps from groundwater
elevation measurement events on
February 27, 2020, August 10, 2020,
February 22, 2021, and August 23,
2021.26 These data sets, which are
summarized in Table I below, generally
indicate that water levels in the bedrock
aquifer are higher than the 422-foot base
elevation beneath significant regions of
the Ash Pond 4 footprint during most of
these four monitoring events,
particularly during winter conditions.
For February 27, 2020 (Figure A–5),
groundwater elevations in the
Tuscumbia limestone ranged from
414.61 to 437.77 ft above MSL.27 TVA’s
interpretive contours depicting the
Tuscumbia limestone bedrock
groundwater elevations for February 27,
2020, indicate that the entire
25 Stantec, Comprehensive Groundwater
Investigation Report, First Amended Consent
Decree # 20–01–2013–900123 Ash Pond 4 and Ash
Stack 5. TVA Colbert Fossil Plant, Prepared for
Tennessee Valley Authority Chattanooga,
Tennessee. May 17, 2019.
26 Permit Application at Figures A–5 through A–
8, respectively.
27 The elevation corresponding to wells CA29BR
and CA22B on Figures A–5 through A–8 were
excluded from this range based on TVA’s footnote
indicating these wells are ‘‘poorly connected to site
wide groundwater flow system.’’
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impoundment is characterized by water
levels greater than or equal to 422 ft
above MSL, except for a very small area
near monitoring well COF–111 near the
eastern boundary. For February 22, 2021
(Figure A–7), measured groundwater
elevation data for the Tuscumbia
limestone aquifer ranged from 411.11 to
436.70 ft above MSL. TVA’s interpretive
contour map for the same period
indicates that groundwater levels at or
above 422 ft above MSL were mapped
at approximately half of the unit’s
footprint. Similarly, on August 23, 2021
(Figure A–8), groundwater elevation
data ranged from 413.47 to 429.07 ft
above MSL and interpretive contours for
same period for the Tuscumbia
limestone bedrock aquifer again indicate
that approximately 50 percent of the
unit’s footprint exhibits groundwater
levels at or above 422 ft above MSL.
Conditions during the August 10, 2020
(Figure A–6), monitoring event show
lower groundwater levels, with
groundwater elevation values for the
Tuscumbia limestone aquifer ranging
from 412.85 to 422.54 ft above MSL.
TVA’s interpretive groundwater
elevation contours for the same period
show groundwater elevations below 422
ft above MSL in all areas except for a
small portion near the southwestern
corner of the unit. It should also be
noted that surface water levels
associated with the four monitoring
events listed above indicate that surface
water levels in the Pickwick Reservoir
are greater than 413.5 ft above MSL (the
lowest documented waste bottom
elevation) for two of the four monitoring
events as shown in Table I. It is also
worth noting that river stage, which
fluctuates, was measured as above the
lowest groundwater elevations
measured in the Tuscumbia limestone
for three of the four time periods
presented in the Permit Application.
Together with the documented
occurrence of solution features in the
limestone and associated preferential
pathways in groundwater, it is
reasonable to expect some degree of
hydraulic communication between the
reservoir/river and the underlying
limestone aquifer. Depending on the
55233
magnitude and duration of the
occurrence of higher river/reservoir
levels, some degree of recharge from the
river to the underlying aquifers may be
expected. It is perhaps partly for this
reason that the CCR in the unit remains
wet, at least intermittently, so many
years after the unit was closed. Despite
the disclaimer,28 which appears on all
the Tuscumbia groundwater elevation
maps in the Permit Application, EPA
believes that the interpretive contours
provided on these maps corroborate the
anisotropic groundwater flow
conditions to which TVA refers. EPA’s
interpretation of this information
confirms the presence of northeast
striking preferential pathways within
the Tuscumbia limestone aquifer. In any
event, the measured head values in the
Tuscumbia limestone aquifer within
and surrounding the unit are hard data
points that enable the simplistic
analysis regarding position of the waste
relative to measured water levels. EPA’s
analysis and reasoning on this subject
are further detailed in Section II.b of the
TSD Volume I.
TABLE I—MAXIMUM AND MINIMUM REPORTED GROUNDWATER ELEVATIONS a FOR THE TUSCUMBIA LIMESTONE AND ASSOCIATED CONTEMPRANEOUS RIVER STAGE ELEVATIONS FOR PICKWICK RESERVOIR ON FOUR MONITORING EVENTS
DURING 2020–2021
Feb 27, 2020
High Groundwater Elevation ............................................................................
Low Groundwater Elevation ............................................................................
River Stage b ....................................................................................................
a All
437.77
414.61
410.95
Aug 10, 2020
Feb 22, 2021
422.54
412.85
414.24
436.7
411.11
412.41
Aug 23, 2021
429.07
413.47
413.79
data presented in feet above MSL, NGVD 29 datum.
stage values obtained from Figures A–5 through A–8 in the Groundwater Plant in the Permit Application.
ddrumheller on DSK120RN23PROD with PROPOSALS3
b River
The groundwater elevations provided
in the Permit Application are based
primarily on data collected from outside
of the unit, without consideration of
actual groundwater levels directly
within and beneath the unit. Although
data from inside the unit were not
provided in the Permit Application,
data from piezometers and monitoring
points within Ash Pond 4 are available
in the Annual Inspection Reports posted
on TVA’s CCR website. EPA reviewed
the water level information reported in
the Annual Inspection Reports from
2016 through 2022.29 These reports
document the change of water levels
within the unit over time since closure
and provide for a direct, more highly
resolved and representative analysis of
actual groundwater levels and
conditions directly within and beneath
the unit. These data demonstrate that
significant areas and volumes of CCR
below the water table have been and
remain sustained within the unit as
discussed in further detail below. These
data also enabled EPA to estimate the
minimum volumes of saturated CCR
that remain in the closed unit under
various observed conditions.
The most recent Annual Inspection
Report from May 2022 states that
‘‘[t]here are 54 automated vibrating wire
piezometers, eight (8) automated slope
inclinometers, and six (6) manual
magnetic extensometers installed at Ash
Disposal Area 4.’’ The Annual
Inspection Reports categorize the
piezometers as ‘‘A’’ or ‘‘B’’ in the
alphanumeric identifiers assigned to
each individual piezometer. Because
many of these ‘‘A’’ piezometers have
recorded ‘‘dry’’ conditions in later
monitoring events, it appears that the
‘‘A’’ series piezometers generally
represent the shallower portions of the
subsurface beneath the unit, e.g.,
screened primarily in CCR materials.
While there seems to be some degree of
overlap in the vertical dimension, the
‘‘B’’ series piezometers appear to be
screened into generally deeper
stratigraphic intervals than the ‘‘A’’
series, and generally reflect water levels
in the deeper portions of the CCR waste
as well as the underlying native aquifer
materials in contact with the waste.
The groundwater elevations measured
in ‘‘A’’ and ‘‘B’’ series piezometers for
the post-closure period from 2019
through 2021 varied over similar ranges.
Groundwater elevations measured in the
‘‘A’’ series ranged from 414.58 to 447.4
28 Permit Application at Note ‘‘1’’ on Figures A–
5 through A–8.
29 The TVA reports are titled: 2022 Engineering
(Annual) Inspection of CCR Facilities dated May 9,
2022; FY2021 Intermediate Inspection of CCR
Facilities dated May 6, 2021; FY2020 Intermediate
Inspection of CCR Facilities dated July 29, 2020;
FY2019 Intermediate Inspection of CCR Facilities
dated August 30, 2019; FY2018 Intermediate
Inspection of CCR Facilities dated September 4,
2018; and FY2017 Intermediate Inspection of CCR
Facilities dated December 15, 2017. Collectively,
EPA is referring to one or more of these reports as
the ‘‘Annual Inspection Reports.’’
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ft above MSL during this post-closure
period whereas groundwater elevations
in the ‘‘B’’ series ranged from 414.5 to
445.1 ft above MSL during the same
period. Average piezometric water
levels in the shallow ‘‘A’’ piezometers
during this post-closure period were
generally at or above 430 ft above MSL
beneath most of the footprint of the unit,
except for a lobe of lower groundwater
elevations (generally measured from 423
to 428 ft above MSL or below) in the
east-central portion of the unit. The only
groundwater elevations measured at or
below 422 ft above MSL were at
locations on the extreme eastern edge of
the impoundment or further eastward in
the vicinity of Cane Creek. At the deeper
‘‘B’’ piezometers, average groundwater
elevations during the post-closure
period from 2019 to 2021 were observed
to be universally greater than 425 ft
above MSL except for a thin strip along
the eastern margin of the impoundment
containing a small area (approximately
15% or less of the unit’s footprint area)
of somewhat lower groundwater
elevations (ranging generally from 416
to 424 ft above MSL), which projects
into the unit in the vicinity of
piezometer COF_P4_VWP03_B. Lastly,
the most recently reported groundwater
elevation measurements in each
piezometer and well (in 2021) continue
to show a similar pattern, with nearly
all groundwater elevation values
between 425 to 440 ft above MSL,
except for a thin strip of lower
groundwater elevations near the
extreme eastern margin of the
impoundment, again with a small lobeshaped area of lower groundwater
elevations (421.5 to 424.2 ft above MSL)
projecting a short distance into the
central part of the unit from the eastcentral edge. Again, groundwater
exceeding the average waste elevation of
422 ft above MSL was measured across
virtually the entire unit.30
30 EPA’s analysis of post-closure (2019–2021)
groundwater elevations within the unit evaluated
‘‘A’’ and ‘‘B’’ series piezometers. It should be noted
that the ‘‘A’’ series also included a number of
additional piezometers with an ‘‘S’’ designation
indicating shallow screened interval depths.
Evaluation of ‘‘A’’ series data also included shallow
alluvium monitoring wells COF–104, –105, and
–111, and CA–17A. Evaluation of ‘‘B’’ series data
also included alluvium monitoring wells COF–104,
–105, and –111. It should be noted that these
monitoring wells are located along the extreme
eastern periphery of the unit or downgradient to the
east of the unit. It is also noted that these few
monitoring wells consistently recorded some of the
lowest groundwater elevations in the combined ‘‘A’’
and ‘‘B’’ data sets. In this this respect, the average
values for the ‘‘A’’ and ‘‘B’’ piezometers are
somewhat lower than they would be if the
monitoring well data were excluded. This is to say
that actual average groundwater elevation
conditions within the unit proper are likely slightly
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EPA also evaluated these data using
common commercially available
software for contouring groundwater
data,31 creating a series of maps that
present a series of potentiometric
surfaces and groundwater elevation
measurements based on monitoring well
and piezometer data from within Ash
Pond 4, for various time frames and
representative values, including preclosure, during or immediately after
closure, and post-closure. These
groundwater elevation contour maps are
available in Section II.b of the TSD
Volume I.
While different software packages
could be used to contour groundwater
data and many different interpolation
methods, EPA’s contouring approach
honors the data and other known
constraints and is a conservate
estimation of site conditions on those
dates. These computer-generated
contour maps are useful to illustrate
what the measured groundwater
elevations reveal: that groundwater
levels decreased immediately after
closure, but even several years later
groundwater levels continue to exceed
not only the lowest documented waste
bottom elevation (413.5 ft above MSL),
but also the average waste bottom
elevation (422 ft above MSL) of the CCR
in the unit. The computer-generated
contours of average groundwater
elevations representing pre-closure
conditions measured at monitoring
wells from January 1, 2016, through
December 31, 2017, indicate
pronounced groundwater mounding
centered on the central and southcentral
portions of the unit where a broad
region of groundwater elevations on the
order of 450 ft above MSL are outlined.
See Section II.b in TSD Volume I.
Contours of average groundwater
elevations over a timeframe that
includes the initiation of unit closure,
measured at monitoring wells and
piezometers from January 1, 2018,
through December 31, 2019, indicate a
reduction in the groundwater elevations
beneath the central part of the unit to
values on the order of 430 ft above MSL.
A significant reduction in groundwater
elevations as compared to pre-closure
conditions is evident from these data.
Id. Further decreases in groundwater
elevations are indicated from computergenerated contours of average
groundwater elevations measured at
monitoring wells and piezometers postclosure from January 1, 2020, through
higher than these assessments reflect due to the
inclusion of the monitoring well data.
31 EPA used EnviroInsite software to visualize
geotechnical data (e.g., contouring groundwater
elevation data from discrete point measurements).
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December 31, 2021. However, the
magnitude of groundwater elevation
decreases is much smaller compared to
the period just after closure, with the
northeastern corner of the unit
indicating the greatest relative decrease.
Id. It is important to note that despite
the post-closure decreases in
groundwater elevations, groundwater
levels currently remain well above the
lowest recorded waste bottom elevation
(413.5 ft above MSL) of CCR in the unit
as well as the average (422-ft above
MSL) waste bottom elevation of CCR at
the preponderance of the impoundment.
It is important to note, however, that
the foregoing analyses are somewhat
skewed to the high side of the range of
groundwater fluctuation because the
Annual Inspection Reports list the
highest recorded value for each location
over the reported time interval
(approximately the previous year). It is
possible that some portions of the unit
are above the water table during certain
times of year or under certain
hydrologic conditions. Nevertheless, the
available reported data strongly suggests
that there is a large and measurable
volume of persistent wet CCR present in
the closed unit. With these caveats,
EPA’s overall analysis of groundwater
elevation data for Ash Pond 4 is as
follows.
Prior to closure, there appears to have
been significant groundwater mounding
beneath Ash Pond 4 that has slowly
decreased since pond closure. Such
mounding resulted in substantially
higher groundwater levels directly
beneath the impoundment that
generally decrease radially (as indicated
by lower levels consistently measured
in the monitoring wells in the
peripheral and downgradient portions
of the unit). As discussed above, it
appears that the ‘‘A’’ piezometers
(assumed shallow) are screened within
the CCR materials and are measuring
piezometric head beneath the
impoundment area and the (assumed)
deeper ‘‘B’’ piezometers are sampling
groundwater in the native geologic
materials and/or CCR near the base of
CCR waste beneath the impoundment.
The reported groundwater elevations in
both the ‘‘A’’ (shallow) and the ‘‘B’’
(deeper) piezometers indicate that
groundwater continues to infiltrate into
the CCR in many portions of the closed
unit as noted in the paragraphs above.
While the assumed deeper piezometers
(‘‘B’’ series) typically have water levels
somewhat closer to those observed in
the monitoring wells peripheral to the
unit, the generally higher elevations in
the shallow (‘‘A’’) piezometers versus
the deeper (‘‘B’’) piezometers indicates
that a downward vertical gradient likely
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existed between the impoundment and
the underlying geologic materials prior
to closure, that the general potential for
downward vertical hydraulic gradients
has been sustained during and following
closure, and that it persists currently,
many years after closure. A detailed
analysis of well/piezometer
construction information, boring logs
and other data are needed to further
confirm and assess persistence,
magnitude, and variability of downward
vertical hydraulic gradients from the
unit to the underlying aquifers.
Upgradient (west) groundwater
elevations were consistently above
waste bottom elevations, whereas
downgradient waste bottom elevations
were consistently near or above
groundwater elevations. In a general
sense, Ash Pond 4 can be described as
a quasi-wedge-shaped body with higher
elevations and generally thicker waste
profiles on the west side, sloping
eastward where generally thinner waste
profiles occur at lower elevations to the
east. While the groundwater table also
generally slopes from west to east, the
groundwater elevation surface (i.e.,
water table) does not fall to the level of
the base of the waste except in small
portions of the eastern half of the unit,
at best, and at worst only near the
extreme eastern margins of the unit.
This equates to a quasi-wedge-shaped
body of saturated waste with generally
higher elevations and greatest
thicknesses to the west, pinching out in
the eastward direction at the eastern
margin of the unit.
These data and analyses underscore
the general concerns that absent active
engineering measures, which the permit
approved by Alabama does not require,
groundwater will continue to infiltrate
into and flow out of Ash Pond 4 and the
waste will remain wet for the
foreseeable future.
iii. Volumes of Saturated CCR Estimates
Based on the available information
concerning the configuration of the CCR
waste mass, elevation and configuration
of the surface defining the interface
between the CCR waste and underlying
native geologic materials, and the
position of the water table under a
variety of conditions, EPA made a series
of calculations to estimate the volume of
CCR in Ash Pond 4 that continues to be
saturated with groundwater. In all the
estimates, the volume of saturated waste
is generally estimated to be the area
within the impoundment where
groundwater elevations exceed the
average bottom elevation of 422 ft above
MSL, using computer contouring
software to create modeled contours of
the groundwater elevation surface
within the unit. Under all scenarios
considered, substantial volumes of CCR
remain saturated by continually
infiltrating groundwater. EPA’s analyses
and the resulting estimates can be found
in Section II.c of the TSD Volume I.
EPA estimates that significant
volumes of saturated CCR currently
remain in the closed unit, ranging from
346,183 to 914,774 CY of CCR. EPA
further estimates that approximately
13% to 35% of the total volume of CCR
in the unit remains in the groundwater,
55235
and that 75% to 97% of the total unit
surface area is underlain by saturated
CCR. Finally, EPA estimates that, on
average, approximately 6 to 13 feet of
the CCR remains saturated with
groundwater. See Table II below.
Under this approach, EPA used a 2ft contour interval to create more
granular digital models of the
groundwater surface elevation.
Computer contouring software was
further used to calculate the areas
contained between successive 2-ft
contour lines and to calculate the
average groundwater elevation for that
subregion. Saturated waste thickness
values were then calculated for each
sub-area containing groundwater
elevations greater than 422-ft above
MSL. Thickness values were then
multiplied by the respective areas
computed for each sub-area to obtain
partial volumes of CCR in the aquifer.
Total volumes of saturated CCR were
then computed by adding the partial
volumes for each sub-area.
Using this approach, three separate
estimates of volumes of saturated CCR
were calculated from average
groundwater elevations reported from
overburden monitoring wells for the
following time periods:
• Spring 2019 (January 1, 2019,
through May 31, 2019),
• Spring 2020 (January 1, 2020,
through May 31, 2020), and
• Spring 2021 (January 1, 2021,
through May 31, 2021).
Table II summarizes the volumes and
areas of saturated CCR calculated for
each of these time intervals.
TABLE II—DEPTH, SURFACE AREA, AND VOLUME ESTIMATES OF SATURATED CCR AT ASH POND 4 FOR 2019–2021
Estimates of saturated CCR
Spring 2019
Total Surface Area of Unit (SY) a ................................................................................................
Total CCR Volume (CY) b ............................................................................................................
Average Thickness of Saturated CCR (ft) ...................................................................................
Surface Area of Unit with CCR in Groundwater (SY) .................................................................
Percentage of Unit Area with CCR in Groundwater (%) .............................................................
Volume Percentage of Saturated CCR (%) ................................................................................
Volume of Saturated CCR (CY) ..................................................................................................
a Source:
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b Source:
275,880
2,600,000
13
263,907
96
35
914,774
Spring 2020
275,880
2,600,000
13
267,657
97
33
858,445
Spring 2021
275,880
2,600,000
6
204,302
75
13
346,183
AECOM. Closure and Post-Closure Plan. October 12, 2016.
CTI and Associates. FY2021 Intermediate Inspection of CCR Facilities. May 6, 2021.
The 2019 and 2020 total estimates of
saturated CCR for the unit were similar,
914,774 and 858,445 CY, respectively.
Total volume estimates for 2021 were
lower (346,183 CY) owing to lower
average groundwater elevations over
that period as compared to 2019 and
2020. It should be noted that daily
precipitation amounts from publicly
available data indicate a greater level of
rainfall in the proximity of the unit in
Spring 2020 as compared to 2021.
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Additionally, ambient groundwater
levels in monitoring wells outside of the
impoundment were generally higher in
2020 as compared to 2021. Lastly, there
is a greater number of monitoring points
with reported water level data for 2020.
It is therefore likely that variations in
local precipitation exert a strong and
variable influence on groundwater
elevations beneath and in the vicinity of
the unit, and therefore the lower levels
in 2021 are not enough to support a
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conclusion that the unit will eventually
dry itself out. In any case, the
supplemental analysis using the more
refined contour intervals is consistent
with and within the upper and lower
bounds of previous estimates, further
corroborating the overall conclusion of
sustained and ongoing presence of
significant volumes of CCR that
continues to be infiltrated by
groundwater from within the unit. The
magnitude of the estimates clearly
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varies in response to fluctuations in
groundwater levels beneath the unit due
to variation in annual precipitation and
other factors, including closure.
However, despite some evidence that
water levels have declined somewhat
since closure, the record supports a
conclusion that substantial volumes of
CCR will continue to be perpetually
inundated by groundwater.
Based on all these data EPA is
proposing to determine that both the
Closure Plan approved by ADEM and
incorporated into the permit, and the
closure itself (which ADEM also
approved) are not consistent with the
requirements in § 257.102(d). Neither
the approved Closure Plan nor any other
document in the record for the permit
accounts for the levels of groundwater
present in the unit prior to closure or
describes any engineering measures
taken to meet each of the Federal CCR
closure-in-place performance standards
in § 257.102(d)(1) and (2) in light of the
groundwater present in the unit. Nor,
based on the post-closure groundwater
elevation data from piezometer wells
from 2019 to the present, did the
approved closure address the
groundwater continuously flowing into
and out of the CCR, as required by the
Federal regulations.
The Federal regulations require that
‘‘prior to installing the final cover
system . . . [f]ree liquids must be
eliminated by removing liquid wastes or
solidifying the remaining wastes and
waste residues.’’ 40 CFR 257.102(d)(2).
Free liquids are defined as all ‘‘liquids
that readily separate from the solid
portion of a waste under ambient
temperature and pressure,’’ regardless of
whether the source of the liquids is from
sluiced water or groundwater. 40 CFR
257.53. As EPA has previously
explained, based on the regulatory
terms, the structure, and context in
which the terms are employed, as well
as the dictionary definitions of ‘‘liquid,’’
and the fact that nothing in the
regulatory definition limits the source of
the liquid, EPA considers groundwater
to be a liquid under the existing
regulation.32 Consequently, the
directive applies to both the
freestanding liquid in the impoundment
and to all separable porewater in the
impoundment, whether the porewater
was derived from sluiced water,
stormwater runoff, or groundwater that
migrates into the impoundment.
TVA’s Annual Inspection Reports
from 2016 through 2018 show that
32 U.S. EPA. Denial of Alternative Closure
Deadline for General James M. Gavin Plant,
Cheshire, Ohio. November 18, 2022. pp 14–42; 88
FR 31,982, 31,992–31,993 (May 18, 2023).
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groundwater was infiltrating into Ash
Pond 4. The average groundwater
elevations measured at monitoring wells
inside Ash Pond 4 from January 1, 2016
through December 31, 2017 were on the
order of 450 feet above MSL (i.e.,
approximately 28 feet above the average
elevation of the CCR) centered on the
central and southcentral portions of the
unit).33 Yet neither the approved
Closure Plan nor any other document in
the record for the permit accounts for
the approximately 28 feet of
groundwater present in the unit prior to
closure, or describes any engineering
measures taken to eliminate the
groundwater. The approved Closure
Plan states only:
Final Closure of the Ash Pond 4 requires
following general tasks: . . . Begin decanting
the Ash Pond 4 using pumps and existing
siphons. Discharged water will be monitored
throughout decanting operations to maintain
compliance with NPDES [National Pollutant
Discharge Elimination System] permitted
limits.
TVA Closure Plan, pp 6–7. As EPA has
previously explained, § 257.102(d)(2)(i)
establishes a clear standard to be met:
‘‘free liquids must be eliminated.’’ 34
The regulation further specifies how
this standard is to be met: by ‘‘removing
liquid wastes or solidifying the
remaining wastes and waste residues.’’
Id. In situations such as this, where the
waste in the unit is inundated with
groundwater, the requirement to
eliminate free liquids thus obligates the
facility to take engineering measures
necessary to ensure that the
groundwater, along with the other free
liquids, has been permanently removed
from the unit prior to installing the final
cover system. See, 40 CFR
257.102(d)(2)(i). Yet neither the Closure
Plan that ADEM approved nor the
permit ADEM issued contained any
such requirements.
Moreover, it is clear from the postclosure 2019–2021 Annual Inspection
Reports that whatever measures were
taken as part of closure did not actually
eliminate free liquids from Ash Pond 4.
These reports document average
groundwater elevations within the Ash
Pond that significantly exceed 422
above MSL. And the most recently
reported groundwater elevation
measurements in 2021 reported nearly
all groundwater elevation at values of
425 to 440 ft above MSL, except for a
33 Tennessee Valley Authority. FY2018
Intermediate Inspection of CCR Facilities.
September 4, 2018; and Tennessee Valley
Authority. FY2017 Intermediate Inspection of CCR
Facilities. December 15, 2017.
34 See, U.S. EPA. Denial of Alternative Closure
Deadline for General James M. Gavin Plant,
Cheshire, Ohio. November 18, 2022. pp 14–42.
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thin strip of lower ground water
elevations near the extreme eastern
margin of the impoundment, again with
a small lobe-shaped area of lower levels
(421.5 to 424.2 ft above MSL) projecting
a short distance into the central part of
the unit. All of this information was
available before ADEM issued the
permit in October 2022, yet the permit
was issued, essentially approving
closure with CCR that will remain
saturated by groundwater, with no
engineering measures to limit
groundwater from continually flowing
into and out of the unit.
A further concern is that, given the
groundwater levels that continue to be
measured in the unit, it is not clear that
the remaining wastes have been
stabilized sufficiently to support the
final cover system, as required by
§ 257.102(d)(2)(ii). What is clear,
however, is that neither the approved
Closure Plan nor ADEM’s permit
provides any details on how this
performance standard was met, given
that groundwater continues to flow into
and out of the unit from the sides and
bottom. The approved Closure Plan
merely summarizes the § 257.102(d)(2)
performance standards, and contains,
for example, no description of how, if at
all, the groundwater levels would be
affected by any of the dewatering
activities associated with unit closure.
Consequently, EPA is proposing to
determine that the approval of the
Closure Plan, and subsequently the unit
closure itself, in the absence of such
information, and the failure to include
measures in the permit requiring TVA to
remedy the omission is not consistent
with § 257.102(d)(2)(ii).
EPA was also unable to find any
description in the ADEM approved
Closure Plan or any other permit
document of engineering measures that
TVA took to ‘‘control, minimize, or
eliminate, to maximum extent feasible’’
either the post-closure infiltration of the
groundwater into the waste or the postclosure releases of CCR or leachate to
the groundwater, as a consequence of
the groundwater that continues to
infiltrate into and be released from the
impoundment from the sides and
bottom of the unit. 40 CFR
257.102(d)(1)(i). Based on the data and
analyses described above, groundwater
continues to infiltrate into the unit and
yet the only measures described in the
Closure Plan and the permit are those
taken to facilitate consolidation and cap
construction. In essence, this means the
Ash Pond will continue releasing CCR
contaminants indefinitely past the waste
boundary unless TVA takes additional
actions that are not required by or
explained in the permit. Given that
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reasonably available engineering
measures exist that can prevent, or at
least control, the flow of groundwater
into the Ash Pond (and consequently
the releases out of the Ash Pond), such
as physical barriers or hydraulic
containment systems, EPA cannot
conclude that TVA’s Closure Plan
adequately describes how the closure
work will meet the requirement to
‘‘control, minimize or eliminate, to the
maximum extent feasible’’ post-closure
infiltration into the unit and postclosure releases of CCR or leachate to
the groundwater. EPA is proposing to
determine that the permit’s exclusive
reliance on engineering measures
related to the consolidation and cap
construction is inconsistent with
§ 257.102(d)(1)(i).
In addition, EPA was unable to
identify any description in the Closure
Plan narrative of how TVA will
‘‘preclude the probability of future
impoundment of water, sediment, or
slurry.’’ 40 CFR 257.102(d)(1)(ii). The
continued presence of groundwater in
the unit constitutes the impoundment of
water, and in the absence of any
engineering measures, such as a slurry
wall, there are no intrinsically obvious
facts to demonstrate that this
performance standard has been met.
Finally, the Closure Plan contains no
discussion of how the closure activities
will minimize the need for additional
maintenance of the Ash Pond beyond a
brief discussion of the final cover
system. 40 CFR 257.102(d)(1)(iv).
EPA raised these issues to ADEM in
comments on the draft Colbert permit.
In response, ADEM did not dispute
EPA’s conclusion that CCR in Ash Pond
4 remains saturated by groundwater.
Instead ADEM stated that EPA’s
comments were based on a
misinterpretation of the Federal
regulations, raising three specific
interpretations of the regulations that
EPA has previously rejected. First,
ADEM stated that ‘‘the Federal CCR
regulations do not require that the
closure account for groundwater levels
either before or after closure.’’ Rather
they claim the only requirements
relevant to groundwater are the location
restrictions applicable to new or
operating units in § 257.60 for an
operating unit.35 To support this point
ADEM argues that § 257.102(d)(1)(i)
does not refer to groundwater. Second,
ADEM argues that the Federal standards
have been met because Colbert has
installed a cover system that meets the
35 Letter
from Stephen Cobb to Carolyn
Hoskinson, Responding to EPA Comments on
Proposed Permit for the Tennessee Valley Authority
Colbert Fossil Plant. October 27, 2022. Enclosure 1,
page 6.
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standard in § 257.102(d)(3), and the
facility has complied with all of the
requirements in the general performance
standard relating to ‘‘infiltration.’’ The
State supports this claim by pointing to
the absence of specific requirements for
an infiltration layer or barrier along the
sides or bottom of a CCR unit, and by
defining ‘‘infiltration’’ to refer
exclusively to vertical infiltration from
the surface, e.g., as rainwater entering
through the cover system. Finally,
ADEM states that ‘‘In the event that it
is determined that the closure activities
conducted at Ash Disposal Area 4, as
described above, are insufficient to
prevent further groundwater
contamination, additional controls or
methods will be considered and
addressed through the ongoing
Assessment of Corrective Measures
(ACM) and selection of a final remedy,’’
that is, as part of corrective action.
EPA has explained, at length, that a
closed, unlined impoundment, where
the CCR remains in groundwater several
feet deep because the facility failed to
take any reasonably available
engineering measures to prevent, or at
least control, the flow of groundwater
into the unit (and consequently the
releases out of the unit), does not meet
the requirements of § 257.102(d).36
Specifically, in the final decision
denying an extension under Part A for
Gavin Generating Station, EPA
expressly rejected the various
interpretations of the regulatory text that
ADEM offers in its October 27 letter.
Specifically, EPA rejected the claim that
the Federal closure regulations do not
require a facility to address groundwater
in the impoundment as part of closure.
As noted above, based on the regulatory
terms, the structure, and context in
which the terms are employed, as well
as the dictionary definitions of ‘‘liquid,’’
and the fact that nothing in the
regulatory definition limits the source of
the liquid, EPA considers groundwater
to be a ‘‘liquid’’ under the existing
regulation. See, Gavin Final Denial, p,
34; Response to Comments (RTC) on
Gavin Proposed Denial, pp. 42–43, 53–
58, 76.37 Moreover, the source of the
liquid is not important with respect to
its basic and fundamental designation as
a liquid. It therefore does not matter
whether the liquid in the surface
impoundment comes from the rain,
waters the facility deliberately places in
36 U.S. EPA. Denial of Alternative Closure
Deadline for General James M. Gavin Plant,
Cheshire, Ohio. November 18, 2022. pp 14–42.
37 U.S. EPA. Denial of Alternative Closure
Deadline for General James M. Gavin Plant
(Cheshire, Ohio) Response to Comments on
Proposed Denial (Docket ID No. EPA–HQ–OLEM–
2021–0590). November 2022.
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55237
the unit, floodwaters from an adjacent
river, or from groundwater—all are
liquids, and once present in the unit,
they have the same potential to create
leachate (another type of liquid), as well
as to contribute to hydraulic head and
drive flows driven by hydraulic
gradients, and potentially destabilize
the cover system.
EPA also explained its decision to
rely on the plain language meaning of
‘‘infiltration,’’ explicitly rejecting the
interpretation that the term refers only
to the vertical migration of liquid
through the cover system. See, Gavin
Final Denial, pp 34–38; RTC pp. 38–47.
Finally, EPA rejected the interpretation
that under part 257 risks from a CCR
unit submerged in groundwater are
properly addressed exclusively as part
of corrective action. Gavin Final Denial,
pp. 41, RTC, pp 65–68, 102.
Accordingly, EPA is proposing to
determine that ADEM’s permit
approved a closure of Ash Pond 4 that
is not consistent with § 257.102(d).
Because Alabama interprets its
regulations to impose different
requirements than the Federal
regulations in part 257, EPA must
determine that the State’s requirements
are ‘‘at least as protective as’’ the
Federal requirements in order to
approve the program. 42 U.S.C.
6945(d)(1)(B)(ii). All the information
available to EPA supports a conclusion
that the closure approved in the Colbert
permit is significantly less protective
than a closure that meets the
requirements under the Federal CCR
regulations. Simply put, this is because
allowing groundwater to continue
flowing through the waste indefinitely
will not protect human health and the
environment. As discussed at length in
88 FR 32008–32012 (May 18, 2023),
there are several ways in which the
failure to remove CCR from the water
table as part of closure can result in
significantly higher risks than a
comparable closure where waste no
longer remains in contact with the water
table.
The Electric Power Research Institute
(EPRI), a coal industry analytical group,
reached similar conclusions in a report
issued in 2006, finding that ‘‘[c]aps are
not effective when CCP is filled below
the water table, because groundwater
flowing through the CCP will generate
leachate even in the absence of vertical
infiltration through the CCP.’’ 38 39
38 CCP means ‘‘coal combustion product,’’
another term for CCR.
39 Electric Power Research Institute. Groundwater
Remediation of Inorganic Constituents at Coal
Combustion Product Management Sites, Overview
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Similarly, an earlier EPRI study
examined the dewatering of three sites,
two with ash situated above the water
table and one with ash in contact with
groundwater. The study concluded:
‘‘[T]he existence of saturated ash will
greatly reduce the effectiveness of any
cap design when the facility is
underlain by geologic materials with
high hydraulic conductivity, because
groundwater will continue to leach ash
constituents.’’ 40 The fact that coal ash is
in contact with groundwater can reduce
the effectiveness of dewatering as well:
‘‘[W]hen ash remains below the water
table, dewatering may be less effective
because groundwater continues to leach
constituents from the saturated ash,
particularly if the impoundment is
underlain by geologic media with
relatively high rates of groundwater
flow. In the case of [the studied site],
concentrations increased because
groundwater contact time with the
saturated ash increased when the
hydraulic gradient of the pond was
removed.’’
Finally, EPA is proposing to
determine that the record fails to
support a finding that ADEM’s
alternative approach of relying on
corrective action to impose additional
controls through the ongoing ACM and
selection of a final remedy will be as
protective as the Federal requirements.
As discussed previously, data that was
available at the time of permit issuance
documents that groundwater elevations
remain within the Ash Pond over three
years after closure was completed, yet
the permit that ADEM issued is silent
on the need to address this as part of the
corrective action process. Moreover, as
discussed in the next section, EPA has
serious concerns about the
protectiveness of the corrective action at
Colbert that ADEM is overseeing; for
example, it has been three years since
TVA posted its initial ACM, and the
facility has still not selected a remedy.
EPA is aware of no information to
support a conclusion that continuing to
allow saturated CCR to remain in Ash
Pond 4 while TVA delays corrective
action will protect human health or the
environment, and ADEM has offered no
explanation to support a conclusion that
it is.
Accordingly, EPA is proposing to
determine that the permit for the Colbert
Plant does not require TVA to achieve
compliance with either § 257.102(d) or
with alternative State standards that
of Technologies, Focusing on Permeable Reactive
Barriers. Technical Report. 2006. 3–6.
40 Electric Power Research Institute. Evaluation
and Modeling of Cap Alternatives at Three Unlined
Coal Ash Impoundments. Technical Report.
2001.1005165.
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EPA has determined to be at least as
protective.
b. Groundwater Monitoring and
Corrective Action Issues
i. Summary of Federal Requirements
The objective of a groundwater
monitoring system is to characterize
groundwater to determine whether it
has been contaminated by the CCR unit
being monitored. This begins in
detection monitoring, by conducting
statistical comparisons between (1) The
background level of a constituent
measured in one or more upgradient
wells, and (2) The level of that same
constituent in a downgradient well. If
the concentration of the constituent in
the downgradient well is higher than
the background concentration by a
statistically significant amount, (i.e., a
statistically significant increase (SSI)
over background has been detected),
this provides evidence of a potential
release from the unit. After an SSI,
assessment monitoring is required for
additional constituents, and the
concentrations of each of those
constituents at downgradient wells are
compared to a groundwater protection
standard established for each
constituent (either background level or
a regulatory limit). Prompt contaminant
detection is important in order for
corrective measures to be developed to
stop migration of contaminants as soon
as possible.
To ensure detection of a release, the
regulations establish a general
performance standard that all
groundwater monitoring systems must
meet: all groundwater monitoring
systems must consist of a sufficient
number of appropriately located wells
that will yield groundwater samples in
the uppermost aquifer that represent the
quality of the background groundwater
and the quality of groundwater passing
the downgradient waste boundary,
monitoring all potential contaminant
pathways. 40 CFR 257.91(a)(1) and (2).
Because hydrogeologic conditions vary
so widely from one site to another, the
regulations do not prescribe the exact
number, location, and depth of
monitoring wells needed to achieve the
general performance standard. Rather
the regulation requires installation of a
minimum of one upgradient and three
downgradient wells, as well as any
additional monitoring wells necessary
to achieve the general performance
standard of accurately representing the
quality of the background groundwater
and the groundwater passing the
downgradient waste boundary,
monitoring all potential contaminant
pathways. 40 CFR 257.91(c)(1) and (2).
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The number, spacing, and depths of the
monitoring wells must be determined
based on a thorough characterization of
the site, including a number of
specifically identified factors relating to
the hydrogeology of the site (e.g., aquifer
thickness, groundwater flow rates and
direction). 40 CFR 257.91(b).
Groundwater elevation measurements
must be obtained around the unit(s) at
sampling events over time to
characterize groundwater flow direction
and identify seasonal and temporal
fluctuations. 40 CFR 257.91(b). Further,
any facility that determines that the
regulatory minimum number of wells is
adequate to meet the performance
standard must document the factual
basis supporting that determination. 40
CFR 257.91(f). In essence, the regulation
establishes a presumption that the
minimum of one upgradient and three
downgradient wells is not sufficient,
and it requires the facility to rebut the
presumption in order to install only this
minimum. See, 80 FR 21399. The
number and placement of the
monitoring wells is critical to proper
characterization of the groundwater.
The Federal CCR regulations establish
a phased approach to monitoring. The
first phase is detection monitoring
where ‘‘indicator’’ constituents are
monitored to determine whether
groundwater is potentially being
contaminated. In selecting the
parameters for detection monitoring,
EPA chose constituents that are present
in CCR and would rapidly move
through the subsurface, and thus
provide an early indication of other
contaminants that may be migrating
from the CCR units. See, 80 FR 21397.
The constituents that are monitored in
detection monitoring are listed in
Appendix III to 40 CFR part 257.
After groundwater samples are
collected during each monitoring event,
the samples are sent to a laboratory for
analysis to determine constituent
concentrations. Once the facility has the
analytical results, it must conduct
statistical analyses to determine the
background level of each constituent in
upgradient groundwater for comparison
with data from downgradient
compliance wells. This stage is also
critical, as even a sufficient number of
properly placed wells will not provide
adequate characterization if the
sampling and analysis of data are not
properly conducted. In order for
upgradient groundwater quality to be
accurately characterized, the statistical
approach must be appropriate for site
conditions and the data sets obtained.
To this end, the regulations require an
owner or operator to select a statistical
approach and meet the performance
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standards applicable to that approach
when analyzing the data. 40 CFR
257.93(f)–(g).
If a facility determines that there is an
SSI over background levels for one or
more of the constituents in Appendix III
at a monitoring well at the
downgradient waste boundary, there is
an opportunity to complete an alternate
source demonstration (ASD) showing
that a source other than the unit (i.e., an
alternate source) was the cause of the
SSI. 40 CFR 257.94(e)(2). A successful
ASD must be sufficient to rebut the
presumption that the CCR unit is the
source of the SSI in a downgradient well
of a properly designed groundwater
monitoring network by demonstrating
that a source other than the CCR unit is
responsible for the SSI. An ASD
requires conclusions that are supported
by site-specific facts and analytical data
in order to rebut the site-specific
monitoring data and analysis that
resulted in an SSI. Speculative or
theoretical bases for the conclusions are
insufficient. If a successful ASD for an
SSI is not completed within 90 days, an
assessment monitoring program must be
initiated. Id.
In assessment monitoring, facilities
are required to monitor for additional
constituents of concern, which are listed
in appendix IV to part 257. Whenever
assessment monitoring results indicate a
statistically significant level (SSL)
exceeding the groundwater protection
standard has been detected at a
downgradient well for any of the
Appendix IV constituents, the facility
must start the process for cleaning up
the contamination by characterizing the
nature and extent of the release and of
site conditions that may affect the
cleanup, and by initiating an assessment
of corrective measures.
As discussed in Unit III.B of this
preamble and TSD Volume III, Alabama
adopted regulations that mirror the
Federal CCR regulations.
ii. TVA Colbert Groundwater
Monitoring Issues
ADEM approved the Groundwater
Monitoring Plan (GWMP) dated
December 10, 2021, and incorporated
the approved plan into the Final
Permit.41 Once ADEM approved and
adopted TVA’s GWMP into the permit,
the GWMP, rather than the referenced
State regulations, became the State
41 Alabama Department of Environmental
Management. Colbert Fossil Plant Coal Combustion
Residual Permit. Permit No. 17–11, October 25,
2022. Section V.A., specifying that ‘‘The Permittee
shall install and/or maintain a groundwater
monitoring system, identified in Table 1, as
specified in 335–13–15–. 06(2) and the approved
groundwater monitoring plan.’’
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requirements with which TVA is
required to comply. After reviewing the
GWMP and all the materials in the
permit record, EPA is proposing to
determine that the groundwater
monitoring network that ADEM
approved is less protective than the
Federal regulations in several regards.
As discussed below and in the technical
support document, EPA identified a
number of deficiencies in the approved
monitoring network.
First, EPA is proposing to determine
that the approved monitoring system
inappropriately includes numerous
monitoring wells located beyond the
waste boundary, as well as an
insufficient number of monitoring wells
at necessary locations and vertical
depths to ensure that all potential
contaminant pathways have been
monitored. In addition, EPA has
identified critical deficiencies in the
construction of a significant number of
the bedrock monitoring wells that call
into question the accuracy of the
monitoring data. As a consequence, EPA
is proposing to determine that ADEM’s
Final Permit fails to require TVA to
‘‘install a groundwater monitoring
system that. . .accurately represent[s]
the quality of the groundwater passing
the waste boundary of the CCR unit,
[and to monitor] all potential
contaminant pathways.’’ 40 CFR
257.91(a)(2).
(1) ADEM Issued a Final Permit That
Approved the Bedrock Wells To Not Be
Installed at the Waste Boundary in
Accordance With § 257.91(a)
The Federal CCR regulations require
that a downgradient monitoring system
‘‘be installed at the waste boundary that
ensures detection of groundwater
contamination in the uppermost
aquifer,’’ and define the uppermost
aquifer as ‘‘the geologic formation
nearest the natural ground surface that
is an aquifer, as well as lower aquifers
that are hydraulically interconnected
with this aquifer within the facility’s
property boundary.’’ 40 CFR 257.53,
257.91(a)(2). The cross sections and
boring logs that were included as
attachments to the Permit Application
confirm that the unconsolidated and
underlying limestone aquifers are
hydraulically interconnected and
communication via vertical migration
can occur. The hydraulic connection
between the Tuscumbia limestone
aquifer, and the Tennessee River/
Pickwick Reservoir and Cane Creek, as
well as the hydrogeologic continuum
between the Tuscumbia limestone and
the overlying epikarst, residuum, and
alluvial units of the upper aquifer
system, all indicate that the Tuscumbia
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is an integral part of the composite
uppermost aquifer system. Accordingly,
the entire horizontal length along the
CCR unit must be monitored in all
hydrogeologic units present, alluvium,
residiuum, epikarst, and bedrock in
accordance with § 257.91.
The approved GWMP includes
bedrock monitoring wells COF–111BR,
COF–112BR, COF–113BR, COF–114BR,
CA17B, CA30B, MC1, MC5C, and COF–
108BR (future installation), CA6
(background), and COF–116BR
(background) as part of the groundwater
monitoring system. However, none of
these bedrock wells are located at the
downgradient waste boundary as
expressly required by § 257.91(a)(2).
Instead, they are located hundreds of
feet away from this boundary. Among
the wells that monitor bedrock, only
COF–111BR is located adjacent to the
downgradient (east) side of the unit and
the other downgradient open-borehole
bedrock wells are located hundreds of
feet to the east, and in many cases on
the other side of Cane Creek.
Another systemic issue is that the
bedrock wells were installed as openborehole completions with long
permanently grouted surface casings,
and as a consequence have significant
potential to systemically exclude zones
that have been ‘‘cased off’’ from the
monitoring well network. Permanent
steel casing installations range from 14.6
to 76.0 feet in length for in-program
wells. These cased off intervals
represent potential data gaps, depending
on the circumstances and geology local
to that specific region of the unit. As a
highly relevant example, well COF–111
is screened from 9–19 feet below ground
surface (bgs). The open interval for the
adjacent well pair, COF–111 BR, is 76–
126 ft bgs. This results in a 57-foot
vertical gap at a critical location
adjacent to the unit’s downgradient
boundary, where the groundwater
quality is entirely unmonitored. This is
significant because the failure to
monitor in the variable and significant
zone of transition from uppermost
alluvium to residuum, epi-karst, and
finally to ‘‘unweathered’’ limestone
would be a significant and systemic data
gap in potential contaminant pathways.
Accordingly, EPA is proposing to
determine that ADEM has approved a
monitoring plan with an insufficient
number of monitoring wells at necessary
locations and vertical depths to ensure
that all potential contaminant pathways
have been monitored.
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(2) ADEM Approved Wells That Were
Not Constructed in Accordance With
§ 257.91(e), and as a Consequence the
Monitoring System Does Not Accurately
Represent the Quality of Groundwater
Flowing From Ash Pond 4
The Federal regulations provide that
‘‘monitoring wells must be cased in a
manner that maintains the integrity of
the monitoring well borehole.’’ 40 CFR
257.91(e). Integrity of the monitoring
well borehole includes all elements of
the well within and including the
borehole itself. Such elements include
the surface casing, generally intended to
isolate deeper geologic materials
(commonly consolidated materials, i.e.,
bedrock) from overlying unconsolidated
materials and associated groundwater,
but also the filter pack, bentonite and
grout seals, screened intervals, riser
pipe, and other constructed monitoring
well elements internal to the borehole
used to isolate and ensure the integrity
of the sampling interval (e.g., screened
interval). The integrity of these elements
individually and as an integrated system
is essential to meeting the performance
standards in § 257.91(a), (b), and (e).
As noted in ADEM’s October 27, 2022
letter, these installations included
installation of a permanently grouted
surface casing. ADEM further indicated
Rotosonic drilling methods were used to
identify the first three-to five-foot zone
of unweathered material, and that a
casing was installed from this depth to
the ground surface. It should be noted
that Rotosonic drilling can be a
disruptive process that may not result in
full recovery of undisturbed samples of
soil or bedrock. For this reason, absent
any additional information, the use of
the Rotosonic method as a tool for
discriminating between weathered,
partially weathered, and unweathered
bedrock, must be used with care,
particularly if sample materials are
altered, pulverized, or otherwise
destroyed or obfuscated by the process
of drilling as indicated by a ‘‘no
recovery’’ zone or interval.42 In a
variable zone of transition from
weathered material (residuum) to
unweathered bedrock (in this case
limestone), recovered samples from
each type of material would likely be
affected by the drilling process to some
degree, and most competent intervals
are often preserved to a greater degree
than decomposed or partially
decomposed intervals. In such a
context, absent documentation
demonstrating a continuous core sample
from the interval in question, with full
recovery, which penetrates and
42 See
Section II.d of TSD Volume I.
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unequivocally identifies the interface
between weathered and unweathered
material, it would not be possible to
confirm that any missing sample
intervals did not simply represent voids
or other potentially permeable zones.
The potential to mischaracterize three-to
five-foot zones as ‘‘competent and
unweathered’’ on the basis of an
incomplete sequence of samples
therefore appears to be substantial. It
should therefore be noted that in this
context a three-to-five-foot penetration
into ‘‘unweathered’’ bedrock would
generally not be considered a
‘‘conservative’’ approach, absent
additional information validating the
integrity of the casing seal and its
effectiveness in isolating the
‘‘unweathered’’ bedrock interval from
the overlying materials. In such a
scenario, at best, the penetration of just
a 3- to 5-foot interval of ‘‘unweathered’’
bedrock with variably weathered
materials just above introduces
uncertainty with respect to the integrity
and effectiveness of the casing in
isolating the open interval from
groundwater in the overlying residuum
and epikarst. Based on information
provided, it is not clear how the
approach (as described) can be
demonstrated to have achieved the
performance criteria outlined in
§ 257.91(e).
In addition, the boring and well
construction logs that were included in
the Permit Application indicate that
nearly one-half of the groundwater wells
surrounding Ash Pond 4 were
constructed as open boreholes in
bedrock, with open hole intervals
ranging from 45 feet up to as much as
100 feet in length. If EPA’s analysis is
accurate, nearly one half of the
groundwater monitoring wells
surrounding Ash Pond 4 appear to not
meet the casing requirements of
§ 257.91(e).
One limitation of open-borehole
bedrock wells of this kind is that the
entire bedrock interval serves as the
monitoring zone. In effect, the long open
interval serves as a reservoir within
which inputs from various fractures
intersected by the borehole are blended,
resulting in an average composition of
some kind. In this situation, it is very
difficult or even impossible to monitor
a specific zone because the
contaminants being monitored could be
diluted to the extent of being nondetectable. On this subject, ADEM’s
October 27, 2022, letter states:
An Interstate Technology and Regulatory
Council guidance document entitled
Characterization and Remediation of
Fractured Rock discusses construction and
design considerations for monitoring wells
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installed in karst aquifers. Section 7.3.3 states
‘‘Where the bedrock has adequate strength
and competency, monitoring wells may be
constructed as an open borehole.’’ Because of
the proven competent nature of the
Tuscumbia Limestone, there is substantial
confidence that the integrity of the
monitoring well borehole will be maintained.
To justify their approval of long open
borehole intervals, ADEM states:
As described above, the karst aquifer
present at this site consists of a rock matrix
with distinct fractures that create preferential
pathways for groundwater flow. Studies
comparing hydraulic properties measured
within different karst aquifers indicate that
conduits typically account for more than 95
percent of the permeability of an aquifer
(Rosenberry et al., 2008). Thus, because the
majority of water within the monitoring well
column will be provided by discrete fractures
of the bedrock unit, the potential for dilution
in the open hole borings would be limited.
While EPA agrees that fractured
intervals in the karst limestone aquifer
are highly relevant as contaminant
migration pathways as compared to the
(unfractured) rock matrix, treating all
discrete fractures that may contribute
groundwater and/or contaminants to a
borehole equally would fail to
‘‘accurately represent the quality of the
groundwater passing the downgradient
waste boundary.’’ 40 CFR 257.91(a)(2).
The implied logical extension—that is,
‘the majority of water in a large open
borehole may be sampled to provide
accurate and representative
groundwater samples—is simplynot
correct. The technical literature
provides a many detailed examples that
illustrate the opposite conclusion. See
Section II.d of TSD Volume I. A more
likely scenario is that specific fractures
serve as contaminant migration conduits
and a long borehole may cross connect
these fractures with fractures containing
clean and/or less contaminated
groundwater. In such a case, the water
in the borehole represents in effect a
blended average of the individual
contributions from the specific fractures
which it cross connects. As no
information has been provided which
indicate the means or methods by which
specific fractures may have been
isolated and more precisely monitored,
EPA is proposing to determine that the
long-screened interval open-borehole
monitoring wells yield blended or
otherwise unrepresentative samples,
and thus do not comply with the
performance standards in § 257.91(a)(1)
and (2) and (e). Many options are
available to redevelop and reconfigure
these existing open boreholes to fully
comply with the regulations, including
installing standard monitoring wells
(e.g., with discrete screened intervals)
within the open boreholes with discrete
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screened intervals targeted to the most
important discrete fracture zones, or a
variety of specialized technologies and
methods developed to address fracturespecific sampling in fractured bedrock
environments. ADEM chose to approve
the GWMP without requiring any of
them.
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(3) ADEM’s Permit Authorizes Intrawell
Data Comparisons That Are Not
Consistent With Federal CCR
Requirements
The approach to intrawell data
comparisons described in the approved
GWMP does not require TVA to achieve
compliance with the requirement in
§ 257.91(a)(1) to establish background
groundwater quality in an upgradient
well unless the criteria in
§ 257.91(a)(1)(i) or (ii) are met. The
approved GWMP contains procedures
that would allow TVA to update the
background data set used in intrawell
comparisons, which would mean
including data in the background
characterization that is potentially
impacted by a release from the CCR
unit.43 See, 40 CFR 257.91(a)(1).
Intrawell comparisons are not simply
a statistical method; in the CCR
regulations, they are an approach to
background characterization. Intrawell
data comparisons use samples taken at
different times from the same well to
characterize both background
groundwater quality and downgradient
compliance groundwater quality. This
means downgradient compliance wells
also serve as background wells.
Alternatively, interwell data
comparisons use samples taken from
different wells—upgradient or
sidegradient wells characterize
background groundwater quality and
downgradient wells to characterize
downgradient groundwater quality.
The Federal CCR regulations do not
mention interwell or intrawell
comparisons specifically; instead, they
establish requirements for
characterizing background. Background
groundwater quality is required to be
established in an upgradient well,
unless a groundwater flow gradient does
not exist or it can be shown that
groundwater samples from a well that is
not upgradient of the CCR unit would
characterize background groundwater
quality as accurately or more accurately
than samples from an upgradient well.
40 CFR 257.91(a)(1)(i),(ii). It also must
be demonstrated that the data were
gathered when the well was known to
43 Tennessee Valley Authority. Colbert Fossil
Plant Ash Pond 4 Permit Application, December 10,
2021. Appendix C Section 2.3, p. 4 of 9 (PDF p. 469
of 603).
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be uncontaminated by the CCR unit.
This generally means that background
data used in intrawell comparisons
must be obtained prior to placement of
CCR in the unit. This also indicates a
strong preference for interwell
comparison, which would necessarily
be used when background is established
in any well other than a downgradient
compliance well (i.e., an upgradient or
side gradient well).
The approach to intrawell data
comparisons described in the approved
GWMP includes procedures to
periodically update intrawell
background data sets. Updating
background data sets may be
appropriate in interwell monitoring,
where background groundwater quality
may change over time due to migration
of contaminants toward a CCR unit from
upgradient sources. However, in
intrawell monitoring, background data
were obtained at compliance wells at
the downgradient boundary of a
monitored CCR unit, prior to placement
of CCR in the unit. After a CCR unit
begins operation, sampling data
obtained from these downgradient wells
cannot be known to be unimpacted by
leakage from the unit.
Samples from downgradient
monitoring wells are intended to
determine whether a release could have
occurred. If concentrations of
constituents monitored at the
downgradient wells change, this would
not represent a change in background
groundwater quality, it would represent
a release from the CCR unit.
Mischaracterizing any increase in
constituent concentration at these wells
over time as a change in ‘‘background’’
would result in elevating background
levels and could mask releases by
preventing detection of SSLs of
constituents, which trigger corrective
action requirements.
Because the procedures for updating
background levels used in intrawell data
comparisons are approved in the Final
Permit, this permit does not require
Colbert to achieve compliance with
either the Federal requirements at
§ 257.91(a)(1) or an alternative State
requirement that is equally protective.
c. TVA Colbert Permit Corrective Action
Issues
In 2018 TVA detected SSLs for cobalt
and arsenic.44 TVA first completed an
ACM to comply with the requirements
of the Federal CCR regulations in July
2019 (‘‘2019 ACM’’). An ACM was
completed in 2021 to comply with a
44 Tennessee Valley Authority. 2019 Annual
Groundwater Monitoring and Corrective Action
Report, TVA Colbert. January 2020. p. 3.
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2018 Consent Decree issued by ADEM
(‘‘2021 CD ACM’’).45 The 2021 CD ACM
included State requirements applicable
to units not regulated by the Federal
program, as well as requirements
applicable to CCR units regulated by the
Federal program.
On October 25, 2022, ADEM issued
the Final Permit to TVA for Ash
Disposal Area 4 (also identified as Ash
Pond 4 in the 2021 CD ACM). The Final
Permit contained only the following
terms and conditions for corrective
action:
C. Assessment of Corrective Measures. The
Permittee must initiate an assessment of
corrective measures as specified in 335–13–
15–.06(7) if any constituent listed in
Appendix IV of 335–13–15 has been detected
at a statistically significant level exceeding
the groundwater protection standard, or
immediately upon detection of a release from
the CCR unit.
1. The permittee must continue to monitor
groundwater in accordance with the
assessment monitoring program while
assessing corrective measures.
2. Selection of Remedy. Based on the
results of the corrective measures assessment,
the Permittee must select a remedy as
specified in 335–13–15–.06(8).
3. Implementation of the Corrective Action
Program. Within 90 days of selecting a
remedy, the Permittee must initiate remedial
activities as specified in 335–13–15–.06(9),
and shall be required to modify the permit
in accordance with Section II.E.9.
In its Colbert Permit RTC, ADEM
explains that:
TVA submitted to the Department an
initial Assessment of Corrective Measures
(ACM) in July of 2019. A revised ACM was
submitted by TVA in April 2021 and is still
undergoing a detailed review to ensure that
the proposed final remedy selected by TVA
conforms to the requirements of ADEM
Admin. Code r. 335–13–15–.06(7) and (8).
The proposed corrective measures will use
monitored natural attenuation (MNA) and
institutional controls, interim responses, and
adaptive management. Should additional
revisions be required, the Department will
review them to ensure compliance with the
requirements of ADEM Admin. Code r. 335–
13–15–.06(7) and (8).
Because an ACM has not been finalized
and a final remedy has not been selected, the
permit does not include provisions for the
remediation of the groundwater at this time.
However, once a final remedy is determined
complete by the Department, the permit will
be revised to include such provisions. The
permit revision to include the final remedy
will include public participation.
The Final Permit issued by ADEM
merely reiterates the Alabama
45 Notice Of Electronic Filing in the Circuit Court
of Colbert County, Alabama. Alabama Department
of Environmental Management v. Tennessee Valley
Aut 20–Cv–2013–900123.00. C001 Alabama
Department of Environmental Management Joint
Motion for Entry of First Amended Consent. Decree.
August 15, 2018.
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regulations, which are the same as the
Federal corrective action requirements.
However, incorporating the regulations
verbatim in the permit does not require
TVA to achieve compliance with those
requirements. This is because ADEM
did not take into account relevant facts
about the status of corrective action at
Colbert, such as whether the 2019 ACM
complied with the regulatory
requirements, or whether the 2021 CD
ACM complied with either the Consent
Decree or the regulations or both.46 Most
importantly, ADEM did not adjudicate
what actions are still necessary in light
of those facts to achieve compliance
with the regulations and include those
actions as requirements in the Final
Permit. As a consequence, EPA is
proposing to determine that the permit
in essence authorizes TVA to continue
to delay selection of a remedy well
beyond the required deadline, in order
to pursue assessment of a remedy that
does not appear to meet the criteria in
§ 257.97(b).
In the Colbert Permit RTC, ADEM
states that it is still reviewing the 2021
CD ACM and has not determined
whether the ACM and TVA’s preferred
remedy (MNA with institutional
controls but no source control measures
beyond the existing closure with waste
remaining in place) complies with the
regulations. It is not clear whether
ADEM provided comments on the 2019
ACM or whether it believes that the
ACM satisfies the requirements in
§§ 257.95 and 257.96, which remain
applicable to Ash Pond 4. ADEM also
states in the Colbert Permit RTC that an
ACM has not been finalized and a final
remedy has not been selected, so the
permit does not include provisions for
the remediation of the groundwater.
Whether or not the 2021 CD ACM meets
the requirements of the regulations is
precisely the type of adjudication
required in a permitting action. What
the permittee is required to do in order
to achieve compliance with the
regulations must be determined prior to
final permit issuance, because the
permit must contain these requirements.
This is the role of a permitting authority
(i.e., ADEM).
Under the Federal regulations, an
assessment of corrective measures that
will ‘‘prevent further releases, remediate
any releases, and restore affected areas
to original conditions’’ is required once
46 The Federal CCR regulations State that an ACM
is complete when it is placed in the facility
operating record. 40 CFR 257.96(d). The regulations
require posting of this information to the publicly
accessible website within 30 days 40 CFR
257.107(d), (h)(8). The 2021 Revised ACM was not
posted to the TVA Colbert CCR website at the time
of EPA’s review.
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corrective action is triggered. 40 CFR
257.96. Section 257.96(c) requires an
analysis of the effectiveness of potential
corrective measures in meeting all
requirements and objectives of the
remedy required by § 257.97, and
mandates that the analysis address at
least the criteria listed in § 257.96(c)(1)
through (3). Based on the results of an
ACM conducted in accordance with
§ 257.96, a remedy that meets the
requirements of § 257.97(b) must be
selected ‘‘as soon as feasible.’’ 40 CFR
257.97(a).
The full extent of corrective action
requirements applicable to Colbert are
not yet known due to numerous
concerns about the adequacy of the
detection and assessment groundwater
monitoring system and its ability to
identify all SSLs. However, based on
review of the Final Permit, the Colbert
Permit RTC, the 2019 ACM, the 2021 CD
ACM, and the January 13, 2023,
Progress Report, EPA has identified a
number of areas in which it appears that
neither the ACMs nor the proposed
remedies are consistent with or as
protective as the Federal
requirements.47 At a minimum, EPA
would have expected the permit to have
clearly established a deadline for
submission of a final ACM and to have
identified specific corrections that must
be made to address the specific
deficiencies discussed in the paragraphs
below.
i. The Colbert Permit Does Not Require
TVA To Complete an ACM That
Includes an Assessment of Source
Control Measures in Accordance With
40 CFR 257.96
40 CFR 257.97(b)(3) requires that all
remedies control the source of releases
in order to reduce or eliminate, to the
maximum extent feasible, further
releases of contaminants into the
environment. Neither the 2019 ACM nor
the 2021 CD ACM contains any
assessment of measures to achieve this
requirement (i.e., source control).
Section 4.2. of the 2019 ACM states,
‘‘Since closure of the Ash Disposal Area
4 CCR Unit serves as a source control
measure, the remedial technologies
considered in the following sections are
focused on addressing the area of
groundwater exhibiting arsenic and
cobalt at concentrations above the
GWPS.’’ The 2021 CD ACM also does
not evaluate any source control
measures, focusing exclusively on three
groundwater remediation alternatives
47 Tennessee Valley Authority. TVA Seventh
Semi-Annual Report on the Progress of Remedy
Selection at Ash Disposal Area 4. January 13, 2023.
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involving MNA.48 However, the
assessment required by § 257.96 must
include more than one source control
measure, and must actually assess how
the various measures would perform
according to the criteria in § 257.96(c).
Here there is no assessment of the one
source control measure identified in the
ACMs—the closure of Ash Pond 4,
which left a significant amount of CCR
in contact with groundwater—and how
it would perform according to the
criteria in § 257.96(c) compared to other
source control alternatives, such as
clean closure or the imposition of
engineering measures to control or
eliminate the groundwater that
continues to flow in and out of the
impoundment.
ADEM’s failure to require submission
of an ACM that actually evaluates
whether the closure of the Ash Pond
meets the source control requirements
in § 257.97(b)(3) also undercuts their
claim that they will use the corrective
action process to address any remaining
concerns with respect to the closure of
the Ash Pond. In its October 27, 2022,
letter to EPA regarding compliance at
TVA Colbert, ADEM states on page 7,
In the event that it is determined that the
closure activities conducted at Ash Disposal
Area 4 . . . are insufficient to prevent further
groundwater contamination, additional
controls or methods will be considered and
addressed through the on-going Assessment
of Corrective Measures (ACM) and selection
of a final remedy . . .
Ash Disposal Area 4 completed
closure in 2018, and groundwater
monitoring in 2022 revealed SSLs of
additional constituents at wells without
prior SSLs, which indicates that the
closure activities were insufficient to
prevent further groundwater
contamination. Yet the permit issued by
ADEM does not require TVA to take any
action to remedy this deficiency.
ii. The Colbert Permit Does Not Require
Collection of Data Needed To
Characterize Site Conditions That May
Affect a Remedy To Support the
Assessments in the ACMs
40 CFR 257.95(g)(1) requires a facility
to characterize the nature and extent of
the release and any relevant site
conditions that may affect the remedy
ultimately selected. The
48 MNA refers to reliance on natural attenuation
processes to achieve corrective action objectives
within a time frame that is reasonable compared to
that offered by other, more active methods. The
‘‘natural attenuation processes’’ at work in such a
remediation approach generally include a variety of
physical, chemical, or biological processes that,
under favorable conditions, act without human
intervention to reduce the mass, toxicity, mobility,
volume, or concentration of contaminants in soil or
groundwater.
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characterization must be sufficient to
support a complete and accurate
assessment of the corrective measures
necessary to effectively clean up all
releases from the CCR unit pursuant to
§ 257.96. The 2019 ACM and 2021 CD
ACM do contain information about the
delineation of the identified releases.
Although, given the concerns discussed
previously about the adequacy of the
downgradient wells in the groundwater
monitoring well network, EPA is
concerned that additional plume
delineations may be needed, because
potential contaminant pathways are
unmonitored and additional releases
may have occurred.
But critically, the reports do not
include any information collected about
site conditions that would affect the
efficacy of any remedies analyzed in the
2019 and 2021 CD ACMs. Site data
needed to assess remedies vary
depending on the remedy being
assessed, but could include: speciated
results of constituent concentrations in
groundwater and soil, in dissolved and
suspended phases; concentrations of
constituents, if present, which are
necessary to complete reactions that
result in immobilization of
contaminants (e.g. iron or sulfur); and
data to confirm the presence of
attenuated and immobilized
contaminants in the subsurface, to
demonstrate attenuation is occurring
naturally. As discussed in subsequent
sections, the absence of such data is
particularly critical with respect to
MNA, which is the only remedy
identified in the 2021 CD ACM. But
neither ACM contains any of these data,
which would be needed to accurately
assess any of the remedies identified in
the 2019 and 2021 ACMs. Yet the Final
Permit does not include terms to
address these deficiencies, such as a
requirement to collect data to
characterize site conditions that would
affect the corrective measures
considered in either ACM, or a deadline
to submit a revised ACM that contains
such data.
iii. Colbert’s Permit Does Not Require an
ACM That Accurately Assesses
Alternatives According to the Criteria in
40 CFR 257.96(c)
40 CFR 257.96(c)(1) requires an
assessment of how well alternative
remedies will control exposure to
residual contamination. Instead, the
2019 ACM assesses potential risks from
any exposure to residual contamination
that may occur. This is inconsistent
with the Federal regulations and is, in
any event, a less useful metric to
evaluate control measure technologies
relative to one another, particularly
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when more than one alternative leaves
contaminants in the environment. This
is because this alternative criterion
serves as an assessment of harm from
the contaminants themselves if they are
not removed from the environment,
rather than an assessment of each
technology’s effectiveness at removing
them. For example, in Table 6–1 in the
2019 ACM—MNA is assessed as low
risk with respect to this alternative
criterion, but it would have assessed
poorly according to the criterion of how
well alternative remedies will control
exposure to residual contamination.
This is less an assessment of MNA’s
effectiveness at meeting the
requirements of § 257.97(b) and more an
assessment of whether those
requirements must be met, which is not
the purpose of the ACM. Moreover, this
conclusion of low risk is unsupported
by data or analysis.
The 2019 ACM also fails to consider
safety impacts and cross-media impacts.
See, 40 CFR 257.96(c)(1). The 2021 CD
ACM does not correct this deficiency as
it entirely fails to assess alternative
remedies with respect to this criterion at
all. The Final Permit issued by ADEM
does not require any actions, by a
deadline, to remedy these deficiencies
in the ACMs.
iv. The Final Permit Allows TVA To
Continue To Pursue a Remedy (MNA)
That Has Not Been Demonstrated To
Meet All of the Requirements in
§ 257.97(b)
The 2019 ACM for Colbert identified
MNA as one of several potential
corrective measures to address
groundwater contamination (i.e.,
hydraulic control and treatment; in-situ
treatment). However, the 2021 CD ACM
considers only MNA as a primary
remedy, which suggests that TVA is
now largely pursuing a remedy that
relies exclusively on MNA.
MNA refers to reliance on natural
attenuation processes to achieve
corrective action objectives within a
time frame that is reasonable compared
to that offered by other, more active
methods. The ‘‘natural attenuation
processes’’ at work in such a
remediation approach could generally
include a variety of physical, chemical,
or biological processes that, under
favorable conditions, act without human
intervention to reduce the mass,
toxicity, mobility, volume, or
concentration of contaminants in soil or
groundwater. However, mass reduction
through degradation generally is not a
viable process for most inorganic
contaminants (i.e., the constituents in
Appendix IV to 40 CFR part 257) in
groundwater, except for radioactive
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55243
decay. These constituents are atoms,
and atoms do not break down or
degrade through any naturally occurring
process unless they are radioactive.
Thus, while MNA can reduce the
concentration or mobility of inorganic
contaminants in groundwater if
immobilization occurs through
adsorption or absorption to subsurface
soils, it does not remove the
contaminants from the environment.
MNA, therefore, would not perform well
with respect to the requirement in
§ 257.97(b)(4), which requires that
remedies ‘‘remove from the
environment as much of the
contaminated material that was released
from the CCR unit as is feasible.’’ This
is particularly true in this circumstance,
where, as discussed in the next sections,
TVA has failed to collect the site data
needed to identify whether any
naturally occurring attenuation may be
occurring on-site, as well as the
mechanism by which it occurs, and to
assess whether site characteristics that
control and sustain this naturally
occurring attenuation are sufficient to
immobilize the entire release.
Assessments in an ACM are relative in
that the expected performance of the
different technologies are compared
with one another according to how well
each alternative meets each regulatory
criterion. Given both the absence of any
evidence of any attenuation
mechanisms occurring at the Ash
Disposal Area 4, and the conclusion in
the 2020 ACM that the other alternatives
such as pump and treat are feasible,
there would appear to be no basis for
assessing MNA more favorably than an
alternative that unquestionably removes
contaminants from the environment.
The Final Permit nevertheless allows
TVA to continue to attempt to validate
MNA as a technology instead of
accurately assessing alternatives based
on-site conditions and selecting a
remedy that meets the requirements in
§ 257.97(b).
v. ADEM Issued a Final Permit That
Impermissibly Allows a Remedy (MNA)
That Is Based on Unsupported
Assessments
The 2019 and 2021 ACMs assessed
the performance of MNA favorably
without any supporting data that
characterize site conditions that may
ultimately affect a remedy, as required
by § 257.95(g)(1). In order to legitimately
consider MNA as required by
§ 257.96(c), site data are needed to
identify any naturally occurring
attenuation that may be occurring, and
to assess whether site characteristics
that control and sustain this naturally
occurring attenuation are sufficient to
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immobilize the entire release. ‘‘It is
necessary to know what specific
mechanism (e.g., what type of sorption
or reduction and oxidation reaction) is
responsible for the attenuation of
inorganics so that the stability of the
mechanism can be evaluated. [. . .]
Changes in a contaminant’s
concentration, pH, oxidation and
reduction potential (ORP), and chemical
speciation may reduce a contaminant’s
stability at a site and release it into the
environment.’’ 49 Determining the
existence, and demonstrating the
irreversibility, of MNA mechanisms is
necessary to assess the performance,
reliability, ease of implementation, and
the time required to begin and complete
the remedy. 40 CFR 257.96(c)(1) and (2).
This information would ultimately be
necessary to assess how well MNA
meets the requirements of § 257.97(b).
MNA of inorganic contaminants
would be assessed most favorably at
sites where immobilization is
demonstrated to be in effect and the
process/mechanism is irreversible.
Immobilization that is not permanent
would require ongoing monitoring in
accordance with § 257.98(a)(1) as long
as immobilized constituents remain in
the aquifer matrix.
ddrumheller on DSK120RN23PROD with PROPOSALS3
(1) The ACMs Do Not Include Data That
Characterize Site Conditions or Identify
Any Attenuation Mechanisms Occurring
at the Ash Disposal Area 4
The site data that were collected focus
only on contaminant concentrations and
trend analyses regarding the presence of
contaminants. The 2019 ACM and 2021
CD ACM do not discuss how
attenuation may be naturally occurring
through any particular MNA
mechanisms (e.g., adsorption,
precipitation, dispersion). EPA was not
able to find any indication in the Final
Permit or supporting documentation to
confirm that the Permittee has identified
the mechanism by which MNA would
occur at the site. Nor is there any
condition in the Final Permit requiring
the development and submission of
such information. The Final Permit
should have required collection of
groundwater data (e.g., pH or oxidation
potential, speciated concentrations of
constituents of concern) as well as
samples to identify the presence of
immobilized constituent in subsurface
soils. The Final Permit also should have
required an amended ACM which
considered this information in the
assessment of all alternatives, including
49 Use of Monitored Natural Attenuation at
Superfund, RCRA Corrective Action, and
Underground Storage Tank Sites, EPA OSWER
Directive 9200.4–17P. April 21, 1999. p. 8.
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assessment of the performance of
identified naturally-occurring
attenuation mechanisms (i.e., MNA).
Determining the existence and
demonstrating the irreversibility of
MNA mechanisms is necessary to
evaluate the performance, reliability,
ease of implementation, and the time
required to begin and complete the
remedy. See, 40 CFR 257.96(c)(1) and
(2). This information would ultimately
be necessary to show that MNA meets
the requirements of § 257.97(b) and
would need to be supported with sitespecific characterization data and
analysis. Yet the Final Permit contained
no terms or conditions requiring TVA to
remedy these deficiencies.
(2) MNA Is Not a Viable Remedy
Without Source Control
From a scientific point of view, source
control is necessary in order for any
MNA remedy to be effective at a
particular site.50 In order to properly
assess MNA, first the attenuation
mechanisms (for inorganic metals, these
include both chemical and physical
reactions) by which the specific
constituents released may be
immobilized at a specific site must be
identified. As discussed above, no
mechanism was identified in either the
2019 or 2021 ACM. After attenuation
mechanisms are identified, it is
necessary to determine whether the
aquifer has the capacity (i.e., the
presence of these reactants available in
sufficient amounts) to provide those
reactions to attenuate the release that
has occurred. If site data are obtained
verifying the localized presence and
availability of reactants, appropriate
types of soil, and other factors needed
to immobilize the constituents, it must
be determined whether they are
available in sufficient quantities to react
with the quantity of constituents
released. This can be done using the
estimated mass of the release that was
calculated in accordance with
§ 257.95(g)(1)(ii), as well as site data
collected to determine the presence and
concentrations of the chemical and
physical materials required to complete
the immobilization reactions. If there
are enough available reactants to
immobilize the entire release, and the
site conditions are right for those
reactions to occur, then MNA may be
effective at immobilizing a release.
However, if the source of a release has
not been controlled (i.e., the CCR
remains in contact with groundwater
and releases are ongoing), then it is
impossible to know if an aquifer has the
capacity to attenuate the release, even if
50 Id.
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attenuation mechanisms have been
identified and site conditions are
favorable for those reactions to occur.
That is because the amounts of
contaminants being released will
continue over time, and releases of new
constituents could occur. Therefore, it is
impossible to determine whether the
aquifer has sufficient chemical and
physical materials required to complete
the immobilization reactions because
the total amount of the release is not yet
known.
At TVA Colbert, source control has
not been achieved. As discussed above,
the closure of Ash Pond 4 has resulted
in continuing releases from the closed
unit, i.e., a continual source of
groundwater contamination from the
unit. Therefore, based on the current
record, MNA is not a viable remedy for
Ash Pond 4. This should have been
addressed prior to permit issuance
during the permit application review
stage or by some other means, such as
a schedule of compliance in the final
permit, e.g., by requiring TVA to submit
a revised ACM that accurately assesses
MNA and includes a corrective measure
which achieves source control in each
alternative assessed.
(3) The Assessment of Cross-Media
Impacts in the ACMs Is Inaccurate and
Not Supported by Data
The table in the 2019 ACM, which
summarizes TVA’s assessment of
groundwater corrective measures, states
that MNA poses a low risk of crossmedia impacts. The reason given is that
‘‘all work activities occur in-situ.’’ This
conclusion is only accurate if natural
attenuation through immobilization is
occurring on-site, but no such showing
has been made. In fact, in the absence
of any information to the contrary, it is
more likely that MNA through dilution
and dispersion would occur, that is, by
mixing with clean groundwater as it
migrates from the unit, ultimately
transferring the contamination from
groundwater to surface water. But the
transfer of contamination from
groundwater to surface water is a crossmedia impact and it only occurs in-situ
until the groundwater reaches the
surface water. The assessment of low
risk of cross-media impacts is therefore
not supported by facts and site data.
See, 40 CFR 257.95(g)(1).
A similar table (6–1) in the 2021 CD
ACM assesses ‘‘potential adverse
impacts’’ as low. Its assessment of the
first alternative, MNA with no
institutional controls or adaptive
management, is favorable even though it
is noted that there would be no
protection of surface water in the short
term. In fact, because all three
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ddrumheller on DSK120RN23PROD with PROPOSALS3
alternatives rely on MNA and do not
include active remediation or
containment, none of them would
protect surface water in the short term.
It is unclear why this concern is not
noted in all the alternatives. There is
also no discussion of long-term impacts
to surface water. Accordingly, EPA is
proposing to determine that the
assessment of these potential remedies
as low risk is not supported by any
evidence, and that the assessment of the
third alternative does not meet the
requirements of § 257.96(c)(1) because it
does not consider impacts to surface
water (i.e., cross-media impacts).
The lack of data to support the
assessments in both ACMs means they
may not accurately reflect MNA’s
‘‘effectiveness of potential corrective
measures in meeting all of the
requirements and objectives’’ in
§ 257.97(b). 40 CFR 257.96(c)
Conclusions without a supporting
assessment or data do not constitute ‘‘an
analysis of the effectiveness of potential
corrective measures.’’ 40 CFR 257.96(c)
(emphasis added). In addition,
inaccurate assessments in an ACM can
ultimately result in selection of a
remedy that will not meet the
requirements of § 257.97(b). The Final
Permit issued by ADEM in October 2022
does not require TVA to take any
actions to remedy the deficiencies in
either the earlier 2019 ACM or
subsequent 2021 CD ACM.
(4) The 2021 CD ACM Is More Deficient
Than the 2019 ACM
Even though the 2021 CD ACM was
developed in response to comments
from ADEM, it not only fails to remedy
the deficiencies in the 2019 ACM, but
also contains provisions that raise
additional concerns. First, the remedial
objectives in section 1.3 of the 2021 CD
ACM do not address the requirements in
§ 257.97(b)(3) or (4) relating to source
control or the removal of the release
from the environment—rather, they only
consider off-site impacts of groundwater
contamination.
It is unclear whether the 2021 ACM
was intended to replace or to
supplement the 2019 ACM. But assessed
on its own merits, the 2021 CD ACM
failed to assess two remedies included
in the 2019 ACM: hydraulic control and
treatment and enhanced in-situ
treatment as primary corrective
measures. Only three alternatives are
considered in the 2021 CD ACM, which
all rely on MNA as the primary
corrective measure. The only
consideration of active corrective
measures is in alternative three, as part
of an adaptive management strategy if
MNA does not meet the remedial
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objectives on its own. Therefore, EPA is
proposing to determine that the 2021 CD
ACM does not meet the requirement in
§ 257.96(a) to assess corrective measures
‘‘to prevent further releases, to
remediate any releases and to restore
affected area to original conditions,’’
because the alternatives, limited to
MNA without additional source control,
would not meet any of these
requirements at the Colbert Plant.
(5) The Ongoing Data Collection and
Model Development Are Not Necessary
To Select a Remedy
According to the January 13, 2023
Progress Report, the facility has delayed
selection of a remedy by, among other
tasks, continuing to monitor the
migration of the release and developing
a computer model to predict
groundwater behavior. It is not
necessary to delay completion of an
ACM or selection of a remedy until a
model can be developed and refined;
the Federal regulations do not require
development of a groundwater model to
complete an ACM or to select a remedy.
Since actual site monitoring data—
rather than an estimate from a model—
is required to characterize the release
sufficiently to assess corrective
measures— the primary use of a model
in this stage of CCR corrective action
would be to estimate the amount of time
needed to complete a remedy. But this
estimate may be accomplished through
other methods (e.g., calculation of the
mass of the release, groundwater flow
velocity, hydraulic conductivity, and
the attenuation capacity of the
downgradient subsurface where MNA
mechanisms have been identified and
can be quantified). Nor is such delay
consistent with the requirements of
§ 257.95(g), which only requires
characterization ‘‘sufficient to support a
complete and accurate assessment of the
corrective measures necessary to
effectively clean up all releases from the
CCR unit pursuant to § 257.96.’’ In order
to support the assessment in the ACM,
this characterization must be complete
prior to the deadline to complete the
ACM.
Based on all of the above, EPA is
proposing to determine that the permit
fails to require the Permittee to select its
remedy ‘‘as soon as feasible,’’ as
required by § 257.97(a). Section 5.C.2 of
the permit, entitled ‘‘Selection of
Remedy,’’ only reiterates the regulatory
requirement that the Permittee must
select a remedy as soon as feasible. It
has been three years since the 2019
ACM for the Ash Pond was placed in
the facility’s operating record, and it is
not clear why the facility has not
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55245
selected a remedy.51 The 2021 CD ACM
does not reflect progress toward
selection of a remedy, as it does not
address any of the deficiencies in the
2019 ACM. For example, even though
the 2021 CD ACM focuses exclusively
on MNA, it still fails to identify any
attenuation mechanism, or to include
any of the supporting data that
characterize site conditions that may
ultimately affect a remedy, as required
by § 257.95(g)(1). For all the reasons
discussed above, EPA is proposing to
determine that neither the 2019 ACM,
the 2021 CD ACM, or the two ACMs
taken together meet the requirements of
§ 257.96 or § 257.97 or support selection
of a compliant remedy. By failing to
require TVA to obtain the necessary
data and submit a revised ACM by a
date certain, the Final Permit appears to
authorize the permittee to continue to
indefinitely delay selecting a remedy,
while the permittee continues to
conduct the same sampling it has
conducted since 2019, that is likely to
be insufficient to support the selection
of that alternative as a remedy.
Accordingly, EPA is proposing to
determine that the permit does not
require compliance with the Federal
requirements and, because it allows the
facility to continue to delay corrective
action, the alternative State requirement
is less protective.
2. Plant Gadsden
EPA reviewed the Final
Determination Initial Permit And
Variance for the Alabama Power
Company, Gadsden Steam Plant (Plant
Gadsden Permit), issued by ADEM
under Permit No. 28–09 on December
18, 2020.52 The permit summary on
Page 1 says:
[t]he Plant Gadsden Ash Pond is a CCR
surface impoundment located in Section 2,
Township 12 South, Range 6 East in Etowah
County, Alabama consisting of approximately
130.22 acres with a disposal area that
consists of approximately 58.73 acres. The
permit requires the Permittee to manage CCR
in accordance with the conditions of the
permit, ADEM Admin. Code r. 335–13–15,
. . . and the approved permit application.
. . .
The Permittee must comply with all
conditions of the permit except to the extent
and for the duration such noncompliance is
authorized by a variance granted by ADEM.
The first variance requests to exclude boron
as an Appendix IV assessment monitoring
51 Tenessee Valley Authority. 2019 Assessment of
Corrective Measures Report for the Ash Pond TVA
Colbert Fossil Plant, Tuscumbia, Alabama. July 15,
2019.
52 Alabama Department of Environmental
Management. Final Determination Initial Permit
And Variance for the Alabama Power Company,
Gadsden Steam Plant, issued under Permit No. 28–
09. December 18, 2020.
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constituent. The second variance requests
groundwater protection standards of 6
micrograms per liter (mg/L) for cobalt; 15 mg/
L for lead; 40 mg/L for lithium; and 100 mg/
L for molybdenum. The third variance
requests the final grade of the cover system
be less than 5 percent and greater than 25
percent. The fourth variance being requested
is from 335–13–15–.03(6) requiring a 100 foot
buffer from the perimeter of the facility
boundary.
a. Plant Gadsden Closure Issues
Section VII.B.1 of Plant Gadsden
Permit contains the following terms and
conditions:
A. Closure Timeframe and Notifications.
The Permittee shall close their CCR units as
specified in 335–13–15–07(2), this permit
and the Application.
B. Criteria for Closure.
1. Cover. Closure of a CCR landfill, surface
impoundment, or any lateral expansion of a
CCR unit must be completed by either
leaving the CCR in place and installing a
final cover system or through removal of the
CCR and decontamination of the CCR unit, as
described in 335–13–15–.07(3)(b) through (j).
The minimum and maximum final grade of
the final cover system may be less than 5
percent and greater than 25 percent, as
specified in the Permit Application. (See
Section IX.C.)
2. Written Closure Plan. The written
closure plan, as part of the Application, must
include, at a minimum, the information
specified in 335–13–15–.07(3)(b) 1.(i)
through (vi).
ddrumheller on DSK120RN23PROD with PROPOSALS3
The Ash Pond was closed by
removing CCR from the southern
portion of the Lower Pond (the area of
the western expansions in the 1970s)
and consolidating the ash in the Lower
Pond to about 30 acres in the northern
portion of the Lower Pond. The CCR in
the Upper Pond (original ash pond prior
to expansions) was regraded to achieve
a minimum 3% slope, and a cover
system was constructed over the regraded Upper Pond and consolidated
ash in the Lower Pond.53
Closure construction activities for the
Ash Pond were certified as completed in
October 2018, and a certification of
completion of closure activities was
later submitted in April 2020, and
approved by ADEM on June 9, 2022.54 55
i. Base of the Impoundment
Plant Gadsden is located in Gadsden,
Alabama, south of the Coosa River. The
Ash Pond is located on the north side
of and adjacent to the Coosa River. The
Permit Application states that the Ash
53 Alabama
Power. Revised Closure Permit
Application for the Plant Gadsden Ash Pond. April
30, 2020. Appendix 6.
54 Alabama Power. Plant Gadsden 2020 Notice of
Closure Completion Plant Gadsden Ash Pond
Alabama Power Company.
55 Alabama Power. Plant Gadsden 2022 Closure
Inspection Gadsden Steam Plant Permit No. 28–09.
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Pond was initially constructed in 1949
and subsequently expanded to the west
in 1976 and 1978.56 The Permit
Application states that the fully
constructed Ash Pond was 75 acres. Id.
at Appendix 8. Alabama Power closed
the Ash Pond by consolidating CCR to
a smaller area within the impoundment
footprint. Id. at Appendix 6. As a result,
the consolidated closed footprint of Ash
Pond 4 decreased to approximately 59
acres. Id. at Appendix 2.
EPA was unable to locate information
in the Permit Application or other
publicly available documents that
characterizes the bottom elevation of the
Ash Pond across its entire footprint.
Nonetheless, similar to the review for
the permit for Plant Colbert, EPA
estimates the average bottom elevation
of the impoundment for purposes of
calculating the volume of CCR that
remains saturated by groundwater. EPA
is estimating that the average bottom
elevation of the closed Ash Pond is 510
ft above MSL.57 This estimate is based
on consideration of the information
available in the Permit Application.
Specifically, EPA considered the
following information: (1) the original
ground surface contours shown on
construction drawings for areas that
were closed by leaving CCR in place; (2)
information showing that the bottom of
the impoundment was lower than the
original ground surface contours at
some locations while the unit was in
operation; and (3) closure-related
drawings portraying an estimated waste
bottom.
EPA’s estimate recognizes that the
original ground surface contours for
most of the impoundment footprint
(both the initial footprint and western
expansions) range between 505 to 515 ft
above MSL, or an average elevation of
510 ft above MSL. In addition, certain
closure drawings show that current
surface elevations in the upper northern
part of the unit are actually lower in
2016 than the original ground surface
elevations depicted on the 1978
expansion drawing. This means that the
original ground surface elevations
shown on the 1949, 1976, and 1978
drawings do not necessarily reflect the
bottom of the impoundment at closure
at all locations within the unit footprint.
The 2016 drawing shows the bottom
elevation at this upper northern part of
56Alabama Power. Revised Closure Permit
Application for the Plant Gadsden Ash Pond. April
30, 2020. Appendix 3.
57USEPA. Volume I: Technical Support
Document for the Proposed Notice to Deny
Alabama’s Coal Combustion Residuals Permit
Program, Supplemental Analyses of Technical
Issues with ADEM Permits. August 2023. Section
III.a.
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the unit to be no higher than 505 to 510
ft above MSL, which is lower than the
original ground contours at this location
that ranged from 510 to 515 ft above
MSL. Finally, the four cross-sections
provided in the Gadsden Permit
Application depict the impoundment
bottom appearing to range between 495
to 510 ft above MSL, but these crosssections are annotated with a note that
the bottom elevations have not been
verified. Based on the available
information, EPA’s estimated average
bottom elevation of 510 ft above MSL is
a reasonable reconciliation of the
available information.
ii. Characterization of Groundwater
Elevations
The CCR program groundwater
monitoring network installed at the unit
consists of fifteen downgradient
monitoring wells (GSD–AP–MW–1
through MW–12 and GSD–AP–PZ–1,
PZ–5, and PZ–6). The following
evaluation of groundwater elevation
data for the unit focuses on the twelve
monitoring wells that are immediately
adjacent to the waste boundary (i.e.,
MW–1 through MW–12). Monitoring
wells PZ–1, PZ–5 and PZ–6 are located
hundreds of feet from the waste
boundary and thus were not considered.
Also, three ‘‘upgradient’’ monitoring
wells (MW–14, –16, and –17) are
located to the southeast on the other
side of the Coosa River and are not
considered with respect to groundwater
elevations within the unit. Based on the
single groundwater flow map included
in the Permit Application,58 based on
August 19, 2019, data, groundwater
elevations in monitoring wells
surrounding the unit ranged from a high
of 512.03 ft above MSL along the
northeastern boundary of the unit
(GSD–AP–MW–3) to 506.95 ft above
MSL along the western boundary (GSD–
AP–MW–7). The potentiometric surface
contour map presented for August 19,
2019, reveals a somewhat radial flow
pattern, with highest groundwater
elevation values recorded along the
northeastern boundary of the facility.
Between monitoring wells GSD–AP–
MW–1 and GSD–AP–MW–4 along the
northeastern boundary of the unit,
groundwater elevation values are
similar, approximately 512 ft above
MSL, resulting in a northwest to
southeast trending ridge-like region of
relatively high groundwater elevations.
Groundwater elevations drop to the
north, northeast, northwest, west and to
58Alabama Power. Revised Closure Permit
Application for the Plant Gadsden Ash Pond. April
30, 2020, Appendix 7, Plant Gadsden Ash Pond
Groundwater Monitoring Plan, Figure 6.
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the south and southwest from this
central axis which is mapped as a
groundwater divide just east of the unit
boundary on the August 19, 2019, map.
There are no data in the Permit
Application that can enable a
determination of groundwater flow
directions to the east and southeast of
the unit, thus the possibility of
unmonitored flow in these directions
has not been ruled out. These
uncertainties notwithstanding (see Unit
IV.C.2.b of this preamble for additional
assessment of uncertainties associated
with the groundwater monitoring
network), the available information
indicates that groundwater from the Ash
Pond generally flows toward the surface
water features represented by the main
stem of the Coosa River as well as
toward the tributary stream segments to
the north and northwest of the unit.
Groundwater elevations within the unit
appear to be primarily controlled by the
consistently higher elevations along the
northeastern boundary of the unit as
well as the lower elevations associated
with the Coosa River to the northwest,
west, and southwest. On August 19,
2019, the elevation of the Coosa River
was reported to be approximately 508 ft
above MSL.59
It is important to note that the
groundwater elevations reported on
August 19, 2019, represent a relatively
low condition, on balance, and
groundwater elevation values measured
at the unit are observed to oscillate over
several feet on average in response to
seasonal rainfall or other variations,
with individual wells immediately
adjacent to the Ash Pond (i.e., GSD–AP–
MW–1 through MW–12) varying over a
range of approximately 3.9 to 8.5 feet
55247
between 2018 and 2022,60 which covers
the period after closure construction
activities for the Ash Pond were
certified as completed in October 2018.
Similarly, the Coosa River levels show
considerable variation, ranging from
503.3 to 512.6 ft above MSL between
2018 and 2022 as monitored by a gauge
located approximately 900 feet
upstream of GSD–AP–MW–11. Given
these fluctuations, EPA considered
additional groundwater elevation data
from documents included on Alabama
Power’s CCR website. Groundwater
elevation data from measurement events
since August 19, 2019, were initially
evaluated to illustrate the range of
groundwater elevation fluctuations at
the site, as summarized in Table III. The
recorded elevations of the Coosa River
on the corresponding dates are also
included on the table.
TABLE III—GROUNDWATER ELEVATION FLUCTUATIONS AT THE ASH POND AND CORRESPONDING COOSA RIVER
ELEVATIONS a
Groundwater elevation
(ft above MSL)
Coosa River elevation
(ft above MSL) b
Date
Maximum
8/19/2019 .....................................................................................................................
4/13/2020 .....................................................................................................................
8/24/2020 .....................................................................................................................
3/15/2021 .....................................................................................................................
10/4/2021 .....................................................................................................................
1/11/2022 .....................................................................................................................
5/5/2022 .......................................................................................................................
10/24/2022 ...................................................................................................................
Minimum
512.03
517.91
512.57
516.98
513.76
515.65
516.18
510.86
506.95
508.71
507.64
507.18
508.03
508.01
507.97
506.64
Range Over 24-Hour
Period
507.6–507.8
507.9–510.3
507.8–508
507–507.4
507.9–508.1
507.8–508.2
507.6–508.1
c 507.5–507.7
a Measured
at groundwater monitoring wells GSD–AP–MW–1 through GSD–AP–MW–12.
U.S. Geological Survey (USGS). See Section III.b.i of TSD Volume I for further details.
data are provisional and may be revised by the USGS.
b Source:
ddrumheller on DSK120RN23PROD with PROPOSALS3
c These
location over this same period of
interest was 5.9 feet.
These values were used in
conjunction with the estimates for the
bottom-of-waste elevation to calculate
estimated volumes of saturated waste, as
presented in the following section.
As shown here, groundwater levels
are variable, and are generally higher
during spring monitoring events (March,
April) as compared to late summer/fall
events (August, October). In
consideration of the 15 groundwater
elevation monitoring events from
October 4, 2018, through October 24,
2022, EPA calculated average minimum,
average maximum, and overall average
groundwater elevations within the unit
over the four-year period, as follows:
Groundwater Elevation (overall
average): 511 ft above MSL
Groundwater Elevation (average
maximum): 514.6 ft above MSL
Groundwater Elevation (average
minimum): 508.6 ft above MSL
The average range of fluctuation
between maximum and minimum
values at a particular monitoring well
Based on available information and
the averages discussed above, EPA
estimated the volume of CCR in the Ash
Pond that, on average, would continue
to be saturated with approximately 1 to
4.6 feet of groundwater.61 Because both
the base elevation of the waste and the
groundwater elevations vary, those
estimates both overstate and
underestimate the degree of saturation.
For example, at its lowest point, the
base of the impoundment measures 505
59Volume I: Technical Support Document for the
Proposed Notice to Deny Alabama’s Coal
Combustion Residuals Permit Program, EPA
Analysis of Alabama CCR Permits. U.S.
Environmental Protection Agency, Office of Land
and Emergency Management (5304T), 1200
Pennsylvania Avenue NW, Washington, DC 20460.
August 2023. Section III.b.i.
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iii. Volumes of Saturated Ash Estimates
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ft above MSL, and the highest elevation
of groundwater was measured at 519.26
ft above MSL (GSD–AP–MW–1 on
February 25, 2019). However, the data
show that even during the periodically
dry conditions in summer when the
groundwater elevations can decline to
values approaching Coosa River surface
levels, significant volumes of saturated
waste may still be present because of
uncertainties with the waste bottom
elevation. If areas of waste are present
below the elevation of the Coosa River,
as some information suggests, these
areas of waste are expected to remain
saturated because, absent any
information to the contrary, it is
presumed that a hydraulic connection
between the uppermost aquifer and the
river exists due to the close proximity
of the Ash Pond to the river. In any case,
60Id
61 Id
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at Section III.c.iv.
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the regular and significant oscillation in
waters levels in the CCR indicate that
significant volumes of saturated CCR
persist routinely despite closure efforts
to date. Moreover, evaluation of water
level elevations over time show that
water levels are higher than the bottom
of the impoundment under most
conditions, and there is no indication
from available information that this
situation will change absent additional
engineering controls.
EPA’s analysis shows that substantial
volumes of saturated CCR currently
remain in the closed impoundment
under conditions where groundwater
elevations were at the overall average or
maximum average levels, ranging from
approximately 95,000 to 436,000 CY,
respectively. Furthermore, these
saturated volume estimates equate to
approximately 8% to 36% of the total
volume of CCR in the Ash Pond with an
average thickness of CCR over the entire
footprint between approximately 1 to
4.6 feet of statured CCR within the unit.
These estimates are further explained in
Section III.c of the TSD Volume I. Table
IV summarizes the volumes and areas of
saturated CCR calculated under both
conditions.
TABLE IV—ESTIMATES OF SATURATED CCR AT PLANT GADSDEN ASH POND
Overall
average
Groundwater elevation condition
ddrumheller on DSK120RN23PROD with PROPOSALS3
Groundwater elevation (ft above MSL) ...................................................................................................................
Average waste bottom (ft above MSL) ....................................................................................................................
Saturated CCR thickness (feet) ...............................................................................................................................
Total CCR in Ash Pond (cubic yards) .....................................................................................................................
Area of Ash Pond (acres) ........................................................................................................................................
Area of Ash Pond (square yards) ............................................................................................................................
Volume of saturated CCR (cubic yards) .................................................................................................................
Fraction of total CCR saturated (%) ........................................................................................................................
Based on EPA’s estimates, the closure
of the Plant Gadsden Ash Pond,
authorized and approved by ADEM,
does not meet the requirements of
§ 257.102(d). Overall, the closure of the
Gadsden Ash Pond presents the same
issues as the closure of the Colbert Ash
Pond 4 discussed in the previous
section. The post-closure groundwater
monitoring data from 2019 through 2021
show that groundwater is still
infiltrating into the Ash Pond. The
average groundwater elevations
measured at monitoring wells
surrounding the Ash Pond from 2018
through 2022 were on the order of 514
ft MSL (i.e., approximately 4 feet above
the average bottom elevation of the
CCR). Yet neither the approved Closure
Plan nor any other document in the
record for the permit accounts for the
levels of groundwater present in the
unit prior to closure or describe any
engineering measures taken to meet
each of the Federal CCR closure-in-place
performance standards in
§ 257.102(d)(1) and (2) in light of the
groundwater present in the unit. Nor
based on the post-closure groundwater
elevation data from piezometer wells
from 2019–2021, did the approved
closure address the groundwater that
continues to saturate the CCR in the
closed unit. EPA is therefore proposing
to determine that the permit for Plant
Gadsden does not require Alabama
Power to achieve compliance with
either § 257.102(d) or with alternative
State standards that EPA has
determined to be at least as protective.
EPA is therefore, proposing to
determine that Alabama’s CCR permit
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program does not satisfy the statutory
requirement in RCRA section
4005(d)(1)(A) or (B).
As previously explained, in situations
such as this, where the waste in the unit
is continually saturated with
groundwater, the requirement to
eliminate free liquids obligates the
facility to take engineering measures to
ensure that the groundwater, along with
the other free liquids, has been
permanently removed from the unit
prior to installing the final cover system.
See, 40 CFR 257.102(d)(2)(i). Yet neither
the Closure Plan that ADEM-approved
nor the permit ADEM issued contained
any such requirements.
While the approved Closure Plans for
the Ash Pond at Plant Gadsden discuss
dewatering techniques employed before
and during closure, it appears the
facility at most eliminated only the ‘‘free
water’’ ponded above the CCR, and only
dewatered the CCR and sediment ‘‘to
the extent necessary to provide a stable
working surface for earthwork
equipment’’ as provided in the closure
and post-closure for the Ash Pond:
2.2 DEWATERING FOR CLOSURE
Free water in the clear pool will be
removed through pumping, maintaining
compliance with the NPDES discharge
limits. The saturated ash will be
dewatered to the extent necessary to
allow a stable working surface for
earthwork equipment. Interstitial water
’’ removal. All water will be sent to an
onsite water treatment system prior to
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511
510
1
1,200,000
58.73
284,253
94,751
7.9
Maximum
average
514.6
510
4.6
1,200,000
58.73
284,253
435,855
36.3
discharge to ensure compliance with the
NPDES discharge limits.62
The ‘‘free water’’ referenced above is
only a subset of the ‘‘free liquids’’ that
must be eliminated; and that standard
(‘‘eliminated’’) applies equally to the
pore water intermingled with the CCR.
See, 40 CFR 257.102(d)(2)(i). The
Closure Plans do not acknowledge the
groundwater within the consolidated
footprint that continues to routinely
flow into the base of the impoundment
and saturate the CCR or describe any
engineering measures to eliminate those
free liquids, despite the continued
saturation. Moreover, it is clear from the
post-closure 2019–2022 monitoring data
that the measures that were taken
during closure did not actually
eliminate the free liquids from Ash
Pond.
A further concern is that, given the
failure to eliminate the free liquids from
the saturated CCR underlying the
consolidated unit, it is not at all clear
that the remaining wastes have been
stabilized sufficiently to support the
final cover system, as required by
§ 257.102(d)(2)(ii). Creating a stable
working surface for earthwork
equipment while the cover system is
being installed is not the same as
ensuring that the unit has been
sufficiently dewatered prior to
installation of the cover system and that
over the long term there will be no
differential settlement of the CCR in the
closed unit that would disrupt the
integrity of the cover system and allow
62 Alabama Power. Revised Closure Permit
Application for the Plant Gadsden Ash Pond. April
30, 2020. Appendix 8, p 2.
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liquids to infiltrate into the closed unit.
Neither the approved Closure Plan nor
ADEM’s permit provides any details of
engineering measures that were taken to
address the groundwater that continues
to flow into and out of the unit from the
sides and bottom. In the absence of such
measures, EPA has no basis for
concluding that the standard in
§ 257.102(d)(2) has been met.
EPA was also unable to find any
description in the ADEM approved
Closure Plan or any other permit
document of engineering measures that
Alabama Power took to ‘‘control,
minimize, or eliminate, to maximum
extent feasible’’ either the post-closure
infiltration of the groundwater into the
waste or the post-closure releases of
CCR or leachate to the groundwater,
resulting from the groundwater that
continues to infiltrate into the
impoundment from the sides and
bottom of the unit. 40 CFR
257.102(d)(1)(i). Based on the data and
analyses described above, groundwater
continues to infiltrate into the unit and
yet the only measures described in the
Closure Plan and the permit are those
taken to facilitate consolidation and cap
construction.63 In essence, this means
the Ash Pond will continue releasing
CCR contaminants indefinitely unless
Alabama Power is taking additional
actions that are not required by or
explained in the permit.
The absence of such measures from
the closure approved by ADEM is
consistent with the State’s interpretation
of its closure requirements, but as
discussed above, it is neither consistent
with, nor as protective as, the Federal
regulations. As with the TVA Colbert
Plant Permit, EPA is proposing to
determine that the record does not
support a finding that ADEM’s
alternative approach of relying on the
existing corrective action process will
be as protective as the Federal
requirements. As discussed in a
subsequent section, EPA has serious
concerns about the protectiveness of the
corrective action at Gadsden that ADEM
is overseeing.
All of this information was available
before ADEM issued the permit in
December 2020, and again when ADEM
approved the completion of closure on
June 9, 2022. Yet the permit continues
to authorize the closure of the unit with
no engineering measures to limit the
groundwater from continually flowing
into and out of the CCR in the unit, and
with no permit terms on the need to
address this as part of the corrective
action process.
63 Id at Appendix B (Infiltration Equivalency
Demonstration) in Appendix 8.
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Accordingly, EPA is proposing to
determine that the permit for Plant
Gadsden does not require Alabama
Power to achieve compliance with
either § 257.102(d) or with alternative
State standards that EPA has
determined to be at least as protective.
b. Plant Gadsden Groundwater
Monitoring Issues
The Plant Gadsden Permit says on
page 1,
Groundwater monitoring and
corrective action requirements in the
permit establish a groundwater
monitoring system of wells that
provides an accurate representation of
the groundwater quality underlying the
unit and a groundwater monitoring plan
to establish appropriate sampling and
analysis of the system to detect the
presence of CCR constituents.
In addition, Section V of the Plant
Gadsden Permit incorporates the GWMP
submitted with the Permit Application,
and directed Alabama Power to comply
with the State regulations and the
approved plan:
Section V. Groundwater Monitoring and
Corrective Action Requirements.
A. Groundwater Monitoring System.
The Permittee shall install and/or
maintain a groundwater monitoring
system, identified in Table 1, as
specified in 335- 13- 15-. 06(2) and the
approved groundwater monitoring plan.
Once ADEM approved and adopted the
GWMP into the permit, the GWMP,
rather than the referenced State
regulations, became the State
requirements with which the facility is
required to comply.
Based on EPA’s review of the
approved groundwater monitoring plan,
EPA is proposing to determine that the
groundwater monitoring well network
ADEM approved does not meet the
performance standards in § 257.91(a) or
(b). As discussed in more detail below,
EPA is proposing to determine that the
approved groundwater monitoring
system is not based on a thorough
characterization of the elements listed
in § 257.91(b). EPA is also proposing to
determine that the groundwater
monitoring system does not ‘‘yield
groundwater samples from the
uppermost aquifer,’’ but has been
screened instead in only a portion of the
aquifer. 40 CFR 257.91(a). Further, it
appears that the background wells were
not installed in locations hydraulically
upgradient of the Ash Pond, and EPA
was unable to locate sufficient
information in the permitting record
demonstrating that the standard for such
wells in § 257.91(a)(1)(i) or (ii) was met.
In addition, based on the documentation
provided in the Permit Application, it
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55249
appears that the downgradient
compliance wells are spaced too far
apart and/or are screened too deeply
and/or shallow to accurately represent
the quality of groundwater passing the
waste boundary and to monitor all
potential contaminant pathways in the
uppermost aquifer. See, 40 CFR
257.91(a)(2). Therefore, EPA is
proposing to determine that ADEM’s
Final Permit fails to require Alabama
Power to achieve compliance with
either the Federal regulations or with an
equally protective State requirement.
i. Failure To Delineate the ‘‘Uppermost
Aquifer’’ and To Base the System on
Thorough Characterization of Site Data
The Federal CCR regulations require
that a groundwater monitoring system
sample ‘‘the uppermost aquifer,’’ which
is defined as ‘‘the geologic formation
nearest the natural ground surface that
is an aquifer, as well as lower aquifers
that are hydraulically interconnected
with this aquifer within the facility’s
property boundary.’’ 40 CFR 257.53,
257.91(a). The design of the monitoring
systems must be based on a thorough
characterization of, among other things,
the ‘‘aquifer thickness, groundwater
flow rate, groundwater flow direction
including seasonal and temporal
fluctuations in groundwater flow; and
saturated and unsaturated geologic units
and fill materials overlying the
uppermost aquifer, materials comprising
the uppermost aquifer, and materials
comprising the confining unit defining
the lower boundary of the uppermost
aquifer.’’ 40 CFR 257.91(b)(1) and (2).
EPA is proposing to determine that
ADEM approved a groundwater
monitoring plan that does not meet
these requirements.
Based on the limited information in
the permit record, it appears the facility
failed to fully define the limits of the
uppermost aquifer, particularly its lower
boundary. The GWMP provided in the
Permit Application provides only
limited characterization of the geologic
units beneath the Ash Pond. In addition,
the technical information provided in
the Permit Application is insufficient to
support a determination of the lateral
and vertical limits of the entire
uppermost aquifer; for example, EPA
found only limited data on the
‘‘saturated and unsaturated geologic
units and fill materials overlying the
uppermost aquifer and materials
comprising the uppermost aquifer.’’ 40
CFR 257.91(b)(2). And EPA was unable
to find adequate information about the
‘‘materials comprising the confining
unit defining the lower boundary of the
uppermost aquifer.’’ Because the
information in the Permit Application
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was inadequate, EPA also consulted
information available on Alabama
Power’s CCR website to understand the
hydrogeology of the site. EPA is
proposing to determine that neither the
information in the Permit Application
nor the additional information available
on Alabama Power’s CCR website
constitutes ‘‘a thorough characterization
of . . . aquifer thickness, groundwater
flow rate, groundwater flow direction
including seasonal and temporal
fluctuations in groundwater flow; and
saturated and unsaturated geologic units
and fill materials overlying the
uppermost aquifer, materials comprising
the uppermost aquifer, and materials
comprising the confining unit defining
the lower boundary of the uppermost
aquifer.’’ 40 CFR 257.91(b)(1) and (2).
A generalized visual representation of
the various lithologies composing the
uppermost aquifer beneath the Ash
Pond can be found in the cross sections
in Figures 5A and 5B (included on
pages 142 and 143) in the Permit
Application and in other places, such as
Figures 4A, 4B, 9, and 10 from the 2021
Semi-Annual Groundwater Monitoring
and Corrective Action (GWMCA) Report
for Plant Gadsden.64 Based on EPA’s
assessment of the available information,
the uppermost aquifer, which has not
yet been fully identified and
characterized, is a composite layered
system consisting of unconsolidated
deposits of alluvial origin on top of a
predominantly mudstone bedrock. The
unconsolidated alluvial deposits consist
of interlayered deposits of silt, sand,
gravel, and clay material. These
unconsolidated alluvial deposits
unconformably overlay a variably
fractured and weathered bedrock
material, predominantly mudstones of
the Conasauga formation. The threedimensional surface represented by the
contact between the uppermost portion
of the (consolidated) bedrock and the
overlying alluvium (unconsolidated),
which can also be described as the topof-rock surface, is a distinct
hydraulically relevant zone of interest.
These points are illustrated (in part) in
the geologic cross-sections on Figures
5A and 5B (included on pages 142 and
143) in the Permit Application, which
show the uppermost aquifer consisting
of layers of sand, silt, gravel, as well as
the underlying Conasauga bedrock
formation. The elevation of this contact
zone changes laterally across the unit,
depending on location, and these
64 Southern Company Services. 2022 SemiAnnual Groundwater Monitoring and Corrective
Action Report, Alabama Power Company Plant
Gadsden Ash Pond. Prepared for Alabama Power
Company. January 31, 2022.
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differences in elevation are important
with respect to the siting of appropriate
monitoring well location and depths.
Immediately located beneath the
unconsolidated alluvial materials is a
zone of degraded bedrock (typically
referred to as ‘‘weathered bedrock’’) in
the uppermost portion of the Conasauga
bedrock. This weathered bedrock
material consists primarily of variably
weathered mudstones which have been
degraded by naturally occuring
processes. The weathered rock zones
vary in thickness laterally and
vertically. This interface between the
unconsolidated alluvial materials and
the underlying bedrock constitutes an
irregular geologic contact, which varies
spatially in terms of the thickness and
degree of the weathered bedrock
material, that is sandwiched between
alluvial deposits above, and lightly
weathered or unweathered bedrock
below. The contact can be thick and
gradational in some areas, and abrupt
and thin in other areas. This variability
demands additional characterization as
it creates the potential for preferential
pathways which may exploit the
weathered interval. While limited
information has been collected from this
interval, a few monitoring wells are
partially screened across the bedrock/
overburden contact, and thus monitor
the weathered bedrock interval to some
degree at those locations. However, the
variable nature of the bedrock/
overburden contact was not sufficiently
characterized to meet the performance
standards in § 257.91(a) or (b), as
discussed in more detail below.
Beneath the uppermost veneer of
weathered bedrock are rocks of the
Conasauga group, which consists of
varying amounts of limestone, dolomite,
and shale, with chert and siltstone
horizons present locally. The 2021
Semi-Annual GWMCA Report states,
‘‘The Limited core logs from the Site
indicate the Conasauga [beneath the Ash
Pond] to be a medium to dark gray
mudstone or shale with noticeable
calcite veining.’’ 65 While the Report
goes on to State, ‘‘The Conasauga
Formation is not considered to be a
water-bearing aquifer at the Site,’’ this
statement conflicts with boring logs and
other information which indicate that
the mudstones of the Conasauga
Formation are locally fractured,
weathered and hydraulically connected
to the alluvium and weathered bedrock
deposits lying above. The lower limits
of the hydraulically connected portions
of the bedrock, however, have not yet
been established, and reporting is not
consistent on this. Both the Permit
65 Id.
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Application and the 2021 Semi-Annual
GWMCA Report generally describe the
aquifer similarly. For example, the 2021
Semi-Annual GWMCA Report 66 states,
The uppermost aquifer beneath the Site
corresponds to a coarse and more
permeable fraction of alluvial
overburden soils and weathered or
fractured rock near the soil-rock
interface. The uppermost aquifer is
typically located at depths between 15
and 50 feet below ground surface (BGS).
Soils are generally poorly graded sands
with layers of clay and well-graded
gravels that overlay a mudstone or shale
bedrock,’’
See also Permit Application at section 3
of the GWMP. As shown on Figures 5A
and 5B in the Permit Application,
bedrock intervals are not included in
the represented monitoring wells and
little characterization appears to have
penetrated the bedrock beyond the
uppermost intervals.
But elsewhere the 2021 Semi-Annual
GWMCA Report states that,
Vertical delineation wells targeted more
permeable/fractured water-bearing
zones within the Conasauga formation
in the upper 50 feet of bedrock.
A further inconsistency appears on
the geologic cross sections included in
the 2021 Semi-Annual GWMCA Report
(see Figures 4A, 4B, 9, and 10), which
indicate the connection of the alluvial
and bedrock zones to depths of over 100
feet into the mudstone bedrock. These
cross sections and the associated boring
logs, some of which were included in
the Permit Application and some of
which were included in the 2021 SemiAnnual GWMCA Report, confirm that
this group of geologic layers and
formations are hydraulically
interconnected to depths of over 100
feet into the bedrock. The totality of this
information forces the conclusions that
the lower limits of the uppermost
aquifer have not been determined and
the uppermost aquifer and hydraulically
connected underlying intervals extends
at least 100 feet into the bedrock.
In other words, based on the available
information, the uppermost aquifer
consists of the alluvial aquifer nearest
the ground surface and at least the
uppermost 100 feet of the hydraulically
connected bedrock beneath it. See, 40
CFR 257.53 (definition of uppermost
aquifer). As such the materials
presented in the Permit Application do
not present a complete or accurate
representation of the uppermost aquifer
and hydraulically connected aquifer
zones beneath it.
In addition, the top-of-bedrock surface
has not been adequately resolved in all
66 Id.
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areas of the site because some boring
logs lack reliable confirmatory data.
According to the boring logs that were
included in the Permit Application,
there are multiple missing intervals of
‘‘no recovery’’ from numerous borings
advanced into bedrock, which indicate
a large potential for hydraulically
significant zones that are currently
insufficiently characterized. As a
consequence, EPA is proposing to
determine that the thickness, variability,
nature, and hydrogeologic significance
of the transitional zone of weathering in
the uppermost part of bedrock has not
been established, as required by
§ 257.91(b).
Furthermore, a hydraulic divide,
generally located along the northeastern
boundary of the unit, indicates the
groundwater hydraulics are more
complex than the current coarse
monitoring network can adequately
evaluate. Additional monitoring points
are needed laterally (and vertically) in
this area to provide the ‘‘thorough
characterization of groundwater flow
rate [and] groundwater flow directions,
including seasonal and temporal
fluctuations in groundwater flow’’
required to support the design of the
groundwater monitoring system
pursuant to § 257.91(b)(1). There are
also insufficient data to allow for the
determination of groundwater flow
directions at the eastern limits of the
Ash Pond. While GSD–AP–MW–12 is
downgradient of GSD–AP–MW–1, there
are no wells or piezometers that would
serve as hydraulic control points to the
east of the Ash Pond to fully
characterize the groundwater flow
directions at the eastern waste
boundary. Furthermore, GSD–AP–MW–
1 consistently has one of the highest
groundwater elevations, and the
possibility of eastward flow beyond the
eastern boundary cannot be ruled out
without additional data. Additional
groundwater monitoring wells are
needed to the northeast, east, and
southeast of the easternmost boundary
of the Ash Pond. In summary, EPA is
proposing to determine that significant
numbers of additional characterization
borings and monitoring wells are
needed to effectively characterize the
alluvial aquifer nearest the ground
surface and hydraulically connected
zones within the weathered bedrock and
upper portion of the bedrock intervals.
See, 40 CFR 257.91(b).
ii. ADEM Issued a Final Permit With
Background Wells That Do Not Meet the
§ 257.91(a)(1) Performance Standard
The Federal CCR regulations require
that a groundwater monitoring system
consist of a sufficient number of wells
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at appropriate locations and depths to
yield samples from the uppermost
aquifer that accurately represent the
quality of the background groundwater
that has not been affected by leakage
from a CCR unit. 40 CFR 257.91(a)(1).
The regulations also specify that
background wells must normally be
hydraulically upgradient of the CCR
unit, unless specific showings have
been made. See, Id. EPA is proposing to
determine that the approved GWMP
fails to document either that the
background wells are upgradient of the
CCR unit or that the wells meet the
performance standards in
§ 257.91(a)(1)(i) or (ii). EPA is also
proposing to determine that the
background wells in the approved
groundwater monitoring system do not
‘‘accurately represent the quality of the
background groundwater’’ because of
differences in the lithology between the
background wells and the majority of
the wells in the downgradient
groundwater monitoring network,
which is discussed in detail below.
At the time of permit issuance, the
approved groundwater monitoring
network installed at the unit consisted
of three ‘‘background’’ monitoring wells
(GSD–AP–MW–14, –16, and –17).
According to the single groundwater
flow map included in the Permit
Application,67 groundwater
predominantly flows toward the main
stem of the Coosa River from both the
southern and northern sides of the river.
The Coosa River acts as a hydraulic
divide between the Ash Pond and the
region to the south of the river where
the background wells are located.
Consequently, the Plant Gadsden
background wells, which are all located
on the southern side of the river, are
hydraulically disconnected from the
Ash Pond, rather than ‘‘upgradient’’ of
the Ash Pond. In addition, they are in
a different flow system and therefore
cannot accurately represent the quality
of the background groundwater at the
Ash Pond.
The Federal regulations specify that
wells that are not hydraulically
upgradient of the CCR unit can only
serve as background wells if one of two
showings have been made: (1) that
hydrogeologic conditions do not allow
the owner or operator to determine
whether wells are hydraulically
upgradient; or (2) sampling at other
wells will be as representative or more
representative of background
groundwater quality than that provided
67 Alabama Power. Revised Closure Permit
Application for the Plant Gadsden Ash Pond. April
30, 2020. Appendix 7, Plant Gadsden Ash Pond
Groundwater Monitoring Plan, Figure 6.
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by the upgradient wells. 40 CFR
257.91(a)(1)(i), (ii).
EPA found nothing in the Permit
Application or on the facility’s CCR
website to indicate that site conditions
made it infeasible to determine whether
background wells could be installed at
locations that are hydraulically
upgradient on the same side of the river.
For example, while on-site access may
be limited due to conditions near the
Ash Pond, there is no discussion about
other access points offsite to the north,
northeast, or east of the unit that may
provide adequate background samples.
In addition, there are site-specific
geologic conditions identified in the
Permit Application that indicate that
sampling at the current background
wells will not ‘‘accurately represent the
quality background groundwater’’
quality at the Ash Pond. 40 CFR
257.91(a)(1). For example, based on the
boring logs presented in the Permit
Application, background monitoring
well GSD–AP–MW–17 is screened in
limestone but nearly all of the bedrock
groundwater monitoring wells
surrounding the Ash Pond are screened
in a different rock type (i.e., mudstone).
In addition, background monitoring
well GSD–AP–MW–16 is screened in
sand and gravel alluvial materials and
based on a note included within the
boring log, it is partially screened into
approximately four feet of limestone
bedrock, whereas numerous wells in the
shallow downgradient compliance
monitoring network surrounding the
Ash Pond are screened just above or
across the interface between mudstone
and overlying overburden materials.
Limestone and mudstone are different
rock types and, based on the boring logs
presented in the Permit Application,
limestone substrates do not appear to
have been penetrated by monitoring
wells installed for the unit’s
downgradient compliance monitoring
network on the northern side of the
river.
Due to fundamental differences
between limestone and mudstone
mineralogy and chemical composition,
it is not clear that ambient geochemical
conditions in the limestone-hosted
aquifer would be representative of an
environment where mudstone
predominates, and site-specific
comparative analysis of both the geology
and geochemistry for the two distinct
geochemical environments and flow
systems is necessary to determine
whether the wells across the river are in
fact sufficiently representative of
conditions within the uppermost aquifer
to serve as representative background
wells. Although the Groundwater
Monitoring Plan included a limited
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narrative at Section 4.2.2, entitled
‘‘Groundwater Geochemistry,’’ the
narrative did not address any known
differences in geology, lithology, or
mineralogy between the two aquifers
that are located on opposite sides of the
river. ADEM nevertheless approved the
plan without requiring the facility to
resolve these issues.
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iii. The Gadsden Final Permit Allows
Insufficient Locations and Depths of
Downgradient Compliance Wells To
Monitor the Uppermost Aquifer
As previously discussed, the Federal
regulations specify that a groundwater
monitoring system must ‘‘consist[ ] of a
sufficient number of wells, installed at
appropriate locations and depths, that
. . . accurately represent the quality of
the groundwater passing the waste
boundary of the CCR unit.’’ 40 CFR
257.91(a)(2). The regulations further
specify that ‘‘[a]ll potential contaminant
pathways must be monitored.’’ Id. But
as discussed in more detail below, EPA
is proposing to determine that ADEM
approved a GWMP with an insufficient
number of wells laterally along the
downgradient perimeter of the unit to
monitor all potential contaminant
pathways. EPA is also proposing to
determine that monitoring wells in the
approved plan were not installed at
appropriate depths to ensure that all
potential contaminant pathways were
monitored. Finally, EPA is proposing to
determine that the approved
groundwater monitoring system fails to
account for preferential pathways
beneath the Ash Pond.
(1) Insufficient Lateral Spacing of
Compliance Wells To Monitor All
Potential Contaminant Pathways
At the time of permit issuance, the
approved groundwater monitoring
network installed at the unit consisted
of only fifteen compliance monitoring
wells (GSD–AP–MW–1 through GSD–
AP–MW–12 and GSD–AP–PZ–1, GSD–
AP–PZ–5 and GSD–AP–PZ–6), at an
impoundment with a perimeter of
approximately 7,500 feet.
Most of the groundwater monitoring
wells that parallel the river for the Plant
Gadsden Ash Pond unit are spaced
approximately 400 to 900 feet apart, and
lateral distribution of wells is somewhat
uniform with downgradient monitoring
wells surrounding the waste boundary
at an average lateral spacing of 630
feet.68 These large lateral well spacings
are particularly problematic to the
68 Southern
Company Services 2022 Annual
Groundwater Monitoring and Corrective Action
Report, Alabama Power Company Plant Gorgas Ash
Pond. Prepared for Alabama Power Company.
February 1, 2023.
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north, northwest, west, and to the
southwest where groundwater
discharges to the Coosa River. Given the
propensity for groundwater to flow
within the preferential pathways that
exist at the site and the close proximity
of the Coosa River to the unit, one
would expect to see a detailed rationale
explaining why these well locations at
large lateral distances were sufficient to
monitor all potential contaminant
pathways. However, EPA’s review of the
approved GWMP did not identify any
such explanation. Therefore, given the
proximity to the Coosa River, the large
well spacings make it likely that all
potential contaminant pathways—such
as the gravel and other coarse material
in the alluvium and fractures, or the
dissolution features at or below the
weathered bedrock surface that may be
causing groundwater to surface water
discharges immediately adjacent to the
Ash Pond—are not currently monitored.
(2) Insufficient Number of
Downgradient Compliance Wells
Installed at Appropriate Depths To
Monitor the Entire Aquifer (Inadequate
Vertical Spacing)
EPA is also proposing to determine
that ADEM approved a GWMP that
lacked ‘‘a sufficient number of wells,
installed at appropriate locations and
depths’’ to ensure that all potential
contaminant pathways in the entire
uppermost aquifer are monitored. As
stated previously, the uppermost aquifer
is a composite layered system consisting
of unconsolidated deposits of alluvial
origin on top of mudstone bedrock. The
unconsolidated alluvial deposits consist
of interlayered deposits of silt, sand,
gravel, and clay material. These
unconsolidated alluvial deposits overlay
a variably fractured and weathered
bedrock material, predominantly
mudstones of the Conasauga formation.
The contact between the uppermost
portion of the (consolidated) bedrock
and the overlying (unconsolidated)
alluvium, which can also be described
as the top-of-rock surface, is a distinct
hydraulically relevant zone of interest,
and many ‘‘downgradient’’ compliance
monitoring wells in the approved
network are screened across this
interface, as is appropriate. However,
although the lower limits of the
hydraulically connected portions of the
bedrock have not yet been established,
as previously discussed, the available
information supports the conclusion
that this group of geologic layers and
formations are hydraulically
interconnected to depths of 100 feet or
more into the bedrock. Consequently,
EPA is proposing to determine that the
entire group of geologic layers and
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formations should have been more
comprehensively monitored. See, 40
CFR 257.53 (definition of uppermost
aquifer).
The downgradient well network
ADEM approved is focused on a narrow
subset of the uppermost geologic layers
associated with river deposition. These
unconsolidated materials occur in
terrace deposits at low elevations near
the current Coosa River channel as well
as at higher topographic levels. These
alluvial deposits are reported to range
from approximately 20 to 30 feet in
thickness. Most of the downgradient
compliance monitoring wells in the
approved network are screened in these
shallow materials, and most of the wells
are screened only in the gravel.69
Additional compliance wells are needed
both at the upper and lower bounds of
the uppermost aquifer system, including
within alluvial deposits and
hydraulically connected weathered
bedrock and bedrock zones, to ensure
all potential contaminant pathways will
be monitored in all relevant flow zones.
A few wells are screened near the top
of the Conasauga bedrock formation,
and a few wells are cross screened
across the interface between the
alluvium (the gravel) and the underlying
bedrock. As depicted on the crosssection in Figure 5A in the Permit
Application, no wells appear to have
been screened in either the sand or silt
layers that are situated above the gravel;
and a single well on the cross-section in
Figure 5B in the Permit Application
appears to be partially screened in the
silt. But additional compliance wells
should have been installed in those
upper zones given that the sand and silt
layers are saturated with groundwater.
Even when the gravel layers were not
present, the well screens were set at the
bottom of the alluvium or at the top of
bedrock, and not in the silts. Wells in
each of the saturated units are needed
in order to monitor all potential
contaminant pathways.
In addition, as previously discussed,
key interfaces, such as the interface
between alluvium and weathered
bedrock have apparently not been fully
characterized; as this portion of the
bedrock system is hydraulically
connected to the overlying alluvium,
additional compliance wells are needed
in the upper part of the bedrock in most
areas of the Ash Pond unit to ensure
that all potential contaminant pathways
are monitored. Additional wells also
69 The Plant Gadsden Permit Application at page
111 includes a statement that ‘‘[m]onitoring wells
target the uppermost aquifer with wells screened in
coarse fractions of the alluvial materials or more
weathered, fractured upper bedrock beneath the
Site.’’
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need to be installed in deeper intervals
of the underlying Conasauga mudstones
which are hydraulically connected the
uppermost zone of weathered bedrock.
The relevant zone of interest in the
upper part of the Conasauga group is at
least 100 feet in thickness, as discussed
previously, but the true thickness of the
uppermost aquifer has not been
determined. As such additional
monitoring wells may need to be
screened more deeply to ensure all
potential contaminant pathways are
monitored.
(3) Preferential Pathways Are Not
Monitored
Preferential pathways have been
documented in the uppermost aquifer
under the Ash Pond. Yet under the
approved GWMP, these significant
potential contaminant pathways do not
appear to be adequately monitored,
despite the express requirement in
§ 257.91(a)(2).
Based on the boring logs and crosssections in the Permit Application and
the 2021 Semi-Annual GWMCA Report,
several types of preferential pathways
are present at the site. These include,
among others, continuous lenses or
channel-like bodies of coarse sand and
gravel in overburden, low-lying areas
along the overburden/bedrock interface,
laterally continuous zones of weathered
bedrock in the uppermost part of the
bedrock section, and zones of fracturing
and/or weathering and/or dissolution
within deeper levels of the bedrock. The
current monitoring network only
incompletely monitors some of these.
While some monitoring wells are
installed in sand and gravel bodies in
the alluvium, it appears that the
monitoring network does not target all
such zones that may be serving as
preferential pathways. As just one
example, consider the southwestern
unit boundary that borders the Coosa
River; as indicated on Figures 5B and 6
of the approved GWMP, while the wells
installed along this boundary (GSD–AP–
MW–8 thru GSD–AP–MW–12) are
screened along a zone where
groundwater flow is likely occurring
along preferential pathways, they are
spaced over 500 feet apart. Considering
the unique geologic conditions at the
site that could result in the presence of
more localized preferential pathways, it
is not known whether the gravel
materials screened by GSD–AP–MW–11
are present elsewhere along this
boundary. In short, there could be sand
and gravel alluvial zones or highly
fractured zones in bedrock near the
bedrock/alluvium interface that have
not been identified and are
unmonitored. EPA is proposing to
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determine that additional borings (and
possibly monitoring wells) should have
been installed along this boundary, and
it appears that this level of detailed
investigation to identify preferential
pathways was not performed elsewhere
along the unit.
It is clear that preferential pathways
in the bedrock exist based on the
characterization and monitoring
Alabama Power conducted as part of the
continuing corrective action at the site.
However, there is little to no discussion
in the Permit Application regarding how
these pathways were identified and how
the lateral/vertical dimensions of the
pathways were delineated to ensure that
compliance wells were installed
correctly to monitor these pathways. As
illustrated on Figures 9 and 10 of the
2021 Semi-Annual GWMCA Report,
assessment monitoring has identified
plumes emanating from the unit to the
northeast in overburden and bedrock.
After installing additional monitoring
wells to delineate the contaminant
plume, Alabama Power identified that
contamination was present deeper in
the Conasauga bedrock formation than
any of the compliance wells previously
installed as part of the groundwater
monitoring system. For example,
Figures 5 and 10 of the 2021 SemiAnnual GWMCA Report indicate that
pathway in bedrock has influenced
migration of a lithium plume beyond
the unit boundary at least hundreds of
feet to the northeast to depths of at least
130 feet into the bedrock. It is
reasonable to expect that similar
pathways may exist also along the same
regional northeast to southwest geologic
strike to the southwest of the unit,
exploiting these same inherent zones of
fracturing in the bedrock, yet the
southwestern waste boundary, along the
Coosa River, generally lacks any
monitoring points in deeper bedrock.
In summary, after reviewing the
GWMP and all the materials in the
permit record, EPA is proposing to
determine that the monitoring network
that ADEM approved is not likely to
detect all groundwater contamination in
the uppermost aquifer and is therefore
less protective than the Federal
regulations.
c. Plant Gadsden Corrective Action
Issues
In January 2020, the first SSLs above
groundwater protection standards were
reported for arsenic and lithium. An
ACM was prepared in July 2020. On
December 18, 2020, ADEM issued the
Final Permit to Alabama Power for
Gadsden Ash Pond. EPA is proposing to
determine that the Final Permit issued
to the Gadsden Ash Pond, as with the
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55253
other permits discussed in this notice,
fails to require Alabama Power to
achieve compliance with the Federal
corrective action requirements.
The Gadsden Final Permit states that
the Permittee is required ‘‘. . . to
manage CCR in accordance with the
conditions of the permit, ADEM Admin.
Code r. 335- 13- 15, ‘Standards for the
Disposal of Coal Combustion Residuals
in Landfills and Surface
Impoundments,’ and the approved
permit application.’’ 70 The permit also
contains the same recitation of the
corrective action regulations as the
Colbert Final Permit did.
Corrective Action
1. Assessment of Corrective Measures.
The Permittee must initiate an
assessment of corrective measures as
specified in 335–13–15–. 06(7) if any
constituent listed in Appendix IV of
335- 13- 15 has been detected at a
statistically significant level exceeding
the groundwater protection standard, or
immediately upon detection of a release
from the CCR unit.
a. The permittee must continue to
monitor groundwater in accordance
with the assessment monitoring
program while assessing corrective
measures.
2. Selection of Remedy. Based on the
results of the corrective measures
assessment, the Permittee must select a
remedy as specified in 335–13–15–.
06(8).
3. Implementation of the Corrective
Action Program. Within 90 days of
selecting a remedy, the Permittee must
initiate remedial activities as specified
in 335–13–15–. 06(9), and shall be
required to modify the permit in
accordance with Section II. E. 9.
In the RTC for the Gadsden Final
Permit, ADEM states that, ‘‘The ACM is
currently under review. Once the final
review is complete, the Department will
provide comments to Alabama Power
related to the submitted ACM and
proposed final remedy.’’ The preferred
remedy in the ACM was MNA with
adaptive site management and
‘‘remediation system enhancement.’’ 71
Any comments provided by ADEM to
70 Alabama Department of Environmental
Management. Initial Permit and Variance, Gadsden
Steam Plant, Permit No. 28–09. December 18, 2020.
PDF p. 2.
71 It is not clear what is meant by ‘‘remediation
system enhancement’’ with respect to MNA,
because MNA relies upon naturally occurring
processes for remediation. The only systems
installed are for performance monitoring. Any
‘‘enhancement’’ would require action on the part of
Alabama Power to remediate the releases and
would be, by definition, a different remedy.
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Alabama Power on the 2020 ACM were
not available for review.
As with Colbert, incorporating the
regulations verbatim in the permit does
not require Gadsden to achieve
compliance with those requirements.
This is because ADEM did not take into
account relevant facts about the status of
corrective action at Gadsden, such as
whether the 2020 ACM, which was
completed more than 2 years prior to
issuance of the permit, complied with
the regulatory requirements. Most
importantly, ADEM did not adjudicate
what actions are still necessary in light
of those facts to achieve compliance
with the regulations and include those
actions as requirements in the Final
Permit.
Whether the 2020 ACM meets the
requirements of the regulations and
what actions Alabama Power must take
to remediate groundwater in compliance
with § 257.97 are precisely the types of
adjudication required in a permit. What
the permittee is required to do in order
to achieve compliance with the
regulations must be determined prior to
final permit issuance, because the
permit must contain these requirements.
This is the role of a permitting authority
(i.e., ADEM). Delaying this decision
effectively allows Alabama Power to
continue operating out of compliance
with the regulations, while operating in
compliance with the permit. In this
case, that means Alabama Power can
continue to pursue a remedy that does
not appear to meet the requirements of
§ 257.97, and consequently, delay or
avoid the cleanup. This results in a
permit program that is less protective
than the Federal regulations.
In sum, EPA is proposing to
determine that, by failing to determine
the adequacy of the revised ACM or the
permittee’s proposed remedy, the
permit in essence authorizes Alabama
Power to continue to pursue a remedy
that does not appear to meet the
requirements in § 257.97(b) and is based
on the results of a deficient ACM.
Accordingly, EPA is proposing to
determine that this permit does not
require compliance with the Federal
requirements and, because it allows the
facility to continue to delay initiating
corrective action that would address the
continuing groundwater contamination,
the State requirement is less protective
than the Federal regulations.
i. Gadsden Final Permit Does Not
Require an ACM That Includes an
Assessment of Source Control Measures
in Accordance With 40 CFR 257.96
40 CFR 257.97(b)(3) requires that all
remedies control the source of releases
in order to reduce or eliminate, to the
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maximum extent feasible, further
releases of contaminants into the
environment. The ACM for Gadsden
contains no assessment of control
measures to achieve this requirement
(i.e., source control). Instead, section 2.5
describes the closure of the unit, which
has already occurred, and states, ‘‘Site
closure appears to have already been
effective in controlling the source and
reducing infiltration into the underlying
aquifer.’’ However, the ACM must
include more than one source control
measure and must actually analyze how
effectively each of the potential
measures would meet the criteria in
§ 257.96(c). See, 40 CFR 257.96(a), (c).
Here, as was the case with Plant Colbert,
there is no assessment of the one source
control measure identified in the
ACM—the closure of the Ash Pond,
which left a significant amount of CCR
in contact with groundwater—and how
effectively it would achieve the criteria
in § 257.96(c) compared to other source
control alternatives, such as clean
closure or the imposition of engineering
measures to control or eliminate the
groundwater that continues to flow in
and out of the impoundment. Yet the
permit issued by ADEM does not
require any actions to remedy these
readily apparent deficiencies.
ADEM’s failure to require Alabama
Power to submit an ACM that actually
evaluates whether the closure of the Ash
Pond meets the source control
requirements in § 257.97(b)(3) also
undercuts their claim that they will use
the corrective action process to address
any remaining concerns with respect to
the closure of the Ash Pond. As
discussed above, closure construction
activities for the Ash Pond were
certified as completed in October 2018,
and a certification of the completion of
closure activities was submitted in April
2020. As discussed above, in the two
years between the time closure was
completed and the permit was issued in
December 2020, groundwater elevations
were measured between 2 and 7 feet
above the average base elevation of the
closed unit. Yet ADEM issued the
permit without evaluating the ACM. Nor
did the State take any further action
when they approved the closure of the
Ash Pond in 2022.
ii. The Gadsden Permit Does Not
Require Alabama Power To Collect Site
Data Needed To Characterize Site
Conditions That May Affect a Remedy
To Support Assessments in the ACM
As discussed above, § 257.95(g)(1)
requires a facility to characterize the
nature and extent of the release and any
relevant site conditions that may affect
the remedy ultimately selected. The
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characterization must be sufficient to
support a complete and accurate
assessment of the corrective measures
necessary to effectively clean up all
releases from the CCR unit pursuant to
§ 257.96. The 2020 ACM delineates
releases but does not characterize any
site conditions that would affect its
preferred remedy of in-situ
immobilization through treatment or
MNA (e.g., testing for the presence of
released constituents in soils to
demonstrate they are being removed
from the groundwater and immobilized
on-site). As discussed in subsequent
sections, these data are necessary to
accurately assess any of the remedies
identified in the ACM, particularly
MNA. The Final Permit issued by
ADEM does not require collection of
these data or any revisions to the ACM
to remedy this deficiency.
iii. The Assessment of In-situ
Geochemical Treatment and MNA in the
ACMs Is More Favorable Than Can Be
Supported by the Available Data
The 2020 ACM for Gadsden identified
in-situ geochemical treatment and MNA
as corrective measures to address
groundwater contamination, in addition
to hydraulic control and treatment. As
discussed previously, MNA relies on
natural processes to treat releases; insitu geochemical treatment adds
chemicals to the subsurface to create
conditions for this immobilization to
occur. For arsenic and lithium, in-situ
geochemical treatment and MNA can
reduce mobility through sorption to
soils, but they do not remove the
contaminants from the environment.
Therefore, MNA and geochemical insitu treatment generally would not
perform well with respect to the
requirement in § 257.97(b)(4) that
remedies ‘‘remove from the
environment as much of the
contaminated material that was released
from the CCR unit as is feasible,’’ since
the constituents remain in the
subsurface soils, albeit immobilized.
In order for immobilization through
MNA or in-situ treatment to be assessed
favorably with respect to reliability, the
chemical reactions and processes
involved in this immobilization must be
demonstrated to be irreversible.
Immobilization that is not permanent
could be reversed, causing contaminants
to be released back into groundwater,
where they can migrate off-site.
Immobilization that is not permanent
would also require ongoing monitoring
in accordance with § 257.98(a)(1) as
long as immobilized constituents
remain in the subsurface. Determining
the viability and demonstrating the
irreversibility of immobilization
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mechanisms is necessary to assess the
performance, reliability, ease of
implementation, and the time required
to begin and complete the remedy. 40
CFR 257.96(c)(1) and (2). These
assessments would need to be
supported with site-specific
characterization data and analysis. This
information would ultimately be
necessary to show that MNA and
geochemical in-situ treatment meet all
the requirements of § 257.97(b), but the
permit record does not include such
information.
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(1) The 2020 ACM Does Not Include
Data That Characterize Site Conditions
or Identify Any Attenuation
Mechanisms Occurring at the Ash Pond
The 2020 ACM assessed the
performance of MNA favorably without
any supporting data to characterize site
conditions that may ultimately affect a
remedy, as required by § 257.95(g)(1).
For example, site-specific groundwater
data (e.g., pH or oxidation potential,
speciated concentrations of constituents
of concern) were not considered in the
assessment narrative, and analytical
results of soil samples to identify the
presence of immobilized constituents in
the subsurface were not provided. The
site data that were collected focus only
on contaminant concentrations and
trend analyses regarding the presence of
contaminants. The ACM also does not
discuss how attenuation may be
naturally occurring through any
particular MNA mechanisms (e.g.,
adsorption, precipitation, dispersion).
EPA was not able to find any indication
in the permit or supporting
documentation to confirm that the
Permittee has identified the
mechanisms by which MNA would
occur at the site for both arsenic and
lithium. Nor is there any condition in
the permit requiring the development
and submission of such information.
(2) MNA Is Not a Viable Remedy
Without Source Control
As discussed previously for Plant
Colbert, MNA is not viable without
source control, because the total amount
of contaminants in the groundwater will
continue to increase as the releases from
the unit continue and potential releases
of new constituents will occur.
Therefore, it is impossible to determine
whether the aquifer has sufficient
chemical and physical materials
required to complete any identified
immobilization reactions because the
total amount of the release is not yet
known.
Source control has not been achieved
here, as releases from the Ash Pond are
ongoing. The closure of the Ash Pond
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with waste remaining in place in the
aquifer has resulted in a continual
source of groundwater contamination
from the unit. Therefore, MNA is not a
viable remedy for the Ash Pond and
should not be included in the 2020
ACM unless the ACM is revised to
include an alternative that achieves
source control.
(3) Plant Gadsden’s Permit Does Not
Require an ACM That Accurately
Assesses Groundwater Remediation
Alternatives According to the Criteria in
40 CFR 257.96(c)
The 2020 ACM also fails to meet the
requirements at § 257.96(c)(3) to
consider safety impacts, cross-media
impacts, and control of exposure to any
residual contamination in its assessment
of MNA. Neither the narrative nor Table
5 in the 2020 ACM consider these
impacts for MNA. Table 5 in the 2020
ACM, in the column labeled ‘‘potential
impacts of remedy’’ assesses the
potential impacts from MNA as ‘‘none.’’
This conclusion is not only
unsupported by data or analysis but is
also inconsistent with other information
in the ACM. The Ash Pond is next to a
river and groundwater flow is depicted
toward the river in Figure 3 in the 2020
ACM. Because no site data were
collected that would demonstrate
immobilization of constituents is
occurring, the only MNA that is known
to occur is dilution and dispersion (i.e.,
the normal transport associated with
groundwater releases). This means that
contaminants are migrating out of the
Ash Pond in groundwater toward the
river. Migration of contamination from
groundwater to surface water is a crossmedia impact. Thus, the assessment of
potential impacts from the remedy for
MNA in Table 5, which includes these
cross-media impacts, should be ‘‘high.’’
The lack of data to support the
assessments in the ACMs means they
may not accurately reflect MNA’s
‘‘effectiveness in meeting all of the
requirements and objectives’’ in
§ 257.97(b). Conclusions without a
supporting assessment or data do not
constitute ‘‘an analysis of the
effectiveness of potential control
measures.’’ 40 CFR 257.96(c) (emphasis
added). Inaccurate assessments in an
ACM can ultimately result in selection
of a remedy that will not meet the
requirements of § 257.97(b). Yet the
Final Permit issued by ADEM does not
require any actions to remedy this
deficiency.
3. Plant Gorgas
EPA reviewed the Initial Permit and
Variance (Final Permit) for the Alabama
Power Company, William C. Gorgas
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55255
Electric Generating Plant (Plant Gorgas),
issued by ADEM under Permit No. 64–
12 on February 28, 2022.72 Plant Gorgas
is located near Parrish, Alabama. The
units covered by the Final Permit
include the Plant Gorgas Ash Pond,
Plant Gorgas Gypsum Pond, Plant
Gorgas Bottom Ash Landfill, and Plant
Gorgas CCR and Gypsum Landfill. The
Plant Gorgas CCR and Gypsum Landfill
is still in operation while the other three
CCR units are in the process of closing
or closed. For this proposal, of the CCR
units at Plant Gorgas, EPA only
evaluated the Final Permit for the Plant
Gorgas Ash Pond (Ash Pond) because it
is directly comparable to the other State
CCR permits evaluated in this proposal,
and because, based on the
characteristics of the unit and the
surrounding hydrogeology, it has the
greatest potential for significant
environmental and human health effects
if mismanaged.
The Plant Gorgas Ash Pond is a ‘‘CCR
surface impoundment located in
Sections 20, 21, 28 and 29, Township 16
South, Range 6 West in Walker County,
Alabama . . . with a disposal area that
consists of approximately 423.32 acres.’’
Final Permit at pg. 2. The Ash Pond is
located southeast of Plant Gorgas on the
opposite side of the Mulberry Fork of
the Black Warrior River. The Permit
Application describes that the Ash Pond
was originally formed by a cross-valley
dam in 1953, with the original dam
located on the northern boundary of the
impoundment adjacent to Mulberry
Fork.73 The original dam was raised to
increase the capacity of the
impoundment in the mid-1970’s, and
then raised once again in 2007. Id. at
Appendix 4. When the Ash Pond was in
operation, the impoundment covered an
approximate area of 420 acres
containing 25 million CY of waste.
EPA has identified issues with
closure, groundwater monitoring
networks, and corrective action at Plant
Gorgas, and we discuss those issues
below.
a. Plant Gorgas Closure Issues
As noted, the closure at Plant Gorgas
is not yet complete. To evaluate the
closures at Plants Colbert and Gadsden,
EPA reviewed the measured postclosure groundwater elevations to
determine whether the § 257.102(d)
performance standards were met. But
since the closure of the Gorgas Ash
72 Alabama Department of Environmental
Management. Initial Permit and Variance William
C. Gorgas Electric Generating Plant Permit Number
64–12. February 28, 2022.
73 Alabama Power Company. Revised Closure
Permit Application for the Plant Gorgas Ash Pond.
April 30, 2020.
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Pond is not yet complete, that same
information (‘‘measured post-closure
groundwater elevations’’) is not
available. As discussed below, however,
it is clear that CCR in the Ash Pond is
currently saturated by groundwater.
Despite the saturated CCR currently in
the unit, it may be possible for the Ash
Pond to close with waste in place if
engineering measures are implemented
to meet the performance standards in
§ 257.102(d). Although some
engineering measures are described in
the Closure Plan, EPA was unable to
locate the information in the permit
record to support a definitive
conclusion that the proposed closure
will meet the performance standards in
§ 257.102(d). For example, EPA was
unable to locate any evaluation of the
expected impact of the proposed
engineering measures on groundwater
elevations conducted by either the
permittee or ADEM. EPA’s inability to
reliably estimate post-closure conditions
is a consequence of the complexity of
the site, the absence of critical
information in the Closure Plan, and the
inadequacy of the groundwater
monitoring system at the site (which is
discussed in the next section).
Nevertheless, as described below, based
on the available information there are
several reasons to determine that it is
unlikely that the proposed closure of the
Ash Pond will meet the performance
standards in § 257.102(d). EPA is
therefore proposing to determine that
the approved Closure Plan fails to
demonstrate that the closure will meet
the performance standards in
§ 257.102(d), as required by
§ 257.102(b)(1)(i). Based on ADEM’s
failure to require the permittee to
provide this information, or to
otherwise resolve the issues presented
below before approving the Closure
Plan, EPA is proposing to determine
that the Final Permit fails to require the
Gorgas Ash Pond to achieve compliance
with either § 257.102(d), or with an
equally protective State alternative. See
42 U.S.C. 6945(d)(1)(B).
i. CCR in the Ash Pond Is Currently
Saturated by Groundwater and Is Likely
To Remain so Once Closure Is Complete
Given the complexity of the site and
the absence of detailed information in
the Permit Application, EPA lacks the
data to reliably estimate the amount of
CCR that will remain saturated after
closure activities are complete. These
deficiencies are significant enough that
ADEM’s approval of a Closure Plan with
these deficiencies, and in the absence of
any evaluation, leads to the conclusion
that the State CCR permit program does
not meet the standard in 42 U.S.C.
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6945(d)(1). However, based on the
available information in the Permit
Application, there are many reasons to
determine that the proposed closure of
the Ash Pond will not meet the
performance standards in § 257.102(d).
Based on the limited data available, EPA
estimates that groundwater will
continue to saturate a substantial
amount of CCR, even after the activities
described in the approved Closure Plan
have been completed. As described
below, available groundwater
measurements recorded between 2021
and 2022 show that groundwater levels
at the Ash Pond continue to be present
above the base of the unlined
impoundment, saturating substantial
amounts of CCR in the closing unit.
Moreover, comparison of groundwater
elevation data from 2021 and 2022 to
elevation data in the same wells for
prior years does not yet indicate any
statistically significant or sustained
declines, further supporting EPA’s
conclusions about future persistence of
saturated CCR waste.
As shown on the center line cross
section B–B’ on construction drawing
G–204 in the Permit Application, the
base of the Ash Pond varies
substantially. In view of this
information, EPA conducted an analysis
using existing monitoring wells near the
waste boundary and south of the
planned closure buttress. Few
monitoring wells are located directly
adjacent to the CCR; most are located
hundreds of feet away from the waste
boundary, with many at distances of
over 1,000 feet away. Faced with these
significant limitations, EPA based
estimates of saturated waste presence
and thickness on the limited available
pairs of wells which are in close
proximity to the waste material and are
located on opposite sides of the main
waste body or larger fingers of CCR
waste. Using this approach allowed for
limited direct comparison of recent
water levels data collected in 2021 and
2022 to the top and bottom elevations of
the CCR in that area of the unit. EPA
considered transects between the
following well pair or pairs of clustered
wells:
• [GS–AP–MW–16S/GS–AP–MW–16D/
GS–AP–PZ–16] to [GP–AP–MW–19]
• [GS–AP–MW–21/GS–AP–MW–21V]
to [GS–AP–MW–1/GS–AP–MW–1R/
GS–AP–MW–46]
• [GS–AP–MW–12/GS–AP–MW–12V]
to [GS–AP–MW–1/GS–AP–MW–1R/
GS–AP–MW–46]
Lastly, it is also important to note that
EPA’s assessment of water levels in this
action focused primarily on those
monitoring wells which were screened
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nearest the CCR in the unit at those
specific locations. These included wells
screened in a variety of different levels
within the uppermost aquifer system. It
must be recognized that this exercise
suffered from the limitations of the well
network as screened interval elevations
varied somewhat from transect to
transect. Regardless of these
complexities, water levels in most
screened intervals were consistently
above the base of the impoundment.
This assessment suggests the
sustained presence of significant
thickness of saturated waste in all of the
areas EPA investigated. For the [GS–
AP–MW–16S/GS–AP–MW–16D/GS–
AP–PZ–16] to [GP–AP–MW–19] transect
near the southern end of the Ash Pond,
reported groundwater elevation
measurements from monitoring wells
GS–AP–MW–16S and GS–AP–MW–19
range from roughly 381 to 407 ft above
MSL. In this area near the center of the
unit, the bottom of the CCR unit is
located at approximately 335 feet above
MSL and the top of the waste at closure
is planned to be roughly 450 feet above
MSL. Based on these data EPA estimates
that at the deepest point of this transect
a layer of CCR between 46 and 72 ft in
thickness is saturated. As stated above,
EPA’s estimates were complicated by
Alabama Power’s failure to install many
of the monitoring wells at the waste
boundary which is inconsistent with the
requirement in § 257.91(a)(2)). In this
case, EPA used data from GS–AP–MW–
16S and GS–AP–MW–19 because, based
on the materials in the Permit
Application, they are a well pair that are
located along opposite sides of the unit
from each other, or in other words, the
two wells span across a large portion of
the unit. Nevertheless, the lateral
distance between GS–AP–MW–16S and
GS–AP–MW–19 is still roughly 2,000
feet, and the bottom unit elevation is
highly variable over that distance given
the incised valley setting in which the
unit sits.
EPA also evaluated the most recent
groundwater elevation data from the
Plant Gorgas 2022 Annual Groundwater
Monitoring and Corrective Action
Report to determine if any recent
closure activity at the site has
influenced groundwater elevations.74
Regarding the impact of closure activity
on groundwater elevations, the report
itself is contradictory. On page 20, the
report indicates that no significant
changes in groundwater elevations or
flow have been noted at the site as ash
74 Southern Company Services 2022 Annual
Groundwater Monitoring and Corrective Action
Report, Alabama Power Company Plant Gorgas Ash
Pond. Prepared for Alabama Power Company.
January 31, 2023.
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pond dewatering activities have not
been initiated. However, on pages 21
and 22, the report states that dewatering
operations began in 2022 and may be
contributing to the groundwater
elevations observed. Further, on page 56
of the report, there is an
acknowledgment that ‘‘[t]he lack of
obvious or significant trends [or changes
in groundwater quality] is likely in part
due to (1) dewatering operations not
starting until the first week of July 2022,
(2) the low permeability nature of the
subsurface flow systems, and (3) the
number of wells that have been recently
installed or replaced (too few data
points for trend analyses).’’ In any
event, EPA’s evaluation indicated that
groundwater elevation data collected in
July 2022 is mostly comparable to
historical data, suggesting little
influence thus far from dewatering
efforts. For example, most decreases in
groundwater elevations were observed
to be less than a few feet. Some larger
decreases (greater than 10 feet) were
observed at the southern portion of the
Ash Pond, but the report indicated that
these decreases may be the result of
resumed mining activity south or
southwest of the Ash Pond, rather than
closure activity related to the Ash Pond.
Therefore, while some uncertainty
remains as to just how much CCR is
currently saturated, the available site
data indicates that considerable areas,
thicknesses, and volumes of saturated
CCR remain in the impoundment.
Similarly, along the [GS–AP–MW–21/
GS–AP–MW–21V] to [GS–AP–MW–1/
GS–AP–MW–1R/GS–AP–MW–46]
transect through Finger 1 of the Ash
Pond, water levels reported in 2021 and
2022 for GS–AP–MW–21 and GS–AP–
MW–46 ranged from 335 to 367 feet
above MSL. The elevation of the bottom
of the CCR is roughly 322 feet above
MSL and the top of the CCR unit is
planned to be approximately 428 feet
above MSL in that part of the unit.
Based on these data EPA estimates that
at the deepest point of this transect a
layer of CCR between 13 and 45 ft in
thickness is saturated.
EPA also considered groundwater and
waste elevations along the [GS–AP–
MW–12/GS–AP–MW–12V] to [GS–AP–
MW–1/GS–AP–MW–1R/GS–AP–MW–
46] transect near the center main valley
of the Ash Pond and extending eastward
along the northern side of Finger 1.
Water levels from 2021 and 2022 from
GS–AP–MW–12 and GS–AP–MW–46
ranged from 360 to 380 feet above MSL.
Given that the bottom of and top of the
CCR are approximately 270 feet and 390
ft above MSL respectively in the center
of the impoundment, EPA estimates that
between 90 to 110 feet of saturated
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waste are present. Similarly, for Finger
1 of the unit, EPA estimates that
between 35 and 55 feet of saturated
waste are present, based on bottom and
top of the CCR being at 325 feet and 430
ft above MSL, respectively. Based on
these limited available data, significant
thicknesses of saturated CCR are present
in these areas.
Lastly, EPA evaluated groundwater
elevations along a north to south
transect, south of the planned closure
buttress, along the west side of the main
valley containing CCR. From north to
south, this included monitoring wells,
GS–AP–MW–12, –13, –14, –47, –15,
–16, and –18. This transect is
approximately 6,150 feet in length, or
over a mile. Over this distance the
available monitoring wells were located
from approximately 25 to 1,100 feet
away from the edge of the CCR waste
and from 50 to 1,500 feet from the
central part of the valley filled with
CCR. EPA used engineering drawings
available in the Permit Application to
estimate CCR top and bottom elevations
adjacent to each groundwater
monitoring point (e.g., construction
drawings G–204, C–200 to C–205). CCR
thickness values varied from 65 to 149
feet along the transect. In some locations
more than one estimate was made due
to the complexity of the subsurface. EPA
then subtracted the CCR waste bottom
elevation from the most recent water
levels for each location (primarily July
18, 2022), to determine the thickness of
saturated CCR, which varied from zero
(no saturated waste) to approximately
115 feet of saturated CCR. This analysis
supported the overall conclusion that
saturated CCR is present in all of these
locations and is therefore likely present
at all locations south of the planned
closure buttress. Even at those locations
where pinpoint estimates of waste
bottom elevations exceeded the
groundwater elevation values, there
were also immediately adjacent
measurements indicating lower
elevations of CCR that were below
groundwater elevation values. For
example, in the GS–AP–MW–15 area,
estimates of waste bottom elevations
varied by over 52 feet: at the lower end
of the range in Finger 6, EPA estimates
there are 13 feet of saturated CCR,
compared with over 65 feet of saturated
waste in the adjacent main valley of the
unit (i.e., station 70+00 on section B–B’
on construction drawing G–204). The
only area arguably without any
saturated CCR is the extreme southern
tip of the unit; on July 18, 2022,
groundwater elevation values at GS–
AP–MW–18 indicate that the waste is
above the water table. However,
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55257
groundwater elevation values measured
at the closely adjacent well, GS–AP–
MW–18R, which is also screened in the
Pratt strata, but more shallowly at
elevations comparable to the waste, on
the same day, indicate approximately 63
feet of saturated waste.
According to the Closure Plan, it
appears that dewatering may have
commenced relatively recently in 2022,
so the measured groundwater elevations
described above from 2022 may not
reflect early stage decreases in hydraulic
head within the unit from any initial
dewatering efforts. But as discussed
below, the Closure Plan contains neither
meaningful details nor supporting
analysis to demonstrate that the
saturated CCR in the consolidated
southern portion of the unit will ever be
dewatered sufficiently to meet the
performance standards in
§ 257.102(d)(2). Moreover, as discussed
below, in the absence of any engineering
measures that would effectively prevent
the continued migration of groundwater
into the closed unit, there is no
information in the Permit Application
that suggests any meaningful decline is
likely in the groundwater elevations
proximal to and within the CCR unit.
Significant thickness of saturated waste
is therefore expected to persist in the
areas south of the closure buttress where
CCR is still present at elevations at or
above the basal excavation level for the
consolidation effort (i.e., > 270 ft above
MSL).
(1) In Order To Close the Ash Pond
With Waste in Place Effective
Engineering Measures Must Be
Implemented
The fact that prior to closure the base
of the Ash Pond intersects with
groundwater does not mean that the
unit may not ultimately be able to meet
the performance standards in
§ 257.102(d) for closure with waste in
place. Depending on the site conditions
a facility may be able to meet these
performance standards by
demonstrating that a combination of
engineering measures and site-specific
circumstances will ensure that, after
closure of the unit has been completed,
the groundwater is no longer in contact
with the waste in the closed unit. In this
case EPA is proposing to determine that
the approved Closure Plan fails to
demonstrate that either performance
standard in § 257.102(d) will be met. In
addition, neither the approved Closure
Plan nor the Permit requires any
engineering measures, such as the slurry
wall proposed for Plant Greene,
described in Unit IV.C.4 of this
preamble, or a groundwater extraction
system (e.g., pumping wells) to control
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or prevent the continued infiltration of
liquids (groundwater) into the CCR from
the sides and beneath. Nor does the
approved Closure Plan or the Permit
require any engineering measure that
will effectively control releases of
leachate to the groundwater. Based on
these facts, and as discussed in more
detail below, EPA is proposing to
determine that the approved Closure
Plan fails to demonstrate that the
closure at Plant Gorgas will meet the
Federal performance standards in
§ 257.102(d) or an equally protective
alternative State standard.
ii. Consistency With 40 CFR
257.102(d)(2)
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As discussed previously, the Federal
CCR regulations applicable to surface
impoundments closing with waste in
place require that ‘‘[f]ree liquids must be
eliminated by removing liquid wastes or
solidifying the remaining waste and
waste residues, [and] remaining wastes
must be stabilized sufficient to support
final cover system.’’ 40 CFR
257.102(d)(2). But due to the lack of
meaningful details and supporting
analysis in the Closure Plan, EPA is
proposing to determine that the Closure
Plan approved by ADEM does not
demonstrate that the proposed closure
at Plant Gorgas will meet either
standard.
According to the approved Closure
Plan, various dewatering techniques
will be employed before and during
closure; however, the Closure Plan
appears to largely limit the use of these
techniques to the CCR in the northern
portion of the unit that will be
excavated and transported to the
consolidated area, and to the areas
under the new Closure Buttress.75 For
example, in the sections specifically
discussing dewatering, the Closure Plan
states:
4.3 Procedures During Closure
4.3.1 Dewatering
This conceptual dewatering plan was
developed to provide a summary of the
removal of free water, interstitial water,
contact water, and surface water as defined
below.
• Free water—water contained in the CCR
unit above the surface of CCR material
• Interstitial water—water within the pore
space of CCR material
• Contact water—surface or ground water
that comes in contact with CCR material
• Surface water—non-contact surface water
at the site that requires management
. . .
75 Alabama Power Company. Revised Closure
Permit Application for the Plant Gorgas Ash Pond.
April 30, 2020. Revised Closure Plan for the Plant
Gorgas Ash Pond. Appendix 11, pp 7–8 (Emphasis
added).
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The free water in the northern portion of the
pond will be decanted by pumping to a water
treatment facility prior to discharge off-site.
The management of the free water levels in
the pond are important for site water
management controls including coordination
with the proposed dredging and other
construction processes. Interstitial water
levels will be monitored in critical areas to
allow for safe excavation and working on ash
as needed to facilitate construction activities.
The main pond free water management
pumps will deliver water to the water
treatment plant for treatment and discharge
up to a treatment rate of 12,000 gpm. The
pumping system will be equipped with a
floating intake, including a sediment curtain
around the intake.
Removal of contact water will be completed
within the limits of the Ash Pond using both
in-situ (in place prior to excavation/
handling) and ex-situ (after initial handling/
excavation) techniques. Dewatering of ash
during closure activities includes removing
water using a variety of methods, including
but not limited to passive, gravity-based
methods (e.g. trench drains, rim ditching,
wick points) and/or active dewatering
methods (e.g. use of the ash thickening plant,
and in-situ pumps or well points) as needed
to allow for CCR removal and transportation.
Ex-situ dewatering techniques consist of but
are not limited to the following: gravity
dewatering (settling basins and/or lateral
trenching), racking and windrowing,
mechanical thickening, and absorbent
desiccation.
EPA expects that Alabama Power
intends to dewater the entire unit to
some extent, if only to ensure that the
consolidated unit can support the
weight of the earthmoving equipment
needed to grade the surface and to
install the cover system. But EPA was
unable to find any discussion of the
methods that will be used to dewater
the significant volumes of saturated CCR
in the southern portion of the
impoundment in sufficient detail to
evaluate whether the free liquids (and
not simply the ‘‘free water’’ defined
above) will be eliminated as required by
§ 257.102(d)(2)(i). For example, on page
three, the Closure Plan states only that
‘‘During closure, the ash pond will be
progressively dewatered as required to
facilitate closure.’’ And on page 5, the
Plan states
Initial stages of construction and dewatering
will include lowering of the pond levels
through pumping and treatment at the onsite
water treatment facility to optimize dredge
performance. Once the desired initial free
water depth is achieved in the pond, further
dewatering will occur incrementally in
response to storm events in order to maintain
the free water at a relatively constant depth
that will lower as ash removal from the
designated areas progresses.
Moreover, the narrative in the Closure
Plan does not explain how the liquids
within the consolidated southern
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portion of the unit will be eliminated in
light of the groundwater that, as
described above, is expected to continue
to saturate the remaining CCR. None of
the proposed engineering measures
mentioned in the Closure Plan are
discussed in sufficient detail to support
a determination that the proposed
measures could effectively remove these
liquids. For example, the approved plan
mentions that a leachate collection
system will be installed at the
downgradient limit of the Closure
Buttress but fails to explain which
liquids the proposed drain system will
capture and how well or extensively it
will do so.
However, based on the limited
information available, the leachate
collection system that ADEM has
approved appears to likely have only a
minimal impact on the level of liquids
in the closed unit, as it is designed to
capture only a limited amount of
leachate. According to the construction
drawings submitted with the Permit
Application, it appears the drain will
only extend approximately 1,200 feet
laterally beneath a portion of the 274acre impoundment and appears to rely
exclusively on gravity to direct any
residual pore water or other free liquids
to the drains. In essence, the leachate
collection system appears to be
designed to only collect leachate along
its 1,200 foot design length, and to only
address residual leachate produced from
limited pore water within the CCR,
which was perhaps expected to drain
over a shorter limited time frame,
during the so-called ‘‘dewatering
phase.’’ But since not all groundwater
leaving the unit will flow to the drain
system, any collection of free liquids
from saturated CCR farther south in the
unit or along the eastern fingers would
be purely coincidental, even without
considering the likely ongoing inputs of
‘‘new’’ groundwater (‘‘contact water’’)
into the system south of the Buttress.76
In addition, to be effective the
leachate treatment system would need
to address not only leachate generated
from short-term ‘‘dewatering’’ activities,
but also the significantly greater longterm volumes of leachate emanating
from the continuously saturated CCR
resulting from ongoing groundwater
inputs into the unit from the sides and
bottom. More critically, the system was
not designed to handle the volumes of
‘‘new’’ leachate that will continue to be
generated from the continued
groundwater flow into the unit. The
Closure Plan therefore appears to have
grossly underestimated the amount of
76 ADEM confirmed these details during
conversations with EPA in July 2022.
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free liquids that will continue to flow
through the saturated waste to the face
drain and associated leachate collection
system.
To illustrate this concern, EPA
performed a rough estimate of potential
recharge to the groundwater system
within the 1,300-acre watershed area
which contains the unit. After
subtracting the 274 acres representing
the closed, capped and consolidated
unit, and assuming all precipitation
directly contacting the cap will be
effectively managed by the drainage
system and other engineering controls,
one is left with 1,026 acres available for
potential recharge to the groundwater
system. Conservatively assuming 1-ft of
effective recharge to groundwater in one
year over the 1,026-acre catchment area
results in approximately 334 million
gallons of effective recharge. Assuming
this total effective recharge is evenly
distributed over time and remains in the
catchment area that contains the unit,
and all flows into the unit, this would
result in a value on the order of 636
gallons per minute of groundwater flow
focused to the subsurface CCR waste
beneath the capped unit. In other words,
additional engineering controls capable
of managing (and treating as necessary)
this additional ongoing input of
groundwater into the unit would be a
minimum necessity for a successful
Closure Plan.
Based on all of the above, it appears
that further engineering measures would
be necessary to ensure that all free
liquids are eliminated prior to installing
the final cover system, as required by
§ 257.102(d)(2)(i).
Additional data are necessary to
demonstrate that saturated CCR will not
be present in the base of the closed unit
prior to the installation of the final
cover system. Absent such data, the
permit record does not support a finding
that the remaining wastes will be
stabilized sufficiently to support the
final cover system, as required by
§ 257.102(d)(2)(ii). If the CCR in the unit
is not sufficiently stabilized, e.g., if it
has not been completely drained,
differential settlement of the CCR after
installation of the cover system is
possible, especially given the
substantial added load from the
consolidation of CCR from the northern
portion of the Ash Pond. If the
settlement is great enough, it could
cause a disruption in the continuity,
and potentially failure of, the final cover
system. Additional information is
needed to determine that the permit
meets Federal requirements. This could
have been accomplished either by
requiring submission of the information
prior to the issuance of the permit or by
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including a permit term requiring
submission of the information, along
with a clause allowing for further permit
conditions if necessary.
iii. Consistency With 40 CFR
257.102(d)(1)(i)
The available information indicates
groundwater is likely to continue to
infiltrate into the unit and yet the only
measures described in the Closure Plan
and the Permit to address this continued
infiltration are those taken to facilitate
consolidation and cap construction. As
explained in previous sections, the
exclusive reliance on a cover system in
this circumstance would not ‘‘control,
minimize, or eliminate, to maximum
extent feasible’’ the post-closure
infiltration of the groundwater into the
waste. 40 CFR 257.102(d)(1)(i).
The approved Closure Plan does not
adequately account for the hydrogeology
of the site, which includes complex
topography, stratigraphy, hydrology,
and other complex site characteristics
such as preferential pathways (faults,
mines, etc.) that make it likely that
groundwater elevations will be higher
than the bottom elevation of the surface
impoundment, even after the cover
system is installed. The cover system
will only prevent liquids (precipitation)
from entering directly into the unit from
the surface/top of the unit. But as shown
on the construction drawings in the
Closure Plan (e.g., drawing C–100),
precipitation will continue to fall onto
the surrounding higher ground surfaces
in the catchment area beyond the lateral
extent of cover system and then
percolate down below the ground
surface, the underlying aquifer will
recharge and groundwater levels will
continue to infiltrate into the CCR from
beneath the unit, as well as from the
sides.
There are commonly used engineering
measures that can prevent, or at least
control, the post-closure flow of
groundwater into the unit; for example,
physical barriers such as slurry walls or
liner systems or by other means such as
hydraulic containment systems (e.g.,
groundwater extraction wells),
additional backfilling to create a buffer
between the bottom of the unit and
groundwater, CCR relocation, etc. EPA
is therefore proposing to determine that
ADEM’s approval of a Closure Plan that
relies exclusively on consolidation and
cap construction to control infiltration
into the Ash Pond is inconsistent with
§ 257.102(d)(1)(i).
EPA is also proposing to determine
that the approved Closure Plan fails to
demonstrate that post-closure releases of
CCR or leachate to the groundwater will
be controlled ‘‘to the maximum extent
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feasible.’’ 40 CFR 257.102(d)(2)(i). While
a leachate collection system is proposed
in the Closure Plan, EPA was unable to
find either analysis or evidence
demonstrating the extent to which the
proposed leachate collection system
will control ‘‘post-closure releases of
CCR or leachate to the groundwater to
the maximum extent feasible.’’ 40 CFR
257.102(d)(2)(i). Moreover, the available
information does not support a
determination that the proposed system
will meet this performance standard. As
previously discussed, the leachate
collection system is not designed to
control the volume of leachate that is
likely to be created from the continued
infiltration of groundwater, nor does it
extend underneath the entire unit.
In addition, there is substantial
evidence that the hydrogeologic
pathways that will allow unimpeded
migration of groundwater into the unit
from the bottom and sides of the unit
will also allow leachate to migrate
laterally and vertically out of the unit at
particular locations. The absence of
natural or engineered hydraulic barriers
along the base and sides of the unit,
which allows for both infiltration and
exfiltration of liquids, will likely result
in additional releases of contaminated
groundwater (i.e., ‘‘plumes’’) out of the
unit via the bottom or sides. For
example, preferential pathways, such as
geologic faults and mine shafts from
former mining operations, are present
beneath the unit that would be expected
to draw contamination from any
uncaptured leachate down into the
aquifer. The existence of preferential
pathways was clearly acknowledged in
the GWMP that was included in the
Permit Application as Appendix C.77
The approved Closure Plan does not
account for these pathways or otherwise
evaluate how well the proposed drain
system will capture liquids. To meet the
performance standard in
§ 257.102(d)(1)(i), the approved Closure
Plan would have to show that the
77 Alabama Power Company. Revised Closure
Permit Application for the Plant Gorgas Ash Pond.
April 30, 2020. Response to Comments, Approved
Groundwater Monitoring Plan included in the
October 20, 2021. For example, the following
statements were made within the RTC for the
GWMP:
[i]n-conjunction [with statements made earlier in
the letter], the geology at Plant Gorgas dictates
preferential flow through coal seams and vertical to
subvertical joints, fractures, and faults. Targeting
such features for monitoring, even if stepped back
from the waste boundary, is technically justified.
This because preferential flow paths concentrate
groundwater migration through enhanced fracture
interconnectivity within otherwise impermeable
rock strata. Therefore, given the travel-times
described [earlier in the letter], and the age of the
facility—it was appropriate to target these features
for determining potential impacts to groundwater.
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leachate will be channeled to the
leachate collection system rather than to
the preferential pathways, EPA was
unable to find anything in the Permit
Application or permit record to show
that either Alabama Power or ADEM
made any such showing. As discussed
previously, the available information
indicates that the face drain and underdesigned leachate collection system
would likely be ineffective in
preventing such releases, given the
under-designed leachate collection
system.
b. Plant Gorgas Groundwater Monitoring
Issues
The Final Permit incorporated the
GWMP submitted with the Permit
Application, and directed Alabama
Power to comply with the State
regulations and the approved plan:
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A. Groundwater Monitoring System. The
Permittee shall install and/or maintain a
groundwater monitoring system, identified in
Table 1, as specified in 335–13–15–.06(2) and
the approved groundwater monitoring plan.
Once ADEM approved and adopted the
GWMP into the permit, the GWMP,
rather than the referenced State
regulations, became the State
requirements with which the facility is
required to comply.
Based on EPA’s review of the
approved GWMP, EPA is proposing to
determine that the groundwater
monitoring well network approved by
ADEM does not meet the performance
standards in § 257.91(a) or (b). As
discussed in more detail below, EPA is
proposing to determine that the
groundwater monitoring system does
not ‘‘yield groundwater samples from
the uppermost aquifer,’’ but has been
screened instead in only a portion of the
aquifer. 40 CFR 257.91(a). EPA is also
proposing to determine that approved
groundwater monitoring system is not
based on a thorough characterization of
any of the elements listed in § 257.91(b).
Further, EPA is proposing to determine
that the approved monitoring system
inappropriately includes numerous
downgradient monitoring wells that are
not located at the waste boundary. See
40 CFR 257.91(a)(2). In addition, based
on the documentation provided in the
Permit Application, it appears that there
are an insufficient number of
monitoring wells at necessary locations
and depths to meet the Federal
performance standards for either the
background wells or the compliance
wells. See, 40 CFR 257.91(a)(1)–(2).
Therefore, EPA is proposing to
determine that ADEM’s Final Permit
fails to require Alabama Power to
achieve compliance with either the
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Federal regulations or with an equally
protective State requirement.
i. Failure To Delineate the ‘‘Uppermost
Aquifer’’
The Federal regulations require that a
groundwater monitoring system sample
‘‘the uppermost aquifer,’’ which is
defined as ‘‘the geologic formation
nearest the natural ground surface that
is an aquifer, as well as lower aquifers
that are hydraulically interconnected
with this aquifer within the facility’s
property boundary.’’ 40 CFR 257.53,
257.91(a). The design of the monitoring
systems must be based on a thorough
characterization of, among other things,
the ‘‘aquifer thickness, groundwater
flow rate, groundwater flow direction
including seasonal and temporal
fluctuations in groundwater flow; and
saturated and unsaturated geologic units
and fill materials overlying the
uppermost aquifer, materials comprising
the uppermost aquifer, and materials
comprising the confining unit defining
the lower boundary of the uppermost
aquifer.’’ 40 CFR 257.91(b)(2). EPA is
proposing to determine that ADEM
approved a groundwater monitoring
plan that does not meet these
requirements.
Based on the limited information in
the permit record, it appears the facility
failed to define both the upper and
lower limits of the uppermost aquifer.
The GWMP provided in the Permit
Application provides only limited
characterization of the geologic units
beneath the Ash Pond. In addition, the
technical information provided in the
Permit Application and available on
Alabama Power’s CCR website is
insufficient to support a determination
of the lateral and vertical limits of the
entire uppermost aquifer; for example,
EPA found only limited data on the
‘‘saturated and unsaturated geologic
units and fill materials overlying the
uppermost aquifer and materials
comprising the uppermost aquifer.’’ 40
CFR 257.91(b)(2). And EPA was only
able to find limited and conflicting
information about the ‘‘materials
comprising the confining unit defining
the lower boundary of the uppermost
aquifer.’’ Id. In the absence of such key
information it is impossible to
determine that the monitoring system
adequately covers the entire uppermost
aquifer, which includes all ‘‘lower
aquifers that are hydraulically
interconnected’’ with the aquifer nearest
the ground surface. 40 CFR 257.53
(definition of ‘‘uppermost aquifer’’).
Nevertheless, ADEM approved Alabama
Power’s GWMP unconditionally.
A representation of the various
aquifers beneath the Ash Pond can be
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obtained by examining the cross
sections found in the 2021 Remedy
Selection Report.78 The uppermost
aquifer may be described in its most
basic expression as a ‘‘layer cake’’ with
interbedded layers of sub-horizontal
sedimentary rocks. As depicted in these
cross sections, for example Figure 9B of
Appendix B of this report, for instance
the aquifer nearest the ground surface is
shown as the Cobb Group. A portion of
the Cobb Group is present in higher
elevations of the site, overlying the Pratt
Group. Both the Cobb and Pratt Groups
are part of the regionally significant
Pottsville Formation. Coal beds known
to be present regionally in the Cobb
Group were not identified near the unit
and Cobb Group rocks near the unit
consist of sandstones, mudstones, and
shales. Some individual sandstone beds
are depicted as having thicknesses of
over 50 feet as well as significant lateral
extent, on the order of thousands of feet.
The Cobb Group also contains thick
laterally extensive mudstones, and the
mudstones are interbedded with thinner
sand layers in the northern part of the
unit. The aggregate thickness of the
Cobb Group is on the order of 200 to 250
feet or more at the unit. As the
stratigraphically highest rock layer, the
Cobb Group thickness varies across the
unit due to differences of the uppermost
surface elevation of the Cobb Group
resulting from differential erosion.
Alluvial materials and/or fill deposits
rest unconformably and discontinuously
on top of the Cobb Group’s upper
erosional surface in many areas of the
unit, particularly to the south. These
Cobb Group stratigraphic intervals are
poorly characterized in comparison to
the underlying Pratt Group, with few
monitoring wells installed in the Cobb
Group rocks.
The upper part of the Pratt Group
includes interbedded sandstones,
siltstones, mudstones, as well as several
distinct coal beds. The uppermost of
these named coal beds is the Pratt Coal
Seam and associated layers, but
additional named coal seams are present
at successively deeper levels, as
described in Section 3 of the approved
GWMP: ‘‘The Pratt Coal Group generally
contains three named coal seams each
separated by 10 to 30 feet of
intraburden. In descending order, they
are, the Pratt, Nickel Plate, and
American coal seams.’’
Beneath the upper part of the Pratt
Group and its named coal seams, a
significant thickness of interbedded
78 Southern Company Services. 2021
Groundwater Remedy Selection Report, Alabama
Power Company Plant Gorgas Ash Pond. Prepared
for Alabama Power Company. December 2021.
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sandstones and mudstones on the order
of 50 feet or more is present. These
intervals are described as the Lower
Pratt Group, which has received
comparatively little characterization and
few monitoring wells. The Pratt Group,
including both the lower and upper
portions, is depicted as having an
aggregate thickness of approximately
200 feet beneath the unit. Differential
erosion, particularly within the main
channel-like finger of the Ash Pond, has
locally resulted in alluvial materials
and/or fill deposits resting
unconformably on top of the Pratt
Group’s upper erosional surface,
particularly in the central part of the
unit.
In the southern portion of the unit,
the Gillespy Group, also of the Pottsville
Formation, is shown on cross sections
as underlying the Pratt Group at great
depths, but characterization of this
interval is extremely limited. The cross
sections in the 2022 Semi-Annual
Groundwater Monitoring and Corrective
Action Report show that the Gillespy
Group also has an aggregate thickness
on the order of 200 feet, yet the upper
and lower contacts between the Gillespy
and underlying and overlying layers is
poorly characterized, particularly with
respect to the lower contact, and the
thus the variability and full vertical
extent (i.e., thickness) of the Gillespy
Group under the Ash Pond has not been
precisely determined. On cross section
F–F’ (Figure 4F), the Gillespy Group is
depicted as just over 200 feet in
thickness. The cross section also depicts
the contact with the underlying Mary
Lee Group mudstones at a depth of
several hundred feet below the unit at
a corresponding elevation just above
MSL. However, it is not clear what data
informs this interpretation as no borings
are known to have penetrated the full
thickness of the Gillespy Group near the
unit based on the cross sections and
monitoring well installation details. As
such the true thickness of the
uppermost aquifer and hydraulically
connected aquifers is not known, nor
has it been established whether the
Gillespy Group constitutes an effective
lower confining unit to the uppermost
or aquifer system. See 40 CFR 257.91(b).
It is also notable that the elevation of the
top of the Gillespy Group is relatively
high near the northern part of the unit,
and differential erosion has resulted in
deposits of overburden, alluvium and/or
fill, including fill/dam materials resting
unconformably on top of the upper part
of the Gillespy Group in the northern
part of the unit, as shown of cross
section F–F’.
The additional relevant geologic
aspects of the aggregate layering which
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constitutes the uppermost aquifer
system includes faulting and folding of
the layering. Following the ‘‘layer cake’’
analogy, the layers of rocks have been
disrupted locally on several steep fault
lines that predominantly strike northnorthwest in the vicinity of the unit, as
such the ‘‘layer cake’’ package of rocks
has been disrupted and contains many
distinct ‘‘slices’’ separated by these
faults. The faults indicate significant
vertical offset on cross sectional
representations, and the rock layers are
locally bent or ‘‘folded’’ near these fault
structures, resulting in steeper dips. The
entire package has been slightly tilted
regionally to the south as if the northern
end of the ‘‘layer cake’s serving platter’’
had been lifted slightly.
The final element, following the
‘‘layer cake’’ analogy, is the ‘‘icing on
the cake.’’ Like drizzled icing,
unconsolidated fill and alluvial
materials irregularly cover the tilted,
faulted, and eroded surface of the ‘‘layer
cake’’ of rock layers. It is expected that
overburden including alluvial materials
(e.g., sands and gravels) originally
present as stream deposits in the incised
erosional stream valleys were covered
by the introduced CCR materials. These
buried alluvial materials therefore
represent the uppermost veneer of the
uppermost aquifer system. Since there
are few wells screened in these former
stream valleys, this element of the
uppermost aquifer system is
significantly underrepresented in the
monitoring network.
(1) Uppermost Aquifer
Within this complex ‘‘layer cake’’
geology of variable sedimentary
layering, Alabama Power screened most
of its monitoring wells in the Upper
Pottsville Aquifer system, which is
described in Section 3.2.2 of the 2022
Semi-Annual Groundwater Monitoring
and Corrective Action Report as follows:
Groundwater occurs in the Pratt Coal Group
of the Upper Pottsville Formation at the site.
The primary occurrences of groundwater in
the uppermost aquifer are: (1) coal seams, (2)
rock fractures or zones of fracture enhanced
permeability, and to a lesser extent (3)
bedding planes. Fractured intervals are
sparse across the site as defined by caliper
logging and tend to occur with greater
density in the upper 100 feet of rock.
Groundwater yield at the site is considered
low and typical of the Pottsville aquifer
system in areas without major geologic
structures. Wells were generally screened in
the Pratt coal seam or across groundwater
yielding fractures. Depth to groundwater
producing zones were highly variable at the
site and typically ranged from 30 to 240 feet
BGS.
It is further noted in Section 3.2.3 of the
2022 Semi-Annual GWMCA Report that,
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Groundwater flow is accomplished primarily
by means of fracture flow, where
groundwater flows along more conductive
secondary discontinuities in the rock mass
such as joints or cleat fabric in coal seams.
Fracture flow in complex geologic media
such as the heterogenous Pottsville
Formation can be complex. Groundwater in
the Pottsville aquifer is most commonly
regarded as confined due to large
permeability contrasts within the aquifer
(Stricklin, 1989). The Pottsville at the Site is
probably better described as a series of
discrete, confined to semi-confined,
groundwater yielding zones where
groundwater elevations can vary significantly
laterally and vertically and are governed by
the heterogeneity of the lithology and degree
of fracture network interconnectivity . . . .
At higher stratigraphic intervals (watertable flow system), groundwater flows
towards the Ash Pond or other surface water
bodies. This flow system is driven by gravity
and mimics the topography of the site.
Within deeper rock strata such as coals of the
Pratt Group (Pratt Coal Group or deep
bedrock flow system), groundwater flows
radially away from the site.
Most of the characterization and
monitoring is concentrated in the
named coal seams of the Pratt Coal
Group, and three primary flow systems
(i.e., aquifers) have been identified, as
follows:
At the Site, the groundwater flow regime
is now grouped into three general flow
systems: (1) shallow water-table flow system,
(2) Pratt Coal flow system, and (3) American
Coal flow system.
In this system of nomenclature, the
Nickel Plate Coal Seam is generally
included within the Pratt Coal System.
EPA also noted that the Pratt Coal
System and the American Coal Systems
are mapped together and separately in
different groundwater monitoring
reports. For example, the approved
GWMP (Figure 6B) has them mapped
together and the 2020 Annual GWMCA
Report 79 has them mapped separately
(Figures 6B and 6C). Accordingly,
subsequent references to aquifers in the
coal seams, below, if not specifically
described as the ‘‘Pratt’’ or ‘‘American’’
aquifers, describe the three coal seam
flow systems of the Pratt Coal Group
jointly as an aggregate combined system.
In addition to the three systems
designated above (shallow water table,
Pratt, and American), lower intervals of
the stratigraphic section have been
designated 80 as another (fourth) system,
which is primarily localized to the
northern part of the unit in the vicinity
79 Southern Company Services. 2020 Annual
Groundwater Monitoring and Corrective Action
Report, Alabama Power Company Plant Gorgas Ash
Pond. Prepared for Alabama Power Company.
January 31, 2021.
80 Id.
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of the Ash Pond dam and northward.81
In this area, the geologic units located
at depths corresponding to the
transition zone from the lower Pratt
Group to rocks of the underlying
Gillespy Group are mapped together as
the ‘‘Base of Pratt to Gillespy
Transition’’ aquifer zone. This interval
is at much higher elevations in the
northern part of the site than in the
southern portion. In any case, based on
these aquifer designations various
interpretive representations of
groundwater flow have been
constructed and were provided in the
Permit Application and annual
monitoring reports. Based on these
interpretations, in the Cobb Group,
above the Pratt Coal Group,
groundwater is within an unconfined
aquifer and flows toward the unit.
Within the Pratt Coal Group,
groundwater flow is interpreted to be
mainly within the American and Pratt
Aquifers and flows radially away from
the unit. However, these interpretations
are informed by insufficient data
considering the large geographic area
represented by the Ash Pond as well as
the topographic and hydrogeologic
complexity. The Ash Pond is
approximately 500 acres and sits within
a watershed of roughly 1,300 acres with
hundreds of feet of topographic relief.
The small number of wells installed in
each of the respective aquifer layers
simply does not allow for a sufficient
level of resolution regarding the true
configuration of the potentiometric
surface and related groundwater flow
directions. As such, the interpretations
represented by the various
potentiometric surface contour maps
included in the 2022 Semi-Annual
GWMCA Report contain a large degree
of uncertainty.82 For example, there are
just a few wells screened in the
unconfined materials above the coal
seams. Figure 6A of the 2022 SemiAnnual GWMCA Report, entitled
Potentiometric Surface Contour Map
(Upper) Water Table Aquifer, February
7, 2022, Plant Gorgas Ash Pond, is
based on just 10 water level monitoring
points over an area hundreds of acres in
size. Figure 6B of the same report
Potentiometric Surface Contour Map,
Pratt Aquifer, February 7, 2022, is based
on just 31 water level monitoring points
over the same area. Figure 6C of the
81 Southern Company Services. 2022 SemiAnnual Groundwater Monitoring and Corrective
Action Report, Alabama Power Company Plant
Gorgas Ash Pond. Prepared for Alabama Power
Company. July 31, 2022. See inset map entitled,
‘‘Generalized Potentiometric Surface Contour
Map—Base of Pratt to Gillespy Transition zone
(North of Dam)’’ included on Figure 6B.
82 Id.
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same report is entitled Potentiometric
Surface Contour Map, American
Aquifer, February 7, 2022. This
interpretation is based on just 21 water
level monitoring points over the same
immense area. Lastly, there are a limited
number of water level monitoring points
(13) that intersect the Gillespy; nearly
all of the these are screened across the
interface between the Gillespy and the
lower part of the Pottsville Formation
(see inset map on Figure 6B) entitled,
Generalized Potentiometric Surface
Contour Map—Base of Pratt to Gillespy
Transition (North of Dam). In summary,
given the large size of the Ash Pond and
the surrounding area, interpretations of
the flow systems are highly generalized
because of the limited number of
monitoring points in each
hydrostratigraphic units.
Additionally, the nature of the lower
boundary of the aggregate ‘‘uppermost
aquifer’’ system has not been
sufficiently characterized or monitored
due to the limited number of wells
installed into this zone, and the
documented importance of fracturing,
where present, such as in the subsurface
beneath the unit, and its association
with increased permeability values.
This issue is discussed below. A key
consideration with respect to the base of
the Pratt to Gillespy transition is
whether this transitional formation
contact represents the boundary
between the materials comprising the
‘‘uppermost aquifer,’’ and materials
comprising the ‘‘confining unit defining
the lower boundary of the uppermost
aquifer.’’ 40 CFR 257.91(b)(2). It is
asserted in the 2022 Semi-Annual
GWMCA Report that,
Except for the far northern portion of the Ash
Pond, conceptually, there is likely to be little
hydraulic communication with strata deeper
than the sandstone unit immediately
underlying the American Coal Seam
(American Coal Flow System). Below this
interval, a low permeability mudstone to
interbedded mudstone-sandstone unit likely
forms a barrier to vertical migration of
groundwater as hydraulic conductivity
values in the 10¥7 centimeter per second
(cm/s) range are reported for shales at the site
as derived from packer testing. This interval
reflects the transition to Gillespy Coal Group.
Additional information presented in
the same report presents contradictory
information regarding the confining
potential of the basal portion of the
Gillespy Coal Group:
However, to the north and underlying the
Ash Pond dam, strong hydraulic gradients
likely force groundwater along vertical
fractures and bedding planes through the
upper part of the Gillespy Coal Group.
Geophysical and hydrophysical logs obtained
in well locations north of the dam suggest
that three to four discrete bedding planes
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occurring between 30 and 90 ft BGS transmit
groundwater. The most prominent typically
occurring at a depth of 49 to 56 ft BGS (likely
Gillespy equivalent; approximately 100 feet
below American Coal Seam).
The potential for vertical flow, within
the Gillespy is further described as
follows:
Strong upward vertical gradients are
observed in paired well locations (see
groundwater elevations in MW–6S/6D and
MW–41HS/HD pairs) installed north of the
ash pond dam. Potentiometric data suggests
upward vertical flows along with northerly
lateral flow.
Lastly, the same report discusses
permeability test results, which again
present an inconsistent picture of the
Gillespy formation’s potential to act as
a ‘‘confining unit defining the lower
boundary of the uppermost aquifer,’’ as
follows:
Forty-three packer tests were conducted
resulting in a range of hydraulic conductivity
(k) values from an estimated low of 7 x 10¥7
cm/sec to a high of 4 x 10¥3 cm/sec, with
most tests (31) in the moderate range (10¥5
cm/sec to 10¥4 cm/sec), two test results in
the more permeable range (10¥3 to 10¥2 cm/
sec), and ten test results in the less permeable
range (10¥6 cm/sec). There is a general trend
of decreasing estimated hydraulic
conductivity with depth. Packer test results
vary over 4 orders of magnitude. Test
intervals at the high end of the data range are
associated with weathered discontinuities
(fractures/joints). Moderate values are
associated with minor fractures or bedding
planes. The lowest values are associated with
more shale intervals without substantial
fractures. Test intervals with coal seams are
in the moderate to high end of the data range.
EPA disagrees that this information
supports a determination that the lower
part of the Gillespy formation
constitutes a ‘‘confining unit defining
the lower boundary of the uppermost
aquifer.’’ The totality of the information
instead supports the opposite
conclusion. Since vertical flow is clearly
a recognized phenomenon within the
Gillespy within the northern part of the
unit, and this flow is described as being
associated with fractures,83 it is logical
to expect similar vertical flow and
enhanced permeability in other areas
where fractures are present. Given the
prevalence of steeply dipping northnorthwest striking fracturing in the area,
as well as the likelihood that the linear
valley that underlies the unit, which
also strikes north northwest, is also
controlled by underlying fractures of
this orientation, it is reasonable to
expect enhanced flow potential along
83 Southern Company Services. 2022 Annual
Groundwater Monitoring and Corrective Action
Report, Alabama Power Company Plant Gorgas Ash
Pond. Prepared for Alabama Power Company.
January 31, 2023. Section 3.2.3.
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and in the vicinity of these fractures
where they may exist. Since the
subsurface directly beneath the unit is
likely the locus of such fracturing (see
Unit IV.C.3.b.i.(4)(c) of this preamble for
more information on the existence of
preferential pathways), it is logical to
determine that vertical permeability is
high beneath the unit where it matters
most. In other words, this situation
suggests that rather than a ‘‘confining
unit defining the lower boundary of the
uppermost aquifer,’’ the near vertical
fracturing which penetrates all units
(see cross sections), including the
Gillespy, creates the opposite condition
in the uppermost aquifer system,
directly beneath the unit. It is therefore
unlikely that the uppermost aquifer
beneath the Ash Pond has been
adequately characterized, and its full
thickness in the vertical dimension
remains unknown based on the
information in the permit record. As
was noted above, the lowest measured
permeability values are associated with
shale intervals without substantial
fractures. Although conditions are not
sufficiently documented directly
beneath the unit, the likely presence of
fractures here would be expected to
invalidate the presence of ‘‘shale
intervals without substantial fractures,’’
and hence the ‘‘lowest measured
permeability values,’’ while present in
other areas around the unit, would
likely not be present directly beneath
the unit.
In sum, the uppermost aquifer
system– that is, the aquifer nearest the
ground surface and the underlying
aquifers that are hydraulically
connected to it—has not been fully
assessed. EPA’s assessment of the
available information is that there are at
least four flow systems that are
appropriately considered the
‘‘uppermost aquifer’’ at the Ash Pond:
(1) the upper unconfined water table
(locally includes unconfined Cobb
Group); (2) the Pratt Coal seam; (3) the
American Coal seam; and (4) the Lower
Pratt/Gillespy Transition zone.
The geologic units above and beneath
the coal seams are sandstones and
interbedded sandstones with mudstone
or shale, and both are capable of storing
and transmitting groundwater, and
therefore should have been more fully
characterized and included in the
monitoring network. In particular, the
depth of the lower confining unit has
not been established, and as such, the
full extent of the uppermost aquifer
system has not yet been established in
the vertical (depth) dimension. At
several locations, the geologic units
immediately below detected
groundwater contamination are entirely
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uncharacterized and unmonitored. This
situation hobbles the monitoring
network’s ability to identify and
evaluate potential migration of
contaminated groundwater out of the
unit at the lower levels, which is
discussed further in Unit
IV.C.3.b.i.(4)(b) of this preamble.
(2) Background Wells Do Not Meet the
40 CFR 257.91(a)(1) Performance
Standard
The Federal CCR regulations require
that a groundwater monitoring system
consist of a sufficient number of wells
at appropriate locations and depths to
yield samples from the uppermost
aquifer that accurately represent the
quality of the background groundwater
that has not been affected by leakage
from a CCR unit. 40 CFR 257.91(a)(1).
The regulations also specify that
background wells must normally be
hydraulically upgradient of the CCR
unit unless specific showings have been
made. See, Id. EPA is proposing to
determine that the approved GWMP
fails to document either that the
background wells are upgradient of the
CCR unit or that the wells meet the
performance standards in
§ 257.91(a)(1)(i) or (ii). EPA is also
proposing to determine that the
background wells in the approved
groundwater monitoring system do not
‘‘accurately represent the quality of the
background groundwater’’ because no
background wells were installed in the
lower flow systems of the uppermost
aquifer: i.e., the Pratt Coal seam; the
American coal seam, and the Lower
Pratt/Gillespy Transition Zone.
Four groundwater monitoring wells
have been used at various times to
characterize background water quality
(GS–AP–MW–8, GS–AP–MW–13, GS–
AP–MW–16S, and GS–AP–MW–17V).
One of the wells, GS–AP–MW–13 was
installed in 2016 and later abandoned in
2019. The three remaining monitoring
wells (GS–AP–MW–8, GS–AP–MW–
16S, and GS–AP–MW–17V) were
installed exclusively in the upper flow
system (i.e., in the upper water table
aquifer/unconfined Cobb Group
formation), where Alabama Power has
concluded that groundwater flows
toward the Ash Pond. No background
wells were ever installed in the three
lower flow systems of the uppermost
aquifer, which is where contamination
is currently present.
According to the 2021 Plant Gorgas
Annual GWMCA Report, to the north
and underlying the Ash Pond dam,
strong hydraulic gradients force
groundwater along vertical fractures and
bedding planes through the upper part
of the Gillespy Coal Group toward the
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Ash Pond.84 The approved GWMP also
provides details regarding vertical
gradients and the potential for using
monitoring wells in the shallow flow
system as background wells. For
example, page 10 states:
It is because vertical flow is the dominant
mechanism for movement through these flow
systems and that is a function of the
Pottsville operating as a series of discrete,
confined to semi-confined groundwater
yielding zones. Upgradient well locations
monitor younger, recharging waters that will
eventually migrate vertically downward into
groundwater yielding zones of the Pratt Coal
Group.
Based on the limited data available it
appears that groundwater in the upper
water table (or un-confined Cobb)
aquifer may migrate downward into the
lower flow systems due to vertical
hydraulic gradients. However, as
discussed at length above, these
interpretations contain a large degree of
uncertainty because they are informed
by very little data, given the size of the
Ash Pond as well as the topographic
and hydrogeologic complexity of the
site. The complexity of the site is of
particular concern here; in addition to
the compositional variability of the
layers, differential fracturing also
creates variable hydraulic conditions
which needed to be carefully considered
in selecting upgradient background well
locations. Lastly, the wells currently
selected for background monitoring
ignore horizontal flow in the lower flow
systems where groundwater
contamination is present and migrating
laterally. EPA is proposing to determine
there is insufficient data to conclude
that the approved background wells
meet the performance standards in
§ 257.91(a)(1).85
EPA is also proposing to determine
that there are insufficient number of
background wells in the approved
groundwater monitoring system. As
discussed in the preceding section,
there are at least four flow systems that
would each require background wells
focused on the specific hydrogeologic
conditions in each of these zones: (1)
The upper water table aquifer; (2) The
Pratt Coal seam; (3) The American Coal
seam; and (4) The Lower Pratt/Gillespy
Transition zone. In addition to these
84 Southern Company Services. 2021 Annual
Groundwater Monitoring and Corrective Action
Report Alabama Power Company Plant Gorgas Ash
Pond. Prepared for Alabama Power Company.
January 31, 2022.
85 Because Alabama Power believes the
background wells to be hydraulically upgradient,
the Permit Application did not include a
demonstration that the background wells will be
‘‘as representative or more representative’’ as
hydraulically up gradient wells. 40 CFR
257.91(a)(1)(ii).
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four, it remains unclear whether other
flow systems should have been included
in the monitoring program, which
would require the installation of
appropriate zone-specific background
wells. For example, the Cobb Group
appears to contain multiple permeable
sandstone units, as do portions of the
Pratt Group both above and below the
named coal seam aquifers. It would
appear that background wells should
have been installed in one or both of
these geological formations to capture
this geologic variability. As noted above,
in addition to the compositional
variability of the layers, differential
fracturing also creates variable
hydraulic conditions that needed to be
more carefully considered in selecting
background well locations.
The Federal regulations require a
monitoring well system that accurately
represents the quality of background
groundwater. 40 CFR 257.91(a)(1).
Background concentrations need to be
determined for the entire uppermost
aquifer system and must be supported
by an explanation of the hydraulic and
geologic factors that validate the
selection of particular locations as
representative background conditions. If
the uppermost aquifer varies laterally
and vertically in terms of geology and
chemical composition, it is necessary
for the background monitoring wells
installed to adequately reflect this same
range of variability (i.e., representative
conditions in these same layers absent
CCR-related impacts). This requires
enough monitoring wells to capture the
variability represented by the natural
system in appropriate dimensions, such
as lateral and/or vertical variability.
Consequently, in cases of multiple flow
systems comprised of variable geology,
as a first order requirement, background
wells in each hydrostratigraphic unit of
interest would be technically necessary.
The specific conditions at Plant
Gorgas further illustrate this; the
geochemistry of the groundwater within
the shallow water table aquifer
(consisting of younger groundwater
within sandstone and shales) would not
represent the geochemistry of deeper
flow systems (consisting of older
groundwater within interbedded
sandstones with coal seams). It is also
uncertain how unique conditions in the
lower flow systems, such as the
presence of coal seams and current and
historical mining operations could affect
background water quality in the lower
flow systems.
In summary, the uncontaminated
‘‘flavors’’ (i.e., representative
conditions) of each relevant aquifer
zone need to be established to provide
a representative direct comparison
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relative to CCR impacts in these same
zones on an ‘‘apples to apples’’ basis.
However, the approved background
monitoring system is insufficient in
terms of general numbers of background
monitoring wells as well as a general
failure to include background
monitoring in key sub-elements of the
layered hydrogeologic system
representing the uppermost aquifer. It
therefore does not appear to accurately
represent the full range of ‘‘background’’
conditions in the uppermost aquifer.
GWMP with an insufficient number of
wells laterally along the downgradient
perimeter of the unit to monitor all
potential contaminant pathways. EPA is
also proposing to determine that
monitoring wells in the approved plan
were not installed at appropriate depths
to ensure that all potential contaminant
pathways were monitored. Finally, EPA
is proposing to determine that the
approved groundwater monitoring
system fails to account for preferential
pathways beneath the Ash Pond.
(3) Compliance Wells Are Not Installed
at the Downgradient Waste Boundary
40 CFR 257.92(a)(2) requires that
downgradient compliance wells ‘‘be
installed at the waste boundary that
ensures detection of groundwater
contamination in the uppermost
aquifer.’’ The waste boundary is ‘‘a
vertical surface located at the
hydraulically downgradient limit of the
CCR unit. The vertical surface extends
down into the uppermost aquifer.’’ 40
CFR 257.53. Notwithstanding this clear
direction, most wells in the monitoring
network installed at Plant Gorgas were
located far from the waste boundary. Yet
ADEM approved the system without
condition or revision.
For example, EPA evaluated well
placement along a north to south
transect, south of the buttress, along the
west side of the main valley containing
CCR. From north to south, this
included, GS–AP–MW–9, –10, –11, 12,
–13, –14, –47, –15, –16, and –18. This
transect is approximately 8,400 feet in
length, or over a mile and a half. Over
this distance the monitoring wells were
located from 55 feet to 510 feet away
from the waste boundary, with and
average distance from the waste
boundary near 295 feet. On average,
over the entire unit, monitoring wells
here were located approximately 740
feet from the waste boundary.
(1) Insufficient Lateral Spacing of
Compliance Wells To Monitor All
Potential Contaminant Pathways
ii. Insufficient Locations and Depths of
Downgradient Compliance Wells To
Monitor the Uppermost Aquifer
As previously discussed, the Federal
regulations specify that a groundwater
monitoring system must ‘‘consist[ ] of a
sufficient number of wells, installed at
appropriate locations and depths, that
. . . accurately represent the quality of
the groundwater passing the waste
boundary of the CCR unit.’’ 40 CFR
257.91(a)(2). The regulations further
specify that ‘‘[a]ll potential contaminant
pathways must be monitored.’’ Id. But
the groundwater monitoring system that
ADEM approved meets none of these
requirements. As discussed in more
detail below, EPA is proposing to
determine that ADEM approved a
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The majority of the compliance wells
along the perimeter of the Plant Gorgas
Ash Pond are spaced hundreds and
sometimes thousands of feet apart. For
example, only a single detection
monitoring well (GS–AP–MW–2) was
installed near the waste boundary to
monitor groundwater over a large area
flowing from the Plant Gorgas Ash Pond
along the northeastern boundary. The
lateral distances from GS–AP–MW–2 to
the adjacent compliance wells to the
north and south, GS–AP–MW–3, and
GS–AP–MW–1R, respectively, both
approach 2,000 feet (as the crow flies).
Furthermore, the waste boundary
between the two compliance wells GS–
AP–MW–2 and GS–AP–MW–1R is
approximately two miles. This
unmonitored two-mile portion of the
waste boundary runs along three sides
of an adjacent offsite 16-acre parcel that
appears to include residential
structures. In effect, this leaves a twomile stretch without any compliance
wells to detect contamination before it
migrates off-site.86 See Figure 5A in the
2021 Plant Gorgas Annual GWMCA
Report.87
This is not an anomaly, and extremely
large lateral well spacings and large
lateral gaps in monitoring well coverage
are not an isolated occurrence. Prior to
closure, the perimeter of the unit was
roughly 14.7 miles in length, and
following closure, the perimeter of the
consolidated CCR will be approximately
7.8 miles in lateral extent.88 Because
86 Two wells (GS–AP–MW–43H and GS–AP–
MW–44HO) are also situated in the vicinity of the
adjacent offsite 16-acre parcel, but these wells are
designed to horizontally delineate the plume of
contamination that has already migrated beyond the
unit boundary.
87 According to a representative from the
Copeland Ferry—Pumpkin Center Water Authority
Publicly Owned Treatment Works, they serve
public drinking water to residents in the vicinity of
the Ash Pond. EPA is also working to confirm
whether nearby households are on public or private
water supply.
88 This approach is further supported in view of
the fact that the original footprint, although
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ADEM approved the groundwater
monitoring system in its current form,
and it appears that the monitoring
network will change little during the
ongoing closure activities, it is
reasonable to evaluate the lateral well
spacing in terms of the current (preclosure) perimeter, i.e., 14.7 miles. Over
this 14.7-mile unit boundary there are
presently only 30 downgradient
compliance wells, indicating an average
spacing of approximately 2,600 feet, or
roughly half a mile between monitoring
wells. Prior to 2021, there were only 20
downgradient compliance wells,
indicating an average lateral spacing of
downgradient compliance wells in the
lateral dimension was on the order of
3,900 feet apart, or almost three quarters
of a mile.
Because wells installed to
characterize the release in accordance
with § 257.95(g)(1)(i) are not located on
the downgradient waste boundary and
are monitored for different constituents
at different frequencies, these wells are
not properly included in an evaluation
of adequacy of the detection and
assessment wells installed to comply
with requirements in § 257.91(a). And
even if EPA were to consider the
delineation wells as part of the
detection and assessment monitoring
systems, that would only bring the total
number of monitoring wells to 68,
which would equate to one well per
every 1,150 feet of boundary.
However, by any reasonable standard,
lateral well spacings on the order of
thousands of feet would be excessive.
While appropriate lateral well spacing is
site-specific, and varies from site to site,
lateral well spacing appropriate for a
site such as the Ash Pond at Plant
Gorgas may be determined by several
factors. These include, but are not
limited to, the character, the degree of
homogeneity, and dimensions of the
emplaced waste body itself; the nature,
variability, and complexity of the
subsurface geology; as well as the
dynamics, complexities, and boundary
conditions of the hydraulic flow system
into which the CCR has been emplaced.
A greater degree of complexity and
variability concerning these elements
would translate to a greater number of
compliance wells in the lateral
dimension, i.e., a smaller inter-well
spacing, for the well network to
adequately monitor such a system.
Conversely, a well characterized system,
based on geological, hydrogeological,
and geotechnical investigations at the
reconfigured, is still integral to the overall closure
strategy. Further, SSLs have been detected in the
reconfigured northern region, which will require
monitoring and/or corrective action into the future.
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site, which has been demonstrated to be
simple, stable, and uniform would allow
for a fewer number of compliance wells
to capture the limited inherent
variability. In addition, factors related to
resolution and uncertainty also affect
the lateral well spacing appropriate to a
given site. In this regard it should be
noted that the Federal regulations
indicate clear expectations regarding
expected levels of resolution, which are
generally described as that necessary to
ensure that all potential contaminant
pathways in the entire uppermost
aquifer are monitored, including
preferential pathways. Uncertainties
and data gaps also equate to the need for
greater levels of monitoring than would
otherwise be required to compensate for
these deficiencies. In other words, if
characterization data are not available to
support a larger minimum lateral well
spacing, a default to a more rigid general
standard is needed, requiring more
wells. At the Ash Pond at Plant Gorgas,
a much smaller lateral well spacing is
needed to meet the requirements. This
is due to (1) The complexity of the
buried CCR; (2) The low resolution and
extreme uncertainties in the
characterization of the groundwater
flow system which encompasses the
unit; (3) The demonstrated complexity
of the geologic layering in the vertical
dimension; and (4) The presence of
significant localized fracturing and
numerous mapped faults which cut
through the unit and surrounding areas.
In a general sense, therefore, instead of
thousands of feet apart, monitoring well
spacings should have been on the order
of hundreds of feet, except where
known features such as narrow buried
erosional stream valleys or fracture
zones dictate even tighter lateral
spacing. For example, the lateral
spacings between wells MW–9, –10,
–11, and –12 ranges from roughly 700–
1,200 feet apart, yet none of these
monitoring wells were located
sufficiently close together to intersect
the mapped fracture which cuts through
this area of the site. A tighter well
spacing is needed to adequately
characterize the site. As another
example, many wells are screened in
zones which intersect underground coal
mines. These mine tunnels represent
potential preferential pathways which
should have been more intensively
monitored. The lateral and vertical
dimensions of these types of
underground workings are knowable
and should be factored into decisions
concerning appropriate monitoring well
spacings to effectively ensure these
preferential pathways are monitored.
Much smaller lateral and vertical wells
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spacings are necessary to meet the
requirements in this scenario, instead of
wells that are thousands of feet apart.
(2) Insufficient Number of
Downgradient Compliance Wells
Installed at Appropriate Depths To
Monitor the Entire Aquifer (Inadequate
Vertical Spacing)
EPA is also proposing to determine
that ADEM approved a GWMP that
lacked ‘‘a sufficient number of wells,
installed at appropriate locations and
depths’’ to ensure that all potential
contaminant pathways in the entire
uppermost aquifer are monitored. As
discussed above, the uppermost aquifer
contains at least four flow systems: (1)
the upper water table; (2) the Pratt Coal
seam; (3) the American Coal seam; and
(4) the Lower Pratt/Gillespy Transition
zone. A system of compliance wells that
meet the performance standards of
§ 257.91(a)(2) must be installed in each
of them. But none of the four flow
systems contain sufficient numbers of
wells to meet these standards.
Nearly all the compliance wells
installed in the three lower flow systems
were screened across the shallow coal
seams located between approximately
250 and 350 ft-MSL, i.e., in the Pratt
Coal seam and the American Coal seam.
Of the eight cross sections reviewed,89
it appears that only two downgradient
compliance wells were screened below
the coal seams in the Lower Pratt/
Gillespy Transition zone (GS–AP–MW–
6S and –6D). These wells are
downgradient due to the unit’s radial
flow at this depth, and two wells are
insufficient to comprehensively monitor
this portion of the uppermost aquifer.
First, all the monitoring wells installed
below the coal seams are focused along
the western and northern section of the
unit, leaving the northeastern,
southwestern, southern, and eastern
sections with little to no data in the
aquifer below the coal seams.
Conservatively, this means the lower
flow systems within the Lower Pratt/
Gillespy Transition for over half of the
pre-closure extent of the unit (at least
237 acres) are not being monitored.
This is further corroborated by the
cross-sections in Figures 11A, 14A, 15,
and 16 of the Groundwater Remedy
Selection Report, which document the
large portions of the uppermost aquifer
below the coal seams where no data
89 Anchor QEA. Prepared for Alabama Power
Company. Plant Gorgas Groundwater Remedy
Selection Report. December 2021. Figures 5A and
5B in the revised GWMP and Figures 9A thru 16
in the
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have been obtained.90 According to
Figure 14A, there appears to be only one
well cluster (GS–AP–MW–6S/6V/6D)
installed below the coal seams,
approximately 900 feet from the edge of
the ash pond immediately downgradient
of the current dam. Given the unit’s preclosure size of 474 acres and a vast
downgradient waste boundary
exceeding fourteen miles in length, this
single well cluster would certainly not
monitor all potential contaminant
pathways in this lower flow system.
There are also only 10 wells screened
in the upper water table (i.e., in the
unconfined materials above the coal
seams in the Cobb Group). As shown in
Figure 6A of the 2022 Semi-Annual
GWMCA Report, entitled Potentiometric
Surface Contour Map (Upper) Water
Table Aquifer, February 7, 2022, Plant
Gorgas Ash Pond, these 10 water level
monitoring points are installed over
hundreds of acres, only 7 of these are
designated as compliance wells, and
there is conflicting information between
the Permit Application and the most
recent Annual GWMCA Report from
2022 regarding the stratigraphic layers
in which these compliance wells are
screened. For example, the 2022 Annual
GWMCA Report only indicates that two
of these 7 wells are screened across the
‘‘shallow water table.’’ EPA therefore is
proposing to determine that the
compliance monitoring with respect to
the shallow unconfined water table
aquifer zone is not adequate to comply
with the regulations.
Similarly, based on the 2022 SemiAnnual GWMCA Report, 52 wells were
installed in the Pratt Group as a whole
across the entire 274-acre Ash Pond.91
Of these, based on the interpretation of
the flow system provided in the 2022
Semi-Annual GWMCA Report, water
levels were measured at 31 wells
installed in Pratt Coal seam,92 and water
levels were measured at 21 wells
screened in the American Coal seam.93
However, the compliance well network
listed in Table 1A in the Permit
Application indicates only 15
compliance wells screened in the Pratt
coal seam zone, and only 11 compliance
90 Id at pp 81, 83 of the revised Groundwater
Monitoring Plan and Figures 9A thru 16.
91 Monitoring wells screened in the Nickel Plate
coal seam are included in the Pratt Coal seam
category for this discussion.
92 Southern Company Services. 2022 SemiAnnual Groundwater Monitoring and Corrective
Action Report, Alabama Power Company, Plant
Gorgas Ash Pond. Prepared for Alabama Power
Company. July 31, 2022. Figure 6B, Potentiometric
Surface Contour Map, Pratt Aquifer, February 7,
2022.
93 Id at Figure 6C of the same report is entitled
Potentiometric Surface Contour Map, American
Aquifer,
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wells screened in the American Coal
seam.
Lastly, based on the interpretation of
the flow system provided in the 2022
Semi-Annual GWMCA Report, water
levels were measured and plotted for 15
wells to inform a representation of
potentiometric contours for the Base of
the Pratt—Gillespy transition zone.94
However, these 15 wells do not appear
to be screened in equivalent levels of
the transition zone and only 13 of these
are listed on Tables 1A (3 Wells), 1B (8
Wells), and 1C (2 wells) in the 2022
Semi-Annual GWMCA Report.
Moreover, not all of 13 wells were
included/depicted on Figure 6B 95 and
only 3 ‘‘Pottsville Fm—Gillespy zone
transition’’ wells are listed as
compliance wells on Table 1A in the
Permit Application. This lack of clarity
concerning the characterization and
monitoring of the transition zone
between the lower Pratt Group and
Gillespy Group, supports EPA’s basic
conclusion above, that the base of the
uppermost aquifer has not been
determined or sufficiently characterized
vertically (or laterally).
In summary, installing so few
compliance monitoring wells over such
great lateral distances and over such
significant vertical intervals cannot
possibly monitor all the potential
contaminant pathways at Plant Gorgas,
given the size of the Ash Pond as well
as the topographic and hydrogeologic
complexity of the site.
(3) Preferential Pathways Are Not
Monitored
Numerous preferential pathways have
been documented in the uppermost
aquifer under the Ash Pond. Yet under
the approved GWMP, none of these
significant potential contaminant
pathways appear to be adequately
monitored, despite the express
requirement in § 257.91(a)(2).
The approved GWMP states that,
‘‘Locally, Pratt Coal Group strata gently
dip (0.5° to 1.0°) to the south and southsouthwest. Figure 5A Geologic CrossSection A–A’ and Figure 5B Geologic
Cross-Section B–B’ illustrate the
geologic layering beneath the site.’’ It is
immediately apparent from these cross
sections that a simple, nearly flat series
of geologic layers is an overly simplistic
representation of the site. As has been
noted in many reports from Alabama
Power in the permit record, the geologic
layering is disrupted in many locations
by mappable faults which indicate
94 Id at inset map on Figure 6B entitled,
Generalized Potentiometric Surface Contour Map—
Base of Pratt to Gillespy Transition (North of Dam).
95 Id.
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significant displacement and have
steepened dips resulting in folding in
some areas of the subsurface.
Nevertheless, the monitoring network
does not include monitoring wells with
screens deliberately targeted to these
mapped faults and associated fractures.
Given the presence of these significant
fault zones, some of which have been
mapped and delineated within the
aquifer, additional monitoring wells
should have been installed to detect
whether CCR contaminants are
migrating beyond the unit boundaries in
pathways that follow these fracture
lines. As an illustrative example, as
shown on Figures 7A, 7B, 8A and 8B of
the 2022 Semi-Annual GWMCA Report,
a series of north-northwest striking
fractures with steep dips to the west cut
through the unit. One such fracture is
mapped from the region of MW–10R
north-northwestward 3600 feet (over
half a mile) to the Mulberry Fork and
beyond, further to the north-northwest.
Monitoring wells MW–12 and 12V are
located hundreds of feet to the east of
the fault and therefore did not intersect
it. Similarly, MW–11 is too far away
from the feature and too shallow, so it
also failed to intersect the feature.
Ultimately it does not appear that any
monitoring wells effectively monitor
this significant potential contaminant
pathway, which is particularly
problematic as the fault appears to
intersect the river in the general
downgradient direction and thus has the
(unassessed) potential to directly
discharge CCR-related contaminants to
the river system. This natural fracturecontrolled ‘‘pipeline’’ represents a likely
conduit for preferential groundwater
flow which follows the strike of the
fracture and thus represents a
significant, unmonitored, potential
contaminant pathway. It is notable that
none of these identified fractures are
included on Figure 5, Monitoring Well
Location Map Plant Gorgas Ash Pond, of
the same report.
Additional preferential pathways are
associated with underground mine
workings which impinge on parts of the
unit. Coal mining operations, including
underground workings, are also well
documented in the vicinity of the site,
and coal beds have been generally
targeted for most of the monitoring well
installations. But while some
monitoring points appear to be screened
at the same horizon as these
underground mine workings, their
lateral extent in the subsurface remains
unknown, and as such the potential for
preferential pathways which exploit
these zones represents a clear data gap.
For example, the geologic cross sections
included in the 2021 Plant Gorgas
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Annual GWMCA Report indicate the
presence of former mine shafts that
could significantly impact groundwater
flow, and therefore warranted additional
characterization and focused
monitoring. These pathways were also
documented in the December 2021
Remedy Selection Report, which ADEM
received 3 months prior to its issuance
of the Plant Gorgas permit in February
2022. In addition, according to the cross
section in Figure 5A in the revised
GWMP and Figure 12A in the
Groundwater Remedy Selection Report,
at least one fault that could serve as a
potential preferential pathway for
groundwater has been mapped
immediately adjacent to the Ash Pond
and penetrates below the coal seams. It
is therefore another significant failure of
the approved groundwater monitoring
system that it does not include wells to
monitor the targeted and delineated
contaminant pathways that follow coal
seams, underground workings, or other
natural and/or man-made features that
can act as preferential pathways for
groundwater and contaminant
migration. See 40 CFR 257.91(a)(2). The
significance of ADEM’s failure to
address this deficiency is illustrated by
the numerous and documented SSIs and
SSLs detected in the monitoring wells
which are screened within the coal
layers.
In summary EPA is proposing to
determine that the groundwater
monitoring network ADEM approved for
the Ash Pond at Plant Gorgas falls far
short of the performance standards in
§ 257.91(a) and (b). The uppermost
aquifer has not been sufficiently
characterized or monitored. In
particular, the lower limits of the
uppermost aquifer and hydraulically
connected aquifers beneath it have not
been defined. Compliance monitoring
wells have not been located at the waste
boundary in most locations. There are
an insufficient number of monitoring
wells along the perimeter of the
downgradient waste boundary, and at
insufficient depths, to monitor all
potential contaminant pathways in the
entire uppermost aquifer, given the
potential for radial flow in deeper
aquifer zones. Finally, numerous
preferential pathways have not been
monitored.
ADEM’s permit does include a permit
condition that states:
The Permittee shall install and maintain
additional groundwater monitoring wells as
necessary to assess changes in the rate and
extent of any plume of contamination or as
otherwise deemed necessary to maintain
compliance with [ADEM Admin. Code] 335–
13–15–. 06. A plan in the form of a permit
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modification request should be submitted to
the Department as required by Section V.D.
55267
It appears the permit record (Final
Permit and RTC) may not reflect all the
relevant information about the status of
corrective actions at Plant Gorgas that
was available to ADEM when the permit
was issued. According to Alabama
Power ‘‘[a] Groundwater Remedy
Selection Report was prepared and
submitted on December 17, 2021, to
meet the requirements of 40 CFR 257.97,
ADEM Admin. Code r. 335–13–15–
.06(8), and Part C of ADEM
Administrative Order AO 18–096–GW
. . .’’.98 The remedy the facility selected
for the Ash Pond, Gypsum Pond, and
Bottom Ash Landfill consists of closure
with waste in place and capping,
permeation grouting at the Ash Pond,
and MNA. Additionally, any comments
that may have been provided by ADEM
to Alabama Power on the 2020 ACM
were not available for review.
The Plant Gorgas Final Permit
contained the same recitation of the
corrective action regulations as the other
permits issued by ADEM. As with the
others, incorporating the regulations
verbatim in the permit does not require
Alabama Power to achieve compliance
with those requirements at Plant Gorgas.
Here as well, it appears that ADEM did
not take into account relevant facts
about the status of corrective action at
Plant Gorgas, such as whether the 2020
revised ACM or the selected remedy
submitted to ADEM in December 2021
complied with the regulatory
requirements. Most importantly, ADEM
did not determine what actions are still
necessary in light of those facts to
achieve compliance with the regulations
and include those actions as
requirements in the Final Permit.
Instead, two months later, ADEM issued
a Final Permit that was silent on the
adequacy of the revised ACM and the
applicant’s selected remedy. Over a year
later, it does not appear that ADEM has
evaluated the adequacy of the revised
ACM and the applicant’s selected
remedy. As a consequence, EPA is
proposing to determine that, by
remaining silent, the permit in essence
authorized Alabama Power to continue
to pursue a remedy based on the results
of an ACM that does not meet the
requirements of § 257.96, even though
the selected remedy does not appear to
meet the requirements in § 257.97(b),
and the ACM identified other measures
that would meet those requirements.
Delaying a decision on the adequacy
of the facility’s selected remedy until
some unspecified point after permit
issuance 99 effectively allows Alabama
Power to continue operating out of
compliance with the regulations, while
operating in compliance with the
permit. Releases continue to migrate offsite during this delay, and in this case,
it appears the contamination may have
already migrated off-site to residential
96 Anchor QEA. Assessment of Corrective
Measures, Plant Gorgas. Prepared for Alabama
Power Company. June 2019 (Revised: February
2020).
97 Alabama Department of Environmental
Management. Initial Permit and Variance, William
C. Gorgas Electric Generating Plant, Permit No. 64–
12, Public Commenters. February 28, 2022.
98 Southern Company Services 2022 Annual
Groundwater Monitoring and Corrective Action
Report, Alabama Power Company Plant Gorgas Ash
Pond. Prepared for Alabama Power Company.
February 1, 2023. p 2.
99 It appears that ADEM has still not evaluated
either the revised 2020 ACM or Alabama Power’s
selected remedy.
However, this condition does not
actually require any action that will
bring the groundwater monitoring
system into compliance; for example, by
requiring the facility to fully
characterize the uppermost aquifer
system or install additional monitoring
wells at the waste boundary. Or, more
broadly, it does nothing to compel the
facility to meet the requirements in 40
CFR 257.91(a) and (b).
c. Plant Gorgas Corrective Action Issues
In November 2018, the first SSLs
above a groundwater protection
standard were detected at the Gorgas
Plant. SSLs were reported for lithium,
arsenic, and molybdenum. The Ash
Pond reported SSLs of all three
constituents; the Gypsum Pond, CCR
Landfill, and Gypsum Landfills reported
SSLs of lithium only; and the Bottom
Ash Landfill reported SSLs of arsenic.
One ACM was developed for all the
units at the facility in June 2019 and
revised in February 2020 (‘‘revised
ACM’’).96 On February 28, 2022, ADEM
issued a Final Permit to Alabama Power
for Plant Gorgas Ash Pond, Gypsum
Pond, and Bottom Ash Landfill.
In the RTC for the Gorgas Final
Permit,97 ADEM states:
In November of 2019, the Department
provided extensive comments to Alabama
Power related to the submitted ACM and
proposed final remedy. The Department’s
comments addressed many of the concerns
raised by commenters, including the
selection of monitored natural attenuation
(MNA) as the final remedy despite providing
limited data to its efficiency as a remedy. To
date, Alabama Power has not submitted a
revised ACM, as the facility has been
collecting additional data to support a final
remedy proposal.
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property.100 101 The sanctioned delay in
implementing an effective remedy with
no schedule for compliance results in a
permit program that is less protective
than the Federal regulations.
EPA is proposing to determine that
the Final Permit contains many of the
same issues discussed with respect to
the other permits. The Final Permit does
not contain a deadline for correction
and resubmittal of the ACM to address
any of the deficiencies ADEM identified
in its 2019 comments, or any response
to Alabama Power’s selected remedy.
EPA has also identified deficiencies in
the revised ACM beyond those ADEM
discussed in the RTC.
i. The Plant Gorgas Final Permit Does
Not Require Collection of Site Data
Needed To Support Assessments in the
ACM
As discussed previously,
§ 257.95(g)(1) requires a facility to
characterize the nature and extent of the
release and any relevant site conditions
that may affect the remedy ultimately
selected. The characterization must be
sufficient to support a complete and
accurate assessment of the corrective
measures necessary to effectively clean
up all releases from the CCR unit
pursuant to § 257.96.
The revised ACM identified MNA as
a corrective measure to address
groundwater contamination, in addition
to other corrective measures (e.g.,
hydraulic control and treatment; in-situ
treatment). The revised ACM delineates
releases of lithium, arsenic, and
molybdenum but does not characterize
the site conditions that would affect
Alabama Power’s selected remedy of
MNA. Although the ACM identifies a
number of potential attenuation
mechanisms that might be effective for
arsenic, lithium, and molybdenum, the
ACM does not demonstrate that any of
these mechanisms occur on site. EPA
was unable to locate any data
confirming that any of those potential
attenuation mechanisms are occurring at
Plant Gorgas. For example, this could
include testing for the presence and
quantity of lithium detected in the
aquifer matrix solids to demonstrate that
the constituent is being removed from
the groundwater and immobilized onsite. But no site data were discussed in
the ACM.
The subsequent Remedy Selection
Report also fails to contain the
necessary site data. Although the
100 Alabama Power. Letter to Mr. Taylor. Alabama
Power Plant Gorgas Ash Pond Closure and
Groundwater Investigations. July 6, 2020.
101 Alabama Power. Letter to Mrs. Salter. Alabama
Power Plant Gorgas Ash Pond Closure and
Groundwater Investigations. October 30, 2020.
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Report, like the ACM, identifies a
number of potential attenuation
mechanisms that might be occurring onsite for arsenic, lithium, and
molybdenum, the Report does not
conclude that any of these mechanisms
occur on-site. Some site data that were
not available in the ACM are discussed
in Section 5.3 of the Remedy Selection
Report, but they do not demonstrate that
any significant amount of lithium,
molybdenum, or arsenic is being
immobilized in the ‘‘solids’’ samples,102
(e.g., aquifer matrix) or otherwise
confirm the presence of attenuated
constituents in the aquatic matrix. The
Report identifies only dispersion and
dilution as an MNA mechanism that
currently occurs at Plant Gorgas.
Ultimately none of the data presented
support selection of MNA as a primary
remedy.
Site data would also be needed to
support any assessment of the
performance, reliability, ease of
implementation, and the time required
to begin and complete the remedy must
also be assessed and supported with site
characterization data and analysis. 40
CFR 257.96(c)(1) and (2). But the Final
Permit issued by ADEM requires neither
the collection of data, or any revisions
to the ACM, or any change in the
facility’s selected remedy to address
these deficiencies.
ii. The Final Permit Does Not Require
Submission of a Revised ACM That
Accurately Assesses MNA
In the revised ACM, Alabama Power
acknowledges that, ‘‘USEPA (2015)
discourages using dilution and
dispersion as primary MNA
mechanisms, as these mechanisms
disperse contaminant mass rather than
immobilize it.’’ 103 ADEM also raised
this as a concern in its 2019 comments
on the original ACM.104 However, as
noted neither the revised ACM or the
Remedy Selection Report identifies any
natural attenuation mechanisms other
than dilution and dispersion that have
been demonstrated to be occurring onsite: ‘‘The performance of MNA requires
further investigation, especially related
to the identification of an attenuating
mechanisms, capacity of the Pottsville
Formation for attenuation, and time to
102 Anchor QEA. Prepared for Alabama Power
Company. Plant Gorgas Groundwater Remedy
Selection Report. December 2021. Tables 6 and 12
in Appendix D.
103 Anchor QEA. Assessment of Corrective
Measures, Plant Gorgas. Prepared for Alabama
Power Company. June 2019 (Revised: February
2020). p. 14.
104 Alabama Department of Environmental
Management. Response to CCR Documents
Submitted to the Department. Alabama Power
Company. November 14, 2019.
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achieve GWPS.’’ 105 This investigation
was not completed prior to completion
of the ACM. Regardless, Alabama Power
assessed the performance of MNA as
‘‘medium’’ based on the dilution and
dispersion (i.e., releases of
contaminants) occurring on-site and the
identification of potential attenuation
mechanisms.
Such a favorable assessment of MNA
is contrary to the requirement in
§ 257.97(b)(4) that ‘‘[r]emedies must
. . . [r]emove from the environment as
much of the contaminated material that
was released from the CCR unit as is
feasible.’’ As previously discussed,
while MNA can reduce the
concentration or mobility of inorganic
contaminants in groundwater if
immobilization occurs through
adsorption or absorption to subsurface
soils, it does not remove the
contaminants from the environment.
MNA, therefore, would not perform well
with respect to the requirement in 40
CFR 257.97(b)(4). This is particularly
true in this circumstance, where
Alabama Power has failed to collect the
site data needed to identify whether any
naturally occurring attenuation may be
occurring on-site, as well as the
mechanism by which it occurs, and to
assess whether site characteristics that
control and sustain this naturally
occurring attenuation are sufficient to
immobilize the entire release. Because
the revised ACM presents no
information that MNA would meet these
requirements, the ACM should have
assessed MNA’s performance and
reliability as ‘‘low.’’
Similarly, in order for MNA through
immobilization to be assessed favorably
with respect to its reliability at meeting
the other requirements in § 257.97(b),
such as the requirement in
§ 257.97(b)(2) to attain groundwater
protection standards, the chemical
reactions and processes involved that
achieve immobilization must be
demonstrated to be present on site and
be permanent. Immobilization that is
not permanent could be reversed,
causing contaminants to be released
back into groundwater and to migrate
off-site. Yet despite the absence of any
data demonstrating immobilization
mechanisms to be present, let alone
permanent, the revised ACM assessed
the reliability of MNA through
immobilization as ‘‘high.’’ This
conclusion is unsupported; since no
immobilization mechanisms were
105 Anchor QEA. Assessment of Corrective
Measures, Plant Gorgas. Prepared for Alabama
Power Company. June 2019 (Revised: February
2020). p. 17.
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demonstrated to be present, they could
not be known to be reliable.
The revised ACM also fails to
consider safety impacts, cross-media
impacts, and control of exposure to any
residual contamination in its assessment
of MNA. See 40 CFR 257.96(c)(3).
Neither the narrative nor Table 5 in the
2020 ACM discuss these impacts for
MNA. Yet Table 5 in the 2020 ACM, in
the column labeled ‘‘potential impacts
of remedy’’ nevertheless concludes that
the potential impacts from MNA are
‘‘none.’’ This conclusion is unsupported
by data or analysis. This conclusion is
also inconsistent with other information
in the revised ACM. The Ash Pond and
Bottom Ash Landfill are both adjacent to
a river. In the revised ACM in Figure 3,
groundwater flow is depicted from the
Ash Pond toward the river. The Bottom
Ash Landfill is also near and upgradient
from an adjacent river. As noted, the
only MNA that is known to occur at the
site is dilution and dispersion (i.e., the
normal transport associated with
groundwater releases.) This means that
contaminants are migrating in
groundwater from the Ash Pond to the
river. Migration of contamination from
groundwater to surface water is a crossmedia impact. Therefore, the assessment
of potential impacts from the remedy for
MNA in Table 5, which includes these
cross-media impacts, should be ‘‘high.’’
Conclusions without a supporting
assessment or data do not constitute ‘‘an
analysis of the effectiveness of potential
control measures.’’ 40 CFR 257.96(c)
(emphasis added). In addition, the lack
of data to support the assessments in the
revised ACM means it may not
accurately reflect MNA’s ‘‘effectiveness
in meeting all of the requirements and
objectives’’ in § 257.97(b). Inaccurate
assessments in an ACM can ultimately
result in selection of a remedy that will
not meet the requirements of
§ 257.97(b), which is what appears to be
occurring here.
In an ACM, technologies’ expected
performances are compared with one
another according to how well each
alternative meets each regulatory
criterion. The Revised ACM identified
MNA as one of several potential
corrective measures to address
groundwater contamination (i.e.,
hydraulic control and treatment; in-situ
treatment). Given both the absence of
any evidence of any attenuation
mechanisms occurring at the Ash Pond,
and the conclusion in the revised ACM
that the other alternatives, such as
pump and treat, are feasible, there
would appear to be no basis for
assessing MNA more favorably than an
alternative that unquestionably removes
contaminants from the environment. For
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the same reasons, there is no apparent
basis for ultimately selecting MNA as
the remedy.
ADEM’s Final Permit contains no
measures to remedy this, even though in
their 2019 comments on the original
ACM, ADEM raised many of the same
issues discussed above. For example,
ADEM requested that Alabama Power
update the ACMs to include detailed
information for each requirement. In
particular, the comments noted that:
Furthermore, ADEM Admin. Code r. 335–
13–15-.06(8)(b)3. and (b)4. require that the
remedy must (1)’’ control the source(s) of
releases so as to reduce or eliminate, to the
maximum extent feasible, further releases of
constituents in Appendix IV into the
environment’’ and (2) ’’ remove from the
environment as much of the contaminated
material that was released from the CCR unit
as feasible . . .’’.The ACMs evaluate a
number of options, with source control (by
consolidating and capping the CCR units)
and monitored natural attenuation (MNA)
proposed as the most effective remedy. The
Department requests a more detailed
justification for the proposed remedies given
that source control will not be achieved for
an average of 10 years and that no other
mechanism is proposed to reduce the
potential for further releases to the’’
maximum extent feasible’.
EPA was unable to find any evidence
that a revised ACM or a more detailed
justification was submitted in response
to ADEM’s concerns. By failing to
require Alabama Power to take any
concrete action to address these
deficiencies, the Final Permit effectively
authorizes the permittee to continue to
indefinitely pursue a remedy that
ADEM previously determined had not
been demonstrated to meet the
requirements in § 257.97(b).
Accordingly, EPA is proposing to
determine that the permit does not
require Alabama Power to achieve
compliance with the Federal
requirements; and because it allows the
facility to continue to delay
implementing a remedy that would
meet the requirements of § 257.97, the
alternate State requirement is less
protective.
4. Plant Greene County
EPA reviewed the Final
Determination Initial Permit and
Variance for the Alabama Power
Company, Greene County Electric
Generating Plant (Plant Greene County
Permit), issued by ADEM under Permit
No. 32–03 on December 18, 2020.106
The permit summary on Page 1 says,
106 Alabama Department of Environmental
Management. Final Determination Initial Permit
and Variance for the Alabama Power Company,
Greene County Electric Generating Plant, issued
under Permit No. 32–03. December 18, 2020.
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[t]he Plant Greene County Ash Pond is a CCR
surface impoundment located in Sections 21
and 28, Township 19 North, Range 3 East in
Greene County, Alabama consisting of
approximately 559.41 acres with a disposal
area that consists of approximately 477.24
acres. The permit requires the Permittee to
manage CCR in accordance with the
conditions of the permit, ADEM Admin.
Code r. 335–13–15, ’’ Standards for the
Disposal of Coal Combustion Residuals in
Landfills and Surface Impoundments,’’ and
the approved permit application.
. . .
The Permittee must comply with all
conditions of the permit except to the extent
and for the duration such noncompliance is
authorized by a variance granted by ADEM.
The first variance requests to exclude boron
as an Appendix IV assessment monitoring
constituent. The second variance requests
groundwater protection standards of 6
micrograms per liter (mg/L) for cobalt; 15 mg/
L for lead; 40 mg/L for lithium; and 100 mg/
L for molybdenum. The third variance
requests the final grade of the cover system
be less than 5 percent and greater than 25
percent. The fourth variance being requested
is from 335–13–15-.03(6) requiring a 100 foot
buffer from the perimeter of the facility
boundary.
As with the other permits evaluated
in this proposal, EPA has identified
issues with ADEM’s approval of the
closure, groundwater monitoring
network, and corrective action at Plant
Greene County, which are discussed
below. As previously discussed, EPA
focused on only a subset of the potential
issues associated with the permit and
limited its review to information in the
permit record (e.g., the Permit
Application) and information publicly
available on Alabama Power’s CCR
website. This is because the purpose of
this review is to determine whether
Alabama’s program meets the statutory
standard for approval, not to reach final
conclusions about an individual
facility’s compliance with the CCR
regulations.
a. Plant Greene County Closure Issues
Plant Greene County had not
completed closure of the Ash Pond
when ADEM issued the Final Permit in
December 2020. But the final permit
ADEM issued looks largely the same as
the permits issued to the other facilities.
ADEM incorporated the Alabama CCR
regulations by reference into the Final
Permit for Plant Greene County, and it
approved and incorporated the Closure
Plan submitted as part of the application
into the Final Permit without
modification.107 The Final Permit
provides:
107 Although the Permit terms are ambiguous, it
appears from the Response to Public Comment that
ADEM approved the Closure Plan submitted as part
of the Permit Application.
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SECTION VII. CLOSURE AND POSTCLOSURE REQUIREMENTS.
A. Closure Timeframe and Notifications. The
Permittee shall close their CCR units as
specified in 335–13–15–07(2), this permit
and the Application.
B. Criteria for Closure.
1. Cover. Closure of a CCR landfill, surface
impoundment, or any lateral expansion of a
CCR unit must be completed by either
leaving the CCR in place and installing a
final cover system or through removal of the
CCR and decontamination of the CCR unit, as
described in 335–13–15-.07(3)(b) through (j).
The minimum and maximum final grade of
the final cover system may be less than 5
percent and greater than 25 percent, as
specified in the Permit Application. (See
Section IX.C.)
2. Written Closure Plan. The written closure
plan, as part of the Application, must
include, at a minimum, the information
specified in 335–13–15-.07(3)(b)1.(i) through
(vi).
3. Initiation of Closure Activities. Except as
provided for in 335–13–15-.07(3)(e)4 and
335–13–15-.07(4), the owner or operator of a
CCR unit must commence closure of the CCR
unit no later than the applicable timeframes
specified in either 335–13–15-.07(3)(e)l or 2.
4. Completion of closure activities. Except as
provided for in 335–13–15-.07(3)(f)2, the
owner or operator must complete closure of
the CCR unit subject to the requirements in
335–13–15–.07(3)(f)l.(i) through (ii).
According to the Closure Plan
submitted with the Permit Application,
Alabama Power intends to remove CCR
from the southern portion of the Ash
Pond and consolidate it within the
northern portion of the existing ash
pond.108 After the excavation and
consolidation have been completed, the
footprint of the remaining waste will
occupy approximately 221 acres. The
Plan calls for the 221 acres of
consolidated waste to be closed in
place, with a final cover system
consisting of an engineered synthetic
turf and geomembrane to be installed on
the consolidated unit. In addition,
according to the Plan, a barrier wall
keyed into the low permeability
Demopolis Chalk will be installed
around the perimeter of the
consolidated CCR material to create a
hydraulic barrier that ‘‘limits the
movement of interstitial water through
the constructed interior dike and
existing northern dike.’’ 109 This
hydraulic barrier will be connected to
the geomembrane of the final cover
system.110 According to the Closure
Plan:
108 Alabama Power Company. Revised Closure
Permit Application for the Plant Greene County Ash
Pond. April 30, 2020. Appendix 9, p 3, 18–19.
109 Id. p.16.
110 Additional details regarding the barrier wall
system are provided in the Permit Application in
Appendix 6 and Appendix 7, entitled ‘‘Draft—
Construction Quality Assurance Plan.’’ Although
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These actions will effectively control the
source of CCR constituents to groundwater by
removing free water and some interstitial
water from the ash, reducing the footprint
area of the ash and preventing further
infiltration of surface water resulting from
rainfall through the ash. Removal of the free
liquid will reduce the volume of water
available to flow from the Ash Pond during
and after closure, while also minimizing the
hydraulic head driving water through the
subsurface.111
In many respects, the outlines of the
closure presented in the Plan could be
implemented to be consistent with the
Federal requirements; however, ADEM
approved the Plan without requiring
Alabama Power to provide the
information necessary to confirm that
several critical closure requirements—
which were not addressed or were
insufficiently described—would be met.
Specifically, neither the Closure Plan
nor other materials in the Permit
Application addressed how the
performance standards in
§ 257.102(d)(2) will be met with respect
to the saturated CCR that it appears will
remain in the base of the consolidated
unit. The Permit could either have
specified what the facility needs to do
to meet the requirements, or ADEM
could have required the facility to
submit a revised Closure Plan. ADEM
did neither, and as a consequence, there
is no binding and enforceable provision
for the facility to comply with these
performance standards. In essence,
ADEM has issued a permit that allows
the facility to decide whether to comply
with § 257.102(b) and (d)(2), rather than
‘‘requiring each CCR unit to achieve
compliance with’’ those provisions. 42
U.S.C. 6945(d)(1).
While it was in operation, the base of
the Ash Pond was in continuous contact
with the groundwater beneath the unit.
Even now groundwater continues to
saturate the CCR in the unit.112 EPA
estimated the amount of saturated CCR
remaining in the Ash Pond using the
same methodologies described above for
Plants Colbert and Gadsden. The
average groundwater elevation from
groundwater monitoring wells in the
vicinity of the Ash Pond between
September 2019 and August 2021 is
84.8 ft above MSL. While the base
the drawings are marked with statements such as
‘‘60 Percent Design Package’’ or ‘‘Issued for 60%
Client Review,’’ and the Construction Quality
Assurance Plan is marked ‘‘Draft,’’ it appears that
ADEM approved these materials with the permit
condition directing the Permittee to close their CCR
units ‘‘as specified in the Application.’’
111 Alabama Power Company. Revised Closure
Permit Application for the Plant Greene County Ash
Pond. April 30, 2020. Appendix 9, p 19.
112 Alabama Power Company. Revised Closure
Permit Application for the Plant Greene County Ash
Pond. April 30, 2020. GWMP pp 220–221.
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elevation for the unit varies, by relying
on an average base elevation of 83 feet,
EPA estimates that, on average, just
under 2 feet in depth of CCR across the
entire footprint of the impoundment is
currently in contact with groundwater.
This equates to roughly 640,000 CY of
saturated waste. Dewatering and pool
drawdown continue at the site, and
when combined with the installation of
the slurry wall, groundwater elevations
would be expected to decrease over
time. However, the extent to which the
CCR will remain saturated once closure
activities are completed cannot be
estimated due to the lack of information
in the relevant documents.
As discussed previously, the Federal
regulations applicable to surface
impoundments closing with waste in
place require that ‘‘[f]ree liquids must be
eliminated by removing liquid wastes or
solidifying the remaining waste and
waste residues, [and that] remaining
wastes must be stabilized sufficient to
support final cover system.’’ 40 CFR
257.102(d)(2). But due to the
deficiencies in the Closure Plan, it is not
clear that the closure approved by
ADEM will meet either standard.
According to the approved Closure
Plan, various dewatering techniques
will be employed before and during
closure; however, the Closure Plan
appears to limit the use of these
techniques to the CCR in the southern
portion of the unit that will be
excavated and transported to the
consolidated area, and to the areas
under the new dike.113 For example, in
the sections specifically discussing
dewatering, the Closure Plan states:
i. Dewatering
Dewatering of the CCR Ponds consists of two
phases: decanting of free water and
dewatering of interstitial water within the
CCR material. Dewatering will be required
prior to ash excavation and throughout
construction. . . .
Interstitial dewatering refers to the removal
of subsurface water within the saturated CCR
material. This dewatering requires lowering
phreatic water levels to improve material
handling for excavation and transport.
Removal of interstitial water will likely
require both passive and active methods of
drainage.
*
*
*
*
*
The CCR material within the subgrade of the
proposed interior dike will be over excavated
and a stable, temporary slope formed to the
interior to allow the dike and barrier wall to
be constructed. During this time, the
subgrade beneath the new dike will be
dewatered (discussed in a following section).
*
*
*
*
*
113 Alabama Power Company. Revised Closure
Permit Application for the Plant Greene County Ash
Pond. April 30, 2020. Appendix 9, pp 5,7, and 9.
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As dewatering continues, CCR material will
be excavated from the closure by removal
areas and placed and compacted in
horizontal lifts on top of the existing CCR
material within the consolidation area.
As discussed previously, the CCR material
will be dewatered in a systematic fashion
prior to and during excavation activities, to
maintain the phreatic surface below the
working elevation of removal operations. For
construction of the closed ash pond, it is
expected that the CCR material will be
handled multiple times prior to final
placement and closure of the pond. CCR
material will be stacked and dewatered to the
proper moisture content prior to placement
in the consolidation area.
(emphasis added).114 The Closure Plan
lacks the required description of how—
or even whether—Alabama Power
intends to dewater the entire unit. For
example, there are inconsistent
statements in the Closure Plan about the
scope of the dewatering activities
Alabama Power intends to conduct. In
one section, there is a reference to
‘‘dewatering of wetter ash across the
site, especially in the southern end of
the pond.’’ But the remainder of the
discussion focuses on a technique that
is unlikely to be used on CCR that is not
intended to be excavated and
transferred, which suggests that
Alabama Power does not intend to fully
dewater all of the CCR in the unit.
Specifically, the Closure Plan states
that:
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Utilization of stacking & casting methods is
anticipated. With this approach, ash with
higher moister[sic] content will be excavated
and stacked in piles to allow for gravity
drainage. A similar technique of windrowing
may be used throughout the site. This
technique involves spreading the wet ash in
thin lifts and rowing/tilling the ash to allow
the moisture to evaporate from the surface.
To expedite interstitial water dewatering and
construction stormwater management, a
capillary break drainage system may also be
considered for the ash excavation/placement
around the interior dike. The drainage system
will help relieve pore water pressure in the
underlying ash as the weight of earthwork
filling is applied.
This is compounded by the Closure
Plan’s repeated references to the
removal of ‘‘free water,’’ rather than the
‘‘free liquids’’ the Federal regulations
specify must be eliminated.115 For
example, on pages 18–19, under the
heading ‘‘f. Achievement of Closure
Performance Standards,’’ the Closure
Plan states:
Free water will be removed, and interstitial
water will be lowered to accomplish the CCR
114 Alabama Power Company. Revised Closure
Permit Application for the Plant Greene County Ash
Pond. April 30, 2020. Appendix 9, pp 7–8.
115 Alabama Power Company. Revised Closure
Permit Application for the Plant Greene County Ash
Pond. April 30, 2020. Appendix 9, pp 5, 7–8, 19.
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removal from the closure by removal areas
and to close in a consolidated footprint.
*
*
*
*
*
These actions will effectively control the
source of CCR constituents to groundwater by
removing free water and some interstitial
water from the ash, reducing the footprint
area of the ash and preventing further
infiltration of surface water resulting from
rainfall through the ash.
(emphasis added). Alabama Power has
defined the term ‘‘free water’’ in other
Closure Plans as ‘‘water contained in the
CCR unit above the surface of CCR
material.’’ 116 Compare, 40 CFR 257.53
(definition of ‘‘free liquids’’).
Moreover, the Closure Plan never
refers to the groundwater within the
northern portion of the unit or describes
any engineering measures that will be
implemented to remove these liquids.
Based on the information provided,
further engineering measures would be
necessary to effectively eliminate these
free liquids from the unit prior to
installing the final cover system,
required by § 257.102(d)(2)(i). Absent
further data demonstrating that
saturated CCR will not be present in the
base of the closed unit prior to the
installation of the final cover system,
the permit record does not support a
finding that the remaining wastes will
be stabilized sufficiently to support the
final cover system, as required by
§ 257.102(d)(2)(ii). If the CCR in the unit
is not sufficiently stabilized, e.g., if it
has not been completely drained prior
to the installation of the final cover
system, differential settlement of the
CCR after installation of the cover
system is possible, especially given the
substantial added load from the
consolidation of CCR from the southern
portion of the Ash Pond. If the
settlement is great enough it could cause
a disruption in the continuity, and
potentially failure, of the final cover
system. Additional information is
needed to determine that the permit
meets Federal requirements. This could
have been accomplished either by
requiring submission of the information
prior to the issuance of the permit or by
including a permit term requiring
submission of the information, along
with a clause allowing for further permit
conditions if necessary.
Based on all of the above, EPA is
proposing to determine that, by failing
to resolve these issues, ADEM’s permit
does not require the Plant Greene
County Ash Pond to achieve compliance
with the Federal requirements for
closure, or with alternative closure
116 See, e.g., Alabama Power Company. Revised
Closure Plan for the Plant Gorgas Ash Pond.
Appendix 11, p 7.
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requirements that are at least as
protective as the Federal requirements.
b. Plant Greene County Groundwater
Monitoring Issues
Based on EPA’s review of the
approved groundwater monitoring well
network, EPA is proposing to determine
that ADEM approved a groundwater
monitoring system that fails to meet the
Federal requirements. As previously
discussed, the Federal regulations
specify that a groundwater monitoring
system must be installed that ‘‘consists
of a sufficient number of wells, installed
at appropriate locations and depths, to
yield groundwater samples from the
uppermost aquifer that accurately
represents the quality of the
groundwater passing the waste
boundary of the CCR unit.’’ 40 CFR
257.91(a)(2). The regulations further
specify that ‘‘[a]ll potential contaminant
pathways must be monitored.’’ Id. But
as discussed in more detail below, EPA
is proposing to determine that ADEM
approved a groundwater monitoring
plan with an insufficient number of
wells laterally along the perimeter of the
unit to monitor all contaminant
pathways. EPA is also proposing to
determine that monitoring wells in the
approved plan were not installed at
appropriate depths to ensure that all
contaminant pathways in the entire
uppermost aquifer were monitored.
These are essentially the same issues
previously discussed with respect to
Plants Gadsden and Gorgas.
i. Insufficient Number of Downgradient
Compliance Wells Installed at
Appropriate Depths To Monitor the
Entire Aquifer (Inadequate Vertical
Spacing)
The downgradient well network
approved by ADEM was focused
primarily on a narrow subset of the
uppermost geologic layers within what
is referred to in the Permit Application
as Unit 2: Poorly Graded Sands With
Gravel Lenses. Other interconnected
portions of the uppermost aquifer are
not being monitored as discussed below.
When evaluating whether monitoring
wells are installed at appropriate depths
(i.e., the adequacy of vertical monitoring
well coverage), it is important to look at
cross-sectional views of the entire
uppermost aquifer in the vertical
dimension to understand
interrelationships of groundwater
monitoring wells, screen depths, and
lithological variations. These points are
illustrated (in part) in the geologic crosssections on Figures 5A and 5B included
on pages 208 and 209 of the Permit
Application, which show that the
uppermost aquifer consists of layers of
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poorly graded sands with gravel lenses
(identified as Unit 2), as well layers of
lean clay to sandy clay (identified as
Unit 1). These cross sections and the
boring logs that were included in the
Permit Application confirm that the two
geologic formations are hydraulically
interconnected and both are therefore
the ‘‘uppermost aquifer.’’ See, 40 CFR
257.53 (defining uppermost aquifer to
include lower hydraulically connected
aquifers). Accordingly, monitoring wells
must be installed in the two formations.
Nearly all of the compliance wells at
the waste boundary of the unit are
screened in Unit 2, well below (in some
cases over 20 feet below) the top of the
uppermost aquifer; as a consequence
there are an insufficient number of wells
across nearly all of Unit 1. More
precisely, EPA found that the
groundwater monitoring well network
for the Ash Pond unit has an
insufficient number of wells screened in
Unit 1 (i.e., a vertical data gap) along at
least three sides, as follows: (1) a 1500foot section of Unit 1 parallel to the
Barge Canal, as shown on Figure 4A,
entitled ‘‘Geologic Cross Section A–A′
Plant Greene County Ash Pond’’; (2) a
6000-foot section of Unit 1 along the
western side of the unit, as shown on
Figure 4B, entitled ‘‘Geologic Cross
Section B–B′ Plant Greene County Ash
Pond’’; and (3) an approximately 2000foot section of Unit 1, along the
northern side of the unit between
groundwater monitoring wells GC–AP–
MW–59–HO and GC–AP–MW–1 as
shown on Figure 4C, entitled ‘‘Geologic
Cross Section C–C′ Plant Greene County
Ash Pond.’’ These figures are found in
the 2021 Plant Greene County Annual
GWMCA Report.117 EPA was unable to
determine if a similar gap currently
exists along the southern side of the
Plant Greene County Ash Pond, because
no cross-section extending along the
southern waste boundary of the unit
was included in either the 2021 Plant
Greene County Annual GWMCA Report
or the Permit Application. The omission
of a cross-section in the Permit
Application that extends along the
southern side of the Ash Pond is
significant because, given the proximity
to the Black Warrior River, which is
located immediately adjacent to the
south and southeast of the Ash Pond,
additional potential contaminant
117 Alabama Power. Plant Greene 2021 Annual
Groundwater Monitoring and Corrective Action
Report. January 31, 2022. Two similar geologic
cross sections are found in the Groundwater
Monitoring Plan included in the Permit
Application. The two geologic cross sections were
included as Figures 4A, for A–A1, and 4B, for B–
B1; however, no geologic cross section for C—C1
was included in the Permit Application.
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pathways that would need to be
monitored would normally be expected
to be present.
ii. Insufficient Lateral Spacing of
Compliance Wells To Monitor All
Potential Contaminant Pathways
EPA is also proposing to determine
that ADEM approved lateral spacing
between wells along the perimeter of the
Ash Pond that is insufficient to meet the
performance standards in § 257.91(b).
Monitoring wells used for the detection
and assessment monitoring program are
spaced approximately one thousand feet
apart with few exceptions. Large lateral
well spacings are particularly
problematic to the east, south and west
of the waste boundary of the unit where
groundwater is expected to discharge to
surface water. Given the proximity to
the various surface water features, such
as the Black Warrior River and the Barge
Canal, the large well spacings make it
likely that potential contaminant
pathways from groundwater discharging
to surface water located immediately
adjacent to the Ash Pond are not being
monitored. This groundwater to surface
water pathway was acknowledged in the
Permit Application with a statement
that reads, as follows: ‘‘Groundwater
that migrates downward into the
surficial aquifer will migrate vertically
through the Unit 1 clay and then,
primarily laterally (horizontal) and to a
lesser extent vertically along more
coarse fractions of the Unit 2 aquifer
toward the Black Warrior River and
barge canal.’’ 118
Based on the concerns discussed
above, EPA is proposing to determine
that by approving the deficient
downgradient groundwater monitoring
well network in the Permit Application,
ADEM’s final permit does not require
Alabama Power to achieve compliance
with the performance standards in
§ 257.91(a)(2), or with an equally
protective alternative.
c. Plant Greene County Corrective
Action Issues
In November 2018, SSLs above the
groundwater protection standards at
Plant Greene County were reported for
arsenic and lithium. An ACM was
prepared in June 2019 (‘‘2019 ACM’’).
On December 18, 2020, ADEM issued a
final permit to Alabama Power for the
Plant Greene County Ash Pond. In the
RTC for the Final Permit, ADEM states:
In November of 2019, the Department
provided extensive comments to Alabama
Power related to the submitted ACM and
118 Alabama Power Company. Revised Closure
Permit Application for the Plant Greene County Ash
Pond. April 30, 2020. PDF pp. 192.
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proposed final remedy. The Department’s
comments addressed many of the concerns
raised by commenters, including the
selection of monitored natural attenuation
(MNA) as the final remedy despite providing
limited data to its efficiency as a remedy. To
date, Alabama Power has not submitted a
revised ACM, as the facility has been
collecting additional data to support a final
remedy proposal.
The Plant Greene County Final Permit
only contained a recitation of the
corrective action regulations, but did
not require Alabama Power to achieve
compliance with those requirements.
This is because the Final Permit does
not require Alabama Power to take
specific actions to correct the
deficiencies in the 2019 ACM, even
though, as discussed in its RTC on the
permit, ADEM identified them a year
before issuing the Final Permit.
Significantly, ADEM did not determine
what actions are still necessary in light
of those facts for Alabama Power to
achieve compliance with the regulations
and include those actions as
requirements in the Final Permit. For
example, the Final Permit does not
require the permittee to take any
particular actions to address ADEM’s
comments on the 2019 ACM or with
respect to Alabama Power’s proposed
remedy, such as specifying the
additional data needed to support the
permittee’s preferred remedy under a set
timetable. As a consequence, EPA is
proposing to determine that the permit
authorized Alabama Power to continue
to indefinitely pursue a remedy that
appears not to meet the requirements of
§ 257.97(b), and that is based on the
results of an ACM that does not meet
the requirements of § 257.96.
Whether the 2019 ACM meets the
requirements of the regulations, and
what actions Alabama Power must take
to remediate groundwater in compliance
with § 257.97 are precisely the types of
issues that must be determined before
the permit is issued. This is because,
once the permit is issued, the
requirements in the permit become the
State requirements with which the
Permittee must comply. 42 U.S.C.
6945(d)(3)(A). And if the permittee is
not in compliance with the regulations,
the permit must specify what the
permittee is required to do in order to
achieve compliance with those
regulations. This is the role of a
permitting authority (i.e., ADEM).
Delaying this decision until after permit
issuance effectively allows Alabama
Power to continue operating out of
compliance with the regulations, while
operating in compliance with the
permit. This results in a permit program
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that is less protective than the Federal
regulations.
As discussed below, EPA is proposing
to determine that the Final Permit fails
to require Alabama Power to achieve
compliance with several of the Federal
corrective action requirements.
These are many of the same
deficiencies that ADEM identified in its
comments on the 2019 ACM, but
declined to remedy in the permit issued
a year and a half later.119
i. The Final Permit Does Not Require
Collection of the Data Needed To
Support Assessments in the ACM
As discussed previously,
§ 257.95(g)(1) requires a facility to
characterize the nature and extent of the
release and any relevant site conditions
that may affect the remedy ultimately
selected. The characterization must be
sufficient to support a complete and
accurate assessment of the corrective
measures necessary to effectively clean
up all releases from the CCR unit
pursuant to § 257.96. The 2019 ACM
delineates releases of arsenic, cobalt,
and lithium but does not characterize
site conditions that would affect any of
the potential remedies identified in the
ACM (e.g., testing for the presence and
quantity of arsenic and lithium detected
in soils to demonstrate they are being
removed from the groundwater and
immobilized on-site.)
The 2019 ACM identified MNA as a
potential corrective measure to address
groundwater contamination, in addition
to other corrective measures (e.g.,
hydraulic control and treatment; in-situ
treatment). However, Alabama Power
failed to collect the site data needed to
identify whether natural attenuation
may be occurring on-site, as well as the
mechanism by which it occurs, and to
assess whether site characteristics that
control and sustain this naturally
occurring attenuation are sufficient to
immobilize the entire release. For
example, in order to accurately assess
MNA, site data are needed to determine
whether immobilization occurs on-site
through adsorption or absorption to
subsurface soils. In addition, data would
be needed to determine whether the
chemical reactions and processes
involved that achieve immobilization
are permanent. Immobilization that is
not permanent could be reversed,
causing contaminants to be released
back into groundwater and to migrate
off-site.
Although the Remedy Selection
Report contained some data regarding
119 Alabama Department of Environmental
Management. Response to CCR Comments
Submitted to the Department, Alabama Power
Company. November 14, 2019. pp 6–7.
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the presence of released constituents in
soils,120 the relative performance,
reliability, ease of implementation, and
the time required to begin and complete
the remedy must also be assessed for
each alternative, including MNA. 40
CFR 257.96(c)(1) and (2). These
assessments must be supported with site
characterization data and analysis, but
no data were provided in the ACM to
support an assessment of MNA against
these criteria, relative to other
alternatives, to support its selection.
The Remedy Selection Report discusses
site data in the context of these criteria
for MNA only, with no side-by-side
assessments of alternatives based on site
data provided. Additionally, the data
discussed in Section 4.3.2 of the
Remedy Selection Report do not
demonstrate that any significant amount
of lithium or cobalt is being
immobilized in the solids samples.121
ii. The Final Permit Does Not Require
Submission of a Revised ACM That
Accurately Assesses MNA According to
the Criteria in 40 CFR 257.96(c)
No naturally occurring attenuation
mechanisms other than dilution and
dispersion were identified at Plant
Greene County in the ACM. Alabama
Power acknowledges in the ACM that,
‘‘USEPA (2015) discourages using
dilution and dispersion as primary
MNA mechanisms, as these mechanisms
disperse contaminant mass rather than
immobilize it.’’ 122 Regardless, Alabama
Power assessed the performance of
MNA as ‘‘medium’’ based on the fact
that the aquifer is sandy and dilution
and dispersion (i.e., releases of
contaminants) are occurring.
This favorable assessment of MNA is
inconsistent with § 257.97(b)(4), which
specifies that ‘‘[r]emedies must . . .
remove from the environment as much
of the contaminated material that was
released from the CCR unit as is
feasible.’’ Neither dilution nor
dispersion removes the contaminants
from the environment. Therefore, at this
site MNA would not meet this
requirement, since the constituents
would remain in the environment, albeit
in a different environment (i.e., the river
rather than the aquifer). Absent
information to support a conclusion that
MNA can meet these requirements at
this site, MNA performance and
reliability should have been assessed as
‘‘does not meet.’’
120 Alabama Power Company. Plant Greene
County Groundwater Remedy Selection Report,
September 2021. Appendix D, Tables 6, 9 and 19.
121 Id at Appendix D, Tables 6 and 12.
122 Alabama Power Company. Assessment of
Corrective Measures Greene County Ash Pond. June
2019, p. 12
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Further, in order for MNA through
immobilization to be assessed favorably
with respect to its reliability at meeting
the other requirements in § 257.97(b),
such as the requirement in
§ 257.97(b)(2) to attain groundwater
protection standards, the chemical
reactions and processes involved that
achieve immobilization must be
demonstrated to be permanent.
Immobilization that is not permanent
could be reversed, causing contaminants
to be released back into groundwater
and to migrate off-site. Assessing the
reliability of MNA through
immobilization as ‘‘high’’ in the ACM
was not supported by data, since no
immobilization mechanisms were
identified, they could not be known to
be reliable. Although Section 4.3.2 of
the Remedy Selection Report contained
some data regarding the presence of
released constituents in soils, the data
do not demonstrate that any significant
amount of lithium or cobalt are being
immobilized in the solid samples,123
and therefore these data do not actually
support selection of MNA as a primary
remedy for these contaminants.124
In another section of the ACM, MNA
was assessed as easy to implement
because no design or construction
would be required. If MNA occurs
through immobilization of constituents
in the subsurface that is not permanent,
this would generally require ongoing
monitoring as long as contaminants
remain in the soil—indefinitely—in
accordance with § 257.98(a)(1). Since
the goal of the remedy would be for
immobilized constituents to remain in
the subsurface indefinitely, monitoring
would be needed to demonstrate
whether this goal is achieved. This is a
much longer compliance monitoring
timeframe than any other alternative,
except possibly in-situ geochemical
manipulation, which means that
implementation is not significantly
easier than alternatives that can be
completed sooner, such as hydraulic
control and treatment.
EPA is also proposing to determine
that the ACM fails to meet the
requirements to consider safety impacts,
cross-media impacts, and control of
exposure to any residual contamination
in its assessment of MNA in either the
narrative or Table 6. See 40 CFR
257.96(c)(3). Table 6, in the column
labeled ‘‘potential impacts of remedy’’
assesses the potential impacts from
MNA as ‘‘none.’’ This conclusion is
123 Alabama Power Company. Plant Greene
County Groundwater Remedy Selection Report,
September 2021. Appendix D, Tables 6 and 12.
124 Some data were provided in the Remedy
Selection Report to indicate arsenic may be
immobilized on-site.
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unsupported by data or analysis. This
conclusion is also inconsistent with
information in the ACM. The Ash Pond
is bounded on three sides by adjacent
surface water features. In the ACM in
Figure 3, groundwater flow is depicted
from the Ash Pond toward surface water
features. Further, as noted Section 4.2.1
of the Groundwater Monitoring Plan,
entitled ‘‘Groundwater Elevations and
Flow,’’ ‘‘[g]roundwater elevations in
monitoring wells located adjacent or
close to the barge canal and the river
appear to demonstrate a temporary
reversal of flow to the groundwater
system associated with recent storm
events.’’ This temporary reversal of flow
indicates a connection between surface
water and groundwater in the vicinity of
the Ash Pond.
Because no site data were presented
to demonstrate that immobilization of
lithium or cobalt is occurring at Plant
Greene, the only MNA that is known to
occur for these two constituents is
dilution and dispersion (i.e., the normal
transport associated with groundwater
releases). This means that these
contaminants are migrating in
groundwater from the Ash Pond to the
river. Migration of contamination from
groundwater to surface water is a crossmedia impact. Therefore, the assessment
of potential impacts from the remedy for
MNA in Table 6, which includes these
cross-media impacts, should be ‘‘high.’’
Conclusions without a supporting
assessment or data do not constitute ‘‘an
analysis of the effectiveness of potential
control measures.’’ 40 CFR 257.96(c)
(emphasis added). In addition, the lack
of data means the ACM does not
sufficiently establish MNA’s
‘‘effectiveness in meeting all of the
requirements and objectives’’ in
§ 257.97(b). Inaccurate assessments in
an ACM can ultimately result in
selection of a remedy that will not meet
the requirements of § 257.97(b).
ADEM identified many of these same
issues in their comments on the 2019
ACM. For example, on page 6, ADEM
states:
ADEM Admin. Code r. 335–13–15–.06(8)
contains substantial requirements that must
be evaluated when selecting a remedy, such
as the long- and short-term effectiveness and
protectiveness of the potential remedy, the
effectiveness of the remedy in controlling the
source to reduce further releases, among
VerDate Sep<11>2014
20:09 Aug 11, 2023
Jkt 259001
many others. The ACMs submitted by APCO
do not match the level of detail required in
the regulations. Please update the ACMs to
include detailed information for each
requirement of this section. Furthermore,
ADEM Admin. Code r. 335–13–15–.06(8)(b)3.
and (b)4. require that the remedy must (1)
‘‘control the source(s) of releases so as to
reduce or eliminate, to the maximum extent
feasible, further releases of constituents in
Appendix IV into the environment’’ and (2)
‘‘remove from the environment as much of
the contaminated material that was released
from the CCR unit as feasible. . .’’.
*
*
*
*
*
The Department requests a more detailed
evaluation of the effectiveness of MNA, or
any other proposed remedy, based on site
specific conditions.
Yet ADEM’s Final Permit does not
require Alabama Power to take any
actions to remedy any of the
deficiencies they identified.
iii. The Permit Does Not Require an
Assessment of Source Control Measures
The permit record contains no
assessment of source control measures.
Section 2.5 of the 2019 ACM describes
the approved closure with waste
remaining in the Ash Pond but contains
no assessment of how well the closure
would control releases. Nor can that
information be found in the Remedy
Selection Report, or the Closure Plan.
Moreover, the ACM neither identifies
nor assesses any alternative measures.
40 CFR 257.96 requires that various
alternatives for source control be
compared in accordance with the
criteria in § 257.96(c).
ADEM raised similar concerns in their
comments, which state:
The ACMs evaluate a number of options,
with source control (by consolidating and
capping the CCR units) and monitored
natural attenuation (MNA) proposed as the
most effective remedy. The Department
requests a more detailed justification for the
proposed remedies given that source control
will not be achieved for an average of 10
years and that no other mechanism is
proposed to reduce the potential for further
releases to the ‘‘maximum extent feasible’’.
Yet the permit ADEM subsequently
issued does not require any actions to
remedy this deficiency.
5. EPA Conclusion About Alabama’s
Implementation of the CCR Regulations
Given the systemic problems noted
above in ADEM’s CCR permits related to
PO 00000
Frm 00056
Fmt 4701
Sfmt 9990
the groundwater monitoring, corrective
action and closure requirements, EPA is
proposing to determine that ADEM’s
implementation of its permit program is
resulting in a State program that is
notably less protective than the Federal
CCR regulations. First, ADEM’s permits
allow closure with waste in place in
unlined surface impoundments, without
requiring any, or sufficient, controls to
prevent groundwater from flowing in
and out of CCR in the units indefinitely.
In such circumstances, the permit will
allow ongoing contamination of
groundwater from CCR impoundments.
Second, ADEM’s permits do not require
Permittees to achieve compliance with
the groundwater monitoring regulations.
The State-issued permits discussed in
this notice approve groundwater
monitoring networks that are
insufficient to accurately determine if a
unit is leaking. Finally, ADEM’s permits
are inadequate related to the
implementation of the corrective action
requirements because they allow
facilities to delay effective responses to
contaminant releases that may pose a
risk to human health and the
environment. Compounding this
problem is the fact that the groundwater
monitoring networks are insufficient
and that means there may be additional
unmonitored releases are occurring.
Ultimately, Alabama’s CCR permit
program Application would not
‘‘require each coal combustion residuals
unit located in the State to achieve
compliance with the applicable [Federal
or other equally protective State]
criteria.’’ 42 U.S.C. 6945(d)(1)(B).
Therefore, EPA is proposing this denial
of Alabama’s CCR permit program
Application.
V. Proposed Action
EPA has preliminarily determined
that the Alabama CCR permit program
does not meet the statutory standard for
approval. Therefore, in accordance with
42 U.S.C. 6945(d), EPA is proposing to
deny the Alabama CCR permit program.
Michael S. Regan,
Administrator.
[FR Doc. 2023–17023 Filed 8–11–23; 8:45 am]
BILLING CODE 6560–50–P
E:\FR\FM\14AUP3.SGM
14AUP3
Agencies
[Federal Register Volume 88, Number 155 (Monday, August 14, 2023)]
[Proposed Rules]
[Pages 55220-55274]
From the Federal Register Online via the Government Publishing Office [www.gpo.gov]
[FR Doc No: 2023-17023]
[[Page 55219]]
Vol. 88
Monday,
No. 155
August 14, 2023
Part III
Environmental Protection Agency
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40 CFR Part 257
Alabama: Denial of State Coal Combustion Residuals Permit Program;
Proposed Rule
Federal Register / Vol. 88, No. 155 / Monday, August 14, 2023 /
Proposed Rules
[[Page 55220]]
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ENVIRONMENTAL PROTECTION AGENCY
40 CFR Part 257
[EPA-HQ-OLEM-2022-0903; FRL 11262-01-OLEM]
Alabama: Denial of State Coal Combustion Residuals Permit Program
AGENCY: Environmental Protection Agency (EPA).
ACTION: Notice of availability; request for comment.
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SUMMARY: Pursuant to section 4005(d) of the Resource Conservation and
Recovery Act (RCRA), the Environmental Protection Agency (EPA or the
Agency) is proposing to deny the Alabama Department of Environmental
Management's (ADEM or Department) Application for approval of the
Alabama coal combustion residuals (CCR) permit program (Application).
After reviewing the State CCR permit program Application submitted by
ADEM on December 29, 2021, and additional relevant materials, and based
on extensive discussions with ADEM regarding its Application, EPA has
preliminarily determined that Alabama's CCR permit program does not
meet the standard for approval under RCRA. This document announces that
EPA is seeking comment on this proposal during a 60-day public comment
period and will be holding an in-person public hearing on EPA's
proposed denial of Alabama's CCR permit program.
DATES:
Comments due. Comments must be received on or before October 13,
2023.
Public Hearing: EPA will hold an in-person public hearing on
September 20, 2023, and a virtual public hearing on September 27, 2023.
Please refer to the SUPPLEMENTARY INFORMATION section for additional
information on the public hearing.
ADDRESSES: You may send comments, identified by Docket ID No. EPA-HQ-
OLEM-OLEM-2022-0903, by any of the following methods:
Federal eRulemaking Portal: https://www.regulations.gov/
(our preferred method). Follow the online instructions for submitting
comments.
Mail: U.S. Environmental Protection Agency, EPA Docket
Center, Office of Land and Emergency Management (OLEM) Docket, Mail
Code 28221T, 1200 Pennsylvania Ave. NW, Washington, DC 20460.
Hand Delivery or Courier (by scheduled appointment only):
EPA Docket Center, WJC West Building, Room 3334, 1301 Constitution
Avenue NW, Washington, DC 20004. The Docket Center's hours of
operations are 8:30 a.m.-4:30 p.m., Monday-Friday (except Federal
holidays).
Instructions: All submissions received must include the Docket ID
No. for this rulemaking. Comments received may be posted without change
to https://www.regulations.gov/, including any personal information
provided. For detailed instructions on sending comments and additional
information on the rulemaking process, see the ``Public Participation''
heading of the SUPPLEMENTARY INFORMATION section of this document.
FOR FURTHER INFORMATION CONTACT: Michelle Lloyd, Office of Resource
Conservation and Recovery, Materials Recovery and Waste Management
Division, U.S. Environmental Protection Agency, 1200 Pennsylvania
Avenue NW, MC: 5304T, Washington, DC 20460; telephone number: (202)
566-0560; email address: [email protected]. For more information
on this notice please visit https://www.epa.gov/coalash.
SUPPLEMENTARY INFORMATION:
Table of Contents
I. Public Participation
A. Written Comments
B. Participation in In-Person Public Hearing
C. Participation in Virtual Public Hearing
II. General Information
A. Overview of Proposed Action
B. Background
C. Statutory Authority
III. The Alabama CCR Permit Program Application
A. Alabama CCR Units and Resources
B. Alabama CCR Regulations
C. Alabama Authority To Regulate CCR
D. Alabama Permits
E. Summary of EPA Communications With Alabama
IV. EPA Analysis of the Alabama Application and Basis for Denial
A. Legal Authority To Evaluate State CCR Program Submittals
1. The Statute Requires EPA To Consider a State's CCR Permits
When Determining Whether To Approve the Program if the Information
Is Available
2. EPA Is Not Required To Approve a Deficient State Program and
Then Redress the Deficiencies Through RCRA's Program Review
Provisions
B. EPA's Analysis of the Alabama CCR Regulations
1. Adequacy of Technical Criteria
2. Review of Generally Applicable Alabama CCR Permit Program
Statutes and Regulations
C. EPA's Analysis of Alabama's Permits Issued Under the State
CCR Regulations
1. Colbert Fossil Plant
2. Plant Gadsden
3. Plant Gorgas
4. Plant Greene County
5. EPA conclusion About Alabama's Implementation of the CCR
Regulations
V. Proposed Action
List of Acronyms
ACM Assessment of Corrective Measures
ADEM Alabama Department of Environmental Management
ASD alternative source demonstration
BGS below ground surface
CBI Confidential Business Information
CCP coal combustion product
CCR coal combustion residuals
CD Consent Decree
CFR Code of Federal Regulations
CY cubic yards
eFile electronic filing system
EPA Environmental Protection Agency
EPRI Electric Power Research Institute
FR Federal Register
GWMCA groundwater monitoring and corrective action
GWMP Groundwater Monitoring Plan
GWPS groundwater protection standard
HSWA Hazardous and Solid Waste Amendments
ICR Information Collection Request
MCL maximum contaminant level
MNA Monitored Natural Attenuation
MSL mean sea level
NOPV Notice of Potential Violation
NPDES National Pollutant Discharge Elimination System
RCRA Resource Conservation and Recovery Act
RTC Response to Comments
SSI statistically significant increase
SSL statistically significant level
TSD Technical Support Document
TVA Tennessee Valley Authority
USGS U.S. Geological Survey
USWAG Utility Solid Waste Activities Group
WBWT waste below the water table
WIIN Water Infrastructure Improvements for the Nation
I. Public Participation
A. Written Comments
Submit your comments, identified by Docket ID No. EPA-HQ-OLEM-OLEM-
2022-0903, at https://www.regulations.gov (our preferred method), or
the other methods identified in the ADDRESSES section. Once submitted,
comments cannot be edited or removed from the docket. EPA may publish
any comment received to its public docket. Do not submit to EPA's
docket at https://www.regulations.gov any information you consider to
be Confidential Business Information (CBI) or other information whose
disclosure is restricted by statute. Multimedia submissions (audio,
video, etc.) must be accompanied by a written comment. The written
comment is considered the official comment and should include
discussion of all points you wish to make. EPA will generally not
consider comments or comment contents located
[[Page 55221]]
outside of the primary submission (i.e., on the web, cloud, or other
file sharing system). For additional submission methods, the full EPA
public comment policy, information about CBI or multimedia submissions,
and general guidance on making effective comments, please visit https://www.epa.gov/dockets/commenting-epa-dockets.
B. Participation in In-Person Public Hearing
EPA will begin pre-registering speakers for the hearing upon
publication of this document in the Federal Register. To register to
speak at the hearing, please use the online registration form available
on EPA's CCR website (https://www.epa.gov/coalash) or contact the
person listed in the FOR FURTHER INFORMATION CONTACT section to
register to speak at the hearing. The last day to pre-register to speak
at the hearing will be September 18, 2023.
EPA will make every effort to follow the schedule as closely as
possible on the day of the hearing; however, please plan for the
hearings to run either ahead of schedule or behind schedule.
Additionally, requests to speak will be taken the day of the hearing at
the hearing registration desk. EPA will make every effort to
accommodate all speakers who arrive and register, although preferences
on speaking times may not be able to be fulfilled.
Each commenter will have five (5) minutes to provide oral
testimony. EPA encourages commenters to provide EPA with a copy of
their oral testimony electronically by emailing it to the person listed
in the FOR FURTHER INFORMATION CONTACT section. EPA also recommends
submitting the text of your oral comments as written comments to the
rulemaking docket. If EPA is anticipating a high attendance, the time
allotment per testimony may be shortened to no shorter than three (3)
minutes per person to accommodate all those wishing to provide
testimony and who have pre-registered. While EPA will make every effort
to accommodate all speakers who do not pre-register, opportunities to
speak may be limited based upon the number of pre-registered speakers.
Therefore, EPA strongly encourages anyone wishing to speak to pre-
register. Participation in the public hearing does not preclude any
entity or individual from submitting a written comment.
EPA may ask clarifying questions during the oral presentations but
will not respond to the presentations at that time. Written statements
and supporting information submitted during the comment period will be
considered with the same weight as oral comments and supporting
information presented at the public hearing.
Please note that any updates made to any aspect of the hearing are
posted online at EPA's CCR website at https://www.epa.gov/coalash.
While EPA expects the hearing to go forward as set forth above, please
monitor our website or contact the person listed in the FOR FURTHER
INFORMATION CONTACT section to determine if there are any updates. EPA
does not intend to publish a document in the Federal Register
announcing updates.
If you require the services of an interpreter or special
accommodations such as audio description, please pre-register for the
hearing with the person listed in the FOR FURTHER INFORMATION CONTACT
section and describe your needs by September 6, 2023. EPA may not be
able to arrange accommodations without advance notice.
C. Participation in Virtual Public Hearing
EPA will begin pre-registering speakers for the hearing upon
publication of this document in the Federal Register. To register to
speak at the virtual hearing, please use the online registration form
available on EPA's CCR website (https://www.epa.gov/coalash) or contact
the person listed in the FOR FURTHER INFORMATION CONTACT section to
register to speak at the hearing. The last day to pre-register to speak
at the hearing will be September 25, 2023.
EPA will make every effort to follow the schedule as closely as
possible on the day of the hearing; however, please plan for the
hearing to run either ahead of schedule or behind schedule.
Additionally, requests to speak will be taken the day of the hearing
according to the procedures specified on EPA's CCR website (https://www.epa.gov/coalash) for this hearing. The Agency will make every
effort to accommodate all speakers who arrive and register, although
preferences on speaking times may not be able to be fulfilled.
Each commenter will have five (5) minutes to provide oral
testimony. EPA encourages commenters to provide EPA with a copy of
their oral testimony electronically (via email) to the person listed in
the FOR FURTHER INFORMATION CONTACT section. If EPA is anticipating a
high attendance, the time allotment per testimony may be shortened to
no shorter than three (3) minutes per person to accommodate all those
wishing to provide testimony and who have pre-registered. While EPA
will make every effort to accommodate all speakers who do not pre-
register, opportunities to speak may be limited based upon the number
of pre-registered speakers. Therefore, EPA strongly encourages anyone
wishing to speak to pre-register. Participation in the virtual public
hearing does not preclude any entity or individual from submitting a
written comment.
EPA may ask clarifying questions during the oral presentations but
will not respond to the presentations at that time. Written statements
and supporting information submitted during the comment period will be
considered with the same weight as oral comments and supporting
information presented at the public hearing. Verbatim transcripts of
the hearings and written statements will be included in the docket for
this action.
Please note that any updates made to any aspect of the hearing will
be posted online on EPA's CCR website at https://www.epa.gov/coalash.
While EPA expects the hearing to go forward as set forth above, please
monitor our website or contact the person listed in the FOR FURTHER
INFORMATION CONTACT section to determine if there are any updates. EPA
does not intend to publish a document in the Federal Register
announcing updates.
If you require the service of a translator, please pre-register for
the hearing and describe your needs on the registration form by
September 13, 2023. If you require special accommodations such as audio
description or closed captioning, please pre-register for the hearing
and describe your needs on the registration form by September 13, 2023.
Alternatively, registrants may notify the person listed in the FOR
FURTHER INFORMATION CONTACT section of any special needs. We may not be
able to arrange accommodations without advanced notice.
II. General Information
A. Overview of Proposed Action
On April 17, 2015, EPA published a final rule, creating 40 CFR part
257, subpart D,\1\ that established a comprehensive set of minimum
Federal requirements for the disposal of CCR in landfills and surface
impoundments (80 FR 21302) (``Federal CCR regulations''). Section 2301
of the 2016 Water Infrastructure Improvements for the Nation (WIIN) Act
amended section 4005 of RCRA, creating a new subsection (d) that
establishes a Federal CCR permit program that is similar to the permit
programs under RCRA
[[Page 55222]]
subtitle C and other environmental statutes. See 42 U.S.C. 6945(d).
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\1\ Unless otherwise specified, all references to part 257 and
part 239 in this notice are to title 40 of the Code of Federal
Regulations (CFR).
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RCRA section 4005(d) also allows states to seek approval for a
State CCR permit program that will operate in lieu of a Federal CCR
permit program in the State. The statute provides that within 180 days
after a State submits an application to the Administrator for approval,
EPA shall approve the State permit program if the Administrator
determines that the State program requires each CCR unit located in the
State to achieve compliance with either the Federal requirements or
other State requirements that EPA determines, after consultation with
the State, are at least as protective as those included in the Federal
CCR regulations. See, 42 U.S.C. 6945(d)(1)(B).
On December 29, 2021, ADEM submitted its State CCR permit program
Application to EPA Region 4 requesting approval of the State's partial
CCR permit program.2 3 ADEM established State CCR
regulations that mirrored the provisions in the Federal CCR regulations
with additional State-specific provisions and clarifications. Though
ADEM primarily adopted the language in the Federal CCR regulations, EPA
reviewed both proposed and final permits Alabama issued under its CCR
program and concluded that ADEM was interpreting its State regulations
in a manner inconsistent with the plain language of the Federal
requirements, and that, as a result, the permits for CCR units in the
State contain permit terms that are neither the same as, nor as
protective as, the Federal CCR regulations. Specifically, EPA
identified deficiencies in ADEM's permits with respect to the closure
requirements for unlined surface impoundments and the associated
groundwater monitoring network and corrective action requirements. EPA
discussed these issues with ADEM, and, despite EPA's concerns, the
State declined to modify the existing permits and proceeded to issue
another CCR permit with the same deficient provisions. Further, ADEM
failed to adequately explain how the permits ensured that each CCR unit
would achieve compliance with either the Federal requirements or other
State requirements that are at least as protective as the requirements
in the Federal CCR regulations.
---------------------------------------------------------------------------
\2\ Alabama Department of Environmental Management. Application
For CCR Permit Program Approval. December 2021.
\3\ In the December 29, 2021 Application, Alabama sought a
partial program approval (rather than full program approval) of the
State's CCR permit program because it is not seeking approval for
some of its CCR regulations. Specifically, ADEM is not seeking
approval for six items that are listed in Unit IV.B.1.b of this
preamble and in the Technical Support Document Volume III. See
Volume III: Technical Support Document for the Proposed Notice to
Deny Alabama's Coal Combustion Residuals Permit Program, EPA
Analysis of Alabama CCR Permitting and Technical Regulations. U.S.
Environmental Protection Agency, Office of Land and Emergency
Management (5304T), 1200 Pennsylvania Avenue NW, Washington, DC
20460. August 2023.
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EPA is proposing to deny Alabama's request for approval of its CCR
permit program Application pursuant to RCRA section 4005(d)(1)(B),
because the State's program does not meet either standard for approval.
42 U.S.C. 6945(d)(1)(B).
B. Background
CCR are generated from the combustion of coal, including solid
fuels classified as anthracite, bituminous coal, subbituminous coal,
and lignite, for the purpose of generating steam to power a generator
to produce electricity or electricity and other thermal energy by
electric utilities and independent power producers. CCR, commonly known
as coal ash, include fly ash, bottom ash, boiler slag, and flue gas
desulfurization materials.
As noted above, on April 17, 2015, EPA published a final rule that
established a comprehensive set of minimum Federal requirements in 40
CFR part 257, subpart D for the disposal of CCR in landfills and
surface impoundments. The rule created a self-implementing program that
regulates the location, design, operating criteria, and groundwater
monitoring and corrective action for CCR units, as well as the closure
and post-closure care of CCR units. The rule also includes requirements
for recordkeeping and notifications for CCR units. EPA has since
amended 40 CFR part 257, subpart D (81 FR 51802, August 5, 2016), (83
FR 36435, July 30, 2018), (85 FR 53516, August 28, 2020), (85 FR 72506,
November 12, 2020). More information on these rules is provided in the
Technical Support Document (TSD) Volume III.
C. Statutory Authority
EPA is issuing this proposed action pursuant to sections 4005(d)
and 7004(b)(1) of RCRA. See 42 U.S.C. 6945(d) and 6974(b)(1). As stated
above, section 2301 of the WIIN Act amended section 4005 of RCRA,
creating a new subsection (d) that establishes a Federal CCR permitting
program similar to permit programs under RCRA subtitle C and other
environmental statutes. See 42 U.S.C. 6945(d).
Under RCRA section 4005(d)(1)(A), 42 U.S.C. 6945(d)(1)(A), states
seeking approval of a permit program must submit to the Administrator,
``in such form as the Administrator may establish, evidence of a permit
program or other system of prior approval and conditions under [S]tate
law for regulation by the State of coal combustion residuals units that
are located in the State.'' EPA shall approve a State permit program if
the Administrator determines that the State program requires each CCR
unit located in the State to achieve compliance with either: (1) The
Federal CCR requirements at 40 CFR part 257, subpart D; or (2) Other
State criteria that the Administrator, after consultation with the
State, determines to be ``at least as protective as'' the Federal
requirements. See 42 U.S.C. 6945(d)(1)(B). The Administrator must make
a final determination, after providing for public notice and an
opportunity for public comment, within 180 days of determining that the
State has submitted a complete application consistent with RCRA section
4005(d)(1)(A).\4\ See 42 U.S.C. 6945(d)(1)(B). EPA may approve a State
CCR permit program in whole or in part. Id. Once approved, the State
permit program operates in lieu of the Federal requirements. See 42
U.S.C. 6945(d)(1)(A). In a State with a partial permit program, only
the State requirements that have been approved operate in lieu of the
Federal requirements, and facilities remain responsible for compliance
with all remaining non-State approved requirements in 40 CFR part 257,
subpart D.
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\4\ See U.S. Environmental Protection Agency. Coal Combustion
Residuals State Permit Program Guidance Document; Interim Final,
August 2017, Office of Land and Emergency Management, Washington, DC
20460 (providing that the 180-day deadline does not start until EPA
determines the application is complete).
---------------------------------------------------------------------------
As noted above, the Federal CCR regulations are self-implementing
and that means that CCR landfills and surface impoundments must comply
with the terms of the rule even prior to obtaining a Federal permit or
permit issued by an approved State, and noncompliance with any
requirement of the Federal CCR regulations can be directly enforced
against the facility. Once a final CCR permit is issued by an approved
State or pursuant to a Federal CCR permit program, however, the terms
of the permit apply in lieu of the terms of the Federal CCR regulations
and/or requirements in an approved State program, and RCRA section
4005(d)(3) provides a permit shield against direct enforcement of the
applicable Federal or State CCR regulations (meaning the permits terms
[[Page 55223]]
become the enforceable requirements for the permittee).
In addition, RCRA section 7004(b) applies to all RCRA programs,
directing that ``public participation in the development, revision,
implementation, and enforcement of any. . .program under this chapter
shall be provided for, encouraged, and assisted by the Administrator
and the States.'' 42 U.S.C. 6974(b)(1).
III. The Alabama CCR Permit Program Application
On December 29, 2021, ADEM submitted its revised CCR permit program
Application to EPA Region 4.\5\ The Application requested approval of
the State's partial CCR permit program.\6\ Alabama's first CCR
regulations were promulgated in 2018 and continued to be revised over
the next several years in response to public comment, discussions
between ADEM and EPA, and changes to the Federal CCR regulations in 40
CFR part 257, subpart D.
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\5\ Application to USEPA Region IV for CCCR Permit Program
Approval in Accordance with Section 4005 of the Resource
Conservation and Recovery Act (RCRA) Alabama Department of
Environmental Management Land Division-Solid Waste Branch. December
2021.
\6\ ADEM previously submitted CCR permit program applications on
July 12, 2018, and February 26, 2021. For purposes of this proposed
action, EPA reviewed the most recent Application submitted on
December 29, 2021.
---------------------------------------------------------------------------
EPA conducted an analysis of the Alabama CCR permit program
Application, including a thorough analysis of ADEM's statutory
authorities for the CCR program, as well as regulations at Alabama
Administrative Code Chapter. 335-13-15, Standards for the Disposal of
Coal Combustion Residuals in Landfills and Impoundments. This analysis
is discussed in Unit IV.B.2.b of this preamble and in the TSD Volume
III. EPA also reviewed Alabama's permitting regulations, as well as
recent and ongoing permit decisions ADEM was making under its CCR
regulations.
A. Alabama CCR Units and Resources
In the Program Narrative in the Application, ADEM identified 16
units that are currently, or have been, used for disposal of CCR (3
landfills and 13 surface impoundments) in Alabama. ADEM stated that it
has the personnel and funding to administer a CCR permit program. The
State also indicated that its program is funded from three sources:
tipping fees collected for the disposal of solid waste, permitting
fees, and civil penalties from enforcement orders.
B. Alabama CCR Regulations
ADEM Administrative Code Chapter 335-13-15 largely replicates the
requirements of 40 CFR part 257, subpart D, for the portions of those
regulations for which the State is seeking approval. In addition to the
technical criteria at ADEM Chapter 335-13-15, ADEM has adopted State-
specific permitting requirements, including public participation
requirements, at ADEM Administrative Code Chapter. 335-13-05. ADEM also
has additional reporting and approval requirements for CCR units, as
described in the TSD Volume III.
C. Alabama Authority To Regulate CCR
ADEM derives its authority to operate the Solid Waste Program,
which includes CCR, in Alabama pursuant to the following statutory
provisions of the Code of Alabama, 1975: (1) Section 22-22A-5 provides
the Department with the authority to administer and enforce the State's
Solid Wastes and Recyclable Materials Management Act, to adopt and
promulgate rules, regulations, and standards through the Environmental
Management Commission, and to develop environmental policy for the
State; and to serve as the State Agency responsible for administering
federally-approved or federally-delegated environmental programs; (2)
Section 22-27-9 provides ADEM with authority over the management of
solid waste in the State (except for the collection and transportation
of nonhazardous and nonmedical solid waste) and the permitting and
operation of solid waste management facilities; and (3) Section 22-27-
12 provides ADEM with the authority to promulgate and adopt rules
establishing requirements for the management of solid waste and to
issue permits with conditions regarding the management of such solid
waste.
D. Alabama Permits
Unlike Georgia, Texas, and Oklahoma (currently the only three
States with EPA approval for State CCR permit programs), Alabama had
already begun implementing its State CCR permit program and issuing
permits prior to its submittal of an Application for EPA approval of
the State's CCR permit program. At the time of submission of ADEM's
December 29, 2021 Application, ADEM had issued permits for the
following CCR facilities: (1) the James H. Miller Electric Generating
Plant (Permit #37-51; issued December 18, 2020); (2) Greene County
Electric Generating Plant (Permit #32-03: issued December 18, 2020);
(3) Gadsden Steam Plant (Permit #28-09, issued December 18, 2020); (4)
James M. Barry Electric Generating Plant (Permit #49-35, issued July 1,
2021); (5) E.C. Gaston Electric Generating Plant (Permit #59-16, issued
May 25, 2021); and (6) Charles R. Lowman Power Plant (Permit #65-06,
issued August 30, 2021). At the time of submission of the December 29,
2021 Application, permits were under development by ADEM at two other
facilities: the William C. Gorgas Electric Generating Plant and
Tennessee Valley Authority (TVA) Plant Colbert. Since the submission of
ADEM's Application, ADEM has proceeded to issue both the Plant Gorgas
Permit (Permit #64-12 issued February 28, 2022) and the TVA Colbert
Permit (Permit #17-11, issued October 25, 2022).
E. Summary of EPA Communications With Alabama
As part of EPA's review of State CCR permit programs, the Agency
engages the State both before and after submittal of a State CCR permit
program application. These discussions serve a number of purposes; for
example, EPA engages in these discussions to help the State determine
the scope of the CCR permit program it wants to adopt (e.g., full or
partial program) and to ensure the State establishes the necessary
State CCR regulations prior to submitting the request for program
approval. EPA also assists the State in determining what to include in
the Narrative Statement component of its permit program application,
which serves as a roadmap to the State's CCR permit program. EPA also
uses these discussions to clarify questions raised during the public
comment period about the State program. To the extent the State
implements its CCR regulations prior to EPA's determination of State
program adequacy, EPA will also discuss the State's interpretation and
implementation of its program to ensure that EPA fully understands the
program and to determine which of the two statutory standards EPA will
use to evaluate the State program. EPA took the same approach with
Alabama as with other states seeking approval, and, as detailed below,
EPA and ADEM have had extensive discussions about the State's CCR
permit program.\7\
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\7\ EPA has attempted to identify all the interactions between
EPA and ADEM with respect to the State's CCR permit program. A
summary of the interactions between EPA and ADEM is included in the
docket to this notice in Volume II: Technical Support Document for
the Proposed Notice to Deny Alabama's Coal Combustion Residuals
Permit Program, Communication Between EPA and ADEM. U.S.
Environmental Protection Agency Office of Land and Emergency
Management (5304T). August 2023. In addition, copies of emails and
letters between EPA and ADEM can be found in the docket.
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[[Page 55224]]
EPA began telephone calls and meetings with ADEM about its
development of an Application for a CCR permit program in January 2018
and continued them through July 2022. In the early calls, EPA and ADEM
discussed the process for EPA to review and approve State CCR permit
programs, ADEM's plans for formally adopting CCR regulations, its
anticipated timeline for submitting a CCR permit program Application to
EPA, and ADEM's permit requirements. During these calls, EPA reviewed
ADEM's submission and sent comments to ADEM on those documents. The
frequency of calls between EPA and ADEM varied depending on the stage
of ADEM's efforts to develop and submit (or re-submit) its CCR permit
program Application. For example, during ADEM's public comment periods
associated with State rulemaking, or during periods of re-working
regulations or documents, calls were held less frequently. When ADEM
had questions or requested EPA input, calls were held more often.
After ADEM's initial CCR regulations became effective in 2018, the
State began to issue permits. Calls were then held on specific
facilities and technical issues that ADEM sought EPA's input on, such
as specific corrective action proposed remedies or closure methods. In
addition, consistent with RCRA section 4005(d), EPA began discussions
with ADEM on specific facilities and permits to evaluate whether ADEM
was requiring, as part of its permit process, each CCR unit in the
State ``to achieve compliance with'' the Federal part 257 standards or
``other State criteria that the Administrator, after consultation with
the State, determines to be at least as protective as'' the Federal
criteria.
Of particular concern to the Agency were facilities that were
closing (or had already closed) unlined CCR surface impoundments while
leaving waste (i.e., CCR) below the water table (WBWT). On March 15,
2022, EPA shared a list of such facilities in Alabama with ADEM and
scheduled discussions regarding the closures and groundwater monitoring
activities at the Greene County Electric Generating Plant and the
Gadsden Steam Plant. Discussions also focused on the William C. Gorgas
Electric Generating Plant. ADEM had issued permits at all three of
these facilities. During these discussions and written communication,
EPA expressed concern that Alabama's permit program appeared to differ
from the Federal program, and that these differences appeared to make
the State's program less protective than the Federal program. The
Agency specifically identified problems with the State's permit
requirements covering closure of unlined surface impoundments,
groundwater monitoring networks, and corrective action. See also Unit
IV.C of this preamble below and the TSD Volume I for a detailed
discussion of the deficiencies in ADEM's CCR permits. In addition to
the concerns raised with respect to Plants Greene, Gorgas, and Gadsden,
EPA has also raised concerns with respect to the TVA Plant Colbert
permit. On June 29, 2022, ADEM posted public notice of the draft permit
for Plant Colbert. Because the proposed permit for Plant Colbert raised
many of the same issues already being discussed with respect to Plants
Greene, Gorgas, and Gadsden, EPA submitted a letter to ADEM outlining
specific concerns with respect to the proposed permit.\8\
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\8\ Letter from Carolyn Hoskinson, Director, Office of Resource
Conservation and Recovery, to Mr. Russell A. Kelly, Chief, Permits
and Services Division, and Mr. Steve Cobb, Chief, Land Division. EPA
Comments on Proposed Permit, Tennessee Valley Authority Colbert
Fossil Plant, Alabama Department of Environmental Management, Permit
No. 17-11. September 15, 2022.
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As a result of these discussions, on July 7, 2022, EPA informed
ADEM via telephone that the Agency was putting on hold its completeness
review of ADEM's CCR permit program Application until Alabama
demonstrated to EPA that the State was implementing its program
consistent with the Federal CCR regulations. Further, EPA explained to
ADEM that it was exploring options for actions to take at the Federal
level with respect to both the CCR permit program Application, and at
specific facilities where there are outstanding concerns.
On October 25, 2022, ADEM proceeded to issue a CCR permit to Plant
Colbert without revising the proposed permit to address EPA's concerns.
In a letter dated October 27, 2022, ADEM responded to EPA's letter
regarding Plant Colbert, presenting an interpretation of the
requirements applicable to closing CCR impoundments that EPA had
previously rejected in the discussions about the interpretation of the
Federal CCR regulations with ADEM described above and in EPA's Part A
proposed and final decisions. See discussion of Part A proposals in
Unit IV.C. of this preamble. To date, the State has not taken action to
revise the permits issued to Plants Colbert, Green, Gorgas, or Gadsden
to address the deficiencies EPA noted to ADEM.
On December 9, 2022, ADEM gave EPA notice of its intent to sue EPA
under section 7002(a)(1)(A) and (1)(B) of RCRA, alleging EPA failed to
perform a nondiscretionary duty to approve the State's CCR permit
program.\9\ Among other things, ADEM asserted that EPA failed to comply
with the statutory requirement to approve the State's CCR permit
program within 180 days of the State's submittal of the permit program
Application on December 29, 2021. On February 1, 2023, EPA responded to
ADEM's Notice of Intent to Sue letter and informed the State that the
180-day timeframe does not start until EPA determines that a State's
Application is administratively complete and that, in this case, EPA
did not start the clock because EPA's concerns with ADEM's
interpretation of the minimum requirements of the Federal CCR
regulations had yet to be resolved and EPA was providing an opportunity
for ADEM to submit further Application information.\10\ EPA further
stated that the Agency could evaluate the State's program on the
current record if ADEM decided not to supplement its Application with
an explanation of how the State's interpretation of its regulations is
at least as protective as the Federal CCR regulations, but EPA
expressed concern that the current record would not support a proposal
to approve the State's partial CCR permit program. Id. On February 17,
2023, ADEM responded to EPA that it did not intend to supplement the
record and that EPA should evaluate its program accordingly.\11\ EPA
thereafter continued to review the Application based on the information
submitted to date, and this notice reflects EPA's proposed conclusions
from that review.
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\9\ Letter from Alabama Attorney General Steve Marshall to EPA
Administrator Michael Regan, Notice of Endangerment and Intent to
Sue under Section 7002(a)(1)(A) and (1)(B) of the Resource
Conservation and Recovery Act. December 9, 2022.
\10\ Letter from Barry Breen, Acting Assistant Administrator,
OLEM, to Lance LeFleur, Director, ADEM, February 1, 2023. Email sent
February 2, 2023.
\11\ Letter from Lance LeFleur, Director, ADEM, to Barry Breen,
Acting Assistant Administrator, OLEM, February 17, 2023.
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IV. EPA Analysis of the Alabama Application and Basis for Denial
As stated above, a State seeking approval of a CCR permit program
can either adopt the Federal CCR requirements or establish State-
specific criteria that are at least as protective as the Federal CCR
requirements. See 42 U.S.C. 6945(d)(1)(B). After a State submits a
complete application, EPA evaluates the State program to determine
whether it ``requires each
[[Page 55225]]
coal combustion residuals unit located in the state to achieve
compliance with the applicable [Federal or other equally protective
State] criteria.'' Id. Specifically, EPA evaluates the terms of the
permit program or other system of prior approval and conditions and the
Narrative Statement, to determine whether by its terms the State
program meets either of these standards for each CCR unit regulated by
the State. As discussed in more detail below and in the TSD Volume III,
to make this determination EPA evaluates not only the CCR specific
requirements but also the State's general authority to issue permits
and impose conditions in those permits, as well as the State's
authority for compliance monitoring and enforcement.\12\ Thus,
collectively, the CCR specific and general permit requirements must
provide the State with sufficient authority to require compliance from
all CCR units located within the State. In addition, if the State
begins issuing CCR permits and overseeing compliance with the permits
prior to EPA's State program approval decision, the Agency must also
consider whether the State in fact ``requires each CCR unit located in
the state to achieve compliance with'' either the Federal criteria in
part 257 or other State criteria that ``are at least as protective as''
the Federal regulations. 42 U.S.C. 6945(d)(1)(B) (emphasis added). See
Unit IV.A of this preamble (discussing the Agency interpretation of
RCRA section 4005(d)).
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\12\ State permit program regulations usually include general
requirements that apply across multiple permit programs (e.g.,
procedures for issuing permits). When new performance standards are
issued for a type of facility or unit (for example, CCR
regulations), states include both general and facility/unit specific
requirements in the State permit program as necessary to develop a
program that satisfies the Federal requirements to support approval
of a State program.
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ADEM adopted regulations that largely mirror the Federal CCR
regulations, but in some places ADEM also added additional or different
criteria to be consistent with its existing solid waste regulations.
When a State adopts the language in the Federal CCR regulations, EPA's
review of the terms of the permit program is generally straightforward,
and, in this case, EPA's review of the express terms of ADEM's CCR
permit program demonstrates that the State program includes all
regulatory provisions required for approval of a partial program.\13\
Thus, the terms of the permit program provide ADEM with the authority
necessary to issue permits that will ensure each CCR unit in the State
achieves the minimum required level of control (i.e., the State has the
authority to issue permits that require compliance with standards that
are at least as protective as those in the Federal CCR regulations).
---------------------------------------------------------------------------
\13\ EPA conducted a thorough review of the terms of Alabama's
CCR permit program submittal, consistent with review of submittals
by states that were granted approval, and that review can be found
in the Volume III: Technical Support Document for the Proposed
Notice to Deny Alabama's Coal Combustion Residuals Permit Program,
EPA Analysis of Alabama CCR Permitting and Technical Regulations.
U.S. Environmental Protection Agency, Office of Land and Emergency
Management (5304T), 1200 Pennsylvania Avenue NW, Washington, DC
20460. August 2023.
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While the statutes and regulations of the Alabama CCR permit
program provide the State with sufficient authority to require
compliance with the Federal requirements or equivalent State
requirements, EPA is proposing to determine that permits issued by ADEM
allow CCR units in the State to comply with alternative requirements
that are less protective than the requirements in the Federal CCR
regulations with respect to groundwater monitoring, corrective action,
and closure. For example, as discussed in more detail in subsequent
sections, ADEM has issued multiple permits allowing CCR in closed units
to remain saturated by groundwater, without requiring any engineering
measures to control the groundwater flowing into and out of the closed
unit. ADEM has also approved groundwater monitoring systems that
contain an inadequate number of wells, and in incorrect locations, to
detect groundwater contamination from the CCR units. Finally, ADEM has
issued multiple permits that effectively allow the permittee to delay
implementation of effective measures to remediate groundwater
contamination both on- and off-site of the facility. Overall, EPA's
review of the permit records demonstrates a consistent pattern of
deficiencies in the permits and a lack of oversight and independent
evaluation of facilities' proposed permit terms on the part of ADEM. In
each case, EPA was unable to locate any evaluation or record of
decision documenting that ADEM had critically evaluated the materials
submitted as part of the permit applications, or otherwise documented
its rationale for adopting those proposed permit terms prior to
approving the application. As a consequence, EPA cannot conclude that
the permits are as protective as the Federal CCR regulations.
As noted above, EPA discussed many of these issues with ADEM and
the State declined to revise the permits to be consistent with the
Federal CCR regulations. ADEM also declined to demonstrate that its
alternative requirements satisfy the requirement in RCRA section
4005(d)(1)(B). Instead, the Alabama Attorney General, on behalf of
ADEM, asserted in the Notice of Intent to Sue that EPA does not have
the authority to consider implementation of the State program when
determining whether a State program is sufficient, and that the Agency
may only look to the ``four corners'' of the State program submission
when evaluating the program for approval. In the Notice of Intent to
Sue, the ``four corners'' of the application are described as being
public participation, guidelines for compliance, guidelines for
enforcement authority, and intervention in civil enforcement
proceedings. Regarding deficiencies in implementation of a State CCR
permit program, the State of Alabama's position must, therefore, be
that EPA first approve a State CCR permit program even if the Agency
knows the State's implementation is deficient prior to approval, and
the Agency must then follow the process for withdrawal of the program
through the program review and withdrawal provisions in RCRA sections
4005(d)(1)(D) and (E), respectively. Id.
EPA does not agree with ADEM's interpretation of the Agency's
authority under RCRA, and the Agency is proposing to deny the program
under RCRA section 4005(d)(1)(B). Though the statute authorizes EPA to
approve a State CCR permit program in whole or in part, implementation
of the groundwater monitoring, corrective action, and closure
regulations are fundamental to an adequate CCR State permit program.
EPA does not see any meaningful way for a State to implement a partial
CCR permit program without the authority to oversee these three major
elements of the CCR program. Thus, EPA is proposing to deny the entire
Alabama CCR State permit program that ADEM submitted for approval.
In Unit IV.A of this preamble, EPA responds to ADEM's position that
RCRA section 4005(d) prohibits EPA from considering the permits issued
under the State CCR permit program when determining whether to approve
the program and that EPA may only address such issues after the State
program is approved. In Unit IV.B of this preamble, the Agency provides
a short summary of EPA's conclusions after review of the express terms
of the ADEM statutes and regulations. In Unit IV.C of this preamble,
EPA identifies specific permits that the Agency believes are deficient
and explains the bases for EPA's proposed determination that they are
inconsistent with the standard for approval in RCRA section
4005(d)(1)(B).
[[Page 55226]]
A. Legal Authority To Evaluate State CCR Program Submittals
For the reasons set forth below, EPA does not agree with ADEM's
assertion that EPA may not consider the State's CCR permit history when
determining whether to approve its permit program. In short, the Agency
interprets the statute to require EPA to consider the CCR permits a
State has issued under its CCR program when determining whether the
State program can be approved, where such information is available
prior to approval.
1. The Statute Requires EPA To Consider a State's CCR Permits When
Determining Whether To Approve the Program if the Information Is
Available
Section 4005(d)(1)(B) of RCRA provides in part that the
Administrator ``shall approve, in whole or in part, a permit program or
other system of prior approval and conditions submitted under
subparagraph (A) if the Administrator determines that the program or
other system requires each coal combustion residuals unit located in
the State to achieve compliance with'' either: (1) The Federal CCR
requirements at 40 CFR part 257 (i.e., the Federal CCR regulations); or
(2) Other State criteria that the Administrator, after consultation
with the State, determines to be at least as protective as the Federal
requirements. 42 U.S.C. 6945(d)(1)(B) (emphasis added). The statute
directs the Administrator to determine whether the State program
``requires each'' CCR unit in the State ``to achieve compliance'' with
either the Federal standard or an alternative State standard at least
as protective as the Federal CCR regulations. This necessarily includes
Agency consideration of both a State's statute and regulations and what
the State actually requires individual CCR units to do, such as in
permits or orders, when such information is available prior to approval
of the State program. By specifying that EPA is to determine that the
State program requires each unit ``to achieve compliance,'' rather than
merely that the State requires compliance or has the authority to
require compliance, Congress indicated that EPA is not restricted to
evaluating the letter of the State's regulations. Moreover, the statute
makes clear that once a permit goes into effect, those are the relevant
requirements applicable to the CCR unit rather than the regulations.
See 42 U.S.C. 6945(d)(3) (specifying that the applicable criteria for
CCR units in an approved State are those contained in the State permit,
rather than the Federal or State regulations). Whether issued permits
comply with Federal requirements or a State program that is at least as
protective is directly relevant to whether the State program ``requires
each CCR unit in the State to achieve compliance.'' If issued permits
do not comply, the State program does not require compliance. EPA
cannot reasonably ignore such information, when available, as it falls
squarely within the ordinary meaning of what the statute expressly
directs EPA to consider. This is particularly true, where, as here, the
Agency knows ADEM is issuing permits to CCR units that do not require
compliance with the Federal CCR regulations, and the State has not
demonstrated that its alternative approach is as protective as the
Federal CCR regulations.
In this case, ADEM adopted into its State regulations the
provisions of the Federal CCR regulations. For this reason, ADEM
believes that EPA must approve the State's CCR program because it in
large part mirrors to the Federal CCR regulations, thus, according to
ADEM, the State program satisfies the requirements for an approvable
program pursuant to RCRA section 4005(d)(1)(B)(i). ADEM is correct that
EPA may approve a State program under this provision based on the fact
that the State's regulations are identical to those in the Federal CCR
regulations, but not where the State interprets the State regulations
to impose significantly different requirements than the Federal CCR
regulations, and the State has issued permits authorizing actions that
the Federal regulations prohibit. Here, despite adopting the language
in the Federal CCR regulations, ADEM has affirmatively stated that it
interprets the State regulations differently than the identically
worded Federal provisions and has issued permits on that basis, even
though the Agency has informed the State on multiple occasions that its
interpretation and implementation of the regulations are not consistent
with the Federal CCR regulations. See Units III.E and IV.C of this
preamble (discussing Alabama's interpretation of ``infiltration'' under
Sec. 257.102(d)(1)(i), among other examples). Based on all of the
information in the record, EPA cannot conclude that Alabama's program
``requires each'' CCR unit in the State ``to achieve compliance with''
the Federal CCR regulations as required by RCRA section
4005(d)(1)(B)(i).
Further, because Alabama is interpreting the language in the
Federal CCR regulations differently than the Agency, Alabama is
essentially submitting ``other State criteria,'' and in order for EPA
to approve such a program, Alabama must provide information to support
a determination that the State criteria are ``at least as protective as
the [Federal CCR regulations]'' consistent with RCRA section
4005(d)(1)(B)(ii). EPA has explained its position to Alabama, most
recently by letter dated February 1, 2023, and Alabama has declined to
provide any explanation, much less an adequate one, of how its program
will require each CCR unit to achieve compliance with standards at
least as protective as the Federal CCR regulations. Accordingly, the
Agency is proposing to deny Alabama's request for approval of its CCR
permit program. This proposed denial is based on all the available
information in the record, and as discussed in Unit IV.C of this
preamble, it demonstrates that the Alabama CCR permits do not require
each CCR unit in the State to achieve compliance with requirements at
least as protective as those contained in the Federal CCR regulations.
2. EPA Is Not Required To Approve a Deficient State Program and Then
Redress the Deficiencies Through RCRA's Program Review Provisions
In addition to the express terms of RCRA section 4005(d)(1)(B), as
explained below, the overall context of RCRA section 4005(d) supports
consideration of State CCR permits when they have been issued prior to
approval of the State program. Even were that not the case, it would be
unreasonable to interpret the statute to require that EPA must approve
a State program based on the four corners of the submission and then
use the program review provisions of RCRA section 4005(d)(1)(D) to
address pre-existing deficiencies in the program. As an initial matter,
EPA questions how it would be reasonable to ignore directly relevant
and readily available information in review of a State program that
will stand in for a Federal program, because once EPA approves a State
program, the requirements of the State program apply instead of the
Federal rules. Further, once a State permit is issued, facilities are
shielded from enforcement of anything other than the provisions of the
State permit. Compounding the problem is the time it would take to go
through the statutorily mandated process to withdraw a deficient
program and the fact that prior noncompliance would be arguably
sanctioned by approval of a State program that is being implemented
improperly.
In this case, all the potential problems that can arise by
approving a State CCR program based solely on the ``four
[[Page 55227]]
corners'' of the State application are in play. Specifically, the State
is interpreting the terms of the State program (i.e., the terms of the
Federal CCR regulations) in a manner that is less protective than the
Federal CCR regulations, the State is issuing permits based on its
flawed interpretation, EPA approval of the State program would be the
equivalent of approving the deficient permits, it would take
considerable time to withdraw the State program after approval, and, in
the interim, facilities would be able to operate under permits that are
less protective than required. Furthermore, the Agency is proposing to
determine, based on the available information, that Alabama's CCR
permit program is deficient under two of the bases provided in RCRA
section 4005(d)(1)(D)(ii), EPA has notified Alabama of the
deficiencies, and the State has declined to address them. See Unit IV.C
of this preamble (discussing the deficiencies in Alabama's CCR
program).
The statute requires EPA to periodically review approved State
programs and provides a process by which EPA can address identified
deficiencies. RCRA sections 4005(d)(1)(D)(i) and 4005(d)(1)(D)(ii),
respectively. The review provisions in RCRA section 4005(d)(1)(D)(i)
require review:
from time to time, as the Administrator determines
necessary, but not less frequently than once every 12 years;
not later than 3 years after the date on which the
Administrator revises the applicable criteria for coal combustion
residuals units under part 257 of title 40, Code of Federal Regulations
(or successor regulations promulgated pursuant to sections 6907(a)(3)
and 6944(a) of this title);
not later than 1 year after the date of a significant
release (as defined by the Administrator), that was not authorized at
the time the release occurred, from a coal combustion residuals unit
located in the State; and
on request of any other State that asserts that the soil,
groundwater, or surface water of the State is or is likely to be
adversely affected by a release or potential release from a coal
combustion residuals unit located in the State for which the program or
other system was approved.
The statute clearly provides for review of State programs whenever
``the Administrator determines necessary,'' in addition to the
situations that mandate EPA review of a State program (e.g., RCRA
section 4005(d)(1)(D)(i)(I) requiring review periodically and at least
every 12 years). Under Alabama's reading of the statute, EPA must
approve a knowingly deficient State program and then undertake a
program review, either mandatory or discretionary, to address the
deficiencies in that same program. Under such circumstances, CCR units
in the State would potentially be allowed to operate in a manner that
is not consistent with the Federal CCR regulations for many years
unless EPA were to undertake a voluntary program review immediately
after approving the program.
An additional factor that argues against Alabama's interpretation
is the fact that RCRA section 4005(d)(1)(D)(ii) provides a process that
EPA must follow to address identified deficiencies in a State CCR
permit program before EPA may withdraw the program, and, during that
time, ADEM could continue to issue permits that are not as protective
as the statute requires. See also 42 U.S.C. 6945(d)(1)(E)(i) (allowing
withdrawal of a State program only after notice to the State and an
opportunity for a hearing). Specifically, under RCRA section
4005(d)(1)(D)(ii), EPA must provide the State with notice of
deficiencies in the State program and an opportunity for a hearing if
the Administrator determines that:
a revision or correction to the permit program or other
system of prior approval and conditions of the State is necessary to
ensure that the permit program or other system of prior approval and
conditions continues to ensure that each coal combustion residuals unit
located in the State achieves compliance with the criteria described in
clauses (i) and (ii) of subparagraph (B);
the State has not implemented an adequate permit program
or other system of prior approval and conditions that requires each
coal combustion residuals unit located in the State to achieve
compliance with the criteria described in subparagraph (B); or
the State has, at any time, approved or failed to revoke a
permit for a coal combustion residuals unit, a release from which
adversely affects or is likely to adversely affect the soil,
groundwater, or surface water of another State.
The information currently available to EPA already indicates that
Alabama's program is deficient under the first two provisions of RCRA
section 4005(d)(1)(D)(ii). First, a revision to Alabama's CCR permit
program is necessary to ensure that each CCR unit located in the State
achieves compliance with State standards that are ``at least as
protective as'' the Federal CCR regulations because Alabama has never
adequately explained how its alternative requirements achieve that
standard. 42 U.S.C. 6945(d)(1)(D)(ii)(I). Second, as explained further
in Unit IV.C. of this preamble, ADEM has not implemented its permit
program in a manner that ``ensures each CCR unit located in the State
achieves compliance with the criteria described in subparagraph (B).''
42 U.S.C. 6945(d)(1)(D)(ii)(II). In addition, EPA has notified Alabama
of these deficiencies on multiple occasions, and the State has not
provided an adequate justification for the position that its
interpretation of the Federal CCR regulations should govern over EPA's
interpretation.
Given Alabama's continued failure to adequately address EPA's
concerns with its CCR program, EPA has no reason to believe that
Alabama will change its interpretation and implementation of its
program if EPA were to approve Alabama's CCR program and then
subsequently proceed with the RCRA section 4005(d)(1)(D)(ii) process to
attempt to resolve the program deficiencies. EPA would then have to go
through the RCRA section 4005(d)(1)(E) process to withdraw the Alabama
program. In that case, EPA would then be back at the point where
Alabama would have to either adopt EPA's interpretation of the Federal
CCR regulations or explain how its alternative interpretation ensures
that the State's program is as least as protective as the Federal CCR
regulations.
The statutory language is clear, and it does not support Alabama's
interpretation. In addition, the Agency believes Alabama's
interpretation could, as in this case, lead to the illogical result
that EPA must approve a State CCR permit program that it believes it
likely will eventually have to withdraw. EPA also declines to adopt
Alabama's suggested approach because the process to withdraw takes
significant time and in the interim Alabama would likely continue to
issue permits that allow CCR units in the State to operate under
conditions that are less protective than those required in the Federal
CCR regulations. Finally, EPA is aware of several CCR permits that
allow units to operate less protectively than required by Federal CCR
regulations and approving Alabama's program would mean that these units
would no longer be subject to the Federal CCR regulations. Thus, if EPA
were to approve Alabama's program now (i.e., after the deficient CCR
permits were issued), the Alabama CCR program, including the facility-
specific permits, would apply in lieu of the Federal CCR
[[Page 55228]]
regulations pursuant to RCRA section 4005(d)(1)(A) and (3).
For all these reasons, EPA does not believe the statute must be
interpreted as Alabama suggests and EPA declines to adopt the State's
interpretation.
B. EPA's Analysis of the Alabama CCR Regulations
Section 4005(d)(1)(A) of RCRA, 42 U.S.C. 6945(d)(1)(A), requires a
State seeking CCR permit program approval to submit to EPA, ``in such
form as the Administrator may establish, evidence of a permit program
or other system of prior approval and conditions under State law for
regulation by the State of coal combustion residuals units that are
located in the State.'' Although the statute directs EPA to establish
the form of such evidence, the statute does not require EPA to
promulgate regulations governing the process or standard for
determining the adequacy of such State programs. EPA, therefore,
developed the Coal Combustion Residuals State Permit Program Guidance
Document; Interim Final (82 FR 38685, August 15, 2017) (the ``Guidance
Document''). The Guidance Document provides recommendations on a
process and standards that states may choose to use to apply for EPA
approval of a State CCR permit program, based on the standards in RCRA
section 4005(d), existing regulations at 40 CFR part 239, and the
Agency's experience in reviewing and approving State programs.
As stated above, State permit programs under RCRA generally include
both sector specific technical regulations (e.g., performance standards
for CCR units) and general State permitting and enforcement provisions
that apply to all the different State RCRA permitting programs. In this
case, Alabama is seeking approval of a partial State CCR permit program
and it established State regulations that are almost the same as the
Federal CCR regulations for the portions of the Federal program for
which the State is seeking approval. To the extent the Federal and
State provisions are different, the differences do not on their face
substantively make the State regulations less protective than the
Federal CCR regulations. EPA reviewed ADEM's CCR regulations and, based
on that review, EPA proposes to find that the express terms of the
regulations provide ADEM with sufficient authority to issue permits
that are at least as protective as those required under the Federal CCR
regulations. See the TSD Volume III (providing a detailed analysis of
the regulatory terms of Alabama's CCR regulations). EPA is proposing to
determine that the terms of the regulations provide the State with
sufficient authority to implement an adequate CCR permit program
despite the fact that the Agency is also proposing to deny the
Application for Alabama CCR permit program based on the State's
issuance of permits under those same regulations. Therefore, the Agency
believes the record would support approval of Alabama's program if the
State either modified its permits to be consistent with the Federal
requirements or demonstrated that its alternative requirements are at
least as protective as the Federal CCR regulations.
EPA briefly discusses its evaluation of the State's regulations
below. A comprehensive evaluation is included in the TSD Volume III in
the docket for this proposed action.
1. Adequacy of Technical Criteria
a. Alabama CCR Regulations
EPA first evaluates the technical criteria that will be included in
each permit the State issues to determine whether they are the same as
the Federal criteria, or to the extent they differ, whether the
modified criteria are ``at least as protective as'' the Federal
requirements. See 42 U.S.C. 6945(d)(1)(B).
On April 20, 2018, ADEM, by and through the Alabama Environmental
Management Commission (EMC), amended ADEM Admin. Code div. 335-13 to:
(1) Modify Chapters 1, 4, and 5 and (2) Add a new Chapter 15: Standards
for the Disposal of Coal Combustion Residuals in Landfills and Surface
Impoundments. These rules became effective on June 8, 2018. In response
to EPA comments and changes to the Federal CCR regulations, ADEM
proposed and finalized several amendments to its CCR rules with the
first revisions becoming effective February 15, 2021. The most recent
revisions became effective December 13, 2021.
ADEM's regulations adopt the Federal CCR regulations amended
through August 28, 2020, and include the corrections EPA made at
Sec. Sec. 257.102(d)(3)(ii) and 257.103(f)(1)(vi) (85 FR 72506,
November 12, 2020) (except for certain provisions outlined below).
EPA has preliminarily determined that the Alabama CCR permit
program contains all the technical criteria in 40 CFR part 257, subpart
D, except for the provisions specifically discussed below. EPA's full
analysis of the terms of the Alabama CCR permit program and how the
Alabama regulations differ from the Federal requirements can be found
in the TSD Volume III.
b. Federal Rule Provisions Excluded From Alabama's Request for Approval
of a Partial Program
Alabama is requesting approval for a partial State CCR program,
rather than a full CCR program that includes all the requirements of
the Federal CCR regulations. ADEM is not seeking approval for the
following six provisions:
1. ADEM Administrative Code r. 335-13-15-.01(1)(d); this State
provision is the analog to the Federal exclusion of inactive surface
impoundments at inactive facilities, found at Sec. 257.50(e), that was
vacated in Utility Solid Waste Activities Group v. EPA, 901 F.3d 414
(per curiam) (USWAG);
2. ADEM Admin. Code r. 335-13-15-.07(4)(f); this State provision is
the analog to the Federal requirement for alternative closure
deadlines, found at 40 CFR 257.103(f);
3. EPA has revised the Federal regulations to granting
Participating State Directors authority to issue certifications in lieu
of requiring a professional engineer (PE) certification. ADEM did not
adopt these provisions; therefore, an owner or operator of a CCR unit
must submit certifications from a PE, as appropriate, as required by
ADEM Admin. Code chapter 335-13-15;
4. The Federal regulations include a provision that authorizes the
suspension of groundwater monitoring requirements under certain
circumstances, found at Sec. 257.90(g), which the State has not
adopted;
5. The Federal regulations include a provision for an alternate
liner demonstration found at Sec. 257.71(d), and the State has not
adopted this Federal provision; and,
6. ADEM Admin. Code r. 335-13-15-.06(6)(h)2.: The State has adopted
the groundwater protection standards for cobalt, lead, lithium, and
molybdenum found at Sec. 257.95(h)(2) but is not seeking approval
because the Federal provision has been challenged and is under
reconsideration.
More detail on the elements of the partial program and EPA's
analysis of the program can be found in the TSD Volume III. With the
exception of specific provisions spelled out in the TSD Volume III, EPA
has preliminarily determined that the Alabama CCR regulations contain
all the technical elements of the portions of the Federal CCR
regulations for which the State is seeking approval.
[[Page 55229]]
2. Review of Generally Applicable Alabama CCR Permit Program Statutes
and Regulations
As explained above, supra note 12, Alabama's CCR permit program
regulations include general requirements that apply across multiple
permit programs, and its Application for approval of a CCR permit
program thus includes both general and facility/unit-specific
requirements in the State CCR permit program. EPA therefore also
evaluated the Alabama CCR permit program as modified to address CCR
units using the process discussed in Units II.C and IV.A of this
preamble. EPA's findings are summarized below and provided in more
detail in in the TSD Volume III for this notice.
In evaluating Alabama's CCR permitting requirements, EPA reviewed
the State's permit requirements for CCR units including applicability,
duration, application process, denial process, and the process for
draft and final permit determinations. EPA also reviewed Alabama's
requirements that apply to modification, suspension, and revocation of
permits. For permit modifications, EPA specifically looked at major and
minor modifications to determine which modifications would require
public participation. After conducting this review, EPA has
preliminarily determined that the Alabama regulations concerning CCR
permit applications and approvals is adequate, and that this aspect of
the Alabama CCR permit program meets the standard for program approval.
Based on RCRA section 7004, 42 U.S.C. 6974, it is EPA's judgment
that an adequate State CCR permit program will ensure that: (1)
Documents for permit determinations are made available for public
review and comment; (2) Final determinations on permit applications are
made known to the public; and (3) Public comments on permit
determinations are considered. Alabama has adopted public participation
opportunities for the CCR program that can provide an inclusive
dialogue, allowing interested parties to talk openly and frankly about
issues within the CCR program and search for mutually agreeable
solutions to differences. EPA reviewed Alabama's public participation
requirements, processes, and procedures including public notices,
public comment periods (including consideration of public comments),
public hearings, and public availability of final determinations. An
overview of the Alabama public participation provisions is provided in
the TSD Volume III. After conducting this review, EPA has preliminarily
determined that the Alabama approach to public participation
requirements provides adequate opportunities for public participation
in the permitting process sufficient to meet the standard for program
approval.
EPA also reviewed Alabama's compliance monitoring authority,
enforcement authority, and the procedures for intervention in civil
enforcement proceedings. It is EPA's judgment that an adequate permit
program should provide the State with the authority to gather
information about compliance, perform inspections, and ensure that
information it gathers provides an adequate basis for enforcement.
ADEM's statutory authority for compliance monitoring for its Solid
Waste Program is set forth in sections 22-27-7, 22-27-9, 22-27-12, 22-
22A-5 and 22-22A-8 of the Code of Alabama, 1975. These portions of the
statute, as well as ADEM Admin. Code rules 335-13-1-.11(2) and 335-13-
6-.01(2) give the Department authority during an inspection to obtain
all information necessary to determine whether the owner/operator is in
compliance with State CCR requirements. This includes authority to
conduct monitoring and testing when necessary.
Based on the information Alabama has submitted on the State's
permitting requirements, EPA has preliminarily determined these aspects
of the Alabama CCR permit program provide the State with the necessary
authority to implement an adequate State program. More detail on the
review and analysis of Alabama's CCR permit program can be found in the
TSD Volume III.
C. EPA's Analysis of Alabama's Permits Issued Under the State CCR
Regulations
EPA conducted a review of Alabama's permitting decisions as part of
the Agency's evaluation of whether ADEM's CCR permit program requires
each coal combustion residual unit located in the State to achieve
compliance with standards at least as protective as the Federal CCR
regulations. 42 U.S.C. 6945(d)(1)(B). Alabama's permitting decisions
issued under its CCR regulations are directly relevant to determining
whether the State's program satisfies this statutory requirement, and
EPA considers such information to be appropriately part of the record
for a decision on the permit program when permit issuance begins prior
to approval of the State program and the Agency has information that
the State's implementation is not sufficiently protective.
ADEM submitted its revised State CCR permit program Application on
December 29, 2021. Less than a month later, on January 11, 2022, EPA
published several proposed decisions responding to requests from owners
and operators of CCR units nationwide for extensions of the April 11,
2021, deadline to cease sending waste to unlined CCR surface
impoundments (Part A proposals). EPA proposed to deny several of the
extension requests because facilities were planning to close unlined
CCR surface impoundments with, among other things, waste remaining in
groundwater without adopting engineering measures to limit the flow of
groundwater into and out of the unit. Soon after issuing the Part A
proposals, several states, utility facilities that own unlined surface
impoundments, and trade groups contacted EPA to object to the Agency's
application of the closure requirements to the unlined surface
impoundments in those proposed decisions. Based on these objections,
EPA was concerned that Alabama's and other states' CCR permit programs
were being interpreted and implemented to allow facilities to close
unlined surface impoundments without complying with all the necessary
requirements in the Federal regulations.
Because of these concerns, on March 15, 2022, EPA sent a list to
ADEM of CCR surface impoundments in Alabama that, based on the
information available to EPA, appear to be inundated by
groundwater.\14\ Over the next several months, EPA and ADEM met several
times to discuss the application of the Federal closure performance
standards to such impoundments, and to better understand how the State
interpreted its own requirements.\15\
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\14\ The CCR surface impoundments with insufficient permits that
are discussed in this Unit of the preamble are all surface
impoundments with WBWT. For a list of all the CCR surface
impoundments EPA identified in Alabama with WBWT, see Email from
Meredith Anderson to Scott Story. CCR units in AL. March 15, 2022.
\15\ Interactions between EPA and Alabama about implementation
of the State program include: April 13, 2022, meeting to discuss the
Federal closure performance standards; three separate meetings to
discuss the proposed closure requirements for Plant Gorgas, Plant
Greene County, and Plant Gadsden; May 10, 2022, meeting to further
discuss the closure performance standard and specifically how ADEM
was interpreting and applying the closure and groundwater monitoring
performance standards at the Ash Pond at Plant Gadsden; and May 28,
2022, meeting to discuss the status of closure activities at Plant
Greene County and Plant Gadsden. A list of EPA/Alabama interactions
is in the Technical Support Document Volume II.
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EPA also started reviewing permits for unlined surface impoundments
in Alabama as part of EPA's review of the State CCR permit program. As
a consequence, in meetings and in correspondence with ADEM, EPA
[[Page 55230]]
expressed concern that Alabama's permit program appeared to differ from
the Federal program, and that these differences appeared to make the
State's program less protective than the Federal program. As a result
of these discussions, on July 7, 2022, EPA informed ADEM via telephone
that EPA would be unable to approve ADEM's CCR permit program
Application until Alabama demonstrated to EPA that the State is
implementing its program to be as protective as the Federal CCR
regulations.\16\ Further, EPA explained to ADEM that it was exploring
options for actions to take at the Federal level with respect to both
the CCR permit program Application and at specific facilities where
there are outstanding concerns.
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\16\ July 7, 2022- Telephone call between Carolyn Hoskinson,
Director of EPA's Office of Resource Conservation and Recovery, and
Stephen Cobb, Chief of the Land Division at the Alabama Department
of Environmental Management.
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Throughout the course of these discussions, and in EPA's nationwide
Part A determinations, EPA explained the existing requirements under
the Federal regulations; in response, ADEM offered notably different
interpretations of some of the obligations under the State's current
closure requirements. Despite the Agency's concerns, the State
continues to implement its CCR program in a manner that is less
protective than the Federal CCR regulations, and Alabama has not
adequately explained how its alternative State program satisfies the
statutory requirement to require each CCR unit in the State to achieve
compliance with either the Federal requirements or with State standards
that are at least as protective as the Federal requirements.
As part of the evaluation of Alabama's CCR program submittal, EPA
reviewed four final State CCR permits issued by ADEM for the following
facilities: Plants Colbert, Gadsden, Greene County, and Gorgas. EPA's
review focused specifically on permits issued to unlined surface
impoundments that have closed or are closing with waste that will
remain in place below the water table, because these units have the
greatest potential to cause significant environmental and human health
effects if mismanaged. EPA limited its review to information in the
permit record (e.g., the Permit Application or information on ADEM's e-
File site) and to information publicly available on each facility's CCR
website, even though the permit record alone should contain all the
information necessary to determine whether the permit is as protective
as the Federal CCR regulations. EPA also did not attempt to catalog
every potential inconsistency between the permits and the Federal CCR
regulations. Instead, EPA concentrated on the permits' consistency with
fundamental aspects of the closure, groundwater monitoring, and
corrective action requirements. EPA took this approach because the
purpose of this review is to determine whether Alabama's program meets
the statutory standard for approval, not to reach final conclusions
about an individual facility's compliance with the CCR regulations.
During its review, EPA identified a consistent pattern of ADEM
issuing permits to CCR units that fail to demonstrate compliance with
fundamental requirements in part 257, without requiring the permittees
to take specific actions to bring the units into compliance. EPA also
identified a consistent pattern of ADEM approving documents submitted
by the facilities, such as closure plans, groundwater monitoring plans,
and assessments of corrective measures, even though the submissions
lacked critical information or are otherwise deficient. ADEM also did
not require the permittees to take any action to cure deficiencies in
the permits even where ADEM previously identified the deficiencies and
requested further information prior to issuing the final permits.
Specifically, EPA is proposing to determine that ADEM issued multiple
permits allowing CCR in closed units to remain saturated by
groundwater, without requiring engineering measures that will control
the groundwater flowing into and out of the closed unit. See, 40 CFR
257.102(d). EPA is also proposing to determine that ADEM approved
groundwater monitoring systems that contain an inadequate number of
wells, and in incorrect locations, to monitor all potential contaminant
pathways and to detect groundwater contamination from the CCR units in
the uppermost aquifer. See, 40 CFR 257.91. Finally, EPA is proposing to
determine that ADEM issued multiple permits that effectively allow the
permittee to delay implementation of effective measures to remediate
groundwater contamination both on- and off-site of the facility. See,
40 CFR 257.96-257.97. Overall, EPA's review of the permit records and
other readily available information documents a consistent pattern of
deficient permits and a lack of oversight and independent evaluation of
facilities' proposed permit terms. In each case, EPA was unable to
locate any evaluation or record of decision documenting that ADEM
critically evaluated the materials submitted as part of the permit
application, or otherwise documented its rationale for adopting them.
For all these reasons, EPA is proposing to conclude that the ADEM
permits discussed below are not as protective as the Federal CCR
regulations.
In the next several sections, EPA discusses specific issues
identified during the review of ADEM's final permits for Plants
Colbert, Gadsden, Greene County, and Gorgas.\17\ Based on EPA's review,
the Agency is proposing to deny Alabama's Application because the
State's CCR permit program does not require each CCR unit in the State
to achieve compliance with either the minimum requirements in the
Federal CCR regulations or with alternative requirements that EPA has
determined to be at least as protective as the Federal provisions.
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\17\ On January 31, 2023, EPA Region 4 sent a Notice of
Potential Violations (NOPV) and Opportunity to Confer to Alabama
Power Company. The NOPV addressed concerns with compliance of
Alabama Power Company's Plant Barry Ash Pond. The NOPV addressed the
following potential violations: failure to meet the criteria for
conducting the closure of the Plant Barry Ash Pond, failure to
establish an adequate groundwater monitoring system, and failure to
address certain site-specific criteria in the Emergency Action Plan.
Although the permit and record for Plant Barry share many of the
flaws in the CCR permits for other unlined surface impoundments in
Alabama, EPA will not address the Plant Barry permit as part of this
action because the enforcement process with the facility is ongoing.
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1. Colbert Fossil Plant
TVA owns and operates the Colbert Fossil Plant (Colbert or Colbert
Plant) located in Colbert County, Alabama, and it submitted a permit
application for the facility dated December 10, 2021.\18\ The plant
property is on the south bank of the Tennessee River, approximately 8
miles west of Tuscumbia, Alabama. The Colbert Fossil Plant was fully
idled and stopped generating electricity in March 2016. The plant had
five generating units with a combined generating capacity of 1,204
megawatts. In accordance with the ADEM Land Division, Solid Waste
Program, Standards for Disposal of Coal Combustion Residuals in
Landfills and Surface Impoundments, Chapter 335-13-15-.02, Ash Disposal
Area 4 (also called Ash Pond 4) is classified as an existing CCR
surface impoundment. Ash Disposal Area 4 is located on the southern
portion of the plant property, approximately 3,000 feet south of the
powerhouse. The CCR surface impoundment is bounded to the west by
Colbert Steam Plant Road, to the east by Cane Creek, and to the south
by Lee Highway. EPA reviewed TVA's permit application and draft and
final permits
[[Page 55231]]
for the Colbert Plant along with associated documents. Issues with
closure, groundwater monitoring networks, and corrective action at the
Colbert Plant are discussed below.
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\18\ Tennessee Valley Authority Colbert Fossil Plant (COF) Ash
Pond 4 Permit Application. Submitted to ADEM. December 10, 2021.
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a. TVA Colbert Closure Issues
The Federal CCR regulations provide two options for closing a CCR
unit: closure by removal and closure with waste in place. 40 CFR
257.102(a). Both options establish specific performance standards. 40
CFR 257.102(c) and (d). TVA closed Ash Pond 4 at Colbert by leaving the
CCR in the unit in place; but, as explained below, the TVA application
for Ash Pond 4 did not comply with the Federal closure standards for
closure with waste in place for unlined surface impoundments and ADEM
issued the permit without addressing the deficiencies.
TVA's Permit Application for the Colbert Plant explains that Ash
Pond 4 was built in 1972 and TVA completed its closure in early 2018,
prior to its application for a permit under the ADEM CCR rules in
Chapter 335-13-15.\19\ TVA elected to close Ash Pond 4 by leaving CCR
in place and constructing a final cover system over the waste, which is
estimated to be 2.6 million cubic yards (CY) of waste.\20\ Closure of
Ash Pond 4 was completed in accordance with a closure and post-closure
care plan dated February 2017, which was approved by ADEM on August 22,
2017.\21\ Closure activities were deemed complete in March 2018 and a
certification report dated September 18, 2018, documenting closure of
Ash Disposal Area 4, was submitted to ADEM.
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\19\ The terms ``Ash Pond 4'' and ``Ash Pond Area 4'' are both
used in the Colbert Plant Permit Application to refer to the
impoundment in question. For purposes of this proposal, EPA is
referring to the impoundment as Ash Pond 4.
\20\ The Permit Application states that the ``total capacity of
Ash Disposal Area 4 is approximately 2.6 million CY, covering
approximately 52 acres.'' EPA is aware that other reports State that
the ``approximate volume of CCR material at the time of the
inspection'' is 3.29 million CY. See, e.g., FY2021 Intermediate
Inspection of CCR Facilities dated May 6, 2021. For purposes of
estimating volumes of saturated CCR in this proposal, EPA is taking
an approach that provides a minimum estimate, relying on the value
presented in the Permit Application to represent the volume of CCR
in the impoundment, instead of relying on the larger estimates
established based on the inspection of the unit.
\21\ Tennessee Valley Authority. Permit Application for CCR
Surface Impoundment, TVA Colbert Fossil Plant Ash Disposal Area 4.
December 10, 2021. Attachment I.
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ADEM's Final Permit, issued in October 2022, provides the following
terms and conditions:
Closure Timeframe and Notifications. The Permittee shall close
their CCR units as specified in 335-13-15-.07(2), this permit and the
Application.
B. Criteria for Closure.
1. Cover. Closure of a CCR landfill, surface impoundment, or any
lateral expansion of a CCR unit must be completed by either leaving the
CCR in place and installing a final cover system or through removal of
the CCR and decontamination of the CCR unit, as described in 335-13-
15-.07(3)(b) through (j). The minimum and maximum final grade of the
final cover system may be less than 5 percent and greater than 25
percent, as specified in the Permit Application, for the Colbert Fossil
Plant Ash Disposal Area 4. Ash Disposal Area 4 may utilize erosion
control measures, as specified in the Permit Application, other than
horizontal terraces. (See Section IX.A. and B.)
2. Written Closure Plan. The written closure plan, as part of the
Application, must include, at a minimum, the information specified in
335-13-15-.07(3)(b)1.(i) through (vi).
According to ADEM, ``[t]he Department adopted the terms of the
closure plan as part of the permit as the Department has previously
approved the plan and determined it meets both State and Federal
regulations for closure of a CCR unit.'' \22\ Once ADEM approved and
adopted TVA's Closure Plan into the permit, the Closure Plan, rather
than the referenced State regulations, became the State requirements
with which TVA is required to comply. See, 42 U.S.C. 6945(d)(3)(A). As
discussed in detail in the next section and summarized in Table II,
between 2019 and 2021, approximately 6 to 13 feet of ash (on average)-
or 13 to 35 percent of the CCR in the closed Ash Pond remains saturated
by groundwater.
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\22\ Letter from Stephen Cobb to Carolyn Hoskinson, Responding
to EPA Comments on Proposed Permit for the
Tennessee Valley Authority Colbert Fossil Plant, October 27,
2022, Enclosure 1, page 6.
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i. The CCR in the Closed Ash Pond 4 Remains Saturated by Groundwater
Neither TVA's Closure Plan, the Permit Application, ADEM's Final
Permit, or any other document in the permitting record specifically
discuss how the closure of Ash Pond 4 would meet the closure
performance standards given the measured groundwater elevations and
hydrogeology of the site. Accordingly, EPA reviewed information in the
Permit Application as well as other publicly available information
available on TVA's CCR website to determine whether groundwater remains
in contact with the CCR in Ash Pond 4 since closure was completed in
March 2018. As described below, available groundwater measurements
recorded between 2018 and 2021 show that, even after closure,
groundwater levels at Ash Pond 4 continue to be present above the base
of the unlined impoundment, saturating a portion of the CCR in the
closed unit. EPA's basis for these findings is described in the
succeeding paragraphs, which summarize EPA's understanding of the base
elevation of Ash Pond 4 (e.g., the lowest extent of CCR in the unit),
the groundwater levels since closure was completed in 2018, and EPA's
estimate of the volume of CCR that remains saturated with liquid
(groundwater). More details on EPA's analyses can be found in TSD
Volume I.\23\
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\23\ Volume I: Technical Support Document for the Proposed
Notice to Deny Alabama's Coal Combustion Residuals Permit Program,
Supplemental Analyses of Technical Issues with ADEM Permits. U.S.
Environmental Protection Agency, Office of Land and Emergency
Management (5304T), 1200 Pennsylvania Avenue NW, Washington, DC
20460. August 2023.
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(1) Base of the Impoundment
Ash Pond 4 is a 52-acre CCR surface impoundment that was created by
constructing a single dike around the perimeter of the impoundment and
two internal divider dikes. EPA was unable to locate information in the
Permit Application or other publicly available documents that fully
describes the as-constructed configuration of the bottom of Ash Pond 4
across its entire footprint prior to the initial receipt of waste.
However, based on information in the Permit Application and documents
referenced in the Permit Application, the lowermost documented
elevations at which CCR occurs within the impoundment varies depending
on the location, ranging from approximately 413.5 to 427.1 ft above
mean sea level (MSL). See TSD Volume I, Section II.a.
EPA also relied on an average elevation to estimate the volume of
CCR in the impoundment remaining in contact with groundwater, rather
than trying to account for what may be as much as a 14-foot difference
across the 52-acre impoundment. Specifically, EPA relied on an average
bottom elevation of 422 ft above MSL, which is the average of elevation
measurements taken at 18 locations within the footprint of the
impoundment based on borings for piezometers and wells. Information on
these borings is found on construction drawings 10W395-7 through 9 and
a report from 2010. See TSD Volume I, Section II.a. This average is
also consistent with several documents in the Permit Application and
other documents that depict the
[[Page 55232]]
base of the impoundment at 422 ft above MSL. For example, Section A-A
of construction drawing 10N292R3 shows a bottom elevation of
approximately 422 ft above MSL in the vicinity of the northern
perimeter dike where the spillways were constructed. Id. at Volume I,
Section II.a.i.3. Another example is a slope stability section
supporting a steady-state seepage analysis that shows a portion of the
base of the impoundment to be at an elevation of 422 ft above MSL. Id.
at Section II.a.i.2. Similarly, design drawings from 2010 for a
temporary rock buttress and sheet pile wall constructed in a portion of
an internal divider dike show the bottom of the impoundment to be 422
ft above MSL at this location. Id. at Section II.a.i.3. A final example
is the liner design demonstration prepared by TVA to comply with Sec.
257.71 that states ``[f]rom information contained in drawing 10N290, it
was assumed the base of the pond is at elevation 422 ft.'' Id. at
Section II.a.iv. However, it is important to note that the use of the
422 ft elevation mark to represent the base of the unit was an effort
to represent average conditions. As noted earlier, the preponderance of
the evidence suggests that base of the impoundment varies depending on
the location, ranging from approximately 413.5 to 427.1 ft above MSL,
but an average value of 422 ft above MSL is technically defensible and
conservatively high. See TSD Volume I, Section II.a. Volumes during
worst case conditions (i.e., when river stages and water tables are
higher than reported values) would be greater, and actual saturated CCR
volumes could be higher than estimated if portions of the unit with
lower documented waste bottom elevations (less than 422 ft above MSL)
were considered. The estimates provided by EPA below and in the TSD
Volume I are reasonable based on the available information provided in
the Permit Application regarding the waste bottom elevations.
ii. Characterization of Groundwater Elevations
Information from TVA's Permit Application clearly supports a
conclusion that at least some portion of the CCR in Ash Pond 4 remains
saturated by continued infiltration of groundwater. The groundwater
elevation maps for 2020 and 2021 provided in the Permit Application
reveal that the lowest measured groundwater elevations range between
just over 414 to just over 416 ft above MSL.\24\ These levels are found
in groundwater monitoring wells COF-105 and CA31A, which are screened
in the residuum/alluvium layer, and consistently measure the lowest
groundwater elevations of any of the wells immediately surrounding Ash
Pond 4. In every measurement reported in the Permit Application, the
groundwater elevations measured in these wells are 0.86 to 2.7 feet
above the lowest documented elevation of CCR within the unit (413.5 ft
above MSL). Furthermore, COF-105 is located approximately 150 feet east
of the unit boundary in the downgradient direction and CA31A is located
approximately 400 feet northeast of the unit boundary in the
downgradient direction. As corroborated by monitoring well and
piezometer data from within the unit, the actual groundwater elevations
directly beneath the unit are generally higher than these minimum
recorded values, which are well beyond the unit boundary in
downgradient directions. This basic information clearly supports a
conclusion that at least some portion of the waste in Ash Pond 4 is wet
under typical conditions.
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\24\ Tennessee Valley Authority. Permit Application for CCR
Surface Impoundment, TVA Colbert Fossil Plant Ash Disposal Area 4.
December 10, 2021. Attachment H, Appendix A, Figures A-1 through A-
4.
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A closer examination of available data from the Permit Application
further supports this conclusion. Assuming that the base of the CCR is
uniformly at 422 ft above MSL, based on the contour intervals depicted
on the groundwater elevation map for February 27, 2020 (Figure A-1),
groundwater elevations range from 414.36 to 437.46 ft above MSL, and
exceed 422 ft above MSL at over fifty percent of the entire Ash Pond 4
footprint. Similarly, the groundwater elevation contours depicting the
February 22, 2021 (Figure A-3), groundwater elevation data documents
water levels ranging from 415.14 to 436.54 ft above MSL, indicating
that water levels greater than 422 ft above MSL are present at one-
third or more of the area within the impoundment.
Even though data from summer monitoring events show that summer
groundwater levels are considerably lower than the data reported for
February 2020 and 2021, there still appears to be a considerable
footprint of wet waste under all reported conditions, and conditions
indicative of groundwater saturation or infiltration into the closed
unit appear to be sustained without interruption in some regions of the
unit. On August 10, 2020 (Figure A-2), groundwater levels ranged from
414.38 to 422.58 ft above MSL and are mapped between 415 and 420 ft
over most of the unit's footprint, with a small portion in the extreme
southwest corner of the mapped area showing higher groundwater levels
of greater than 420 ft. On August 23, 2021 (Figure A-4), groundwater
elevations ranged from 414.79 to 429.00 ft above MSL and are mapped as
being greater than 422 ft above MSL beneath a somewhat larger portion
of the impoundment's surface area in the southwestern corner, with the
remainder of groundwater elevations in the unit mapped between 415 and
420 ft above MSL.
The Permit Application also presents groundwater elevation contour
maps for the Tuscumbia limestone bedrock aquifer for 2020 and 2021.
This is appropriate as there is an abundance of information contained
in the materials presented for the Permit Application, the annual
groundwater monitoring reports, and the 2019 Comprehensive Groundwater
Investigation Report that indicates that the Tuscumbia limestone
aquifer is in direct contact and is in direct hydraulic communication
with the overlying residuum/alluvium aquifer.\25\ In this respect, EPA
interprets the Tuscumbia limestone aquifer to be part of the uppermost
aquifer system for the unit. EPA's analysis in this regard is included
in Section II.b of the TSD Volume I.
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\25\ Stantec, Comprehensive Groundwater Investigation Report,
First Amended Consent Decree # 20-01-2013-900123 Ash Pond 4 and Ash
Stack 5. TVA Colbert Fossil Plant, Prepared for Tennessee Valley
Authority Chattanooga, Tennessee. May 17, 2019.
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For the Tuscumbia limestone, the Permit Application included four
contour maps from groundwater elevation measurement events on February
27, 2020, August 10, 2020, February 22, 2021, and August 23, 2021.\26\
These data sets, which are summarized in Table I below, generally
indicate that water levels in the bedrock aquifer are higher than the
422-foot base elevation beneath significant regions of the Ash Pond 4
footprint during most of these four monitoring events, particularly
during winter conditions. For February 27, 2020 (Figure A-5),
groundwater elevations in the Tuscumbia limestone ranged from 414.61 to
437.77 ft above MSL.\27\ TVA's interpretive contours depicting the
Tuscumbia limestone bedrock groundwater elevations for February 27,
2020, indicate that the entire
[[Page 55233]]
impoundment is characterized by water levels greater than or equal to
422 ft above MSL, except for a very small area near monitoring well
COF-111 near the eastern boundary. For February 22, 2021 (Figure A-7),
measured groundwater elevation data for the Tuscumbia limestone aquifer
ranged from 411.11 to 436.70 ft above MSL. TVA's interpretive contour
map for the same period indicates that groundwater levels at or above
422 ft above MSL were mapped at approximately half of the unit's
footprint. Similarly, on August 23, 2021 (Figure A-8), groundwater
elevation data ranged from 413.47 to 429.07 ft above MSL and
interpretive contours for same period for the Tuscumbia limestone
bedrock aquifer again indicate that approximately 50 percent of the
unit's footprint exhibits groundwater levels at or above 422 ft above
MSL. Conditions during the August 10, 2020 (Figure A-6), monitoring
event show lower groundwater levels, with groundwater elevation values
for the Tuscumbia limestone aquifer ranging from 412.85 to 422.54 ft
above MSL. TVA's interpretive groundwater elevation contours for the
same period show groundwater elevations below 422 ft above MSL in all
areas except for a small portion near the southwestern corner of the
unit. It should also be noted that surface water levels associated with
the four monitoring events listed above indicate that surface water
levels in the Pickwick Reservoir are greater than 413.5 ft above MSL
(the lowest documented waste bottom elevation) for two of the four
monitoring events as shown in Table I. It is also worth noting that
river stage, which fluctuates, was measured as above the lowest
groundwater elevations measured in the Tuscumbia limestone for three of
the four time periods presented in the Permit Application.
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\26\ Permit Application at Figures A-5 through A-8,
respectively.
\27\ The elevation corresponding to wells CA29BR and CA22B on
Figures A-5 through A-8 were excluded from this range based on TVA's
footnote indicating these wells are ``poorly connected to site wide
groundwater flow system.''
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Together with the documented occurrence of solution features in the
limestone and associated preferential pathways in groundwater, it is
reasonable to expect some degree of hydraulic communication between the
reservoir/river and the underlying limestone aquifer. Depending on the
magnitude and duration of the occurrence of higher river/reservoir
levels, some degree of recharge from the river to the underlying
aquifers may be expected. It is perhaps partly for this reason that the
CCR in the unit remains wet, at least intermittently, so many years
after the unit was closed. Despite the disclaimer,\28\ which appears on
all the Tuscumbia groundwater elevation maps in the Permit Application,
EPA believes that the interpretive contours provided on these maps
corroborate the anisotropic groundwater flow conditions to which TVA
refers. EPA's interpretation of this information confirms the presence
of northeast striking preferential pathways within the Tuscumbia
limestone aquifer. In any event, the measured head values in the
Tuscumbia limestone aquifer within and surrounding the unit are hard
data points that enable the simplistic analysis regarding position of
the waste relative to measured water levels. EPA's analysis and
reasoning on this subject are further detailed in Section II.b of the
TSD Volume I.
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\28\ Permit Application at Note ``1'' on Figures A-5 through A-
8.
Table I--Maximum and Minimum Reported Groundwater Elevations a for the Tuscumbia Limestone and Associated
Contempraneous River Stage Elevations for Pickwick Reservoir on Four Monitoring Events During 2020-2021
----------------------------------------------------------------------------------------------------------------
Feb 27, 2020 Aug 10, 2020 Feb 22, 2021 Aug 23, 2021
----------------------------------------------------------------------------------------------------------------
High Groundwater Elevation...................... 437.77 422.54 436.7 429.07
Low Groundwater Elevation....................... 414.61 412.85 411.11 413.47
River Stage \b\................................. 410.95 414.24 412.41 413.79
----------------------------------------------------------------------------------------------------------------
\a\ All data presented in feet above MSL, NGVD 29 datum.
\b\ River stage values obtained from Figures A-5 through A-8 in the Groundwater Plant in the Permit Application.
The groundwater elevations provided in the Permit Application are
based primarily on data collected from outside of the unit, without
consideration of actual groundwater levels directly within and beneath
the unit. Although data from inside the unit were not provided in the
Permit Application, data from piezometers and monitoring points within
Ash Pond 4 are available in the Annual Inspection Reports posted on
TVA's CCR website. EPA reviewed the water level information reported in
the Annual Inspection Reports from 2016 through 2022.\29\ These reports
document the change of water levels within the unit over time since
closure and provide for a direct, more highly resolved and
representative analysis of actual groundwater levels and conditions
directly within and beneath the unit. These data demonstrate that
significant areas and volumes of CCR below the water table have been
and remain sustained within the unit as discussed in further detail
below. These data also enabled EPA to estimate the minimum volumes of
saturated CCR that remain in the closed unit under various observed
conditions.
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\29\ The TVA reports are titled: 2022 Engineering (Annual)
Inspection of CCR Facilities dated May 9, 2022; FY2021 Intermediate
Inspection of CCR Facilities dated May 6, 2021; FY2020 Intermediate
Inspection of CCR Facilities dated July 29, 2020; FY2019
Intermediate Inspection of CCR Facilities dated August 30, 2019;
FY2018 Intermediate Inspection of CCR Facilities dated September 4,
2018; and FY2017 Intermediate Inspection of CCR Facilities dated
December 15, 2017. Collectively, EPA is referring to one or more of
these reports as the ``Annual Inspection Reports.''
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The most recent Annual Inspection Report from May 2022 states that
``[t]here are 54 automated vibrating wire piezometers, eight (8)
automated slope inclinometers, and six (6) manual magnetic
extensometers installed at Ash Disposal Area 4.'' The Annual Inspection
Reports categorize the piezometers as ``A'' or ``B'' in the
alphanumeric identifiers assigned to each individual piezometer.
Because many of these ``A'' piezometers have recorded ``dry''
conditions in later monitoring events, it appears that the ``A'' series
piezometers generally represent the shallower portions of the
subsurface beneath the unit, e.g., screened primarily in CCR materials.
While there seems to be some degree of overlap in the vertical
dimension, the ``B'' series piezometers appear to be screened into
generally deeper stratigraphic intervals than the ``A'' series, and
generally reflect water levels in the deeper portions of the CCR waste
as well as the underlying native aquifer materials in contact with the
waste.
The groundwater elevations measured in ``A'' and ``B'' series
piezometers for the post-closure period from 2019 through 2021 varied
over similar ranges. Groundwater elevations measured in the ``A''
series ranged from 414.58 to 447.4
[[Page 55234]]
ft above MSL during this post-closure period whereas groundwater
elevations in the ``B'' series ranged from 414.5 to 445.1 ft above MSL
during the same period. Average piezometric water levels in the shallow
``A'' piezometers during this post-closure period were generally at or
above 430 ft above MSL beneath most of the footprint of the unit,
except for a lobe of lower groundwater elevations (generally measured
from 423 to 428 ft above MSL or below) in the east-central portion of
the unit. The only groundwater elevations measured at or below 422 ft
above MSL were at locations on the extreme eastern edge of the
impoundment or further eastward in the vicinity of Cane Creek. At the
deeper ``B'' piezometers, average groundwater elevations during the
post-closure period from 2019 to 2021 were observed to be universally
greater than 425 ft above MSL except for a thin strip along the eastern
margin of the impoundment containing a small area (approximately 15% or
less of the unit's footprint area) of somewhat lower groundwater
elevations (ranging generally from 416 to 424 ft above MSL), which
projects into the unit in the vicinity of piezometer COF_P4_VWP03_B.
Lastly, the most recently reported groundwater elevation measurements
in each piezometer and well (in 2021) continue to show a similar
pattern, with nearly all groundwater elevation values between 425 to
440 ft above MSL, except for a thin strip of lower groundwater
elevations near the extreme eastern margin of the impoundment, again
with a small lobe-shaped area of lower groundwater elevations (421.5 to
424.2 ft above MSL) projecting a short distance into the central part
of the unit from the east-central edge. Again, groundwater exceeding
the average waste elevation of 422 ft above MSL was measured across
virtually the entire unit.\30\
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\30\ EPA's analysis of post-closure (2019-2021) groundwater
elevations within the unit evaluated ``A'' and ``B'' series
piezometers. It should be noted that the ``A'' series also included
a number of additional piezometers with an ``S'' designation
indicating shallow screened interval depths. Evaluation of ``A''
series data also included shallow alluvium monitoring wells COF-104,
-105, and -111, and CA-17A. Evaluation of ``B'' series data also
included alluvium monitoring wells COF-104, -105, and -111. It
should be noted that these monitoring wells are located along the
extreme eastern periphery of the unit or downgradient to the east of
the unit. It is also noted that these few monitoring wells
consistently recorded some of the lowest groundwater elevations in
the combined ``A'' and ``B'' data sets. In this this respect, the
average values for the ``A'' and ``B'' piezometers are somewhat
lower than they would be if the monitoring well data were excluded.
This is to say that actual average groundwater elevation conditions
within the unit proper are likely slightly higher than these
assessments reflect due to the inclusion of the monitoring well
data.
---------------------------------------------------------------------------
EPA also evaluated these data using common commercially available
software for contouring groundwater data,\31\ creating a series of maps
that present a series of potentiometric surfaces and groundwater
elevation measurements based on monitoring well and piezometer data
from within Ash Pond 4, for various time frames and representative
values, including pre-closure, during or immediately after closure, and
post-closure. These groundwater elevation contour maps are available in
Section II.b of the TSD Volume I.
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\31\ EPA used EnviroInsite software to visualize geotechnical
data (e.g., contouring groundwater elevation data from discrete
point measurements).
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While different software packages could be used to contour
groundwater data and many different interpolation methods, EPA's
contouring approach honors the data and other known constraints and is
a conservate estimation of site conditions on those dates. These
computer-generated contour maps are useful to illustrate what the
measured groundwater elevations reveal: that groundwater levels
decreased immediately after closure, but even several years later
groundwater levels continue to exceed not only the lowest documented
waste bottom elevation (413.5 ft above MSL), but also the average waste
bottom elevation (422 ft above MSL) of the CCR in the unit. The
computer-generated contours of average groundwater elevations
representing pre-closure conditions measured at monitoring wells from
January 1, 2016, through December 31, 2017, indicate pronounced
groundwater mounding centered on the central and southcentral portions
of the unit where a broad region of groundwater elevations on the order
of 450 ft above MSL are outlined. See Section II.b in TSD Volume I.
Contours of average groundwater elevations over a timeframe that
includes the initiation of unit closure, measured at monitoring wells
and piezometers from January 1, 2018, through December 31, 2019,
indicate a reduction in the groundwater elevations beneath the central
part of the unit to values on the order of 430 ft above MSL. A
significant reduction in groundwater elevations as compared to pre-
closure conditions is evident from these data. Id. Further decreases in
groundwater elevations are indicated from computer-generated contours
of average groundwater elevations measured at monitoring wells and
piezometers post-closure from January 1, 2020, through December 31,
2021. However, the magnitude of groundwater elevation decreases is much
smaller compared to the period just after closure, with the
northeastern corner of the unit indicating the greatest relative
decrease. Id. It is important to note that despite the post-closure
decreases in groundwater elevations, groundwater levels currently
remain well above the lowest recorded waste bottom elevation (413.5 ft
above MSL) of CCR in the unit as well as the average (422-ft above MSL)
waste bottom elevation of CCR at the preponderance of the impoundment.
It is important to note, however, that the foregoing analyses are
somewhat skewed to the high side of the range of groundwater
fluctuation because the Annual Inspection Reports list the highest
recorded value for each location over the reported time interval
(approximately the previous year). It is possible that some portions of
the unit are above the water table during certain times of year or
under certain hydrologic conditions. Nevertheless, the available
reported data strongly suggests that there is a large and measurable
volume of persistent wet CCR present in the closed unit. With these
caveats, EPA's overall analysis of groundwater elevation data for Ash
Pond 4 is as follows.
Prior to closure, there appears to have been significant
groundwater mounding beneath Ash Pond 4 that has slowly decreased since
pond closure. Such mounding resulted in substantially higher
groundwater levels directly beneath the impoundment that generally
decrease radially (as indicated by lower levels consistently measured
in the monitoring wells in the peripheral and downgradient portions of
the unit). As discussed above, it appears that the ``A'' piezometers
(assumed shallow) are screened within the CCR materials and are
measuring piezometric head beneath the impoundment area and the
(assumed) deeper ``B'' piezometers are sampling groundwater in the
native geologic materials and/or CCR near the base of CCR waste beneath
the impoundment. The reported groundwater elevations in both the ``A''
(shallow) and the ``B'' (deeper) piezometers indicate that groundwater
continues to infiltrate into the CCR in many portions of the closed
unit as noted in the paragraphs above. While the assumed deeper
piezometers (``B'' series) typically have water levels somewhat closer
to those observed in the monitoring wells peripheral to the unit, the
generally higher elevations in the shallow (``A'') piezometers versus
the deeper (``B'') piezometers indicates that a downward vertical
gradient likely
[[Page 55235]]
existed between the impoundment and the underlying geologic materials
prior to closure, that the general potential for downward vertical
hydraulic gradients has been sustained during and following closure,
and that it persists currently, many years after closure. A detailed
analysis of well/piezometer construction information, boring logs and
other data are needed to further confirm and assess persistence,
magnitude, and variability of downward vertical hydraulic gradients
from the unit to the underlying aquifers.
Upgradient (west) groundwater elevations were consistently above
waste bottom elevations, whereas downgradient waste bottom elevations
were consistently near or above groundwater elevations. In a general
sense, Ash Pond 4 can be described as a quasi-wedge-shaped body with
higher elevations and generally thicker waste profiles on the west
side, sloping eastward where generally thinner waste profiles occur at
lower elevations to the east. While the groundwater table also
generally slopes from west to east, the groundwater elevation surface
(i.e., water table) does not fall to the level of the base of the waste
except in small portions of the eastern half of the unit, at best, and
at worst only near the extreme eastern margins of the unit. This
equates to a quasi-wedge-shaped body of saturated waste with generally
higher elevations and greatest thicknesses to the west, pinching out in
the eastward direction at the eastern margin of the unit.
These data and analyses underscore the general concerns that absent
active engineering measures, which the permit approved by Alabama does
not require, groundwater will continue to infiltrate into and flow out
of Ash Pond 4 and the waste will remain wet for the foreseeable future.
iii. Volumes of Saturated CCR Estimates
Based on the available information concerning the configuration of
the CCR waste mass, elevation and configuration of the surface defining
the interface between the CCR waste and underlying native geologic
materials, and the position of the water table under a variety of
conditions, EPA made a series of calculations to estimate the volume of
CCR in Ash Pond 4 that continues to be saturated with groundwater. In
all the estimates, the volume of saturated waste is generally estimated
to be the area within the impoundment where groundwater elevations
exceed the average bottom elevation of 422 ft above MSL, using computer
contouring software to create modeled contours of the groundwater
elevation surface within the unit. Under all scenarios considered,
substantial volumes of CCR remain saturated by continually infiltrating
groundwater. EPA's analyses and the resulting estimates can be found in
Section II.c of the TSD Volume I.
EPA estimates that significant volumes of saturated CCR currently
remain in the closed unit, ranging from 346,183 to 914,774 CY of CCR.
EPA further estimates that approximately 13% to 35% of the total volume
of CCR in the unit remains in the groundwater, and that 75% to 97% of
the total unit surface area is underlain by saturated CCR. Finally, EPA
estimates that, on average, approximately 6 to 13 feet of the CCR
remains saturated with groundwater. See Table II below.
Under this approach, EPA used a 2-ft contour interval to create
more granular digital models of the groundwater surface elevation.
Computer contouring software was further used to calculate the areas
contained between successive 2-ft contour lines and to calculate the
average groundwater elevation for that subregion. Saturated waste
thickness values were then calculated for each sub-area containing
groundwater elevations greater than 422-ft above MSL. Thickness values
were then multiplied by the respective areas computed for each sub-area
to obtain partial volumes of CCR in the aquifer. Total volumes of
saturated CCR were then computed by adding the partial volumes for each
sub-area.
Using this approach, three separate estimates of volumes of
saturated CCR were calculated from average groundwater elevations
reported from overburden monitoring wells for the following time
periods:
Spring 2019 (January 1, 2019, through May 31, 2019),
Spring 2020 (January 1, 2020, through May 31, 2020), and
Spring 2021 (January 1, 2021, through May 31, 2021).
Table II summarizes the volumes and areas of saturated CCR
calculated for each of these time intervals.
Table II--Depth, Surface Area, and Volume Estimates of Saturated CCR at Ash Pond 4 for 2019-2021
----------------------------------------------------------------------------------------------------------------
Estimates of saturated CCR Spring 2019 Spring 2020 Spring 2021
----------------------------------------------------------------------------------------------------------------
Total Surface Area of Unit (SY) \a\............................. 275,880 275,880 275,880
Total CCR Volume (CY) \b\....................................... 2,600,000 2,600,000 2,600,000
Average Thickness of Saturated CCR (ft)......................... 13 13 6
Surface Area of Unit with CCR in Groundwater (SY)............... 263,907 267,657 204,302
Percentage of Unit Area with CCR in Groundwater (%)............. 96 97 75
Volume Percentage of Saturated CCR (%).......................... 35 33 13
Volume of Saturated CCR (CY).................................... 914,774 858,445 346,183
----------------------------------------------------------------------------------------------------------------
\a\ Source: AECOM. Closure and Post-Closure Plan. October 12, 2016.
\b\ Source: CTI and Associates. FY2021 Intermediate Inspection of CCR Facilities. May 6, 2021.
The 2019 and 2020 total estimates of saturated CCR for the unit
were similar, 914,774 and 858,445 CY, respectively. Total volume
estimates for 2021 were lower (346,183 CY) owing to lower average
groundwater elevations over that period as compared to 2019 and 2020.
It should be noted that daily precipitation amounts from publicly
available data indicate a greater level of rainfall in the proximity of
the unit in Spring 2020 as compared to 2021. Additionally, ambient
groundwater levels in monitoring wells outside of the impoundment were
generally higher in 2020 as compared to 2021. Lastly, there is a
greater number of monitoring points with reported water level data for
2020. It is therefore likely that variations in local precipitation
exert a strong and variable influence on groundwater elevations beneath
and in the vicinity of the unit, and therefore the lower levels in 2021
are not enough to support a conclusion that the unit will eventually
dry itself out. In any case, the supplemental analysis using the more
refined contour intervals is consistent with and within the upper and
lower bounds of previous estimates, further corroborating the overall
conclusion of sustained and ongoing presence of significant volumes of
CCR that continues to be infiltrated by groundwater from within the
unit. The magnitude of the estimates clearly
[[Page 55236]]
varies in response to fluctuations in groundwater levels beneath the
unit due to variation in annual precipitation and other factors,
including closure. However, despite some evidence that water levels
have declined somewhat since closure, the record supports a conclusion
that substantial volumes of CCR will continue to be perpetually
inundated by groundwater.
Based on all these data EPA is proposing to determine that both the
Closure Plan approved by ADEM and incorporated into the permit, and the
closure itself (which ADEM also approved) are not consistent with the
requirements in Sec. 257.102(d). Neither the approved Closure Plan nor
any other document in the record for the permit accounts for the levels
of groundwater present in the unit prior to closure or describes any
engineering measures taken to meet each of the Federal CCR closure-in-
place performance standards in Sec. 257.102(d)(1) and (2) in light of
the groundwater present in the unit. Nor, based on the post-closure
groundwater elevation data from piezometer wells from 2019 to the
present, did the approved closure address the groundwater continuously
flowing into and out of the CCR, as required by the Federal
regulations.
The Federal regulations require that ``prior to installing the
final cover system . . . [f]ree liquids must be eliminated by removing
liquid wastes or solidifying the remaining wastes and waste residues.''
40 CFR 257.102(d)(2). Free liquids are defined as all ``liquids that
readily separate from the solid portion of a waste under ambient
temperature and pressure,'' regardless of whether the source of the
liquids is from sluiced water or groundwater. 40 CFR 257.53. As EPA has
previously explained, based on the regulatory terms, the structure, and
context in which the terms are employed, as well as the dictionary
definitions of ``liquid,'' and the fact that nothing in the regulatory
definition limits the source of the liquid, EPA considers groundwater
to be a liquid under the existing regulation.\32\ Consequently, the
directive applies to both the freestanding liquid in the impoundment
and to all separable porewater in the impoundment, whether the
porewater was derived from sluiced water, stormwater runoff, or
groundwater that migrates into the impoundment.
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\32\ U.S. EPA. Denial of Alternative Closure Deadline for
General James M. Gavin Plant, Cheshire, Ohio. November 18, 2022. pp
14-42; 88 FR 31,982, 31,992-31,993 (May 18, 2023).
---------------------------------------------------------------------------
TVA's Annual Inspection Reports from 2016 through 2018 show that
groundwater was infiltrating into Ash Pond 4. The average groundwater
elevations measured at monitoring wells inside Ash Pond 4 from January
1, 2016 through December 31, 2017 were on the order of 450 feet above
MSL (i.e., approximately 28 feet above the average elevation of the
CCR) centered on the central and southcentral portions of the
unit).\33\ Yet neither the approved Closure Plan nor any other document
in the record for the permit accounts for the approximately 28 feet of
groundwater present in the unit prior to closure, or describes any
engineering measures taken to eliminate the groundwater. The approved
Closure Plan states only:
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\33\ Tennessee Valley Authority. FY2018 Intermediate Inspection
of CCR Facilities. September 4, 2018; and Tennessee Valley
Authority. FY2017 Intermediate Inspection of CCR Facilities.
December 15, 2017.
Final Closure of the Ash Pond 4 requires following general
tasks: . . . Begin decanting the Ash Pond 4 using pumps and existing
siphons. Discharged water will be monitored throughout decanting
operations to maintain compliance with NPDES [National Pollutant
---------------------------------------------------------------------------
Discharge Elimination System] permitted limits.
TVA Closure Plan, pp 6-7. As EPA has previously explained, Sec.
257.102(d)(2)(i) establishes a clear standard to be met: ``free liquids
must be eliminated.'' \34\ The regulation further specifies how this
standard is to be met: by ``removing liquid wastes or solidifying the
remaining wastes and waste residues.'' Id. In situations such as this,
where the waste in the unit is inundated with groundwater, the
requirement to eliminate free liquids thus obligates the facility to
take engineering measures necessary to ensure that the groundwater,
along with the other free liquids, has been permanently removed from
the unit prior to installing the final cover system. See, 40 CFR
257.102(d)(2)(i). Yet neither the Closure Plan that ADEM approved nor
the permit ADEM issued contained any such requirements.
---------------------------------------------------------------------------
\34\ See, U.S. EPA. Denial of Alternative Closure Deadline for
General James M. Gavin Plant, Cheshire, Ohio. November 18, 2022. pp
14-42.
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Moreover, it is clear from the post-closure 2019-2021 Annual
Inspection Reports that whatever measures were taken as part of closure
did not actually eliminate free liquids from Ash Pond 4. These reports
document average groundwater elevations within the Ash Pond that
significantly exceed 422 above MSL. And the most recently reported
groundwater elevation measurements in 2021 reported nearly all
groundwater elevation at values of 425 to 440 ft above MSL, except for
a thin strip of lower ground water elevations near the extreme eastern
margin of the impoundment, again with a small lobe-shaped area of lower
levels (421.5 to 424.2 ft above MSL) projecting a short distance into
the central part of the unit. All of this information was available
before ADEM issued the permit in October 2022, yet the permit was
issued, essentially approving closure with CCR that will remain
saturated by groundwater, with no engineering measures to limit
groundwater from continually flowing into and out of the unit.
A further concern is that, given the groundwater levels that
continue to be measured in the unit, it is not clear that the remaining
wastes have been stabilized sufficiently to support the final cover
system, as required by Sec. 257.102(d)(2)(ii). What is clear, however,
is that neither the approved Closure Plan nor ADEM's permit provides
any details on how this performance standard was met, given that
groundwater continues to flow into and out of the unit from the sides
and bottom. The approved Closure Plan merely summarizes the Sec.
257.102(d)(2) performance standards, and contains, for example, no
description of how, if at all, the groundwater levels would be affected
by any of the dewatering activities associated with unit closure.
Consequently, EPA is proposing to determine that the approval of the
Closure Plan, and subsequently the unit closure itself, in the absence
of such information, and the failure to include measures in the permit
requiring TVA to remedy the omission is not consistent with Sec.
257.102(d)(2)(ii).
EPA was also unable to find any description in the ADEM approved
Closure Plan or any other permit document of engineering measures that
TVA took to ``control, minimize, or eliminate, to maximum extent
feasible'' either the post-closure infiltration of the groundwater into
the waste or the post-closure releases of CCR or leachate to the
groundwater, as a consequence of the groundwater that continues to
infiltrate into and be released from the impoundment from the sides and
bottom of the unit. 40 CFR 257.102(d)(1)(i). Based on the data and
analyses described above, groundwater continues to infiltrate into the
unit and yet the only measures described in the Closure Plan and the
permit are those taken to facilitate consolidation and cap
construction. In essence, this means the Ash Pond will continue
releasing CCR contaminants indefinitely past the waste boundary unless
TVA takes additional actions that are not required by or explained in
the permit. Given that
[[Page 55237]]
reasonably available engineering measures exist that can prevent, or at
least control, the flow of groundwater into the Ash Pond (and
consequently the releases out of the Ash Pond), such as physical
barriers or hydraulic containment systems, EPA cannot conclude that
TVA's Closure Plan adequately describes how the closure work will meet
the requirement to ``control, minimize or eliminate, to the maximum
extent feasible'' post-closure infiltration into the unit and post-
closure releases of CCR or leachate to the groundwater. EPA is
proposing to determine that the permit's exclusive reliance on
engineering measures related to the consolidation and cap construction
is inconsistent with Sec. 257.102(d)(1)(i).
In addition, EPA was unable to identify any description in the
Closure Plan narrative of how TVA will ``preclude the probability of
future impoundment of water, sediment, or slurry.'' 40 CFR
257.102(d)(1)(ii). The continued presence of groundwater in the unit
constitutes the impoundment of water, and in the absence of any
engineering measures, such as a slurry wall, there are no intrinsically
obvious facts to demonstrate that this performance standard has been
met. Finally, the Closure Plan contains no discussion of how the
closure activities will minimize the need for additional maintenance of
the Ash Pond beyond a brief discussion of the final cover system. 40
CFR 257.102(d)(1)(iv).
EPA raised these issues to ADEM in comments on the draft Colbert
permit. In response, ADEM did not dispute EPA's conclusion that CCR in
Ash Pond 4 remains saturated by groundwater. Instead ADEM stated that
EPA's comments were based on a misinterpretation of the Federal
regulations, raising three specific interpretations of the regulations
that EPA has previously rejected. First, ADEM stated that ``the Federal
CCR regulations do not require that the closure account for groundwater
levels either before or after closure.'' Rather they claim the only
requirements relevant to groundwater are the location restrictions
applicable to new or operating units in Sec. 257.60 for an operating
unit.\35\ To support this point ADEM argues that Sec. 257.102(d)(1)(i)
does not refer to groundwater. Second, ADEM argues that the Federal
standards have been met because Colbert has installed a cover system
that meets the standard in Sec. 257.102(d)(3), and the facility has
complied with all of the requirements in the general performance
standard relating to ``infiltration.'' The State supports this claim by
pointing to the absence of specific requirements for an infiltration
layer or barrier along the sides or bottom of a CCR unit, and by
defining ``infiltration'' to refer exclusively to vertical infiltration
from the surface, e.g., as rainwater entering through the cover system.
Finally, ADEM states that ``In the event that it is determined that the
closure activities conducted at Ash Disposal Area 4, as described
above, are insufficient to prevent further groundwater contamination,
additional controls or methods will be considered and addressed through
the ongoing Assessment of Corrective Measures (ACM) and selection of a
final remedy,'' that is, as part of corrective action.
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\35\ Letter from Stephen Cobb to Carolyn Hoskinson, Responding
to EPA Comments on Proposed Permit for the Tennessee Valley
Authority Colbert Fossil Plant. October 27, 2022. Enclosure 1, page
6.
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EPA has explained, at length, that a closed, unlined impoundment,
where the CCR remains in groundwater several feet deep because the
facility failed to take any reasonably available engineering measures
to prevent, or at least control, the flow of groundwater into the unit
(and consequently the releases out of the unit), does not meet the
requirements of Sec. 257.102(d).\36\ Specifically, in the final
decision denying an extension under Part A for Gavin Generating
Station, EPA expressly rejected the various interpretations of the
regulatory text that ADEM offers in its October 27 letter.
Specifically, EPA rejected the claim that the Federal closure
regulations do not require a facility to address groundwater in the
impoundment as part of closure. As noted above, based on the regulatory
terms, the structure, and context in which the terms are employed, as
well as the dictionary definitions of ``liquid,'' and the fact that
nothing in the regulatory definition limits the source of the liquid,
EPA considers groundwater to be a ``liquid'' under the existing
regulation. See, Gavin Final Denial, p, 34; Response to Comments (RTC)
on Gavin Proposed Denial, pp. 42-43, 53-58, 76.\37\ Moreover, the
source of the liquid is not important with respect to its basic and
fundamental designation as a liquid. It therefore does not matter
whether the liquid in the surface impoundment comes from the rain,
waters the facility deliberately places in the unit, floodwaters from
an adjacent river, or from groundwater--all are liquids, and once
present in the unit, they have the same potential to create leachate
(another type of liquid), as well as to contribute to hydraulic head
and drive flows driven by hydraulic gradients, and potentially
destabilize the cover system.
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\36\ U.S. EPA. Denial of Alternative Closure Deadline for
General James M. Gavin Plant, Cheshire, Ohio. November 18, 2022. pp
14-42.
\37\ U.S. EPA. Denial of Alternative Closure Deadline for
General James M. Gavin Plant (Cheshire, Ohio) Response to Comments
on Proposed Denial (Docket ID No. EPA-HQ-OLEM-2021-0590). November
2022.
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EPA also explained its decision to rely on the plain language
meaning of ``infiltration,'' explicitly rejecting the interpretation
that the term refers only to the vertical migration of liquid through
the cover system. See, Gavin Final Denial, pp 34-38; RTC pp. 38-47.
Finally, EPA rejected the interpretation that under part 257 risks from
a CCR unit submerged in groundwater are properly addressed exclusively
as part of corrective action. Gavin Final Denial, pp. 41, RTC, pp 65-
68, 102. Accordingly, EPA is proposing to determine that ADEM's permit
approved a closure of Ash Pond 4 that is not consistent with Sec.
257.102(d).
Because Alabama interprets its regulations to impose different
requirements than the Federal regulations in part 257, EPA must
determine that the State's requirements are ``at least as protective
as'' the Federal requirements in order to approve the program. 42
U.S.C. 6945(d)(1)(B)(ii). All the information available to EPA supports
a conclusion that the closure approved in the Colbert permit is
significantly less protective than a closure that meets the
requirements under the Federal CCR regulations. Simply put, this is
because allowing groundwater to continue flowing through the waste
indefinitely will not protect human health and the environment. As
discussed at length in 88 FR 32008-32012 (May 18, 2023), there are
several ways in which the failure to remove CCR from the water table as
part of closure can result in significantly higher risks than a
comparable closure where waste no longer remains in contact with the
water table.
The Electric Power Research Institute (EPRI), a coal industry
analytical group, reached similar conclusions in a report issued in
2006, finding that ``[c]aps are not effective when CCP is filled below
the water table, because groundwater flowing through the CCP will
generate leachate even in the absence of vertical infiltration through
the CCP.'' 38 39
[[Page 55238]]
Similarly, an earlier EPRI study examined the dewatering of three
sites, two with ash situated above the water table and one with ash in
contact with groundwater. The study concluded: ``[T]he existence of
saturated ash will greatly reduce the effectiveness of any cap design
when the facility is underlain by geologic materials with high
hydraulic conductivity, because groundwater will continue to leach ash
constituents.'' \40\ The fact that coal ash is in contact with
groundwater can reduce the effectiveness of dewatering as well:
``[W]hen ash remains below the water table, dewatering may be less
effective because groundwater continues to leach constituents from the
saturated ash, particularly if the impoundment is underlain by geologic
media with relatively high rates of groundwater flow. In the case of
[the studied site], concentrations increased because groundwater
contact time with the saturated ash increased when the hydraulic
gradient of the pond was removed.''
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\38\ CCP means ``coal combustion product,'' another term for
CCR.
\39\ Electric Power Research Institute. Groundwater Remediation
of Inorganic Constituents at Coal Combustion Product Management
Sites, Overview of Technologies, Focusing on Permeable Reactive
Barriers. Technical Report. 2006. 3-6.
\40\ Electric Power Research Institute. Evaluation and Modeling
of Cap Alternatives at Three Unlined Coal Ash Impoundments.
Technical Report. 2001.1005165.
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Finally, EPA is proposing to determine that the record fails to
support a finding that ADEM's alternative approach of relying on
corrective action to impose additional controls through the ongoing ACM
and selection of a final remedy will be as protective as the Federal
requirements. As discussed previously, data that was available at the
time of permit issuance documents that groundwater elevations remain
within the Ash Pond over three years after closure was completed, yet
the permit that ADEM issued is silent on the need to address this as
part of the corrective action process. Moreover, as discussed in the
next section, EPA has serious concerns about the protectiveness of the
corrective action at Colbert that ADEM is overseeing; for example, it
has been three years since TVA posted its initial ACM, and the facility
has still not selected a remedy. EPA is aware of no information to
support a conclusion that continuing to allow saturated CCR to remain
in Ash Pond 4 while TVA delays corrective action will protect human
health or the environment, and ADEM has offered no explanation to
support a conclusion that it is.
Accordingly, EPA is proposing to determine that the permit for the
Colbert Plant does not require TVA to achieve compliance with either
Sec. 257.102(d) or with alternative State standards that EPA has
determined to be at least as protective.
b. Groundwater Monitoring and Corrective Action Issues
i. Summary of Federal Requirements
The objective of a groundwater monitoring system is to characterize
groundwater to determine whether it has been contaminated by the CCR
unit being monitored. This begins in detection monitoring, by
conducting statistical comparisons between (1) The background level of
a constituent measured in one or more upgradient wells, and (2) The
level of that same constituent in a downgradient well. If the
concentration of the constituent in the downgradient well is higher
than the background concentration by a statistically significant
amount, (i.e., a statistically significant increase (SSI) over
background has been detected), this provides evidence of a potential
release from the unit. After an SSI, assessment monitoring is required
for additional constituents, and the concentrations of each of those
constituents at downgradient wells are compared to a groundwater
protection standard established for each constituent (either background
level or a regulatory limit). Prompt contaminant detection is important
in order for corrective measures to be developed to stop migration of
contaminants as soon as possible.
To ensure detection of a release, the regulations establish a
general performance standard that all groundwater monitoring systems
must meet: all groundwater monitoring systems must consist of a
sufficient number of appropriately located wells that will yield
groundwater samples in the uppermost aquifer that represent the quality
of the background groundwater and the quality of groundwater passing
the downgradient waste boundary, monitoring all potential contaminant
pathways. 40 CFR 257.91(a)(1) and (2). Because hydrogeologic conditions
vary so widely from one site to another, the regulations do not
prescribe the exact number, location, and depth of monitoring wells
needed to achieve the general performance standard. Rather the
regulation requires installation of a minimum of one upgradient and
three downgradient wells, as well as any additional monitoring wells
necessary to achieve the general performance standard of accurately
representing the quality of the background groundwater and the
groundwater passing the downgradient waste boundary, monitoring all
potential contaminant pathways. 40 CFR 257.91(c)(1) and (2). The
number, spacing, and depths of the monitoring wells must be determined
based on a thorough characterization of the site, including a number of
specifically identified factors relating to the hydrogeology of the
site (e.g., aquifer thickness, groundwater flow rates and direction).
40 CFR 257.91(b). Groundwater elevation measurements must be obtained
around the unit(s) at sampling events over time to characterize
groundwater flow direction and identify seasonal and temporal
fluctuations. 40 CFR 257.91(b). Further, any facility that determines
that the regulatory minimum number of wells is adequate to meet the
performance standard must document the factual basis supporting that
determination. 40 CFR 257.91(f). In essence, the regulation establishes
a presumption that the minimum of one upgradient and three downgradient
wells is not sufficient, and it requires the facility to rebut the
presumption in order to install only this minimum. See, 80 FR 21399.
The number and placement of the monitoring wells is critical to proper
characterization of the groundwater.
The Federal CCR regulations establish a phased approach to
monitoring. The first phase is detection monitoring where ``indicator''
constituents are monitored to determine whether groundwater is
potentially being contaminated. In selecting the parameters for
detection monitoring, EPA chose constituents that are present in CCR
and would rapidly move through the subsurface, and thus provide an
early indication of other contaminants that may be migrating from the
CCR units. See, 80 FR 21397. The constituents that are monitored in
detection monitoring are listed in Appendix III to 40 CFR part 257.
After groundwater samples are collected during each monitoring
event, the samples are sent to a laboratory for analysis to determine
constituent concentrations. Once the facility has the analytical
results, it must conduct statistical analyses to determine the
background level of each constituent in upgradient groundwater for
comparison with data from downgradient compliance wells. This stage is
also critical, as even a sufficient number of properly placed wells
will not provide adequate characterization if the sampling and analysis
of data are not properly conducted. In order for upgradient groundwater
quality to be accurately characterized, the statistical approach must
be appropriate for site conditions and the data sets obtained. To this
end, the regulations require an owner or operator to select a
statistical approach and meet the performance
[[Page 55239]]
standards applicable to that approach when analyzing the data. 40 CFR
257.93(f)-(g).
If a facility determines that there is an SSI over background
levels for one or more of the constituents in Appendix III at a
monitoring well at the downgradient waste boundary, there is an
opportunity to complete an alternate source demonstration (ASD) showing
that a source other than the unit (i.e., an alternate source) was the
cause of the SSI. 40 CFR 257.94(e)(2). A successful ASD must be
sufficient to rebut the presumption that the CCR unit is the source of
the SSI in a downgradient well of a properly designed groundwater
monitoring network by demonstrating that a source other than the CCR
unit is responsible for the SSI. An ASD requires conclusions that are
supported by site-specific facts and analytical data in order to rebut
the site-specific monitoring data and analysis that resulted in an SSI.
Speculative or theoretical bases for the conclusions are insufficient.
If a successful ASD for an SSI is not completed within 90 days, an
assessment monitoring program must be initiated. Id.
In assessment monitoring, facilities are required to monitor for
additional constituents of concern, which are listed in appendix IV to
part 257. Whenever assessment monitoring results indicate a
statistically significant level (SSL) exceeding the groundwater
protection standard has been detected at a downgradient well for any of
the Appendix IV constituents, the facility must start the process for
cleaning up the contamination by characterizing the nature and extent
of the release and of site conditions that may affect the cleanup, and
by initiating an assessment of corrective measures.
As discussed in Unit III.B of this preamble and TSD Volume III,
Alabama adopted regulations that mirror the Federal CCR regulations.
ii. TVA Colbert Groundwater Monitoring Issues
ADEM approved the Groundwater Monitoring Plan (GWMP) dated December
10, 2021, and incorporated the approved plan into the Final Permit.\41\
Once ADEM approved and adopted TVA's GWMP into the permit, the GWMP,
rather than the referenced State regulations, became the State
requirements with which TVA is required to comply. After reviewing the
GWMP and all the materials in the permit record, EPA is proposing to
determine that the groundwater monitoring network that ADEM approved is
less protective than the Federal regulations in several regards. As
discussed below and in the technical support document, EPA identified a
number of deficiencies in the approved monitoring network.
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\41\ Alabama Department of Environmental Management. Colbert
Fossil Plant Coal Combustion Residual Permit. Permit No. 17-11,
October 25, 2022. Section V.A., specifying that ``The Permittee
shall install and/or maintain a groundwater monitoring system,
identified in Table 1, as specified in 335-13-15-. 06(2) and the
approved groundwater monitoring plan.''
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First, EPA is proposing to determine that the approved monitoring
system inappropriately includes numerous monitoring wells located
beyond the waste boundary, as well as an insufficient number of
monitoring wells at necessary locations and vertical depths to ensure
that all potential contaminant pathways have been monitored. In
addition, EPA has identified critical deficiencies in the construction
of a significant number of the bedrock monitoring wells that call into
question the accuracy of the monitoring data. As a consequence, EPA is
proposing to determine that ADEM's Final Permit fails to require TVA to
``install a groundwater monitoring system that. . .accurately
represent[s] the quality of the groundwater passing the waste boundary
of the CCR unit, [and to monitor] all potential contaminant pathways.''
40 CFR 257.91(a)(2).
(1) ADEM Issued a Final Permit That Approved the Bedrock Wells To Not
Be Installed at the Waste Boundary in Accordance With Sec. 257.91(a)
The Federal CCR regulations require that a downgradient monitoring
system ``be installed at the waste boundary that ensures detection of
groundwater contamination in the uppermost aquifer,'' and define the
uppermost aquifer as ``the geologic formation nearest the natural
ground surface that is an aquifer, as well as lower aquifers that are
hydraulically interconnected with this aquifer within the facility's
property boundary.'' 40 CFR 257.53, 257.91(a)(2). The cross sections
and boring logs that were included as attachments to the Permit
Application confirm that the unconsolidated and underlying limestone
aquifers are hydraulically interconnected and communication via
vertical migration can occur. The hydraulic connection between the
Tuscumbia limestone aquifer, and the Tennessee River/Pickwick Reservoir
and Cane Creek, as well as the hydrogeologic continuum between the
Tuscumbia limestone and the overlying epikarst, residuum, and alluvial
units of the upper aquifer system, all indicate that the Tuscumbia is
an integral part of the composite uppermost aquifer system.
Accordingly, the entire horizontal length along the CCR unit must be
monitored in all hydrogeologic units present, alluvium, residiuum,
epikarst, and bedrock in accordance with Sec. 257.91.
The approved GWMP includes bedrock monitoring wells COF-111BR, COF-
112BR, COF-113BR, COF-114BR, CA17B, CA30B, MC1, MC5C, and COF-108BR
(future installation), CA6 (background), and COF-116BR (background) as
part of the groundwater monitoring system. However, none of these
bedrock wells are located at the downgradient waste boundary as
expressly required by Sec. 257.91(a)(2). Instead, they are located
hundreds of feet away from this boundary. Among the wells that monitor
bedrock, only COF-111BR is located adjacent to the downgradient (east)
side of the unit and the other downgradient open-borehole bedrock wells
are located hundreds of feet to the east, and in many cases on the
other side of Cane Creek.
Another systemic issue is that the bedrock wells were installed as
open-borehole completions with long permanently grouted surface
casings, and as a consequence have significant potential to
systemically exclude zones that have been ``cased off'' from the
monitoring well network. Permanent steel casing installations range
from 14.6 to 76.0 feet in length for in-program wells. These cased off
intervals represent potential data gaps, depending on the circumstances
and geology local to that specific region of the unit. As a highly
relevant example, well COF-111 is screened from 9-19 feet below ground
surface (bgs). The open interval for the adjacent well pair, COF-111
BR, is 76-126 ft bgs. This results in a 57-foot vertical gap at a
critical location adjacent to the unit's downgradient boundary, where
the groundwater quality is entirely unmonitored. This is significant
because the failure to monitor in the variable and significant zone of
transition from uppermost alluvium to residuum, epi-karst, and finally
to ``unweathered'' limestone would be a significant and systemic data
gap in potential contaminant pathways. Accordingly, EPA is proposing to
determine that ADEM has approved a monitoring plan with an insufficient
number of monitoring wells at necessary locations and vertical depths
to ensure that all potential contaminant pathways have been monitored.
[[Page 55240]]
(2) ADEM Approved Wells That Were Not Constructed in Accordance With
Sec. 257.91(e), and as a Consequence the Monitoring System Does Not
Accurately Represent the Quality of Groundwater Flowing From Ash Pond 4
The Federal regulations provide that ``monitoring wells must be
cased in a manner that maintains the integrity of the monitoring well
borehole.'' 40 CFR 257.91(e). Integrity of the monitoring well borehole
includes all elements of the well within and including the borehole
itself. Such elements include the surface casing, generally intended to
isolate deeper geologic materials (commonly consolidated materials,
i.e., bedrock) from overlying unconsolidated materials and associated
groundwater, but also the filter pack, bentonite and grout seals,
screened intervals, riser pipe, and other constructed monitoring well
elements internal to the borehole used to isolate and ensure the
integrity of the sampling interval (e.g., screened interval). The
integrity of these elements individually and as an integrated system is
essential to meeting the performance standards in Sec. 257.91(a), (b),
and (e).
As noted in ADEM's October 27, 2022 letter, these installations
included installation of a permanently grouted surface casing. ADEM
further indicated Rotosonic drilling methods were used to identify the
first three-to five-foot zone of unweathered material, and that a
casing was installed from this depth to the ground surface. It should
be noted that Rotosonic drilling can be a disruptive process that may
not result in full recovery of undisturbed samples of soil or bedrock.
For this reason, absent any additional information, the use of the
Rotosonic method as a tool for discriminating between weathered,
partially weathered, and unweathered bedrock, must be used with care,
particularly if sample materials are altered, pulverized, or otherwise
destroyed or obfuscated by the process of drilling as indicated by a
``no recovery'' zone or interval.\42\ In a variable zone of transition
from weathered material (residuum) to unweathered bedrock (in this case
limestone), recovered samples from each type of material would likely
be affected by the drilling process to some degree, and most competent
intervals are often preserved to a greater degree than decomposed or
partially decomposed intervals. In such a context, absent documentation
demonstrating a continuous core sample from the interval in question,
with full recovery, which penetrates and unequivocally identifies the
interface between weathered and unweathered material, it would not be
possible to confirm that any missing sample intervals did not simply
represent voids or other potentially permeable zones. The potential to
mischaracterize three-to five-foot zones as ``competent and
unweathered'' on the basis of an incomplete sequence of samples
therefore appears to be substantial. It should therefore be noted that
in this context a three-to-five-foot penetration into ``unweathered''
bedrock would generally not be considered a ``conservative'' approach,
absent additional information validating the integrity of the casing
seal and its effectiveness in isolating the ``unweathered'' bedrock
interval from the overlying materials. In such a scenario, at best, the
penetration of just a 3- to 5-foot interval of ``unweathered'' bedrock
with variably weathered materials just above introduces uncertainty
with respect to the integrity and effectiveness of the casing in
isolating the open interval from groundwater in the overlying residuum
and epikarst. Based on information provided, it is not clear how the
approach (as described) can be demonstrated to have achieved the
performance criteria outlined in Sec. 257.91(e).
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\42\ See Section II.d of TSD Volume I.
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In addition, the boring and well construction logs that were
included in the Permit Application indicate that nearly one-half of the
groundwater wells surrounding Ash Pond 4 were constructed as open
boreholes in bedrock, with open hole intervals ranging from 45 feet up
to as much as 100 feet in length. If EPA's analysis is accurate, nearly
one half of the groundwater monitoring wells surrounding Ash Pond 4
appear to not meet the casing requirements of Sec. 257.91(e).
One limitation of open-borehole bedrock wells of this kind is that
the entire bedrock interval serves as the monitoring zone. In effect,
the long open interval serves as a reservoir within which inputs from
various fractures intersected by the borehole are blended, resulting in
an average composition of some kind. In this situation, it is very
difficult or even impossible to monitor a specific zone because the
contaminants being monitored could be diluted to the extent of being
non-detectable. On this subject, ADEM's October 27, 2022, letter
states:
An Interstate Technology and Regulatory Council guidance
document entitled Characterization and Remediation of Fractured Rock
discusses construction and design considerations for monitoring
wells installed in karst aquifers. Section 7.3.3 states ``Where the
bedrock has adequate strength and competency, monitoring wells may
be constructed as an open borehole.'' Because of the proven
competent nature of the Tuscumbia Limestone, there is substantial
confidence that the integrity of the monitoring well borehole will
be maintained.
To justify their approval of long open borehole intervals, ADEM
states:
As described above, the karst aquifer present at this site
consists of a rock matrix with distinct fractures that create
preferential pathways for groundwater flow. Studies comparing
hydraulic properties measured within different karst aquifers
indicate that conduits typically account for more than 95 percent of
the permeability of an aquifer (Rosenberry et al., 2008). Thus,
because the majority of water within the monitoring well column will
be provided by discrete fractures of the bedrock unit, the potential
for dilution in the open hole borings would be limited.
While EPA agrees that fractured intervals in the karst limestone
aquifer are highly relevant as contaminant migration pathways as
compared to the (unfractured) rock matrix, treating all discrete
fractures that may contribute groundwater and/or contaminants to a
borehole equally would fail to ``accurately represent the quality of
the groundwater passing the downgradient waste boundary.'' 40 CFR
257.91(a)(2). The implied logical extension--that is, `the majority of
water in a large open borehole may be sampled to provide accurate and
representative groundwater samples--is simplynot correct. The technical
literature provides a many detailed examples that illustrate the
opposite conclusion. See Section II.d of TSD Volume I. A more likely
scenario is that specific fractures serve as contaminant migration
conduits and a long borehole may cross connect these fractures with
fractures containing clean and/or less contaminated groundwater. In
such a case, the water in the borehole represents in effect a blended
average of the individual contributions from the specific fractures
which it cross connects. As no information has been provided which
indicate the means or methods by which specific fractures may have been
isolated and more precisely monitored, EPA is proposing to determine
that the long-screened interval open-borehole monitoring wells yield
blended or otherwise unrepresentative samples, and thus do not comply
with the performance standards in Sec. 257.91(a)(1) and (2) and (e).
Many options are available to redevelop and reconfigure these existing
open boreholes to fully comply with the regulations, including
installing standard monitoring wells (e.g., with discrete screened
intervals) within the open boreholes with discrete
[[Page 55241]]
screened intervals targeted to the most important discrete fracture
zones, or a variety of specialized technologies and methods developed
to address fracture-specific sampling in fractured bedrock
environments. ADEM chose to approve the GWMP without requiring any of
them.
(3) ADEM's Permit Authorizes Intrawell Data Comparisons That Are Not
Consistent With Federal CCR Requirements
The approach to intrawell data comparisons described in the
approved GWMP does not require TVA to achieve compliance with the
requirement in Sec. 257.91(a)(1) to establish background groundwater
quality in an upgradient well unless the criteria in Sec.
257.91(a)(1)(i) or (ii) are met. The approved GWMP contains procedures
that would allow TVA to update the background data set used in
intrawell comparisons, which would mean including data in the
background characterization that is potentially impacted by a release
from the CCR unit.\43\ See, 40 CFR 257.91(a)(1).
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\43\ Tennessee Valley Authority. Colbert Fossil Plant Ash Pond 4
Permit Application, December 10, 2021. Appendix C Section 2.3, p. 4
of 9 (PDF p. 469 of 603).
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Intrawell comparisons are not simply a statistical method; in the
CCR regulations, they are an approach to background characterization.
Intrawell data comparisons use samples taken at different times from
the same well to characterize both background groundwater quality and
downgradient compliance groundwater quality. This means downgradient
compliance wells also serve as background wells. Alternatively,
interwell data comparisons use samples taken from different wells--
upgradient or sidegradient wells characterize background groundwater
quality and downgradient wells to characterize downgradient groundwater
quality.
The Federal CCR regulations do not mention interwell or intrawell
comparisons specifically; instead, they establish requirements for
characterizing background. Background groundwater quality is required
to be established in an upgradient well, unless a groundwater flow
gradient does not exist or it can be shown that groundwater samples
from a well that is not upgradient of the CCR unit would characterize
background groundwater quality as accurately or more accurately than
samples from an upgradient well. 40 CFR 257.91(a)(1)(i),(ii). It also
must be demonstrated that the data were gathered when the well was
known to be uncontaminated by the CCR unit. This generally means that
background data used in intrawell comparisons must be obtained prior to
placement of CCR in the unit. This also indicates a strong preference
for interwell comparison, which would necessarily be used when
background is established in any well other than a downgradient
compliance well (i.e., an upgradient or side gradient well).
The approach to intrawell data comparisons described in the
approved GWMP includes procedures to periodically update intrawell
background data sets. Updating background data sets may be appropriate
in interwell monitoring, where background groundwater quality may
change over time due to migration of contaminants toward a CCR unit
from upgradient sources. However, in intrawell monitoring, background
data were obtained at compliance wells at the downgradient boundary of
a monitored CCR unit, prior to placement of CCR in the unit. After a
CCR unit begins operation, sampling data obtained from these
downgradient wells cannot be known to be unimpacted by leakage from the
unit.
Samples from downgradient monitoring wells are intended to
determine whether a release could have occurred. If concentrations of
constituents monitored at the downgradient wells change, this would not
represent a change in background groundwater quality, it would
represent a release from the CCR unit. Mischaracterizing any increase
in constituent concentration at these wells over time as a change in
``background'' would result in elevating background levels and could
mask releases by preventing detection of SSLs of constituents, which
trigger corrective action requirements.
Because the procedures for updating background levels used in
intrawell data comparisons are approved in the Final Permit, this
permit does not require Colbert to achieve compliance with either the
Federal requirements at Sec. 257.91(a)(1) or an alternative State
requirement that is equally protective.
c. TVA Colbert Permit Corrective Action Issues
In 2018 TVA detected SSLs for cobalt and arsenic.\44\ TVA first
completed an ACM to comply with the requirements of the Federal CCR
regulations in July 2019 (``2019 ACM''). An ACM was completed in 2021
to comply with a 2018 Consent Decree issued by ADEM (``2021 CD
ACM'').\45\ The 2021 CD ACM included State requirements applicable to
units not regulated by the Federal program, as well as requirements
applicable to CCR units regulated by the Federal program.
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\44\ Tennessee Valley Authority. 2019 Annual Groundwater
Monitoring and Corrective Action Report, TVA Colbert. January 2020.
p. 3.
\45\ Notice Of Electronic Filing in the Circuit Court of Colbert
County, Alabama. Alabama Department of Environmental Management v.
Tennessee Valley Aut 20-Cv-2013-900123.00. C001 Alabama Department
of Environmental Management Joint Motion for Entry of First Amended
Consent. Decree. August 15, 2018.
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On October 25, 2022, ADEM issued the Final Permit to TVA for Ash
Disposal Area 4 (also identified as Ash Pond 4 in the 2021 CD ACM). The
Final Permit contained only the following terms and conditions for
corrective action:
C. Assessment of Corrective Measures. The Permittee must
initiate an assessment of corrective measures as specified in 335-
13-15-.06(7) if any constituent listed in Appendix IV of 335-13-15
has been detected at a statistically significant level exceeding the
groundwater protection standard, or immediately upon detection of a
release from the CCR unit.
1. The permittee must continue to monitor groundwater in
accordance with the assessment monitoring program while assessing
corrective measures.
2. Selection of Remedy. Based on the results of the corrective
measures assessment, the Permittee must select a remedy as specified
in 335-13-15-.06(8).
3. Implementation of the Corrective Action Program. Within 90
days of selecting a remedy, the Permittee must initiate remedial
activities as specified in 335-13-15-.06(9), and shall be required
to modify the permit in accordance with Section II.E.9.
In its Colbert Permit RTC, ADEM explains that:
TVA submitted to the Department an initial Assessment of
Corrective Measures (ACM) in July of 2019. A revised ACM was
submitted by TVA in April 2021 and is still undergoing a detailed
review to ensure that the proposed final remedy selected by TVA
conforms to the requirements of ADEM Admin. Code r. 335-13-15-.06(7)
and (8). The proposed corrective measures will use monitored natural
attenuation (MNA) and institutional controls, interim responses, and
adaptive management. Should additional revisions be required, the
Department will review them to ensure compliance with the
requirements of ADEM Admin. Code r. 335-13-15-.06(7) and (8).
Because an ACM has not been finalized and a final remedy has not
been selected, the permit does not include provisions for the
remediation of the groundwater at this time. However, once a final
remedy is determined complete by the Department, the permit will be
revised to include such provisions. The permit revision to include
the final remedy will include public participation.
The Final Permit issued by ADEM merely reiterates the Alabama
[[Page 55242]]
regulations, which are the same as the Federal corrective action
requirements. However, incorporating the regulations verbatim in the
permit does not require TVA to achieve compliance with those
requirements. This is because ADEM did not take into account relevant
facts about the status of corrective action at Colbert, such as whether
the 2019 ACM complied with the regulatory requirements, or whether the
2021 CD ACM complied with either the Consent Decree or the regulations
or both.\46\ Most importantly, ADEM did not adjudicate what actions are
still necessary in light of those facts to achieve compliance with the
regulations and include those actions as requirements in the Final
Permit. As a consequence, EPA is proposing to determine that the permit
in essence authorizes TVA to continue to delay selection of a remedy
well beyond the required deadline, in order to pursue assessment of a
remedy that does not appear to meet the criteria in Sec. 257.97(b).
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\46\ The Federal CCR regulations State that an ACM is complete
when it is placed in the facility operating record. 40 CFR
257.96(d). The regulations require posting of this information to
the publicly accessible website within 30 days 40 CFR 257.107(d),
(h)(8). The 2021 Revised ACM was not posted to the TVA Colbert CCR
website at the time of EPA's review.
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In the Colbert Permit RTC, ADEM states that it is still reviewing
the 2021 CD ACM and has not determined whether the ACM and TVA's
preferred remedy (MNA with institutional controls but no source control
measures beyond the existing closure with waste remaining in place)
complies with the regulations. It is not clear whether ADEM provided
comments on the 2019 ACM or whether it believes that the ACM satisfies
the requirements in Sec. Sec. 257.95 and 257.96, which remain
applicable to Ash Pond 4. ADEM also states in the Colbert Permit RTC
that an ACM has not been finalized and a final remedy has not been
selected, so the permit does not include provisions for the remediation
of the groundwater. Whether or not the 2021 CD ACM meets the
requirements of the regulations is precisely the type of adjudication
required in a permitting action. What the permittee is required to do
in order to achieve compliance with the regulations must be determined
prior to final permit issuance, because the permit must contain these
requirements. This is the role of a permitting authority (i.e., ADEM).
Under the Federal regulations, an assessment of corrective measures
that will ``prevent further releases, remediate any releases, and
restore affected areas to original conditions'' is required once
corrective action is triggered. 40 CFR 257.96. Section 257.96(c)
requires an analysis of the effectiveness of potential corrective
measures in meeting all requirements and objectives of the remedy
required by Sec. 257.97, and mandates that the analysis address at
least the criteria listed in Sec. 257.96(c)(1) through (3). Based on
the results of an ACM conducted in accordance with Sec. 257.96, a
remedy that meets the requirements of Sec. 257.97(b) must be selected
``as soon as feasible.'' 40 CFR 257.97(a).
The full extent of corrective action requirements applicable to
Colbert are not yet known due to numerous concerns about the adequacy
of the detection and assessment groundwater monitoring system and its
ability to identify all SSLs. However, based on review of the Final
Permit, the Colbert Permit RTC, the 2019 ACM, the 2021 CD ACM, and the
January 13, 2023, Progress Report, EPA has identified a number of areas
in which it appears that neither the ACMs nor the proposed remedies are
consistent with or as protective as the Federal requirements.\47\ At a
minimum, EPA would have expected the permit to have clearly established
a deadline for submission of a final ACM and to have identified
specific corrections that must be made to address the specific
deficiencies discussed in the paragraphs below.
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\47\ Tennessee Valley Authority. TVA Seventh Semi-Annual Report
on the Progress of Remedy Selection at Ash Disposal Area 4. January
13, 2023.
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i. The Colbert Permit Does Not Require TVA To Complete an ACM That
Includes an Assessment of Source Control Measures in Accordance With 40
CFR 257.96
40 CFR 257.97(b)(3) requires that all remedies control the source
of releases in order to reduce or eliminate, to the maximum extent
feasible, further releases of contaminants into the environment.
Neither the 2019 ACM nor the 2021 CD ACM contains any assessment of
measures to achieve this requirement (i.e., source control). Section
4.2. of the 2019 ACM states, ``Since closure of the Ash Disposal Area 4
CCR Unit serves as a source control measure, the remedial technologies
considered in the following sections are focused on addressing the area
of groundwater exhibiting arsenic and cobalt at concentrations above
the GWPS.'' The 2021 CD ACM also does not evaluate any source control
measures, focusing exclusively on three groundwater remediation
alternatives involving MNA.\48\ However, the assessment required by
Sec. 257.96 must include more than one source control measure, and
must actually assess how the various measures would perform according
to the criteria in Sec. 257.96(c). Here there is no assessment of the
one source control measure identified in the ACMs--the closure of Ash
Pond 4, which left a significant amount of CCR in contact with
groundwater--and how it would perform according to the criteria in
Sec. 257.96(c) compared to other source control alternatives, such as
clean closure or the imposition of engineering measures to control or
eliminate the groundwater that continues to flow in and out of the
impoundment.
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\48\ MNA refers to reliance on natural attenuation processes to
achieve corrective action objectives within a time frame that is
reasonable compared to that offered by other, more active methods.
The ``natural attenuation processes'' at work in such a remediation
approach generally include a variety of physical, chemical, or
biological processes that, under favorable conditions, act without
human intervention to reduce the mass, toxicity, mobility, volume,
or concentration of contaminants in soil or groundwater.
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ADEM's failure to require submission of an ACM that actually
evaluates whether the closure of the Ash Pond meets the source control
requirements in Sec. 257.97(b)(3) also undercuts their claim that they
will use the corrective action process to address any remaining
concerns with respect to the closure of the Ash Pond. In its October
27, 2022, letter to EPA regarding compliance at TVA Colbert, ADEM
states on page 7,
In the event that it is determined that the closure activities
conducted at Ash Disposal Area 4 . . . are insufficient to prevent
further groundwater contamination, additional controls or methods
will be considered and addressed through the on-going Assessment of
Corrective Measures (ACM) and selection of a final remedy . . .
Ash Disposal Area 4 completed closure in 2018, and groundwater
monitoring in 2022 revealed SSLs of additional constituents at wells
without prior SSLs, which indicates that the closure activities were
insufficient to prevent further groundwater contamination. Yet the
permit issued by ADEM does not require TVA to take any action to remedy
this deficiency.
ii. The Colbert Permit Does Not Require Collection of Data Needed To
Characterize Site Conditions That May Affect a Remedy To Support the
Assessments in the ACMs
40 CFR 257.95(g)(1) requires a facility to characterize the nature
and extent of the release and any relevant site conditions that may
affect the remedy ultimately selected. The
[[Page 55243]]
characterization must be sufficient to support a complete and accurate
assessment of the corrective measures necessary to effectively clean up
all releases from the CCR unit pursuant to Sec. 257.96. The 2019 ACM
and 2021 CD ACM do contain information about the delineation of the
identified releases. Although, given the concerns discussed previously
about the adequacy of the downgradient wells in the groundwater
monitoring well network, EPA is concerned that additional plume
delineations may be needed, because potential contaminant pathways are
unmonitored and additional releases may have occurred.
But critically, the reports do not include any information
collected about site conditions that would affect the efficacy of any
remedies analyzed in the 2019 and 2021 CD ACMs. Site data needed to
assess remedies vary depending on the remedy being assessed, but could
include: speciated results of constituent concentrations in groundwater
and soil, in dissolved and suspended phases; concentrations of
constituents, if present, which are necessary to complete reactions
that result in immobilization of contaminants (e.g. iron or sulfur);
and data to confirm the presence of attenuated and immobilized
contaminants in the subsurface, to demonstrate attenuation is occurring
naturally. As discussed in subsequent sections, the absence of such
data is particularly critical with respect to MNA, which is the only
remedy identified in the 2021 CD ACM. But neither ACM contains any of
these data, which would be needed to accurately assess any of the
remedies identified in the 2019 and 2021 ACMs. Yet the Final Permit
does not include terms to address these deficiencies, such as a
requirement to collect data to characterize site conditions that would
affect the corrective measures considered in either ACM, or a deadline
to submit a revised ACM that contains such data.
iii. Colbert's Permit Does Not Require an ACM That Accurately Assesses
Alternatives According to the Criteria in 40 CFR 257.96(c)
40 CFR 257.96(c)(1) requires an assessment of how well alternative
remedies will control exposure to residual contamination. Instead, the
2019 ACM assesses potential risks from any exposure to residual
contamination that may occur. This is inconsistent with the Federal
regulations and is, in any event, a less useful metric to evaluate
control measure technologies relative to one another, particularly when
more than one alternative leaves contaminants in the environment. This
is because this alternative criterion serves as an assessment of harm
from the contaminants themselves if they are not removed from the
environment, rather than an assessment of each technology's
effectiveness at removing them. For example, in Table 6-1 in the 2019
ACM--MNA is assessed as low risk with respect to this alternative
criterion, but it would have assessed poorly according to the criterion
of how well alternative remedies will control exposure to residual
contamination. This is less an assessment of MNA's effectiveness at
meeting the requirements of Sec. 257.97(b) and more an assessment of
whether those requirements must be met, which is not the purpose of the
ACM. Moreover, this conclusion of low risk is unsupported by data or
analysis.
The 2019 ACM also fails to consider safety impacts and cross-media
impacts. See, 40 CFR 257.96(c)(1). The 2021 CD ACM does not correct
this deficiency as it entirely fails to assess alternative remedies
with respect to this criterion at all. The Final Permit issued by ADEM
does not require any actions, by a deadline, to remedy these
deficiencies in the ACMs.
iv. The Final Permit Allows TVA To Continue To Pursue a Remedy (MNA)
That Has Not Been Demonstrated To Meet All of the Requirements in Sec.
257.97(b)
The 2019 ACM for Colbert identified MNA as one of several potential
corrective measures to address groundwater contamination (i.e.,
hydraulic control and treatment; in-situ treatment). However, the 2021
CD ACM considers only MNA as a primary remedy, which suggests that TVA
is now largely pursuing a remedy that relies exclusively on MNA.
MNA refers to reliance on natural attenuation processes to achieve
corrective action objectives within a time frame that is reasonable
compared to that offered by other, more active methods. The ``natural
attenuation processes'' at work in such a remediation approach could
generally include a variety of physical, chemical, or biological
processes that, under favorable conditions, act without human
intervention to reduce the mass, toxicity, mobility, volume, or
concentration of contaminants in soil or groundwater. However, mass
reduction through degradation generally is not a viable process for
most inorganic contaminants (i.e., the constituents in Appendix IV to
40 CFR part 257) in groundwater, except for radioactive decay. These
constituents are atoms, and atoms do not break down or degrade through
any naturally occurring process unless they are radioactive.
Thus, while MNA can reduce the concentration or mobility of
inorganic contaminants in groundwater if immobilization occurs through
adsorption or absorption to subsurface soils, it does not remove the
contaminants from the environment. MNA, therefore, would not perform
well with respect to the requirement in Sec. 257.97(b)(4), which
requires that remedies ``remove from the environment as much of the
contaminated material that was released from the CCR unit as is
feasible.'' This is particularly true in this circumstance, where, as
discussed in the next sections, TVA has failed to collect the site data
needed to identify whether any naturally occurring attenuation may be
occurring on-site, as well as the mechanism by which it occurs, and to
assess whether site characteristics that control and sustain this
naturally occurring attenuation are sufficient to immobilize the entire
release. Assessments in an ACM are relative in that the expected
performance of the different technologies are compared with one another
according to how well each alternative meets each regulatory criterion.
Given both the absence of any evidence of any attenuation mechanisms
occurring at the Ash Disposal Area 4, and the conclusion in the 2020
ACM that the other alternatives such as pump and treat are feasible,
there would appear to be no basis for assessing MNA more favorably than
an alternative that unquestionably removes contaminants from the
environment. The Final Permit nevertheless allows TVA to continue to
attempt to validate MNA as a technology instead of accurately assessing
alternatives based on-site conditions and selecting a remedy that meets
the requirements in Sec. 257.97(b).
v. ADEM Issued a Final Permit That Impermissibly Allows a Remedy (MNA)
That Is Based on Unsupported Assessments
The 2019 and 2021 ACMs assessed the performance of MNA favorably
without any supporting data that characterize site conditions that may
ultimately affect a remedy, as required by Sec. 257.95(g)(1). In order
to legitimately consider MNA as required by Sec. 257.96(c), site data
are needed to identify any naturally occurring attenuation that may be
occurring, and to assess whether site characteristics that control and
sustain this naturally occurring attenuation are sufficient to
[[Page 55244]]
immobilize the entire release. ``It is necessary to know what specific
mechanism (e.g., what type of sorption or reduction and oxidation
reaction) is responsible for the attenuation of inorganics so that the
stability of the mechanism can be evaluated. [. . .] Changes in a
contaminant's concentration, pH, oxidation and reduction potential
(ORP), and chemical speciation may reduce a contaminant's stability at
a site and release it into the environment.'' \49\ Determining the
existence, and demonstrating the irreversibility, of MNA mechanisms is
necessary to assess the performance, reliability, ease of
implementation, and the time required to begin and complete the remedy.
40 CFR 257.96(c)(1) and (2). This information would ultimately be
necessary to assess how well MNA meets the requirements of Sec.
257.97(b).
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\49\ Use of Monitored Natural Attenuation at Superfund, RCRA
Corrective Action, and Underground Storage Tank Sites, EPA OSWER
Directive 9200.4-17P. April 21, 1999. p. 8.
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MNA of inorganic contaminants would be assessed most favorably at
sites where immobilization is demonstrated to be in effect and the
process/mechanism is irreversible. Immobilization that is not permanent
would require ongoing monitoring in accordance with Sec. 257.98(a)(1)
as long as immobilized constituents remain in the aquifer matrix.
(1) The ACMs Do Not Include Data That Characterize Site Conditions or
Identify Any Attenuation Mechanisms Occurring at the Ash Disposal Area
4
The site data that were collected focus only on contaminant
concentrations and trend analyses regarding the presence of
contaminants. The 2019 ACM and 2021 CD ACM do not discuss how
attenuation may be naturally occurring through any particular MNA
mechanisms (e.g., adsorption, precipitation, dispersion). EPA was not
able to find any indication in the Final Permit or supporting
documentation to confirm that the Permittee has identified the
mechanism by which MNA would occur at the site. Nor is there any
condition in the Final Permit requiring the development and submission
of such information. The Final Permit should have required collection
of groundwater data (e.g., pH or oxidation potential, speciated
concentrations of constituents of concern) as well as samples to
identify the presence of immobilized constituent in subsurface soils.
The Final Permit also should have required an amended ACM which
considered this information in the assessment of all alternatives,
including assessment of the performance of identified naturally-
occurring attenuation mechanisms (i.e., MNA).
Determining the existence and demonstrating the irreversibility of
MNA mechanisms is necessary to evaluate the performance, reliability,
ease of implementation, and the time required to begin and complete the
remedy. See, 40 CFR 257.96(c)(1) and (2). This information would
ultimately be necessary to show that MNA meets the requirements of
Sec. 257.97(b) and would need to be supported with site-specific
characterization data and analysis. Yet the Final Permit contained no
terms or conditions requiring TVA to remedy these deficiencies.
(2) MNA Is Not a Viable Remedy Without Source Control
From a scientific point of view, source control is necessary in
order for any MNA remedy to be effective at a particular site.\50\ In
order to properly assess MNA, first the attenuation mechanisms (for
inorganic metals, these include both chemical and physical reactions)
by which the specific constituents released may be immobilized at a
specific site must be identified. As discussed above, no mechanism was
identified in either the 2019 or 2021 ACM. After attenuation mechanisms
are identified, it is necessary to determine whether the aquifer has
the capacity (i.e., the presence of these reactants available in
sufficient amounts) to provide those reactions to attenuate the release
that has occurred. If site data are obtained verifying the localized
presence and availability of reactants, appropriate types of soil, and
other factors needed to immobilize the constituents, it must be
determined whether they are available in sufficient quantities to react
with the quantity of constituents released. This can be done using the
estimated mass of the release that was calculated in accordance with
Sec. 257.95(g)(1)(ii), as well as site data collected to determine the
presence and concentrations of the chemical and physical materials
required to complete the immobilization reactions. If there are enough
available reactants to immobilize the entire release, and the site
conditions are right for those reactions to occur, then MNA may be
effective at immobilizing a release. However, if the source of a
release has not been controlled (i.e., the CCR remains in contact with
groundwater and releases are ongoing), then it is impossible to know if
an aquifer has the capacity to attenuate the release, even if
attenuation mechanisms have been identified and site conditions are
favorable for those reactions to occur. That is because the amounts of
contaminants being released will continue over time, and releases of
new constituents could occur. Therefore, it is impossible to determine
whether the aquifer has sufficient chemical and physical materials
required to complete the immobilization reactions because the total
amount of the release is not yet known.
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\50\ Id.
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At TVA Colbert, source control has not been achieved. As discussed
above, the closure of Ash Pond 4 has resulted in continuing releases
from the closed unit, i.e., a continual source of groundwater
contamination from the unit. Therefore, based on the current record,
MNA is not a viable remedy for Ash Pond 4. This should have been
addressed prior to permit issuance during the permit application review
stage or by some other means, such as a schedule of compliance in the
final permit, e.g., by requiring TVA to submit a revised ACM that
accurately assesses MNA and includes a corrective measure which
achieves source control in each alternative assessed.
(3) The Assessment of Cross-Media Impacts in the ACMs Is Inaccurate and
Not Supported by Data
The table in the 2019 ACM, which summarizes TVA's assessment of
groundwater corrective measures, states that MNA poses a low risk of
cross-media impacts. The reason given is that ``all work activities
occur in-situ.'' This conclusion is only accurate if natural
attenuation through immobilization is occurring on-site, but no such
showing has been made. In fact, in the absence of any information to
the contrary, it is more likely that MNA through dilution and
dispersion would occur, that is, by mixing with clean groundwater as it
migrates from the unit, ultimately transferring the contamination from
groundwater to surface water. But the transfer of contamination from
groundwater to surface water is a cross-media impact and it only occurs
in-situ until the groundwater reaches the surface water. The assessment
of low risk of cross-media impacts is therefore not supported by facts
and site data. See, 40 CFR 257.95(g)(1).
A similar table (6-1) in the 2021 CD ACM assesses ``potential
adverse impacts'' as low. Its assessment of the first alternative, MNA
with no institutional controls or adaptive management, is favorable
even though it is noted that there would be no protection of surface
water in the short term. In fact, because all three
[[Page 55245]]
alternatives rely on MNA and do not include active remediation or
containment, none of them would protect surface water in the short
term. It is unclear why this concern is not noted in all the
alternatives. There is also no discussion of long-term impacts to
surface water. Accordingly, EPA is proposing to determine that the
assessment of these potential remedies as low risk is not supported by
any evidence, and that the assessment of the third alternative does not
meet the requirements of Sec. 257.96(c)(1) because it does not
consider impacts to surface water (i.e., cross-media impacts).
The lack of data to support the assessments in both ACMs means they
may not accurately reflect MNA's ``effectiveness of potential
corrective measures in meeting all of the requirements and objectives''
in Sec. 257.97(b). 40 CFR 257.96(c) Conclusions without a supporting
assessment or data do not constitute ``an analysis of the effectiveness
of potential corrective measures.'' 40 CFR 257.96(c) (emphasis added).
In addition, inaccurate assessments in an ACM can ultimately result in
selection of a remedy that will not meet the requirements of Sec.
257.97(b). The Final Permit issued by ADEM in October 2022 does not
require TVA to take any actions to remedy the deficiencies in either
the earlier 2019 ACM or subsequent 2021 CD ACM.
(4) The 2021 CD ACM Is More Deficient Than the 2019 ACM
Even though the 2021 CD ACM was developed in response to comments
from ADEM, it not only fails to remedy the deficiencies in the 2019
ACM, but also contains provisions that raise additional concerns.
First, the remedial objectives in section 1.3 of the 2021 CD ACM do not
address the requirements in Sec. 257.97(b)(3) or (4) relating to
source control or the removal of the release from the environment--
rather, they only consider off-site impacts of groundwater
contamination.
It is unclear whether the 2021 ACM was intended to replace or to
supplement the 2019 ACM. But assessed on its own merits, the 2021 CD
ACM failed to assess two remedies included in the 2019 ACM: hydraulic
control and treatment and enhanced in-situ treatment as primary
corrective measures. Only three alternatives are considered in the 2021
CD ACM, which all rely on MNA as the primary corrective measure. The
only consideration of active corrective measures is in alternative
three, as part of an adaptive management strategy if MNA does not meet
the remedial objectives on its own. Therefore, EPA is proposing to
determine that the 2021 CD ACM does not meet the requirement in Sec.
257.96(a) to assess corrective measures ``to prevent further releases,
to remediate any releases and to restore affected area to original
conditions,'' because the alternatives, limited to MNA without
additional source control, would not meet any of these requirements at
the Colbert Plant.
(5) The Ongoing Data Collection and Model Development Are Not Necessary
To Select a Remedy
According to the January 13, 2023 Progress Report, the facility has
delayed selection of a remedy by, among other tasks, continuing to
monitor the migration of the release and developing a computer model to
predict groundwater behavior. It is not necessary to delay completion
of an ACM or selection of a remedy until a model can be developed and
refined; the Federal regulations do not require development of a
groundwater model to complete an ACM or to select a remedy. Since
actual site monitoring data-- rather than an estimate from a model-- is
required to characterize the release sufficiently to assess corrective
measures-- the primary use of a model in this stage of CCR corrective
action would be to estimate the amount of time needed to complete a
remedy. But this estimate may be accomplished through other methods
(e.g., calculation of the mass of the release, groundwater flow
velocity, hydraulic conductivity, and the attenuation capacity of the
downgradient subsurface where MNA mechanisms have been identified and
can be quantified). Nor is such delay consistent with the requirements
of Sec. 257.95(g), which only requires characterization ``sufficient
to support a complete and accurate assessment of the corrective
measures necessary to effectively clean up all releases from the CCR
unit pursuant to Sec. 257.96.'' In order to support the assessment in
the ACM, this characterization must be complete prior to the deadline
to complete the ACM.
Based on all of the above, EPA is proposing to determine that the
permit fails to require the Permittee to select its remedy ``as soon as
feasible,'' as required by Sec. 257.97(a). Section 5.C.2 of the
permit, entitled ``Selection of Remedy,'' only reiterates the
regulatory requirement that the Permittee must select a remedy as soon
as feasible. It has been three years since the 2019 ACM for the Ash
Pond was placed in the facility's operating record, and it is not clear
why the facility has not selected a remedy.\51\ The 2021 CD ACM does
not reflect progress toward selection of a remedy, as it does not
address any of the deficiencies in the 2019 ACM. For example, even
though the 2021 CD ACM focuses exclusively on MNA, it still fails to
identify any attenuation mechanism, or to include any of the supporting
data that characterize site conditions that may ultimately affect a
remedy, as required by Sec. 257.95(g)(1). For all the reasons
discussed above, EPA is proposing to determine that neither the 2019
ACM, the 2021 CD ACM, or the two ACMs taken together meet the
requirements of Sec. 257.96 or Sec. 257.97 or support selection of a
compliant remedy. By failing to require TVA to obtain the necessary
data and submit a revised ACM by a date certain, the Final Permit
appears to authorize the permittee to continue to indefinitely delay
selecting a remedy, while the permittee continues to conduct the same
sampling it has conducted since 2019, that is likely to be insufficient
to support the selection of that alternative as a remedy. Accordingly,
EPA is proposing to determine that the permit does not require
compliance with the Federal requirements and, because it allows the
facility to continue to delay corrective action, the alternative State
requirement is less protective.
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\51\ Tenessee Valley Authority. 2019 Assessment of Corrective
Measures Report for the Ash Pond TVA Colbert Fossil Plant,
Tuscumbia, Alabama. July 15, 2019.
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2. Plant Gadsden
EPA reviewed the Final Determination Initial Permit And Variance
for the Alabama Power Company, Gadsden Steam Plant (Plant Gadsden
Permit), issued by ADEM under Permit No. 28-09 on December 18,
2020.\52\ The permit summary on Page 1 says:
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\52\ Alabama Department of Environmental Management. Final
Determination Initial Permit And Variance for the Alabama Power
Company, Gadsden Steam Plant, issued under Permit No. 28-09.
December 18, 2020.
[t]he Plant Gadsden Ash Pond is a CCR surface impoundment located in
Section 2, Township 12 South, Range 6 East in Etowah County, Alabama
consisting of approximately 130.22 acres with a disposal area that
consists of approximately 58.73 acres. The permit requires the
Permittee to manage CCR in accordance with the conditions of the
permit, ADEM Admin. Code r. 335-13-15, . . . and the approved permit
application.
. . .
The Permittee must comply with all conditions of the permit except
to the extent and for the duration such noncompliance is authorized
by a variance granted by ADEM. The first variance requests to
exclude boron as an Appendix IV assessment monitoring
[[Page 55246]]
constituent. The second variance requests groundwater protection
standards of 6 micrograms per liter ([micro]g/L) for cobalt; 15
[micro]g/L for lead; 40 [micro]g/L for lithium; and 100 [micro]g/L
for molybdenum. The third variance requests the final grade of the
cover system be less than 5 percent and greater than 25 percent. The
fourth variance being requested is from 335-13-15-.03(6) requiring a
100 foot buffer from the perimeter of the facility boundary.
a. Plant Gadsden Closure Issues
Section VII.B.1 of Plant Gadsden Permit contains the following
terms and conditions:
A. Closure Timeframe and Notifications. The Permittee shall
close their CCR units as specified in 335-13-15-07(2), this permit
and the Application.
B. Criteria for Closure.
1. Cover. Closure of a CCR landfill, surface impoundment, or any
lateral expansion of a CCR unit must be completed by either leaving
the CCR in place and installing a final cover system or through
removal of the CCR and decontamination of the CCR unit, as described
in 335-13-15-.07(3)(b) through (j). The minimum and maximum final
grade of the final cover system may be less than 5 percent and
greater than 25 percent, as specified in the Permit Application.
(See Section IX.C.)
2. Written Closure Plan. The written closure plan, as part of
the Application, must include, at a minimum, the information
specified in 335-13-15-.07(3)(b) 1.(i) through (vi).
The Ash Pond was closed by removing CCR from the southern portion
of the Lower Pond (the area of the western expansions in the 1970s) and
consolidating the ash in the Lower Pond to about 30 acres in the
northern portion of the Lower Pond. The CCR in the Upper Pond (original
ash pond prior to expansions) was regraded to achieve a minimum 3%
slope, and a cover system was constructed over the re-graded Upper Pond
and consolidated ash in the Lower Pond.\53\
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\53\ Alabama Power. Revised Closure Permit Application for the
Plant Gadsden Ash Pond. April 30, 2020. Appendix 6.
---------------------------------------------------------------------------
Closure construction activities for the Ash Pond were certified as
completed in October 2018, and a certification of completion of closure
activities was later submitted in April 2020, and approved by ADEM on
June 9, 2022.54 55
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\54\ Alabama Power. Plant Gadsden 2020 Notice of Closure
Completion Plant Gadsden Ash Pond Alabama Power Company.
\55\ Alabama Power. Plant Gadsden 2022 Closure Inspection
Gadsden Steam Plant Permit No. 28-09.
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i. Base of the Impoundment
Plant Gadsden is located in Gadsden, Alabama, south of the Coosa
River. The Ash Pond is located on the north side of and adjacent to the
Coosa River. The Permit Application states that the Ash Pond was
initially constructed in 1949 and subsequently expanded to the west in
1976 and 1978.\56\ The Permit Application states that the fully
constructed Ash Pond was 75 acres. Id. at Appendix 8. Alabama Power
closed the Ash Pond by consolidating CCR to a smaller area within the
impoundment footprint. Id. at Appendix 6. As a result, the consolidated
closed footprint of Ash Pond 4 decreased to approximately 59 acres. Id.
at Appendix 2.
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\56\ Alabama Power. Revised Closure Permit Application for the
Plant Gadsden Ash Pond. April 30, 2020. Appendix 3.
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EPA was unable to locate information in the Permit Application or
other publicly available documents that characterizes the bottom
elevation of the Ash Pond across its entire footprint. Nonetheless,
similar to the review for the permit for Plant Colbert, EPA estimates
the average bottom elevation of the impoundment for purposes of
calculating the volume of CCR that remains saturated by groundwater.
EPA is estimating that the average bottom elevation of the closed Ash
Pond is 510 ft above MSL.\57\ This estimate is based on consideration
of the information available in the Permit Application. Specifically,
EPA considered the following information: (1) the original ground
surface contours shown on construction drawings for areas that were
closed by leaving CCR in place; (2) information showing that the bottom
of the impoundment was lower than the original ground surface contours
at some locations while the unit was in operation; and (3) closure-
related drawings portraying an estimated waste bottom.
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\57\ USEPA. Volume I: Technical Support Document for the
Proposed Notice to Deny Alabama's Coal Combustion Residuals Permit
Program, Supplemental Analyses of Technical Issues with ADEM
Permits. August 2023. Section III.a.
---------------------------------------------------------------------------
EPA's estimate recognizes that the original ground surface contours
for most of the impoundment footprint (both the initial footprint and
western expansions) range between 505 to 515 ft above MSL, or an
average elevation of 510 ft above MSL. In addition, certain closure
drawings show that current surface elevations in the upper northern
part of the unit are actually lower in 2016 than the original ground
surface elevations depicted on the 1978 expansion drawing. This means
that the original ground surface elevations shown on the 1949, 1976,
and 1978 drawings do not necessarily reflect the bottom of the
impoundment at closure at all locations within the unit footprint. The
2016 drawing shows the bottom elevation at this upper northern part of
the unit to be no higher than 505 to 510 ft above MSL, which is lower
than the original ground contours at this location that ranged from 510
to 515 ft above MSL. Finally, the four cross-sections provided in the
Gadsden Permit Application depict the impoundment bottom appearing to
range between 495 to 510 ft above MSL, but these cross-sections are
annotated with a note that the bottom elevations have not been
verified. Based on the available information, EPA's estimated average
bottom elevation of 510 ft above MSL is a reasonable reconciliation of
the available information.
ii. Characterization of Groundwater Elevations
The CCR program groundwater monitoring network installed at the
unit consists of fifteen downgradient monitoring wells (GSD-AP-MW-1
through MW-12 and GSD-AP-PZ-1, PZ-5, and PZ-6). The following
evaluation of groundwater elevation data for the unit focuses on the
twelve monitoring wells that are immediately adjacent to the waste
boundary (i.e., MW-1 through MW-12). Monitoring wells PZ-1, PZ-5 and
PZ-6 are located hundreds of feet from the waste boundary and thus were
not considered. Also, three ``upgradient'' monitoring wells (MW-14, -
16, and -17) are located to the southeast on the other side of the
Coosa River and are not considered with respect to groundwater
elevations within the unit. Based on the single groundwater flow map
included in the Permit Application,\58\ based on August 19, 2019, data,
groundwater elevations in monitoring wells surrounding the unit ranged
from a high of 512.03 ft above MSL along the northeastern boundary of
the unit (GSD-AP-MW-3) to 506.95 ft above MSL along the western
boundary (GSD-AP-MW-7). The potentiometric surface contour map
presented for August 19, 2019, reveals a somewhat radial flow pattern,
with highest groundwater elevation values recorded along the
northeastern boundary of the facility. Between monitoring wells GSD-AP-
MW-1 and GSD-AP-MW-4 along the northeastern boundary of the unit,
groundwater elevation values are similar, approximately 512 ft above
MSL, resulting in a northwest to southeast trending ridge-like region
of relatively high groundwater elevations.
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\58\ Alabama Power. Revised Closure Permit Application for the
Plant Gadsden Ash Pond. April 30, 2020, Appendix 7, Plant Gadsden
Ash Pond Groundwater Monitoring Plan, Figure 6.
---------------------------------------------------------------------------
Groundwater elevations drop to the north, northeast, northwest,
west and to
[[Page 55247]]
the south and southwest from this central axis which is mapped as a
groundwater divide just east of the unit boundary on the August 19,
2019, map. There are no data in the Permit Application that can enable
a determination of groundwater flow directions to the east and
southeast of the unit, thus the possibility of unmonitored flow in
these directions has not been ruled out. These uncertainties
notwithstanding (see Unit IV.C.2.b of this preamble for additional
assessment of uncertainties associated with the groundwater monitoring
network), the available information indicates that groundwater from the
Ash Pond generally flows toward the surface water features represented
by the main stem of the Coosa River as well as toward the tributary
stream segments to the north and northwest of the unit. Groundwater
elevations within the unit appear to be primarily controlled by the
consistently higher elevations along the northeastern boundary of the
unit as well as the lower elevations associated with the Coosa River to
the northwest, west, and southwest. On August 19, 2019, the elevation
of the Coosa River was reported to be approximately 508 ft above
MSL.\59\
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\59\ Volume I: Technical Support Document for the Proposed
Notice to Deny Alabama's Coal Combustion Residuals Permit Program,
EPA Analysis of Alabama CCR Permits. U.S. Environmental Protection
Agency, Office of Land and Emergency Management (5304T), 1200
Pennsylvania Avenue NW, Washington, DC 20460. August 2023. Section
III.b.i.
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It is important to note that the groundwater elevations reported on
August 19, 2019, represent a relatively low condition, on balance, and
groundwater elevation values measured at the unit are observed to
oscillate over several feet on average in response to seasonal rainfall
or other variations, with individual wells immediately adjacent to the
Ash Pond (i.e., GSD-AP-MW-1 through MW-12) varying over a range of
approximately 3.9 to 8.5 feet between 2018 and 2022,\60\ which covers
the period after closure construction activities for the Ash Pond were
certified as completed in October 2018. Similarly, the Coosa River
levels show considerable variation, ranging from 503.3 to 512.6 ft
above MSL between 2018 and 2022 as monitored by a gauge located
approximately 900 feet upstream of GSD-AP-MW-11. Given these
fluctuations, EPA considered additional groundwater elevation data from
documents included on Alabama Power's CCR website. Groundwater
elevation data from measurement events since August 19, 2019, were
initially evaluated to illustrate the range of groundwater elevation
fluctuations at the site, as summarized in Table III. The recorded
elevations of the Coosa River on the corresponding dates are also
included on the table.
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\60\ Id at Section III.c.iii.
Table III--Groundwater Elevation Fluctuations at the Ash Pond and Corresponding Coosa River Elevations a
----------------------------------------------------------------------------------------------------------------
Groundwater elevation (ft Coosa River elevation
above MSL) (ft above MSL) \b\
Date --------------------------------------------------------
Range Over 24-Hour
Maximum Minimum Period
----------------------------------------------------------------------------------------------------------------
8/19/2019.............................................. 512.03 506.95 507.6-507.8
4/13/2020.............................................. 517.91 508.71 507.9-510.3
8/24/2020.............................................. 512.57 507.64 507.8-508
3/15/2021.............................................. 516.98 507.18 507-507.4
10/4/2021.............................................. 513.76 508.03 507.9-508.1
1/11/2022.............................................. 515.65 508.01 507.8-508.2
5/5/2022............................................... 516.18 507.97 507.6-508.1
10/24/2022............................................. 510.86 506.64 \c\ 507.5-507.7
----------------------------------------------------------------------------------------------------------------
\a\ Measured at groundwater monitoring wells GSD-AP-MW-1 through GSD-AP-MW-12.
\b\ Source: U.S. Geological Survey (USGS). See Section III.b.i of TSD Volume I for further details.
\c\ These data are provisional and may be revised by the USGS.
As shown here, groundwater levels are variable, and are generally
higher during spring monitoring events (March, April) as compared to
late summer/fall events (August, October). In consideration of the 15
groundwater elevation monitoring events from October 4, 2018, through
October 24, 2022, EPA calculated average minimum, average maximum, and
overall average groundwater elevations within the unit over the four-
year period, as follows:
Groundwater Elevation (overall average): 511 ft above MSL
Groundwater Elevation (average maximum): 514.6 ft above MSL
Groundwater Elevation (average minimum): 508.6 ft above MSL
The average range of fluctuation between maximum and minimum values
at a particular monitoring well location over this same period of
interest was 5.9 feet.
These values were used in conjunction with the estimates for the
bottom-of-waste elevation to calculate estimated volumes of saturated
waste, as presented in the following section.
iii. Volumes of Saturated Ash Estimates
Based on available information and the averages discussed above,
EPA estimated the volume of CCR in the Ash Pond that, on average, would
continue to be saturated with approximately 1 to 4.6 feet of
groundwater.\61\ Because both the base elevation of the waste and the
groundwater elevations vary, those estimates both overstate and
underestimate the degree of saturation. For example, at its lowest
point, the base of the impoundment measures 505 ft above MSL, and the
highest elevation of groundwater was measured at 519.26 ft above MSL
(GSD-AP-MW-1 on February 25, 2019). However, the data show that even
during the periodically dry conditions in summer when the groundwater
elevations can decline to values approaching Coosa River surface
levels, significant volumes of saturated waste may still be present
because of uncertainties with the waste bottom elevation. If areas of
waste are present below the elevation of the Coosa River, as some
information suggests, these areas of waste are expected to remain
saturated because, absent any information to the contrary, it is
presumed that a hydraulic connection between the uppermost aquifer and
the river exists due to the close proximity of the Ash Pond to the
river. In any case,
[[Page 55248]]
the regular and significant oscillation in waters levels in the CCR
indicate that significant volumes of saturated CCR persist routinely
despite closure efforts to date. Moreover, evaluation of water level
elevations over time show that water levels are higher than the bottom
of the impoundment under most conditions, and there is no indication
from available information that this situation will change absent
additional engineering controls.
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\61\ Id at Section III.c.iv.
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EPA's analysis shows that substantial volumes of saturated CCR
currently remain in the closed impoundment under conditions where
groundwater elevations were at the overall average or maximum average
levels, ranging from approximately 95,000 to 436,000 CY, respectively.
Furthermore, these saturated volume estimates equate to approximately
8% to 36% of the total volume of CCR in the Ash Pond with an average
thickness of CCR over the entire footprint between approximately 1 to
4.6 feet of statured CCR within the unit. These estimates are further
explained in Section III.c of the TSD Volume I. Table IV summarizes the
volumes and areas of saturated CCR calculated under both conditions.
Table IV--Estimates of Saturated CCR at Plant Gadsden Ash Pond
------------------------------------------------------------------------
Overall Maximum
Groundwater elevation condition average average
------------------------------------------------------------------------
Groundwater elevation (ft above MSL).... 511 514.6
Average waste bottom (ft above MSL)..... 510 510
Saturated CCR thickness (feet).......... 1 4.6
Total CCR in Ash Pond (cubic yards)..... 1,200,000 1,200,000
Area of Ash Pond (acres)................ 58.73 58.73
Area of Ash Pond (square yards)......... 284,253 284,253
Volume of saturated CCR (cubic yards)... 94,751 435,855
Fraction of total CCR saturated (%)..... 7.9 36.3
------------------------------------------------------------------------
Based on EPA's estimates, the closure of the Plant Gadsden Ash
Pond, authorized and approved by ADEM, does not meet the requirements
of Sec. 257.102(d). Overall, the closure of the Gadsden Ash Pond
presents the same issues as the closure of the Colbert Ash Pond 4
discussed in the previous section. The post-closure groundwater
monitoring data from 2019 through 2021 show that groundwater is still
infiltrating into the Ash Pond. The average groundwater elevations
measured at monitoring wells surrounding the Ash Pond from 2018 through
2022 were on the order of 514 ft MSL (i.e., approximately 4 feet above
the average bottom elevation of the CCR). Yet neither the approved
Closure Plan nor any other document in the record for the permit
accounts for the levels of groundwater present in the unit prior to
closure or describe any engineering measures taken to meet each of the
Federal CCR closure-in-place performance standards in Sec.
257.102(d)(1) and (2) in light of the groundwater present in the unit.
Nor based on the post-closure groundwater elevation data from
piezometer wells from 2019-2021, did the approved closure address the
groundwater that continues to saturate the CCR in the closed unit. EPA
is therefore proposing to determine that the permit for Plant Gadsden
does not require Alabama Power to achieve compliance with either Sec.
257.102(d) or with alternative State standards that EPA has determined
to be at least as protective. EPA is therefore, proposing to determine
that Alabama's CCR permit program does not satisfy the statutory
requirement in RCRA section 4005(d)(1)(A) or (B).
As previously explained, in situations such as this, where the
waste in the unit is continually saturated with groundwater, the
requirement to eliminate free liquids obligates the facility to take
engineering measures to ensure that the groundwater, along with the
other free liquids, has been permanently removed from the unit prior to
installing the final cover system. See, 40 CFR 257.102(d)(2)(i). Yet
neither the Closure Plan that ADEM-approved nor the permit ADEM issued
contained any such requirements.
While the approved Closure Plans for the Ash Pond at Plant Gadsden
discuss dewatering techniques employed before and during closure, it
appears the facility at most eliminated only the ``free water'' ponded
above the CCR, and only dewatered the CCR and sediment ``to the extent
necessary to provide a stable working surface for earthwork equipment''
as provided in the closure and post-closure for the Ash Pond:
2.2 DEWATERING FOR CLOSURE
Free water in the clear pool will be removed through pumping,
maintaining compliance with the NPDES discharge limits. The saturated
ash will be dewatered to the extent necessary to allow a stable working
surface for earthwork equipment. Interstitial water '' removal. All
water will be sent to an onsite water treatment system prior to
discharge to ensure compliance with the NPDES discharge limits.\62\
---------------------------------------------------------------------------
\62\ Alabama Power. Revised Closure Permit Application for the
Plant Gadsden Ash Pond. April 30, 2020. Appendix 8, p 2.
---------------------------------------------------------------------------
The ``free water'' referenced above is only a subset of the ``free
liquids'' that must be eliminated; and that standard (``eliminated'')
applies equally to the pore water intermingled with the CCR. See, 40
CFR 257.102(d)(2)(i). The Closure Plans do not acknowledge the
groundwater within the consolidated footprint that continues to
routinely flow into the base of the impoundment and saturate the CCR or
describe any engineering measures to eliminate those free liquids,
despite the continued saturation. Moreover, it is clear from the post-
closure 2019-2022 monitoring data that the measures that were taken
during closure did not actually eliminate the free liquids from Ash
Pond.
A further concern is that, given the failure to eliminate the free
liquids from the saturated CCR underlying the consolidated unit, it is
not at all clear that the remaining wastes have been stabilized
sufficiently to support the final cover system, as required by Sec.
257.102(d)(2)(ii). Creating a stable working surface for earthwork
equipment while the cover system is being installed is not the same as
ensuring that the unit has been sufficiently dewatered prior to
installation of the cover system and that over the long term there will
be no differential settlement of the CCR in the closed unit that would
disrupt the integrity of the cover system and allow
[[Page 55249]]
liquids to infiltrate into the closed unit. Neither the approved
Closure Plan nor ADEM's permit provides any details of engineering
measures that were taken to address the groundwater that continues to
flow into and out of the unit from the sides and bottom. In the absence
of such measures, EPA has no basis for concluding that the standard in
Sec. 257.102(d)(2) has been met.
EPA was also unable to find any description in the ADEM approved
Closure Plan or any other permit document of engineering measures that
Alabama Power took to ``control, minimize, or eliminate, to maximum
extent feasible'' either the post-closure infiltration of the
groundwater into the waste or the post-closure releases of CCR or
leachate to the groundwater, resulting from the groundwater that
continues to infiltrate into the impoundment from the sides and bottom
of the unit. 40 CFR 257.102(d)(1)(i). Based on the data and analyses
described above, groundwater continues to infiltrate into the unit and
yet the only measures described in the Closure Plan and the permit are
those taken to facilitate consolidation and cap construction.\63\ In
essence, this means the Ash Pond will continue releasing CCR
contaminants indefinitely unless Alabama Power is taking additional
actions that are not required by or explained in the permit.
---------------------------------------------------------------------------
\63\ Id at Appendix B (Infiltration Equivalency Demonstration)
in Appendix 8.
---------------------------------------------------------------------------
The absence of such measures from the closure approved by ADEM is
consistent with the State's interpretation of its closure requirements,
but as discussed above, it is neither consistent with, nor as
protective as, the Federal regulations. As with the TVA Colbert Plant
Permit, EPA is proposing to determine that the record does not support
a finding that ADEM's alternative approach of relying on the existing
corrective action process will be as protective as the Federal
requirements. As discussed in a subsequent section, EPA has serious
concerns about the protectiveness of the corrective action at Gadsden
that ADEM is overseeing.
All of this information was available before ADEM issued the permit
in December 2020, and again when ADEM approved the completion of
closure on June 9, 2022. Yet the permit continues to authorize the
closure of the unit with no engineering measures to limit the
groundwater from continually flowing into and out of the CCR in the
unit, and with no permit terms on the need to address this as part of
the corrective action process.
Accordingly, EPA is proposing to determine that the permit for
Plant Gadsden does not require Alabama Power to achieve compliance with
either Sec. 257.102(d) or with alternative State standards that EPA
has determined to be at least as protective.
b. Plant Gadsden Groundwater Monitoring Issues
The Plant Gadsden Permit says on page 1,
Groundwater monitoring and corrective action requirements in the
permit establish a groundwater monitoring system of wells that provides
an accurate representation of the groundwater quality underlying the
unit and a groundwater monitoring plan to establish appropriate
sampling and analysis of the system to detect the presence of CCR
constituents.
In addition, Section V of the Plant Gadsden Permit incorporates the
GWMP submitted with the Permit Application, and directed Alabama Power
to comply with the State regulations and the approved plan:
Section V. Groundwater Monitoring and Corrective Action Requirements.
A. Groundwater Monitoring System. The Permittee shall install and/or
maintain a groundwater monitoring system, identified in Table 1, as
specified in 335- 13- 15-. 06(2) and the approved groundwater
monitoring plan.
Once ADEM approved and adopted the GWMP into the permit, the GWMP,
rather than the referenced State regulations, became the State
requirements with which the facility is required to comply.
Based on EPA's review of the approved groundwater monitoring plan,
EPA is proposing to determine that the groundwater monitoring well
network ADEM approved does not meet the performance standards in Sec.
257.91(a) or (b). As discussed in more detail below, EPA is proposing
to determine that the approved groundwater monitoring system is not
based on a thorough characterization of the elements listed in Sec.
257.91(b). EPA is also proposing to determine that the groundwater
monitoring system does not ``yield groundwater samples from the
uppermost aquifer,'' but has been screened instead in only a portion of
the aquifer. 40 CFR 257.91(a). Further, it appears that the background
wells were not installed in locations hydraulically upgradient of the
Ash Pond, and EPA was unable to locate sufficient information in the
permitting record demonstrating that the standard for such wells in
Sec. 257.91(a)(1)(i) or (ii) was met. In addition, based on the
documentation provided in the Permit Application, it appears that the
downgradient compliance wells are spaced too far apart and/or are
screened too deeply and/or shallow to accurately represent the quality
of groundwater passing the waste boundary and to monitor all potential
contaminant pathways in the uppermost aquifer. See, 40 CFR
257.91(a)(2). Therefore, EPA is proposing to determine that ADEM's
Final Permit fails to require Alabama Power to achieve compliance with
either the Federal regulations or with an equally protective State
requirement.
i. Failure To Delineate the ``Uppermost Aquifer'' and To Base the
System on Thorough Characterization of Site Data
The Federal CCR regulations require that a groundwater monitoring
system sample ``the uppermost aquifer,'' which is defined as ``the
geologic formation nearest the natural ground surface that is an
aquifer, as well as lower aquifers that are hydraulically
interconnected with this aquifer within the facility's property
boundary.'' 40 CFR 257.53, 257.91(a). The design of the monitoring
systems must be based on a thorough characterization of, among other
things, the ``aquifer thickness, groundwater flow rate, groundwater
flow direction including seasonal and temporal fluctuations in
groundwater flow; and saturated and unsaturated geologic units and fill
materials overlying the uppermost aquifer, materials comprising the
uppermost aquifer, and materials comprising the confining unit defining
the lower boundary of the uppermost aquifer.'' 40 CFR 257.91(b)(1) and
(2). EPA is proposing to determine that ADEM approved a groundwater
monitoring plan that does not meet these requirements.
Based on the limited information in the permit record, it appears
the facility failed to fully define the limits of the uppermost
aquifer, particularly its lower boundary. The GWMP provided in the
Permit Application provides only limited characterization of the
geologic units beneath the Ash Pond. In addition, the technical
information provided in the Permit Application is insufficient to
support a determination of the lateral and vertical limits of the
entire uppermost aquifer; for example, EPA found only limited data on
the ``saturated and unsaturated geologic units and fill materials
overlying the uppermost aquifer and materials comprising the uppermost
aquifer.'' 40 CFR 257.91(b)(2). And EPA was unable to find adequate
information about the ``materials comprising the confining unit
defining the lower boundary of the uppermost aquifer.'' Because the
information in the Permit Application
[[Page 55250]]
was inadequate, EPA also consulted information available on Alabama
Power's CCR website to understand the hydrogeology of the site. EPA is
proposing to determine that neither the information in the Permit
Application nor the additional information available on Alabama Power's
CCR website constitutes ``a thorough characterization of . . . aquifer
thickness, groundwater flow rate, groundwater flow direction including
seasonal and temporal fluctuations in groundwater flow; and saturated
and unsaturated geologic units and fill materials overlying the
uppermost aquifer, materials comprising the uppermost aquifer, and
materials comprising the confining unit defining the lower boundary of
the uppermost aquifer.'' 40 CFR 257.91(b)(1) and (2).
A generalized visual representation of the various lithologies
composing the uppermost aquifer beneath the Ash Pond can be found in
the cross sections in Figures 5A and 5B (included on pages 142 and 143)
in the Permit Application and in other places, such as Figures 4A, 4B,
9, and 10 from the 2021 Semi-Annual Groundwater Monitoring and
Corrective Action (GWMCA) Report for Plant Gadsden.\64\ Based on EPA's
assessment of the available information, the uppermost aquifer, which
has not yet been fully identified and characterized, is a composite
layered system consisting of unconsolidated deposits of alluvial origin
on top of a predominantly mudstone bedrock. The unconsolidated alluvial
deposits consist of interlayered deposits of silt, sand, gravel, and
clay material. These unconsolidated alluvial deposits unconformably
overlay a variably fractured and weathered bedrock material,
predominantly mudstones of the Conasauga formation. The three-
dimensional surface represented by the contact between the uppermost
portion of the (consolidated) bedrock and the overlying alluvium
(unconsolidated), which can also be described as the top-of-rock
surface, is a distinct hydraulically relevant zone of interest. These
points are illustrated (in part) in the geologic cross-sections on
Figures 5A and 5B (included on pages 142 and 143) in the Permit
Application, which show the uppermost aquifer consisting of layers of
sand, silt, gravel, as well as the underlying Conasauga bedrock
formation. The elevation of this contact zone changes laterally across
the unit, depending on location, and these differences in elevation are
important with respect to the siting of appropriate monitoring well
location and depths.
---------------------------------------------------------------------------
\64\ Southern Company Services. 2022 Semi-Annual Groundwater
Monitoring and Corrective Action Report, Alabama Power Company Plant
Gadsden Ash Pond. Prepared for Alabama Power Company. January 31,
2022.
---------------------------------------------------------------------------
Immediately located beneath the unconsolidated alluvial materials
is a zone of degraded bedrock (typically referred to as ``weathered
bedrock'') in the uppermost portion of the Conasauga bedrock. This
weathered bedrock material consists primarily of variably weathered
mudstones which have been degraded by naturally occuring processes. The
weathered rock zones vary in thickness laterally and vertically. This
interface between the unconsolidated alluvial materials and the
underlying bedrock constitutes an irregular geologic contact, which
varies spatially in terms of the thickness and degree of the weathered
bedrock material, that is sandwiched between alluvial deposits above,
and lightly weathered or unweathered bedrock below. The contact can be
thick and gradational in some areas, and abrupt and thin in other
areas. This variability demands additional characterization as it
creates the potential for preferential pathways which may exploit the
weathered interval. While limited information has been collected from
this interval, a few monitoring wells are partially screened across the
bedrock/overburden contact, and thus monitor the weathered bedrock
interval to some degree at those locations. However, the variable
nature of the bedrock/overburden contact was not sufficiently
characterized to meet the performance standards in Sec. 257.91(a) or
(b), as discussed in more detail below.
Beneath the uppermost veneer of weathered bedrock are rocks of the
Conasauga group, which consists of varying amounts of limestone,
dolomite, and shale, with chert and siltstone horizons present locally.
The 2021 Semi-Annual GWMCA Report states, ``The Limited core logs from
the Site indicate the Conasauga [beneath the Ash Pond] to be a medium
to dark gray mudstone or shale with noticeable calcite veining.'' \65\
While the Report goes on to State, ``The Conasauga Formation is not
considered to be a water-bearing aquifer at the Site,'' this statement
conflicts with boring logs and other information which indicate that
the mudstones of the Conasauga Formation are locally fractured,
weathered and hydraulically connected to the alluvium and weathered
bedrock deposits lying above. The lower limits of the hydraulically
connected portions of the bedrock, however, have not yet been
established, and reporting is not consistent on this. Both the Permit
Application and the 2021 Semi-Annual GWMCA Report generally describe
the aquifer similarly. For example, the 2021 Semi-Annual GWMCA Report
\66\ states,
---------------------------------------------------------------------------
\65\ Id.
\66\ Id.
The uppermost aquifer beneath the Site corresponds to a coarse and more
permeable fraction of alluvial overburden soils and weathered or
fractured rock near the soil-rock interface. The uppermost aquifer is
typically located at depths between 15 and 50 feet below ground surface
(BGS). Soils are generally poorly graded sands with layers of clay and
well-graded gravels that overlay a mudstone or shale bedrock,''
See also Permit Application at section 3 of the GWMP. As shown on
Figures 5A and 5B in the Permit Application, bedrock intervals are not
included in the represented monitoring wells and little
characterization appears to have penetrated the bedrock beyond the
uppermost intervals.
But elsewhere the 2021 Semi-Annual GWMCA Report states that,
Vertical delineation wells targeted more permeable/fractured water-
bearing zones within the Conasauga formation in the upper 50 feet of
bedrock.
A further inconsistency appears on the geologic cross sections
included in the 2021 Semi-Annual GWMCA Report (see Figures 4A, 4B, 9,
and 10), which indicate the connection of the alluvial and bedrock
zones to depths of over 100 feet into the mudstone bedrock. These cross
sections and the associated boring logs, some of which were included in
the Permit Application and some of which were included in the 2021
Semi-Annual GWMCA Report, confirm that this group of geologic layers
and formations are hydraulically interconnected to depths of over 100
feet into the bedrock. The totality of this information forces the
conclusions that the lower limits of the uppermost aquifer have not
been determined and the uppermost aquifer and hydraulically connected
underlying intervals extends at least 100 feet into the bedrock.
In other words, based on the available information, the uppermost
aquifer consists of the alluvial aquifer nearest the ground surface and
at least the uppermost 100 feet of the hydraulically connected bedrock
beneath it. See, 40 CFR 257.53 (definition of uppermost aquifer). As
such the materials presented in the Permit Application do not present a
complete or accurate representation of the uppermost aquifer and
hydraulically connected aquifer zones beneath it.
In addition, the top-of-bedrock surface has not been adequately
resolved in all
[[Page 55251]]
areas of the site because some boring logs lack reliable confirmatory
data. According to the boring logs that were included in the Permit
Application, there are multiple missing intervals of ``no recovery''
from numerous borings advanced into bedrock, which indicate a large
potential for hydraulically significant zones that are currently
insufficiently characterized. As a consequence, EPA is proposing to
determine that the thickness, variability, nature, and hydrogeologic
significance of the transitional zone of weathering in the uppermost
part of bedrock has not been established, as required by Sec.
257.91(b).
Furthermore, a hydraulic divide, generally located along the
northeastern boundary of the unit, indicates the groundwater hydraulics
are more complex than the current coarse monitoring network can
adequately evaluate. Additional monitoring points are needed laterally
(and vertically) in this area to provide the ``thorough
characterization of groundwater flow rate [and] groundwater flow
directions, including seasonal and temporal fluctuations in groundwater
flow'' required to support the design of the groundwater monitoring
system pursuant to Sec. 257.91(b)(1). There are also insufficient data
to allow for the determination of groundwater flow directions at the
eastern limits of the Ash Pond. While GSD-AP-MW-12 is downgradient of
GSD-AP-MW-1, there are no wells or piezometers that would serve as
hydraulic control points to the east of the Ash Pond to fully
characterize the groundwater flow directions at the eastern waste
boundary. Furthermore, GSD-AP-MW-1 consistently has one of the highest
groundwater elevations, and the possibility of eastward flow beyond the
eastern boundary cannot be ruled out without additional data.
Additional groundwater monitoring wells are needed to the northeast,
east, and southeast of the easternmost boundary of the Ash Pond. In
summary, EPA is proposing to determine that significant numbers of
additional characterization borings and monitoring wells are needed to
effectively characterize the alluvial aquifer nearest the ground
surface and hydraulically connected zones within the weathered bedrock
and upper portion of the bedrock intervals. See, 40 CFR 257.91(b).
ii. ADEM Issued a Final Permit With Background Wells That Do Not Meet
the Sec. 257.91(a)(1) Performance Standard
The Federal CCR regulations require that a groundwater monitoring
system consist of a sufficient number of wells at appropriate locations
and depths to yield samples from the uppermost aquifer that accurately
represent the quality of the background groundwater that has not been
affected by leakage from a CCR unit. 40 CFR 257.91(a)(1). The
regulations also specify that background wells must normally be
hydraulically upgradient of the CCR unit, unless specific showings have
been made. See, Id. EPA is proposing to determine that the approved
GWMP fails to document either that the background wells are upgradient
of the CCR unit or that the wells meet the performance standards in
Sec. 257.91(a)(1)(i) or (ii). EPA is also proposing to determine that
the background wells in the approved groundwater monitoring system do
not ``accurately represent the quality of the background groundwater''
because of differences in the lithology between the background wells
and the majority of the wells in the downgradient groundwater
monitoring network, which is discussed in detail below.
At the time of permit issuance, the approved groundwater monitoring
network installed at the unit consisted of three ``background''
monitoring wells (GSD-AP-MW-14, -16, and -17). According to the single
groundwater flow map included in the Permit Application,\67\
groundwater predominantly flows toward the main stem of the Coosa River
from both the southern and northern sides of the river. The Coosa River
acts as a hydraulic divide between the Ash Pond and the region to the
south of the river where the background wells are located.
Consequently, the Plant Gadsden background wells, which are all located
on the southern side of the river, are hydraulically disconnected from
the Ash Pond, rather than ``upgradient'' of the Ash Pond. In addition,
they are in a different flow system and therefore cannot accurately
represent the quality of the background groundwater at the Ash Pond.
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\67\ Alabama Power. Revised Closure Permit Application for the
Plant Gadsden Ash Pond. April 30, 2020. Appendix 7, Plant Gadsden
Ash Pond Groundwater Monitoring Plan, Figure 6.
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The Federal regulations specify that wells that are not
hydraulically upgradient of the CCR unit can only serve as background
wells if one of two showings have been made: (1) that hydrogeologic
conditions do not allow the owner or operator to determine whether
wells are hydraulically upgradient; or (2) sampling at other wells will
be as representative or more representative of background groundwater
quality than that provided by the upgradient wells. 40 CFR
257.91(a)(1)(i), (ii).
EPA found nothing in the Permit Application or on the facility's
CCR website to indicate that site conditions made it infeasible to
determine whether background wells could be installed at locations that
are hydraulically upgradient on the same side of the river. For
example, while on-site access may be limited due to conditions near the
Ash Pond, there is no discussion about other access points offsite to
the north, northeast, or east of the unit that may provide adequate
background samples. In addition, there are site-specific geologic
conditions identified in the Permit Application that indicate that
sampling at the current background wells will not ``accurately
represent the quality background groundwater'' quality at the Ash Pond.
40 CFR 257.91(a)(1). For example, based on the boring logs presented in
the Permit Application, background monitoring well GSD-AP-MW-17 is
screened in limestone but nearly all of the bedrock groundwater
monitoring wells surrounding the Ash Pond are screened in a different
rock type (i.e., mudstone). In addition, background monitoring well
GSD-AP-MW-16 is screened in sand and gravel alluvial materials and
based on a note included within the boring log, it is partially
screened into approximately four feet of limestone bedrock, whereas
numerous wells in the shallow downgradient compliance monitoring
network surrounding the Ash Pond are screened just above or across the
interface between mudstone and overlying overburden materials.
Limestone and mudstone are different rock types and, based on the
boring logs presented in the Permit Application, limestone substrates
do not appear to have been penetrated by monitoring wells installed for
the unit's downgradient compliance monitoring network on the northern
side of the river.
Due to fundamental differences between limestone and mudstone
mineralogy and chemical composition, it is not clear that ambient
geochemical conditions in the limestone-hosted aquifer would be
representative of an environment where mudstone predominates, and site-
specific comparative analysis of both the geology and geochemistry for
the two distinct geochemical environments and flow systems is necessary
to determine whether the wells across the river are in fact
sufficiently representative of conditions within the uppermost aquifer
to serve as representative background wells. Although the Groundwater
Monitoring Plan included a limited
[[Page 55252]]
narrative at Section 4.2.2, entitled ``Groundwater Geochemistry,'' the
narrative did not address any known differences in geology, lithology,
or mineralogy between the two aquifers that are located on opposite
sides of the river. ADEM nevertheless approved the plan without
requiring the facility to resolve these issues.
iii. The Gadsden Final Permit Allows Insufficient Locations and Depths
of Downgradient Compliance Wells To Monitor the Uppermost Aquifer
As previously discussed, the Federal regulations specify that a
groundwater monitoring system must ``consist[ ] of a sufficient number
of wells, installed at appropriate locations and depths, that . . .
accurately represent the quality of the groundwater passing the waste
boundary of the CCR unit.'' 40 CFR 257.91(a)(2). The regulations
further specify that ``[a]ll potential contaminant pathways must be
monitored.'' Id. But as discussed in more detail below, EPA is
proposing to determine that ADEM approved a GWMP with an insufficient
number of wells laterally along the downgradient perimeter of the unit
to monitor all potential contaminant pathways. EPA is also proposing to
determine that monitoring wells in the approved plan were not installed
at appropriate depths to ensure that all potential contaminant pathways
were monitored. Finally, EPA is proposing to determine that the
approved groundwater monitoring system fails to account for
preferential pathways beneath the Ash Pond.
(1) Insufficient Lateral Spacing of Compliance Wells To Monitor All
Potential Contaminant Pathways
At the time of permit issuance, the approved groundwater monitoring
network installed at the unit consisted of only fifteen compliance
monitoring wells (GSD-AP-MW-1 through GSD-AP-MW-12 and GSD-AP-PZ-1,
GSD-AP-PZ-5 and GSD-AP-PZ-6), at an impoundment with a perimeter of
approximately 7,500 feet.
Most of the groundwater monitoring wells that parallel the river
for the Plant Gadsden Ash Pond unit are spaced approximately 400 to 900
feet apart, and lateral distribution of wells is somewhat uniform with
downgradient monitoring wells surrounding the waste boundary at an
average lateral spacing of 630 feet.\68\ These large lateral well
spacings are particularly problematic to the north, northwest, west,
and to the southwest where groundwater discharges to the Coosa River.
Given the propensity for groundwater to flow within the preferential
pathways that exist at the site and the close proximity of the Coosa
River to the unit, one would expect to see a detailed rationale
explaining why these well locations at large lateral distances were
sufficient to monitor all potential contaminant pathways. However,
EPA's review of the approved GWMP did not identify any such
explanation. Therefore, given the proximity to the Coosa River, the
large well spacings make it likely that all potential contaminant
pathways--such as the gravel and other coarse material in the alluvium
and fractures, or the dissolution features at or below the weathered
bedrock surface that may be causing groundwater to surface water
discharges immediately adjacent to the Ash Pond--are not currently
monitored.
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\68\ Southern Company Services 2022 Annual Groundwater
Monitoring and Corrective Action Report, Alabama Power Company Plant
Gorgas Ash Pond. Prepared for Alabama Power Company. February 1,
2023.
---------------------------------------------------------------------------
(2) Insufficient Number of Downgradient Compliance Wells Installed at
Appropriate Depths To Monitor the Entire Aquifer (Inadequate Vertical
Spacing)
EPA is also proposing to determine that ADEM approved a GWMP that
lacked ``a sufficient number of wells, installed at appropriate
locations and depths'' to ensure that all potential contaminant
pathways in the entire uppermost aquifer are monitored. As stated
previously, the uppermost aquifer is a composite layered system
consisting of unconsolidated deposits of alluvial origin on top of
mudstone bedrock. The unconsolidated alluvial deposits consist of
interlayered deposits of silt, sand, gravel, and clay material. These
unconsolidated alluvial deposits overlay a variably fractured and
weathered bedrock material, predominantly mudstones of the Conasauga
formation. The contact between the uppermost portion of the
(consolidated) bedrock and the overlying (unconsolidated) alluvium,
which can also be described as the top-of-rock surface, is a distinct
hydraulically relevant zone of interest, and many ``downgradient''
compliance monitoring wells in the approved network are screened across
this interface, as is appropriate. However, although the lower limits
of the hydraulically connected portions of the bedrock have not yet
been established, as previously discussed, the available information
supports the conclusion that this group of geologic layers and
formations are hydraulically interconnected to depths of 100 feet or
more into the bedrock. Consequently, EPA is proposing to determine that
the entire group of geologic layers and formations should have been
more comprehensively monitored. See, 40 CFR 257.53 (definition of
uppermost aquifer).
The downgradient well network ADEM approved is focused on a narrow
subset of the uppermost geologic layers associated with river
deposition. These unconsolidated materials occur in terrace deposits at
low elevations near the current Coosa River channel as well as at
higher topographic levels. These alluvial deposits are reported to
range from approximately 20 to 30 feet in thickness. Most of the
downgradient compliance monitoring wells in the approved network are
screened in these shallow materials, and most of the wells are screened
only in the gravel.\69\ Additional compliance wells are needed both at
the upper and lower bounds of the uppermost aquifer system, including
within alluvial deposits and hydraulically connected weathered bedrock
and bedrock zones, to ensure all potential contaminant pathways will be
monitored in all relevant flow zones.
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\69\ The Plant Gadsden Permit Application at page 111 includes a
statement that ``[m]onitoring wells target the uppermost aquifer
with wells screened in coarse fractions of the alluvial materials or
more weathered, fractured upper bedrock beneath the Site.''
---------------------------------------------------------------------------
A few wells are screened near the top of the Conasauga bedrock
formation, and a few wells are cross screened across the interface
between the alluvium (the gravel) and the underlying bedrock. As
depicted on the cross-section in Figure 5A in the Permit Application,
no wells appear to have been screened in either the sand or silt layers
that are situated above the gravel; and a single well on the cross-
section in Figure 5B in the Permit Application appears to be partially
screened in the silt. But additional compliance wells should have been
installed in those upper zones given that the sand and silt layers are
saturated with groundwater. Even when the gravel layers were not
present, the well screens were set at the bottom of the alluvium or at
the top of bedrock, and not in the silts. Wells in each of the
saturated units are needed in order to monitor all potential
contaminant pathways.
In addition, as previously discussed, key interfaces, such as the
interface between alluvium and weathered bedrock have apparently not
been fully characterized; as this portion of the bedrock system is
hydraulically connected to the overlying alluvium, additional
compliance wells are needed in the upper part of the bedrock in most
areas of the Ash Pond unit to ensure that all potential contaminant
pathways are monitored. Additional wells also
[[Page 55253]]
need to be installed in deeper intervals of the underlying Conasauga
mudstones which are hydraulically connected the uppermost zone of
weathered bedrock. The relevant zone of interest in the upper part of
the Conasauga group is at least 100 feet in thickness, as discussed
previously, but the true thickness of the uppermost aquifer has not
been determined. As such additional monitoring wells may need to be
screened more deeply to ensure all potential contaminant pathways are
monitored.
(3) Preferential Pathways Are Not Monitored
Preferential pathways have been documented in the uppermost aquifer
under the Ash Pond. Yet under the approved GWMP, these significant
potential contaminant pathways do not appear to be adequately
monitored, despite the express requirement in Sec. 257.91(a)(2).
Based on the boring logs and cross-sections in the Permit
Application and the 2021 Semi-Annual GWMCA Report, several types of
preferential pathways are present at the site. These include, among
others, continuous lenses or channel-like bodies of coarse sand and
gravel in overburden, low-lying areas along the overburden/bedrock
interface, laterally continuous zones of weathered bedrock in the
uppermost part of the bedrock section, and zones of fracturing and/or
weathering and/or dissolution within deeper levels of the bedrock. The
current monitoring network only incompletely monitors some of these.
While some monitoring wells are installed in sand and gravel bodies
in the alluvium, it appears that the monitoring network does not target
all such zones that may be serving as preferential pathways. As just
one example, consider the southwestern unit boundary that borders the
Coosa River; as indicated on Figures 5B and 6 of the approved GWMP,
while the wells installed along this boundary (GSD-AP-MW-8 thru GSD-AP-
MW-12) are screened along a zone where groundwater flow is likely
occurring along preferential pathways, they are spaced over 500 feet
apart. Considering the unique geologic conditions at the site that
could result in the presence of more localized preferential pathways,
it is not known whether the gravel materials screened by GSD-AP-MW-11
are present elsewhere along this boundary. In short, there could be
sand and gravel alluvial zones or highly fractured zones in bedrock
near the bedrock/alluvium interface that have not been identified and
are unmonitored. EPA is proposing to determine that additional borings
(and possibly monitoring wells) should have been installed along this
boundary, and it appears that this level of detailed investigation to
identify preferential pathways was not performed elsewhere along the
unit.
It is clear that preferential pathways in the bedrock exist based
on the characterization and monitoring Alabama Power conducted as part
of the continuing corrective action at the site. However, there is
little to no discussion in the Permit Application regarding how these
pathways were identified and how the lateral/vertical dimensions of the
pathways were delineated to ensure that compliance wells were installed
correctly to monitor these pathways. As illustrated on Figures 9 and 10
of the 2021 Semi-Annual GWMCA Report, assessment monitoring has
identified plumes emanating from the unit to the northeast in
overburden and bedrock. After installing additional monitoring wells to
delineate the contaminant plume, Alabama Power identified that
contamination was present deeper in the Conasauga bedrock formation
than any of the compliance wells previously installed as part of the
groundwater monitoring system. For example, Figures 5 and 10 of the
2021 Semi-Annual GWMCA Report indicate that pathway in bedrock has
influenced migration of a lithium plume beyond the unit boundary at
least hundreds of feet to the northeast to depths of at least 130 feet
into the bedrock. It is reasonable to expect that similar pathways may
exist also along the same regional northeast to southwest geologic
strike to the southwest of the unit, exploiting these same inherent
zones of fracturing in the bedrock, yet the southwestern waste
boundary, along the Coosa River, generally lacks any monitoring points
in deeper bedrock.
In summary, after reviewing the GWMP and all the materials in the
permit record, EPA is proposing to determine that the monitoring
network that ADEM approved is not likely to detect all groundwater
contamination in the uppermost aquifer and is therefore less protective
than the Federal regulations.
c. Plant Gadsden Corrective Action Issues
In January 2020, the first SSLs above groundwater protection
standards were reported for arsenic and lithium. An ACM was prepared in
July 2020. On December 18, 2020, ADEM issued the Final Permit to
Alabama Power for Gadsden Ash Pond. EPA is proposing to determine that
the Final Permit issued to the Gadsden Ash Pond, as with the other
permits discussed in this notice, fails to require Alabama Power to
achieve compliance with the Federal corrective action requirements.
The Gadsden Final Permit states that the Permittee is required ``.
. . to manage CCR in accordance with the conditions of the permit, ADEM
Admin. Code r. 335- 13- 15, `Standards for the Disposal of Coal
Combustion Residuals in Landfills and Surface Impoundments,' and the
approved permit application.'' \70\ The permit also contains the same
recitation of the corrective action regulations as the Colbert Final
Permit did.
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\70\ Alabama Department of Environmental Management. Initial
Permit and Variance, Gadsden Steam Plant, Permit No. 28-09. December
18, 2020. PDF p. 2.
---------------------------------------------------------------------------
Corrective Action
1. Assessment of Corrective Measures. The Permittee must initiate
an assessment of corrective measures as specified in 335-13-15-. 06(7)
if any constituent listed in Appendix IV of 335- 13- 15 has been
detected at a statistically significant level exceeding the groundwater
protection standard, or immediately upon detection of a release from
the CCR unit.
a. The permittee must continue to monitor groundwater in accordance
with the assessment monitoring program while assessing corrective
measures.
2. Selection of Remedy. Based on the results of the corrective
measures assessment, the Permittee must select a remedy as specified in
335-13-15-. 06(8).
3. Implementation of the Corrective Action Program. Within 90 days
of selecting a remedy, the Permittee must initiate remedial activities
as specified in 335-13-15-. 06(9), and shall be required to modify the
permit in accordance with Section II. E. 9.
In the RTC for the Gadsden Final Permit, ADEM states that, ``The
ACM is currently under review. Once the final review is complete, the
Department will provide comments to Alabama Power related to the
submitted ACM and proposed final remedy.'' The preferred remedy in the
ACM was MNA with adaptive site management and ``remediation system
enhancement.'' \71\ Any comments provided by ADEM to
[[Page 55254]]
Alabama Power on the 2020 ACM were not available for review.
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\71\ It is not clear what is meant by ``remediation system
enhancement'' with respect to MNA, because MNA relies upon naturally
occurring processes for remediation. The only systems installed are
for performance monitoring. Any ``enhancement'' would require action
on the part of Alabama Power to remediate the releases and would be,
by definition, a different remedy.
---------------------------------------------------------------------------
As with Colbert, incorporating the regulations verbatim in the
permit does not require Gadsden to achieve compliance with those
requirements. This is because ADEM did not take into account relevant
facts about the status of corrective action at Gadsden, such as whether
the 2020 ACM, which was completed more than 2 years prior to issuance
of the permit, complied with the regulatory requirements. Most
importantly, ADEM did not adjudicate what actions are still necessary
in light of those facts to achieve compliance with the regulations and
include those actions as requirements in the Final Permit.
Whether the 2020 ACM meets the requirements of the regulations and
what actions Alabama Power must take to remediate groundwater in
compliance with Sec. 257.97 are precisely the types of adjudication
required in a permit. What the permittee is required to do in order to
achieve compliance with the regulations must be determined prior to
final permit issuance, because the permit must contain these
requirements. This is the role of a permitting authority (i.e., ADEM).
Delaying this decision effectively allows Alabama Power to continue
operating out of compliance with the regulations, while operating in
compliance with the permit. In this case, that means Alabama Power can
continue to pursue a remedy that does not appear to meet the
requirements of Sec. 257.97, and consequently, delay or avoid the
cleanup. This results in a permit program that is less protective than
the Federal regulations.
In sum, EPA is proposing to determine that, by failing to determine
the adequacy of the revised ACM or the permittee's proposed remedy, the
permit in essence authorizes Alabama Power to continue to pursue a
remedy that does not appear to meet the requirements in Sec. 257.97(b)
and is based on the results of a deficient ACM. Accordingly, EPA is
proposing to determine that this permit does not require compliance
with the Federal requirements and, because it allows the facility to
continue to delay initiating corrective action that would address the
continuing groundwater contamination, the State requirement is less
protective than the Federal regulations.
i. Gadsden Final Permit Does Not Require an ACM That Includes an
Assessment of Source Control Measures in Accordance With 40 CFR 257.96
40 CFR 257.97(b)(3) requires that all remedies control the source
of releases in order to reduce or eliminate, to the maximum extent
feasible, further releases of contaminants into the environment. The
ACM for Gadsden contains no assessment of control measures to achieve
this requirement (i.e., source control). Instead, section 2.5 describes
the closure of the unit, which has already occurred, and states, ``Site
closure appears to have already been effective in controlling the
source and reducing infiltration into the underlying aquifer.''
However, the ACM must include more than one source control measure and
must actually analyze how effectively each of the potential measures
would meet the criteria in Sec. 257.96(c). See, 40 CFR 257.96(a), (c).
Here, as was the case with Plant Colbert, there is no assessment of the
one source control measure identified in the ACM--the closure of the
Ash Pond, which left a significant amount of CCR in contact with
groundwater--and how effectively it would achieve the criteria in Sec.
257.96(c) compared to other source control alternatives, such as clean
closure or the imposition of engineering measures to control or
eliminate the groundwater that continues to flow in and out of the
impoundment. Yet the permit issued by ADEM does not require any actions
to remedy these readily apparent deficiencies.
ADEM's failure to require Alabama Power to submit an ACM that
actually evaluates whether the closure of the Ash Pond meets the source
control requirements in Sec. 257.97(b)(3) also undercuts their claim
that they will use the corrective action process to address any
remaining concerns with respect to the closure of the Ash Pond. As
discussed above, closure construction activities for the Ash Pond were
certified as completed in October 2018, and a certification of the
completion of closure activities was submitted in April 2020. As
discussed above, in the two years between the time closure was
completed and the permit was issued in December 2020, groundwater
elevations were measured between 2 and 7 feet above the average base
elevation of the closed unit. Yet ADEM issued the permit without
evaluating the ACM. Nor did the State take any further action when they
approved the closure of the Ash Pond in 2022.
ii. The Gadsden Permit Does Not Require Alabama Power To Collect Site
Data Needed To Characterize Site Conditions That May Affect a Remedy To
Support Assessments in the ACM
As discussed above, Sec. 257.95(g)(1) requires a facility to
characterize the nature and extent of the release and any relevant site
conditions that may affect the remedy ultimately selected. The
characterization must be sufficient to support a complete and accurate
assessment of the corrective measures necessary to effectively clean up
all releases from the CCR unit pursuant to Sec. 257.96. The 2020 ACM
delineates releases but does not characterize any site conditions that
would affect its preferred remedy of in-situ immobilization through
treatment or MNA (e.g., testing for the presence of released
constituents in soils to demonstrate they are being removed from the
groundwater and immobilized on-site). As discussed in subsequent
sections, these data are necessary to accurately assess any of the
remedies identified in the ACM, particularly MNA. The Final Permit
issued by ADEM does not require collection of these data or any
revisions to the ACM to remedy this deficiency.
iii. The Assessment of In-situ Geochemical Treatment and MNA in the
ACMs Is More Favorable Than Can Be Supported by the Available Data
The 2020 ACM for Gadsden identified in-situ geochemical treatment
and MNA as corrective measures to address groundwater contamination, in
addition to hydraulic control and treatment. As discussed previously,
MNA relies on natural processes to treat releases; in-situ geochemical
treatment adds chemicals to the subsurface to create conditions for
this immobilization to occur. For arsenic and lithium, in-situ
geochemical treatment and MNA can reduce mobility through sorption to
soils, but they do not remove the contaminants from the environment.
Therefore, MNA and geochemical in-situ treatment generally would not
perform well with respect to the requirement in Sec. 257.97(b)(4) that
remedies ``remove from the environment as much of the contaminated
material that was released from the CCR unit as is feasible,'' since
the constituents remain in the subsurface soils, albeit immobilized.
In order for immobilization through MNA or in-situ treatment to be
assessed favorably with respect to reliability, the chemical reactions
and processes involved in this immobilization must be demonstrated to
be irreversible. Immobilization that is not permanent could be
reversed, causing contaminants to be released back into groundwater,
where they can migrate off-site. Immobilization that is not permanent
would also require ongoing monitoring in accordance with Sec.
257.98(a)(1) as long as immobilized constituents remain in the
subsurface. Determining the viability and demonstrating the
irreversibility of immobilization
[[Page 55255]]
mechanisms is necessary to assess the performance, reliability, ease of
implementation, and the time required to begin and complete the remedy.
40 CFR 257.96(c)(1) and (2). These assessments would need to be
supported with site-specific characterization data and analysis. This
information would ultimately be necessary to show that MNA and
geochemical in-situ treatment meet all the requirements of Sec.
257.97(b), but the permit record does not include such information.
(1) The 2020 ACM Does Not Include Data That Characterize Site
Conditions or Identify Any Attenuation Mechanisms Occurring at the Ash
Pond
The 2020 ACM assessed the performance of MNA favorably without any
supporting data to characterize site conditions that may ultimately
affect a remedy, as required by Sec. 257.95(g)(1). For example, site-
specific groundwater data (e.g., pH or oxidation potential, speciated
concentrations of constituents of concern) were not considered in the
assessment narrative, and analytical results of soil samples to
identify the presence of immobilized constituents in the subsurface
were not provided. The site data that were collected focus only on
contaminant concentrations and trend analyses regarding the presence of
contaminants. The ACM also does not discuss how attenuation may be
naturally occurring through any particular MNA mechanisms (e.g.,
adsorption, precipitation, dispersion). EPA was not able to find any
indication in the permit or supporting documentation to confirm that
the Permittee has identified the mechanisms by which MNA would occur at
the site for both arsenic and lithium. Nor is there any condition in
the permit requiring the development and submission of such
information.
(2) MNA Is Not a Viable Remedy Without Source Control
As discussed previously for Plant Colbert, MNA is not viable
without source control, because the total amount of contaminants in the
groundwater will continue to increase as the releases from the unit
continue and potential releases of new constituents will occur.
Therefore, it is impossible to determine whether the aquifer has
sufficient chemical and physical materials required to complete any
identified immobilization reactions because the total amount of the
release is not yet known.
Source control has not been achieved here, as releases from the Ash
Pond are ongoing. The closure of the Ash Pond with waste remaining in
place in the aquifer has resulted in a continual source of groundwater
contamination from the unit. Therefore, MNA is not a viable remedy for
the Ash Pond and should not be included in the 2020 ACM unless the ACM
is revised to include an alternative that achieves source control.
(3) Plant Gadsden's Permit Does Not Require an ACM That Accurately
Assesses Groundwater Remediation Alternatives According to the Criteria
in 40 CFR 257.96(c)
The 2020 ACM also fails to meet the requirements at Sec.
257.96(c)(3) to consider safety impacts, cross-media impacts, and
control of exposure to any residual contamination in its assessment of
MNA. Neither the narrative nor Table 5 in the 2020 ACM consider these
impacts for MNA. Table 5 in the 2020 ACM, in the column labeled
``potential impacts of remedy'' assesses the potential impacts from MNA
as ``none.'' This conclusion is not only unsupported by data or
analysis but is also inconsistent with other information in the ACM.
The Ash Pond is next to a river and groundwater flow is depicted toward
the river in Figure 3 in the 2020 ACM. Because no site data were
collected that would demonstrate immobilization of constituents is
occurring, the only MNA that is known to occur is dilution and
dispersion (i.e., the normal transport associated with groundwater
releases). This means that contaminants are migrating out of the Ash
Pond in groundwater toward the river. Migration of contamination from
groundwater to surface water is a cross-media impact. Thus, the
assessment of potential impacts from the remedy for MNA in Table 5,
which includes these cross-media impacts, should be ``high.''
The lack of data to support the assessments in the ACMs means they
may not accurately reflect MNA's ``effectiveness in meeting all of the
requirements and objectives'' in Sec. 257.97(b). Conclusions without a
supporting assessment or data do not constitute ``an analysis of the
effectiveness of potential control measures.'' 40 CFR 257.96(c)
(emphasis added). Inaccurate assessments in an ACM can ultimately
result in selection of a remedy that will not meet the requirements of
Sec. 257.97(b). Yet the Final Permit issued by ADEM does not require
any actions to remedy this deficiency.
3. Plant Gorgas
EPA reviewed the Initial Permit and Variance (Final Permit) for the
Alabama Power Company, William C. Gorgas Electric Generating Plant
(Plant Gorgas), issued by ADEM under Permit No. 64-12 on February 28,
2022.\72\ Plant Gorgas is located near Parrish, Alabama. The units
covered by the Final Permit include the Plant Gorgas Ash Pond, Plant
Gorgas Gypsum Pond, Plant Gorgas Bottom Ash Landfill, and Plant Gorgas
CCR and Gypsum Landfill. The Plant Gorgas CCR and Gypsum Landfill is
still in operation while the other three CCR units are in the process
of closing or closed. For this proposal, of the CCR units at Plant
Gorgas, EPA only evaluated the Final Permit for the Plant Gorgas Ash
Pond (Ash Pond) because it is directly comparable to the other State
CCR permits evaluated in this proposal, and because, based on the
characteristics of the unit and the surrounding hydrogeology, it has
the greatest potential for significant environmental and human health
effects if mismanaged.
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\72\ Alabama Department of Environmental Management. Initial
Permit and Variance William C. Gorgas Electric Generating Plant
Permit Number 64-12. February 28, 2022.
---------------------------------------------------------------------------
The Plant Gorgas Ash Pond is a ``CCR surface impoundment located in
Sections 20, 21, 28 and 29, Township 16 South, Range 6 West in Walker
County, Alabama . . . with a disposal area that consists of
approximately 423.32 acres.'' Final Permit at pg. 2. The Ash Pond is
located southeast of Plant Gorgas on the opposite side of the Mulberry
Fork of the Black Warrior River. The Permit Application describes that
the Ash Pond was originally formed by a cross-valley dam in 1953, with
the original dam located on the northern boundary of the impoundment
adjacent to Mulberry Fork.\73\ The original dam was raised to increase
the capacity of the impoundment in the mid-1970's, and then raised once
again in 2007. Id. at Appendix 4. When the Ash Pond was in operation,
the impoundment covered an approximate area of 420 acres containing 25
million CY of waste.
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\73\ Alabama Power Company. Revised Closure Permit Application
for the Plant Gorgas Ash Pond. April 30, 2020.
---------------------------------------------------------------------------
EPA has identified issues with closure, groundwater monitoring
networks, and corrective action at Plant Gorgas, and we discuss those
issues below.
a. Plant Gorgas Closure Issues
As noted, the closure at Plant Gorgas is not yet complete. To
evaluate the closures at Plants Colbert and Gadsden, EPA reviewed the
measured post-closure groundwater elevations to determine whether the
Sec. 257.102(d) performance standards were met. But since the closure
of the Gorgas Ash
[[Page 55256]]
Pond is not yet complete, that same information (``measured post-
closure groundwater elevations'') is not available. As discussed below,
however, it is clear that CCR in the Ash Pond is currently saturated by
groundwater. Despite the saturated CCR currently in the unit, it may be
possible for the Ash Pond to close with waste in place if engineering
measures are implemented to meet the performance standards in Sec.
257.102(d). Although some engineering measures are described in the
Closure Plan, EPA was unable to locate the information in the permit
record to support a definitive conclusion that the proposed closure
will meet the performance standards in Sec. 257.102(d). For example,
EPA was unable to locate any evaluation of the expected impact of the
proposed engineering measures on groundwater elevations conducted by
either the permittee or ADEM. EPA's inability to reliably estimate
post-closure conditions is a consequence of the complexity of the site,
the absence of critical information in the Closure Plan, and the
inadequacy of the groundwater monitoring system at the site (which is
discussed in the next section). Nevertheless, as described below, based
on the available information there are several reasons to determine
that it is unlikely that the proposed closure of the Ash Pond will meet
the performance standards in Sec. 257.102(d). EPA is therefore
proposing to determine that the approved Closure Plan fails to
demonstrate that the closure will meet the performance standards in
Sec. 257.102(d), as required by Sec. 257.102(b)(1)(i). Based on
ADEM's failure to require the permittee to provide this information, or
to otherwise resolve the issues presented below before approving the
Closure Plan, EPA is proposing to determine that the Final Permit fails
to require the Gorgas Ash Pond to achieve compliance with either Sec.
257.102(d), or with an equally protective State alternative. See 42
U.S.C. 6945(d)(1)(B).
i. CCR in the Ash Pond Is Currently Saturated by Groundwater and Is
Likely To Remain so Once Closure Is Complete
Given the complexity of the site and the absence of detailed
information in the Permit Application, EPA lacks the data to reliably
estimate the amount of CCR that will remain saturated after closure
activities are complete. These deficiencies are significant enough that
ADEM's approval of a Closure Plan with these deficiencies, and in the
absence of any evaluation, leads to the conclusion that the State CCR
permit program does not meet the standard in 42 U.S.C. 6945(d)(1).
However, based on the available information in the Permit Application,
there are many reasons to determine that the proposed closure of the
Ash Pond will not meet the performance standards in Sec. 257.102(d).
Based on the limited data available, EPA estimates that groundwater
will continue to saturate a substantial amount of CCR, even after the
activities described in the approved Closure Plan have been completed.
As described below, available groundwater measurements recorded between
2021 and 2022 show that groundwater levels at the Ash Pond continue to
be present above the base of the unlined impoundment, saturating
substantial amounts of CCR in the closing unit. Moreover, comparison of
groundwater elevation data from 2021 and 2022 to elevation data in the
same wells for prior years does not yet indicate any statistically
significant or sustained declines, further supporting EPA's conclusions
about future persistence of saturated CCR waste.
As shown on the center line cross section B-B' on construction
drawing G-204 in the Permit Application, the base of the Ash Pond
varies substantially. In view of this information, EPA conducted an
analysis using existing monitoring wells near the waste boundary and
south of the planned closure buttress. Few monitoring wells are located
directly adjacent to the CCR; most are located hundreds of feet away
from the waste boundary, with many at distances of over 1,000 feet
away. Faced with these significant limitations, EPA based estimates of
saturated waste presence and thickness on the limited available pairs
of wells which are in close proximity to the waste material and are
located on opposite sides of the main waste body or larger fingers of
CCR waste. Using this approach allowed for limited direct comparison of
recent water levels data collected in 2021 and 2022 to the top and
bottom elevations of the CCR in that area of the unit. EPA considered
transects between the following well pair or pairs of clustered wells:
[GS-AP-MW-16S/GS-AP-MW-16D/GS-AP-PZ-16] to [GP-AP-MW-19]
[GS-AP-MW-21/GS-AP-MW-21V] to [GS-AP-MW-1/GS-AP-MW-1R/GS-AP-
MW-46]
[GS-AP-MW-12/GS-AP-MW-12V] to [GS-AP-MW-1/GS-AP-MW-1R/GS-AP-
MW-46]
Lastly, it is also important to note that EPA's assessment of water
levels in this action focused primarily on those monitoring wells which
were screened nearest the CCR in the unit at those specific locations.
These included wells screened in a variety of different levels within
the uppermost aquifer system. It must be recognized that this exercise
suffered from the limitations of the well network as screened interval
elevations varied somewhat from transect to transect. Regardless of
these complexities, water levels in most screened intervals were
consistently above the base of the impoundment.
This assessment suggests the sustained presence of significant
thickness of saturated waste in all of the areas EPA investigated. For
the [GS-AP-MW-16S/GS-AP-MW-16D/GS-AP-PZ-16] to [GP-AP-MW-19] transect
near the southern end of the Ash Pond, reported groundwater elevation
measurements from monitoring wells GS-AP-MW-16S and GS-AP-MW-19 range
from roughly 381 to 407 ft above MSL. In this area near the center of
the unit, the bottom of the CCR unit is located at approximately 335
feet above MSL and the top of the waste at closure is planned to be
roughly 450 feet above MSL. Based on these data EPA estimates that at
the deepest point of this transect a layer of CCR between 46 and 72 ft
in thickness is saturated. As stated above, EPA's estimates were
complicated by Alabama Power's failure to install many of the
monitoring wells at the waste boundary which is inconsistent with the
requirement in Sec. 257.91(a)(2)). In this case, EPA used data from
GS-AP-MW-16S and GS-AP-MW-19 because, based on the materials in the
Permit Application, they are a well pair that are located along
opposite sides of the unit from each other, or in other words, the two
wells span across a large portion of the unit. Nevertheless, the
lateral distance between GS-AP-MW-16S and GS-AP-MW-19 is still roughly
2,000 feet, and the bottom unit elevation is highly variable over that
distance given the incised valley setting in which the unit sits.
EPA also evaluated the most recent groundwater elevation data from
the Plant Gorgas 2022 Annual Groundwater Monitoring and Corrective
Action Report to determine if any recent closure activity at the site
has influenced groundwater elevations.\74\ Regarding the impact of
closure activity on groundwater elevations, the report itself is
contradictory. On page 20, the report indicates that no significant
changes in groundwater elevations or flow have been noted at the site
as ash
[[Page 55257]]
pond dewatering activities have not been initiated. However, on pages
21 and 22, the report states that dewatering operations began in 2022
and may be contributing to the groundwater elevations observed.
Further, on page 56 of the report, there is an acknowledgment that
``[t]he lack of obvious or significant trends [or changes in
groundwater quality] is likely in part due to (1) dewatering operations
not starting until the first week of July 2022, (2) the low
permeability nature of the subsurface flow systems, and (3) the number
of wells that have been recently installed or replaced (too few data
points for trend analyses).'' In any event, EPA's evaluation indicated
that groundwater elevation data collected in July 2022 is mostly
comparable to historical data, suggesting little influence thus far
from dewatering efforts. For example, most decreases in groundwater
elevations were observed to be less than a few feet. Some larger
decreases (greater than 10 feet) were observed at the southern portion
of the Ash Pond, but the report indicated that these decreases may be
the result of resumed mining activity south or southwest of the Ash
Pond, rather than closure activity related to the Ash Pond. Therefore,
while some uncertainty remains as to just how much CCR is currently
saturated, the available site data indicates that considerable areas,
thicknesses, and volumes of saturated CCR remain in the impoundment.
---------------------------------------------------------------------------
\74\ Southern Company Services 2022 Annual Groundwater
Monitoring and Corrective Action Report, Alabama Power Company Plant
Gorgas Ash Pond. Prepared for Alabama Power Company. January 31,
2023.
---------------------------------------------------------------------------
Similarly, along the [GS-AP-MW-21/GS-AP-MW-21V] to [GS-AP-MW-1/GS-
AP-MW-1R/GS-AP-MW-46] transect through Finger 1 of the Ash Pond, water
levels reported in 2021 and 2022 for GS-AP-MW-21 and GS-AP-MW-46 ranged
from 335 to 367 feet above MSL. The elevation of the bottom of the CCR
is roughly 322 feet above MSL and the top of the CCR unit is planned to
be approximately 428 feet above MSL in that part of the unit. Based on
these data EPA estimates that at the deepest point of this transect a
layer of CCR between 13 and 45 ft in thickness is saturated.
EPA also considered groundwater and waste elevations along the [GS-
AP-MW-12/GS-AP-MW-12V] to [GS-AP-MW-1/GS-AP-MW-1R/GS-AP-MW-46] transect
near the center main valley of the Ash Pond and extending eastward
along the northern side of Finger 1. Water levels from 2021 and 2022
from GS-AP-MW-12 and GS-AP-MW-46 ranged from 360 to 380 feet above MSL.
Given that the bottom of and top of the CCR are approximately 270 feet
and 390 ft above MSL respectively in the center of the impoundment, EPA
estimates that between 90 to 110 feet of saturated waste are present.
Similarly, for Finger 1 of the unit, EPA estimates that between 35 and
55 feet of saturated waste are present, based on bottom and top of the
CCR being at 325 feet and 430 ft above MSL, respectively. Based on
these limited available data, significant thicknesses of saturated CCR
are present in these areas.
Lastly, EPA evaluated groundwater elevations along a north to south
transect, south of the planned closure buttress, along the west side of
the main valley containing CCR. From north to south, this included
monitoring wells, GS-AP-MW-12, -13, -14, -47, -15, -16, and -18. This
transect is approximately 6,150 feet in length, or over a mile. Over
this distance the available monitoring wells were located from
approximately 25 to 1,100 feet away from the edge of the CCR waste and
from 50 to 1,500 feet from the central part of the valley filled with
CCR. EPA used engineering drawings available in the Permit Application
to estimate CCR top and bottom elevations adjacent to each groundwater
monitoring point (e.g., construction drawings G-204, C-200 to C-205).
CCR thickness values varied from 65 to 149 feet along the transect. In
some locations more than one estimate was made due to the complexity of
the subsurface. EPA then subtracted the CCR waste bottom elevation from
the most recent water levels for each location (primarily July 18,
2022), to determine the thickness of saturated CCR, which varied from
zero (no saturated waste) to approximately 115 feet of saturated CCR.
This analysis supported the overall conclusion that saturated CCR is
present in all of these locations and is therefore likely present at
all locations south of the planned closure buttress. Even at those
locations where pinpoint estimates of waste bottom elevations exceeded
the groundwater elevation values, there were also immediately adjacent
measurements indicating lower elevations of CCR that were below
groundwater elevation values. For example, in the GS-AP-MW-15 area,
estimates of waste bottom elevations varied by over 52 feet: at the
lower end of the range in Finger 6, EPA estimates there are 13 feet of
saturated CCR, compared with over 65 feet of saturated waste in the
adjacent main valley of the unit (i.e., station 70+00 on section B-B'
on construction drawing G-204). The only area arguably without any
saturated CCR is the extreme southern tip of the unit; on July 18,
2022, groundwater elevation values at GS-AP-MW-18 indicate that the
waste is above the water table. However, groundwater elevation values
measured at the closely adjacent well, GS-AP-MW-18R, which is also
screened in the Pratt strata, but more shallowly at elevations
comparable to the waste, on the same day, indicate approximately 63
feet of saturated waste.
According to the Closure Plan, it appears that dewatering may have
commenced relatively recently in 2022, so the measured groundwater
elevations described above from 2022 may not reflect early stage
decreases in hydraulic head within the unit from any initial dewatering
efforts. But as discussed below, the Closure Plan contains neither
meaningful details nor supporting analysis to demonstrate that the
saturated CCR in the consolidated southern portion of the unit will
ever be dewatered sufficiently to meet the performance standards in
Sec. 257.102(d)(2). Moreover, as discussed below, in the absence of
any engineering measures that would effectively prevent the continued
migration of groundwater into the closed unit, there is no information
in the Permit Application that suggests any meaningful decline is
likely in the groundwater elevations proximal to and within the CCR
unit. Significant thickness of saturated waste is therefore expected to
persist in the areas south of the closure buttress where CCR is still
present at elevations at or above the basal excavation level for the
consolidation effort (i.e., > 270 ft above MSL).
(1) In Order To Close the Ash Pond With Waste in Place Effective
Engineering Measures Must Be Implemented
The fact that prior to closure the base of the Ash Pond intersects
with groundwater does not mean that the unit may not ultimately be able
to meet the performance standards in Sec. 257.102(d) for closure with
waste in place. Depending on the site conditions a facility may be able
to meet these performance standards by demonstrating that a combination
of engineering measures and site-specific circumstances will ensure
that, after closure of the unit has been completed, the groundwater is
no longer in contact with the waste in the closed unit. In this case
EPA is proposing to determine that the approved Closure Plan fails to
demonstrate that either performance standard in Sec. 257.102(d) will
be met. In addition, neither the approved Closure Plan nor the Permit
requires any engineering measures, such as the slurry wall proposed for
Plant Greene, described in Unit IV.C.4 of this preamble, or a
groundwater extraction system (e.g., pumping wells) to control
[[Page 55258]]
or prevent the continued infiltration of liquids (groundwater) into the
CCR from the sides and beneath. Nor does the approved Closure Plan or
the Permit require any engineering measure that will effectively
control releases of leachate to the groundwater. Based on these facts,
and as discussed in more detail below, EPA is proposing to determine
that the approved Closure Plan fails to demonstrate that the closure at
Plant Gorgas will meet the Federal performance standards in Sec.
257.102(d) or an equally protective alternative State standard.
ii. Consistency With 40 CFR 257.102(d)(2)
As discussed previously, the Federal CCR regulations applicable to
surface impoundments closing with waste in place require that ``[f]ree
liquids must be eliminated by removing liquid wastes or solidifying the
remaining waste and waste residues, [and] remaining wastes must be
stabilized sufficient to support final cover system.'' 40 CFR
257.102(d)(2). But due to the lack of meaningful details and supporting
analysis in the Closure Plan, EPA is proposing to determine that the
Closure Plan approved by ADEM does not demonstrate that the proposed
closure at Plant Gorgas will meet either standard.
According to the approved Closure Plan, various dewatering
techniques will be employed before and during closure; however, the
Closure Plan appears to largely limit the use of these techniques to
the CCR in the northern portion of the unit that will be excavated and
transported to the consolidated area, and to the areas under the new
Closure Buttress.\75\ For example, in the sections specifically
discussing dewatering, the Closure Plan states:
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\75\ Alabama Power Company. Revised Closure Permit Application
for the Plant Gorgas Ash Pond. April 30, 2020. Revised Closure Plan
for the Plant Gorgas Ash Pond. Appendix 11, pp 7-8 (Emphasis added).
4.3 Procedures During Closure
4.3.1 Dewatering
This conceptual dewatering plan was developed to provide a summary
of the removal of free water, interstitial water, contact water, and
surface water as defined below.
Free water--water contained in the CCR unit above the
surface of CCR material
Interstitial water--water within the pore space of CCR
material
Contact water--surface or ground water that comes in
contact with CCR material
Surface water--non-contact surface water at the site that
requires management
. . .
The free water in the northern portion of the pond will be decanted
by pumping to a water treatment facility prior to discharge off-
site. The management of the free water levels in the pond are
important for site water management controls including coordination
with the proposed dredging and other construction processes.
Interstitial water levels will be monitored in critical areas to
allow for safe excavation and working on ash as needed to facilitate
construction activities.
The main pond free water management pumps will deliver water to the
water treatment plant for treatment and discharge up to a treatment
rate of 12,000 gpm. The pumping system will be equipped with a
floating intake, including a sediment curtain around the intake.
Removal of contact water will be completed within the limits of the
Ash Pond using both in-situ (in place prior to excavation/handling)
and ex-situ (after initial handling/excavation) techniques.
Dewatering of ash during closure activities includes removing water
using a variety of methods, including but not limited to passive,
gravity-based methods (e.g. trench drains, rim ditching, wick
points) and/or active dewatering methods (e.g. use of the ash
thickening plant, and in-situ pumps or well points) as needed to
allow for CCR removal and transportation. Ex-situ dewatering
techniques consist of but are not limited to the following: gravity
dewatering (settling basins and/or lateral trenching), racking and
windrowing, mechanical thickening, and absorbent desiccation.
EPA expects that Alabama Power intends to dewater the entire unit to
some extent, if only to ensure that the consolidated unit can support
the weight of the earthmoving equipment needed to grade the surface and
to install the cover system. But EPA was unable to find any discussion
of the methods that will be used to dewater the significant volumes of
saturated CCR in the southern portion of the impoundment in sufficient
detail to evaluate whether the free liquids (and not simply the ``free
water'' defined above) will be eliminated as required by Sec.
257.102(d)(2)(i). For example, on page three, the Closure Plan states
only that ``During closure, the ash pond will be progressively
dewatered as required to facilitate closure.'' And on page 5, the Plan
states
Initial stages of construction and dewatering will include lowering
of the pond levels through pumping and treatment at the onsite water
treatment facility to optimize dredge performance. Once the desired
initial free water depth is achieved in the pond, further dewatering
will occur incrementally in response to storm events in order to
maintain the free water at a relatively constant depth that will
lower as ash removal from the designated areas progresses.
Moreover, the narrative in the Closure Plan does not explain how
the liquids within the consolidated southern portion of the unit will
be eliminated in light of the groundwater that, as described above, is
expected to continue to saturate the remaining CCR. None of the
proposed engineering measures mentioned in the Closure Plan are
discussed in sufficient detail to support a determination that the
proposed measures could effectively remove these liquids. For example,
the approved plan mentions that a leachate collection system will be
installed at the downgradient limit of the Closure Buttress but fails
to explain which liquids the proposed drain system will capture and how
well or extensively it will do so.
However, based on the limited information available, the leachate
collection system that ADEM has approved appears to likely have only a
minimal impact on the level of liquids in the closed unit, as it is
designed to capture only a limited amount of leachate. According to the
construction drawings submitted with the Permit Application, it appears
the drain will only extend approximately 1,200 feet laterally beneath a
portion of the 274-acre impoundment and appears to rely exclusively on
gravity to direct any residual pore water or other free liquids to the
drains. In essence, the leachate collection system appears to be
designed to only collect leachate along its 1,200 foot design length,
and to only address residual leachate produced from limited pore water
within the CCR, which was perhaps expected to drain over a shorter
limited time frame, during the so-called ``dewatering phase.'' But
since not all groundwater leaving the unit will flow to the drain
system, any collection of free liquids from saturated CCR farther south
in the unit or along the eastern fingers would be purely coincidental,
even without considering the likely ongoing inputs of ``new''
groundwater (``contact water'') into the system south of the
Buttress.\76\
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\76\ ADEM confirmed these details during conversations with EPA
in July 2022.
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In addition, to be effective the leachate treatment system would
need to address not only leachate generated from short-term
``dewatering'' activities, but also the significantly greater long-term
volumes of leachate emanating from the continuously saturated CCR
resulting from ongoing groundwater inputs into the unit from the sides
and bottom. More critically, the system was not designed to handle the
volumes of ``new'' leachate that will continue to be generated from the
continued groundwater flow into the unit. The Closure Plan therefore
appears to have grossly underestimated the amount of
[[Page 55259]]
free liquids that will continue to flow through the saturated waste to
the face drain and associated leachate collection system.
To illustrate this concern, EPA performed a rough estimate of
potential recharge to the groundwater system within the 1,300-acre
watershed area which contains the unit. After subtracting the 274 acres
representing the closed, capped and consolidated unit, and assuming all
precipitation directly contacting the cap will be effectively managed
by the drainage system and other engineering controls, one is left with
1,026 acres available for potential recharge to the groundwater system.
Conservatively assuming 1-ft of effective recharge to groundwater in
one year over the 1,026-acre catchment area results in approximately
334 million gallons of effective recharge. Assuming this total
effective recharge is evenly distributed over time and remains in the
catchment area that contains the unit, and all flows into the unit,
this would result in a value on the order of 636 gallons per minute of
groundwater flow focused to the subsurface CCR waste beneath the capped
unit. In other words, additional engineering controls capable of
managing (and treating as necessary) this additional ongoing input of
groundwater into the unit would be a minimum necessity for a successful
Closure Plan.
Based on all of the above, it appears that further engineering
measures would be necessary to ensure that all free liquids are
eliminated prior to installing the final cover system, as required by
Sec. 257.102(d)(2)(i).
Additional data are necessary to demonstrate that saturated CCR
will not be present in the base of the closed unit prior to the
installation of the final cover system. Absent such data, the permit
record does not support a finding that the remaining wastes will be
stabilized sufficiently to support the final cover system, as required
by Sec. 257.102(d)(2)(ii). If the CCR in the unit is not sufficiently
stabilized, e.g., if it has not been completely drained, differential
settlement of the CCR after installation of the cover system is
possible, especially given the substantial added load from the
consolidation of CCR from the northern portion of the Ash Pond. If the
settlement is great enough, it could cause a disruption in the
continuity, and potentially failure of, the final cover system.
Additional information is needed to determine that the permit meets
Federal requirements. This could have been accomplished either by
requiring submission of the information prior to the issuance of the
permit or by including a permit term requiring submission of the
information, along with a clause allowing for further permit conditions
if necessary.
iii. Consistency With 40 CFR 257.102(d)(1)(i)
The available information indicates groundwater is likely to
continue to infiltrate into the unit and yet the only measures
described in the Closure Plan and the Permit to address this continued
infiltration are those taken to facilitate consolidation and cap
construction. As explained in previous sections, the exclusive reliance
on a cover system in this circumstance would not ``control, minimize,
or eliminate, to maximum extent feasible'' the post-closure
infiltration of the groundwater into the waste. 40 CFR
257.102(d)(1)(i).
The approved Closure Plan does not adequately account for the
hydrogeology of the site, which includes complex topography,
stratigraphy, hydrology, and other complex site characteristics such as
preferential pathways (faults, mines, etc.) that make it likely that
groundwater elevations will be higher than the bottom elevation of the
surface impoundment, even after the cover system is installed. The
cover system will only prevent liquids (precipitation) from entering
directly into the unit from the surface/top of the unit. But as shown
on the construction drawings in the Closure Plan (e.g., drawing C-100),
precipitation will continue to fall onto the surrounding higher ground
surfaces in the catchment area beyond the lateral extent of cover
system and then percolate down below the ground surface, the underlying
aquifer will recharge and groundwater levels will continue to
infiltrate into the CCR from beneath the unit, as well as from the
sides.
There are commonly used engineering measures that can prevent, or
at least control, the post-closure flow of groundwater into the unit;
for example, physical barriers such as slurry walls or liner systems or
by other means such as hydraulic containment systems (e.g., groundwater
extraction wells), additional backfilling to create a buffer between
the bottom of the unit and groundwater, CCR relocation, etc. EPA is
therefore proposing to determine that ADEM's approval of a Closure Plan
that relies exclusively on consolidation and cap construction to
control infiltration into the Ash Pond is inconsistent with Sec.
257.102(d)(1)(i).
EPA is also proposing to determine that the approved Closure Plan
fails to demonstrate that post-closure releases of CCR or leachate to
the groundwater will be controlled ``to the maximum extent feasible.''
40 CFR 257.102(d)(2)(i). While a leachate collection system is proposed
in the Closure Plan, EPA was unable to find either analysis or evidence
demonstrating the extent to which the proposed leachate collection
system will control ``post-closure releases of CCR or leachate to the
groundwater to the maximum extent feasible.'' 40 CFR 257.102(d)(2)(i).
Moreover, the available information does not support a determination
that the proposed system will meet this performance standard. As
previously discussed, the leachate collection system is not designed to
control the volume of leachate that is likely to be created from the
continued infiltration of groundwater, nor does it extend underneath
the entire unit.
In addition, there is substantial evidence that the hydrogeologic
pathways that will allow unimpeded migration of groundwater into the
unit from the bottom and sides of the unit will also allow leachate to
migrate laterally and vertically out of the unit at particular
locations. The absence of natural or engineered hydraulic barriers
along the base and sides of the unit, which allows for both
infiltration and exfiltration of liquids, will likely result in
additional releases of contaminated groundwater (i.e., ``plumes'') out
of the unit via the bottom or sides. For example, preferential
pathways, such as geologic faults and mine shafts from former mining
operations, are present beneath the unit that would be expected to draw
contamination from any uncaptured leachate down into the aquifer. The
existence of preferential pathways was clearly acknowledged in the GWMP
that was included in the Permit Application as Appendix C.\77\
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\77\ Alabama Power Company. Revised Closure Permit Application
for the Plant Gorgas Ash Pond. April 30, 2020. Response to Comments,
Approved Groundwater Monitoring Plan included in the October 20,
2021. For example, the following statements were made within the RTC
for the GWMP:
[i]n-conjunction [with statements made earlier in the letter],
the geology at Plant Gorgas dictates preferential flow through coal
seams and vertical to subvertical joints, fractures, and faults.
Targeting such features for monitoring, even if stepped back from
the waste boundary, is technically justified. This because
preferential flow paths concentrate groundwater migration through
enhanced fracture interconnectivity within otherwise impermeable
rock strata. Therefore, given the travel-times described [earlier in
the letter], and the age of the facility--it was appropriate to
target these features for determining potential impacts to
groundwater.
---------------------------------------------------------------------------
The approved Closure Plan does not account for these pathways or
otherwise evaluate how well the proposed drain system will capture
liquids. To meet the performance standard in Sec. 257.102(d)(1)(i),
the approved Closure Plan would have to show that the
[[Page 55260]]
leachate will be channeled to the leachate collection system rather
than to the preferential pathways, EPA was unable to find anything in
the Permit Application or permit record to show that either Alabama
Power or ADEM made any such showing. As discussed previously, the
available information indicates that the face drain and under-designed
leachate collection system would likely be ineffective in preventing
such releases, given the under-designed leachate collection system.
b. Plant Gorgas Groundwater Monitoring Issues
The Final Permit incorporated the GWMP submitted with the Permit
Application, and directed Alabama Power to comply with the State
regulations and the approved plan:
A. Groundwater Monitoring System. The Permittee shall install and/or
maintain a groundwater monitoring system, identified in Table 1, as
specified in 335-13-15-.06(2) and the approved groundwater
monitoring plan.
Once ADEM approved and adopted the GWMP into the permit, the GWMP,
rather than the referenced State regulations, became the State
requirements with which the facility is required to comply.
Based on EPA's review of the approved GWMP, EPA is proposing to
determine that the groundwater monitoring well network approved by ADEM
does not meet the performance standards in Sec. 257.91(a) or (b). As
discussed in more detail below, EPA is proposing to determine that the
groundwater monitoring system does not ``yield groundwater samples from
the uppermost aquifer,'' but has been screened instead in only a
portion of the aquifer. 40 CFR 257.91(a). EPA is also proposing to
determine that approved groundwater monitoring system is not based on a
thorough characterization of any of the elements listed in Sec.
257.91(b). Further, EPA is proposing to determine that the approved
monitoring system inappropriately includes numerous downgradient
monitoring wells that are not located at the waste boundary. See 40 CFR
257.91(a)(2). In addition, based on the documentation provided in the
Permit Application, it appears that there are an insufficient number of
monitoring wells at necessary locations and depths to meet the Federal
performance standards for either the background wells or the compliance
wells. See, 40 CFR 257.91(a)(1)-(2). Therefore, EPA is proposing to
determine that ADEM's Final Permit fails to require Alabama Power to
achieve compliance with either the Federal regulations or with an
equally protective State requirement.
i. Failure To Delineate the ``Uppermost Aquifer''
The Federal regulations require that a groundwater monitoring
system sample ``the uppermost aquifer,'' which is defined as ``the
geologic formation nearest the natural ground surface that is an
aquifer, as well as lower aquifers that are hydraulically
interconnected with this aquifer within the facility's property
boundary.'' 40 CFR 257.53, 257.91(a). The design of the monitoring
systems must be based on a thorough characterization of, among other
things, the ``aquifer thickness, groundwater flow rate, groundwater
flow direction including seasonal and temporal fluctuations in
groundwater flow; and saturated and unsaturated geologic units and fill
materials overlying the uppermost aquifer, materials comprising the
uppermost aquifer, and materials comprising the confining unit defining
the lower boundary of the uppermost aquifer.'' 40 CFR 257.91(b)(2). EPA
is proposing to determine that ADEM approved a groundwater monitoring
plan that does not meet these requirements.
Based on the limited information in the permit record, it appears
the facility failed to define both the upper and lower limits of the
uppermost aquifer. The GWMP provided in the Permit Application provides
only limited characterization of the geologic units beneath the Ash
Pond. In addition, the technical information provided in the Permit
Application and available on Alabama Power's CCR website is
insufficient to support a determination of the lateral and vertical
limits of the entire uppermost aquifer; for example, EPA found only
limited data on the ``saturated and unsaturated geologic units and fill
materials overlying the uppermost aquifer and materials comprising the
uppermost aquifer.'' 40 CFR 257.91(b)(2). And EPA was only able to find
limited and conflicting information about the ``materials comprising
the confining unit defining the lower boundary of the uppermost
aquifer.'' Id. In the absence of such key information it is impossible
to determine that the monitoring system adequately covers the entire
uppermost aquifer, which includes all ``lower aquifers that are
hydraulically interconnected'' with the aquifer nearest the ground
surface. 40 CFR 257.53 (definition of ``uppermost aquifer'').
Nevertheless, ADEM approved Alabama Power's GWMP unconditionally.
A representation of the various aquifers beneath the Ash Pond can
be obtained by examining the cross sections found in the 2021 Remedy
Selection Report.\78\ The uppermost aquifer may be described in its
most basic expression as a ``layer cake'' with interbedded layers of
sub-horizontal sedimentary rocks. As depicted in these cross sections,
for example Figure 9B of Appendix B of this report, for instance the
aquifer nearest the ground surface is shown as the Cobb Group. A
portion of the Cobb Group is present in higher elevations of the site,
overlying the Pratt Group. Both the Cobb and Pratt Groups are part of
the regionally significant Pottsville Formation. Coal beds known to be
present regionally in the Cobb Group were not identified near the unit
and Cobb Group rocks near the unit consist of sandstones, mudstones,
and shales. Some individual sandstone beds are depicted as having
thicknesses of over 50 feet as well as significant lateral extent, on
the order of thousands of feet. The Cobb Group also contains thick
laterally extensive mudstones, and the mudstones are interbedded with
thinner sand layers in the northern part of the unit. The aggregate
thickness of the Cobb Group is on the order of 200 to 250 feet or more
at the unit. As the stratigraphically highest rock layer, the Cobb
Group thickness varies across the unit due to differences of the
uppermost surface elevation of the Cobb Group resulting from
differential erosion. Alluvial materials and/or fill deposits rest
unconformably and discontinuously on top of the Cobb Group's upper
erosional surface in many areas of the unit, particularly to the south.
These Cobb Group stratigraphic intervals are poorly characterized in
comparison to the underlying Pratt Group, with few monitoring wells
installed in the Cobb Group rocks.
---------------------------------------------------------------------------
\78\ Southern Company Services. 2021 Groundwater Remedy
Selection Report, Alabama Power Company Plant Gorgas Ash Pond.
Prepared for Alabama Power Company. December 2021.
---------------------------------------------------------------------------
The upper part of the Pratt Group includes interbedded sandstones,
siltstones, mudstones, as well as several distinct coal beds. The
uppermost of these named coal beds is the Pratt Coal Seam and
associated layers, but additional named coal seams are present at
successively deeper levels, as described in Section 3 of the approved
GWMP: ``The Pratt Coal Group generally contains three named coal seams
each separated by 10 to 30 feet of intraburden. In descending order,
they are, the Pratt, Nickel Plate, and American coal seams.''
Beneath the upper part of the Pratt Group and its named coal seams,
a significant thickness of interbedded
[[Page 55261]]
sandstones and mudstones on the order of 50 feet or more is present.
These intervals are described as the Lower Pratt Group, which has
received comparatively little characterization and few monitoring
wells. The Pratt Group, including both the lower and upper portions, is
depicted as having an aggregate thickness of approximately 200 feet
beneath the unit. Differential erosion, particularly within the main
channel-like finger of the Ash Pond, has locally resulted in alluvial
materials and/or fill deposits resting unconformably on top of the
Pratt Group's upper erosional surface, particularly in the central part
of the unit.
In the southern portion of the unit, the Gillespy Group, also of
the Pottsville Formation, is shown on cross sections as underlying the
Pratt Group at great depths, but characterization of this interval is
extremely limited. The cross sections in the 2022 Semi-Annual
Groundwater Monitoring and Corrective Action Report show that the
Gillespy Group also has an aggregate thickness on the order of 200
feet, yet the upper and lower contacts between the Gillespy and
underlying and overlying layers is poorly characterized, particularly
with respect to the lower contact, and the thus the variability and
full vertical extent (i.e., thickness) of the Gillespy Group under the
Ash Pond has not been precisely determined. On cross section F-F'
(Figure 4F), the Gillespy Group is depicted as just over 200 feet in
thickness. The cross section also depicts the contact with the
underlying Mary Lee Group mudstones at a depth of several hundred feet
below the unit at a corresponding elevation just above MSL. However, it
is not clear what data informs this interpretation as no borings are
known to have penetrated the full thickness of the Gillespy Group near
the unit based on the cross sections and monitoring well installation
details. As such the true thickness of the uppermost aquifer and
hydraulically connected aquifers is not known, nor has it been
established whether the Gillespy Group constitutes an effective lower
confining unit to the uppermost or aquifer system. See 40 CFR
257.91(b). It is also notable that the elevation of the top of the
Gillespy Group is relatively high near the northern part of the unit,
and differential erosion has resulted in deposits of overburden,
alluvium and/or fill, including fill/dam materials resting
unconformably on top of the upper part of the Gillespy Group in the
northern part of the unit, as shown of cross section F-F'.
The additional relevant geologic aspects of the aggregate layering
which constitutes the uppermost aquifer system includes faulting and
folding of the layering. Following the ``layer cake'' analogy, the
layers of rocks have been disrupted locally on several steep fault
lines that predominantly strike north-northwest in the vicinity of the
unit, as such the ``layer cake'' package of rocks has been disrupted
and contains many distinct ``slices'' separated by these faults. The
faults indicate significant vertical offset on cross sectional
representations, and the rock layers are locally bent or ``folded''
near these fault structures, resulting in steeper dips. The entire
package has been slightly tilted regionally to the south as if the
northern end of the ``layer cake's serving platter'' had been lifted
slightly.
The final element, following the ``layer cake'' analogy, is the
``icing on the cake.'' Like drizzled icing, unconsolidated fill and
alluvial materials irregularly cover the tilted, faulted, and eroded
surface of the ``layer cake'' of rock layers. It is expected that
overburden including alluvial materials (e.g., sands and gravels)
originally present as stream deposits in the incised erosional stream
valleys were covered by the introduced CCR materials. These buried
alluvial materials therefore represent the uppermost veneer of the
uppermost aquifer system. Since there are few wells screened in these
former stream valleys, this element of the uppermost aquifer system is
significantly underrepresented in the monitoring network.
(1) Uppermost Aquifer
Within this complex ``layer cake'' geology of variable sedimentary
layering, Alabama Power screened most of its monitoring wells in the
Upper Pottsville Aquifer system, which is described in Section 3.2.2 of
the 2022 Semi-Annual Groundwater Monitoring and Corrective Action
Report as follows:
Groundwater occurs in the Pratt Coal Group of the Upper Pottsville
Formation at the site. The primary occurrences of groundwater in the
uppermost aquifer are: (1) coal seams, (2) rock fractures or zones
of fracture enhanced permeability, and to a lesser extent (3)
bedding planes. Fractured intervals are sparse across the site as
defined by caliper logging and tend to occur with greater density in
the upper 100 feet of rock.
Groundwater yield at the site is considered low and typical of the
Pottsville aquifer system in areas without major geologic
structures. Wells were generally screened in the Pratt coal seam or
across groundwater yielding fractures. Depth to groundwater
producing zones were highly variable at the site and typically
ranged from 30 to 240 feet BGS.
It is further noted in Section 3.2.3 of the 2022 Semi-Annual GWMCA
Report that,
Groundwater flow is accomplished primarily by means of fracture
flow, where groundwater flows along more conductive secondary
discontinuities in the rock mass such as joints or cleat fabric in
coal seams. Fracture flow in complex geologic media such as the
heterogenous Pottsville Formation can be complex. Groundwater in the
Pottsville aquifer is most commonly regarded as confined due to
large permeability contrasts within the aquifer (Stricklin, 1989).
The Pottsville at the Site is probably better described as a series
of discrete, confined to semi-confined, groundwater yielding zones
where groundwater elevations can vary significantly laterally and
vertically and are governed by the heterogeneity of the lithology
and degree of fracture network interconnectivity . . . .
At higher stratigraphic intervals (water-table flow system),
groundwater flows towards the Ash Pond or other surface water
bodies. This flow system is driven by gravity and mimics the
topography of the site. Within deeper rock strata such as coals of
the Pratt Group (Pratt Coal Group or deep bedrock flow system),
groundwater flows radially away from the site.
Most of the characterization and monitoring is concentrated in the
named coal seams of the Pratt Coal Group, and three primary flow
systems (i.e., aquifers) have been identified, as follows:
At the Site, the groundwater flow regime is now grouped into
three general flow systems: (1) shallow water-table flow system, (2)
Pratt Coal flow system, and (3) American Coal flow system.
In this system of nomenclature, the Nickel Plate Coal Seam is
generally included within the Pratt Coal System. EPA also noted that
the Pratt Coal System and the American Coal Systems are mapped together
and separately in different groundwater monitoring reports. For
example, the approved GWMP (Figure 6B) has them mapped together and the
2020 Annual GWMCA Report \79\ has them mapped separately (Figures 6B
and 6C). Accordingly, subsequent references to aquifers in the coal
seams, below, if not specifically described as the ``Pratt'' or
``American'' aquifers, describe the three coal seam flow systems of the
Pratt Coal Group jointly as an aggregate combined system.
---------------------------------------------------------------------------
\79\ Southern Company Services. 2020 Annual Groundwater
Monitoring and Corrective Action Report, Alabama Power Company Plant
Gorgas Ash Pond. Prepared for Alabama Power Company. January 31,
2021.
---------------------------------------------------------------------------
In addition to the three systems designated above (shallow water
table, Pratt, and American), lower intervals of the stratigraphic
section have been designated \80\ as another (fourth) system, which is
primarily localized to the northern part of the unit in the vicinity
[[Page 55262]]
of the Ash Pond dam and northward.\81\ In this area, the geologic units
located at depths corresponding to the transition zone from the lower
Pratt Group to rocks of the underlying Gillespy Group are mapped
together as the ``Base of Pratt to Gillespy Transition'' aquifer zone.
This interval is at much higher elevations in the northern part of the
site than in the southern portion. In any case, based on these aquifer
designations various interpretive representations of groundwater flow
have been constructed and were provided in the Permit Application and
annual monitoring reports. Based on these interpretations, in the Cobb
Group, above the Pratt Coal Group, groundwater is within an unconfined
aquifer and flows toward the unit. Within the Pratt Coal Group,
groundwater flow is interpreted to be mainly within the American and
Pratt Aquifers and flows radially away from the unit. However, these
interpretations are informed by insufficient data considering the large
geographic area represented by the Ash Pond as well as the topographic
and hydrogeologic complexity. The Ash Pond is approximately 500 acres
and sits within a watershed of roughly 1,300 acres with hundreds of
feet of topographic relief. The small number of wells installed in each
of the respective aquifer layers simply does not allow for a sufficient
level of resolution regarding the true configuration of the
potentiometric surface and related groundwater flow directions. As
such, the interpretations represented by the various potentiometric
surface contour maps included in the 2022 Semi-Annual GWMCA Report
contain a large degree of uncertainty.\82\ For example, there are just
a few wells screened in the unconfined materials above the coal seams.
Figure 6A of the 2022 Semi-Annual GWMCA Report, entitled Potentiometric
Surface Contour Map (Upper) Water Table Aquifer, February 7, 2022,
Plant Gorgas Ash Pond, is based on just 10 water level monitoring
points over an area hundreds of acres in size. Figure 6B of the same
report Potentiometric Surface Contour Map, Pratt Aquifer, February 7,
2022, is based on just 31 water level monitoring points over the same
area. Figure 6C of the same report is entitled Potentiometric Surface
Contour Map, American Aquifer, February 7, 2022. This interpretation is
based on just 21 water level monitoring points over the same immense
area. Lastly, there are a limited number of water level monitoring
points (13) that intersect the Gillespy; nearly all of the these are
screened across the interface between the Gillespy and the lower part
of the Pottsville Formation (see inset map on Figure 6B) entitled,
Generalized Potentiometric Surface Contour Map--Base of Pratt to
Gillespy Transition (North of Dam). In summary, given the large size of
the Ash Pond and the surrounding area, interpretations of the flow
systems are highly generalized because of the limited number of
monitoring points in each hydrostratigraphic units.
---------------------------------------------------------------------------
\80\ Id.
\81\ Southern Company Services. 2022 Semi-Annual Groundwater
Monitoring and Corrective Action Report, Alabama Power Company Plant
Gorgas Ash Pond. Prepared for Alabama Power Company. July 31, 2022.
See inset map entitled, ``Generalized Potentiometric Surface Contour
Map--Base of Pratt to Gillespy Transition zone (North of Dam)''
included on Figure 6B.
\82\ Id.
---------------------------------------------------------------------------
Additionally, the nature of the lower boundary of the aggregate
``uppermost aquifer'' system has not been sufficiently characterized or
monitored due to the limited number of wells installed into this zone,
and the documented importance of fracturing, where present, such as in
the subsurface beneath the unit, and its association with increased
permeability values. This issue is discussed below. A key consideration
with respect to the base of the Pratt to Gillespy transition is whether
this transitional formation contact represents the boundary between the
materials comprising the ``uppermost aquifer,'' and materials
comprising the ``confining unit defining the lower boundary of the
uppermost aquifer.'' 40 CFR 257.91(b)(2). It is asserted in the 2022
Semi-Annual GWMCA Report that,
Except for the far northern portion of the Ash Pond, conceptually,
there is likely to be little hydraulic communication with strata
deeper than the sandstone unit immediately underlying the American
Coal Seam (American Coal Flow System). Below this interval, a low
permeability mudstone to interbedded mudstone-sandstone unit likely
forms a barrier to vertical migration of groundwater as hydraulic
conductivity values in the 10-\7\ centimeter per second
(cm/s) range are reported for shales at the site as derived from
packer testing. This interval reflects the transition to Gillespy
Coal Group.
Additional information presented in the same report presents
contradictory information regarding the confining potential of the
basal portion of the Gillespy Coal Group:
However, to the north and underlying the Ash Pond dam, strong
hydraulic gradients likely force groundwater along vertical
fractures and bedding planes through the upper part of the Gillespy
Coal Group. Geophysical and hydrophysical logs obtained in well
locations north of the dam suggest that three to four discrete
bedding planes occurring between 30 and 90 ft BGS transmit
groundwater. The most prominent typically occurring at a depth of 49
to 56 ft BGS (likely Gillespy equivalent; approximately 100 feet
below American Coal Seam).
The potential for vertical flow, within the Gillespy is further
described as follows:
Strong upward vertical gradients are observed in paired well
locations (see groundwater elevations in MW-6S/6D and MW-41HS/HD
pairs) installed north of the ash pond dam. Potentiometric data
suggests upward vertical flows along with northerly lateral flow.
Lastly, the same report discusses permeability test results, which
again present an inconsistent picture of the Gillespy formation's
potential to act as a ``confining unit defining the lower boundary of
the uppermost aquifer,'' as follows:
Forty-three packer tests were conducted resulting in a range of
hydraulic conductivity (k) values from an estimated low of 7 x
10-\7\ cm/sec to a high of 4 x 10-\3\ cm/sec,
with most tests (31) in the moderate range (10-\5\ cm/sec
to 10-\4\ cm/sec), two test results in the more permeable
range (10-\3\ to 10-\2\ cm/sec), and ten test
results in the less permeable range (10-\6\ cm/sec).
There is a general trend of decreasing estimated hydraulic
conductivity with depth. Packer test results vary over 4 orders of
magnitude. Test intervals at the high end of the data range are
associated with weathered discontinuities (fractures/joints).
Moderate values are associated with minor fractures or bedding
planes. The lowest values are associated with more shale intervals
without substantial fractures. Test intervals with coal seams are in
the moderate to high end of the data range.
EPA disagrees that this information supports a determination that
the lower part of the Gillespy formation constitutes a ``confining unit
defining the lower boundary of the uppermost aquifer.'' The totality of
the information instead supports the opposite conclusion. Since
vertical flow is clearly a recognized phenomenon within the Gillespy
within the northern part of the unit, and this flow is described as
being associated with fractures,\83\ it is logical to expect similar
vertical flow and enhanced permeability in other areas where fractures
are present. Given the prevalence of steeply dipping north-northwest
striking fracturing in the area, as well as the likelihood that the
linear valley that underlies the unit, which also strikes north
northwest, is also controlled by underlying fractures of this
orientation, it is reasonable to expect enhanced flow potential along
[[Page 55263]]
and in the vicinity of these fractures where they may exist. Since the
subsurface directly beneath the unit is likely the locus of such
fracturing (see Unit IV.C.3.b.i.(4)(c) of this preamble for more
information on the existence of preferential pathways), it is logical
to determine that vertical permeability is high beneath the unit where
it matters most. In other words, this situation suggests that rather
than a ``confining unit defining the lower boundary of the uppermost
aquifer,'' the near vertical fracturing which penetrates all units (see
cross sections), including the Gillespy, creates the opposite condition
in the uppermost aquifer system, directly beneath the unit. It is
therefore unlikely that the uppermost aquifer beneath the Ash Pond has
been adequately characterized, and its full thickness in the vertical
dimension remains unknown based on the information in the permit
record. As was noted above, the lowest measured permeability values are
associated with shale intervals without substantial fractures. Although
conditions are not sufficiently documented directly beneath the unit,
the likely presence of fractures here would be expected to invalidate
the presence of ``shale intervals without substantial fractures,'' and
hence the ``lowest measured permeability values,'' while present in
other areas around the unit, would likely not be present directly
beneath the unit.
---------------------------------------------------------------------------
\83\ Southern Company Services. 2022 Annual Groundwater
Monitoring and Corrective Action Report, Alabama Power Company Plant
Gorgas Ash Pond. Prepared for Alabama Power Company. January 31,
2023. Section 3.2.3.
---------------------------------------------------------------------------
In sum, the uppermost aquifer system- that is, the aquifer nearest
the ground surface and the underlying aquifers that are hydraulically
connected to it--has not been fully assessed. EPA's assessment of the
available information is that there are at least four flow systems that
are appropriately considered the ``uppermost aquifer'' at the Ash Pond:
(1) the upper unconfined water table (locally includes unconfined Cobb
Group); (2) the Pratt Coal seam; (3) the American Coal seam; and (4)
the Lower Pratt/Gillespy Transition zone.
The geologic units above and beneath the coal seams are sandstones
and interbedded sandstones with mudstone or shale, and both are capable
of storing and transmitting groundwater, and therefore should have been
more fully characterized and included in the monitoring network. In
particular, the depth of the lower confining unit has not been
established, and as such, the full extent of the uppermost aquifer
system has not yet been established in the vertical (depth) dimension.
At several locations, the geologic units immediately below detected
groundwater contamination are entirely uncharacterized and unmonitored.
This situation hobbles the monitoring network's ability to identify and
evaluate potential migration of contaminated groundwater out of the
unit at the lower levels, which is discussed further in Unit
IV.C.3.b.i.(4)(b) of this preamble.
(2) Background Wells Do Not Meet the 40 CFR 257.91(a)(1) Performance
Standard
The Federal CCR regulations require that a groundwater monitoring
system consist of a sufficient number of wells at appropriate locations
and depths to yield samples from the uppermost aquifer that accurately
represent the quality of the background groundwater that has not been
affected by leakage from a CCR unit. 40 CFR 257.91(a)(1). The
regulations also specify that background wells must normally be
hydraulically upgradient of the CCR unit unless specific showings have
been made. See, Id. EPA is proposing to determine that the approved
GWMP fails to document either that the background wells are upgradient
of the CCR unit or that the wells meet the performance standards in
Sec. 257.91(a)(1)(i) or (ii). EPA is also proposing to determine that
the background wells in the approved groundwater monitoring system do
not ``accurately represent the quality of the background groundwater''
because no background wells were installed in the lower flow systems of
the uppermost aquifer: i.e., the Pratt Coal seam; the American coal
seam, and the Lower Pratt/Gillespy Transition Zone.
Four groundwater monitoring wells have been used at various times
to characterize background water quality (GS-AP-MW-8, GS-AP-MW-13, GS-
AP-MW-16S, and GS-AP-MW-17V). One of the wells, GS-AP-MW-13 was
installed in 2016 and later abandoned in 2019. The three remaining
monitoring wells (GS-AP-MW-8, GS-AP-MW-16S, and GS-AP-MW-17V) were
installed exclusively in the upper flow system (i.e., in the upper
water table aquifer/unconfined Cobb Group formation), where Alabama
Power has concluded that groundwater flows toward the Ash Pond. No
background wells were ever installed in the three lower flow systems of
the uppermost aquifer, which is where contamination is currently
present.
According to the 2021 Plant Gorgas Annual GWMCA Report, to the
north and underlying the Ash Pond dam, strong hydraulic gradients force
groundwater along vertical fractures and bedding planes through the
upper part of the Gillespy Coal Group toward the Ash Pond.\84\ The
approved GWMP also provides details regarding vertical gradients and
the potential for using monitoring wells in the shallow flow system as
background wells. For example, page 10 states:
---------------------------------------------------------------------------
\84\ Southern Company Services. 2021 Annual Groundwater
Monitoring and Corrective Action Report Alabama Power Company Plant
Gorgas Ash Pond. Prepared for Alabama Power Company. January 31,
2022.
It is because vertical flow is the dominant mechanism for movement
through these flow systems and that is a function of the Pottsville
operating as a series of discrete, confined to semi-confined
groundwater yielding zones. Upgradient well locations monitor
younger, recharging waters that will eventually migrate vertically
---------------------------------------------------------------------------
downward into groundwater yielding zones of the Pratt Coal Group.
Based on the limited data available it appears that groundwater in
the upper water table (or un-confined Cobb) aquifer may migrate
downward into the lower flow systems due to vertical hydraulic
gradients. However, as discussed at length above, these interpretations
contain a large degree of uncertainty because they are informed by very
little data, given the size of the Ash Pond as well as the topographic
and hydrogeologic complexity of the site. The complexity of the site is
of particular concern here; in addition to the compositional
variability of the layers, differential fracturing also creates
variable hydraulic conditions which needed to be carefully considered
in selecting upgradient background well locations. Lastly, the wells
currently selected for background monitoring ignore horizontal flow in
the lower flow systems where groundwater contamination is present and
migrating laterally. EPA is proposing to determine there is
insufficient data to conclude that the approved background wells meet
the performance standards in Sec. 257.91(a)(1).\85\
---------------------------------------------------------------------------
\85\ Because Alabama Power believes the background wells to be
hydraulically upgradient, the Permit Application did not include a
demonstration that the background wells will be ``as representative
or more representative'' as hydraulically up gradient wells. 40 CFR
257.91(a)(1)(ii).
---------------------------------------------------------------------------
EPA is also proposing to determine that there are insufficient
number of background wells in the approved groundwater monitoring
system. As discussed in the preceding section, there are at least four
flow systems that would each require background wells focused on the
specific hydrogeologic conditions in each of these zones: (1) The upper
water table aquifer; (2) The Pratt Coal seam; (3) The American Coal
seam; and (4) The Lower Pratt/Gillespy Transition zone. In addition to
these
[[Page 55264]]
four, it remains unclear whether other flow systems should have been
included in the monitoring program, which would require the
installation of appropriate zone-specific background wells. For
example, the Cobb Group appears to contain multiple permeable sandstone
units, as do portions of the Pratt Group both above and below the named
coal seam aquifers. It would appear that background wells should have
been installed in one or both of these geological formations to capture
this geologic variability. As noted above, in addition to the
compositional variability of the layers, differential fracturing also
creates variable hydraulic conditions that needed to be more carefully
considered in selecting background well locations.
The Federal regulations require a monitoring well system that
accurately represents the quality of background groundwater. 40 CFR
257.91(a)(1). Background concentrations need to be determined for the
entire uppermost aquifer system and must be supported by an explanation
of the hydraulic and geologic factors that validate the selection of
particular locations as representative background conditions. If the
uppermost aquifer varies laterally and vertically in terms of geology
and chemical composition, it is necessary for the background monitoring
wells installed to adequately reflect this same range of variability
(i.e., representative conditions in these same layers absent CCR-
related impacts). This requires enough monitoring wells to capture the
variability represented by the natural system in appropriate
dimensions, such as lateral and/or vertical variability. Consequently,
in cases of multiple flow systems comprised of variable geology, as a
first order requirement, background wells in each hydrostratigraphic
unit of interest would be technically necessary.
The specific conditions at Plant Gorgas further illustrate this;
the geochemistry of the groundwater within the shallow water table
aquifer (consisting of younger groundwater within sandstone and shales)
would not represent the geochemistry of deeper flow systems (consisting
of older groundwater within interbedded sandstones with coal seams). It
is also uncertain how unique conditions in the lower flow systems, such
as the presence of coal seams and current and historical mining
operations could affect background water quality in the lower flow
systems.
In summary, the uncontaminated ``flavors'' (i.e., representative
conditions) of each relevant aquifer zone need to be established to
provide a representative direct comparison relative to CCR impacts in
these same zones on an ``apples to apples'' basis. However, the
approved background monitoring system is insufficient in terms of
general numbers of background monitoring wells as well as a general
failure to include background monitoring in key sub-elements of the
layered hydrogeologic system representing the uppermost aquifer. It
therefore does not appear to accurately represent the full range of
``background'' conditions in the uppermost aquifer.
(3) Compliance Wells Are Not Installed at the Downgradient Waste
Boundary
40 CFR 257.92(a)(2) requires that downgradient compliance wells
``be installed at the waste boundary that ensures detection of
groundwater contamination in the uppermost aquifer.'' The waste
boundary is ``a vertical surface located at the hydraulically
downgradient limit of the CCR unit. The vertical surface extends down
into the uppermost aquifer.'' 40 CFR 257.53. Notwithstanding this clear
direction, most wells in the monitoring network installed at Plant
Gorgas were located far from the waste boundary. Yet ADEM approved the
system without condition or revision.
For example, EPA evaluated well placement along a north to south
transect, south of the buttress, along the west side of the main valley
containing CCR. From north to south, this included, GS-AP-MW-9, -10, -
11, 12, -13, -14, -47, -15, -16, and -18. This transect is
approximately 8,400 feet in length, or over a mile and a half. Over
this distance the monitoring wells were located from 55 feet to 510
feet away from the waste boundary, with and average distance from the
waste boundary near 295 feet. On average, over the entire unit,
monitoring wells here were located approximately 740 feet from the
waste boundary.
ii. Insufficient Locations and Depths of Downgradient Compliance Wells
To Monitor the Uppermost Aquifer
As previously discussed, the Federal regulations specify that a
groundwater monitoring system must ``consist[ ] of a sufficient number
of wells, installed at appropriate locations and depths, that . . .
accurately represent the quality of the groundwater passing the waste
boundary of the CCR unit.'' 40 CFR 257.91(a)(2). The regulations
further specify that ``[a]ll potential contaminant pathways must be
monitored.'' Id. But the groundwater monitoring system that ADEM
approved meets none of these requirements. As discussed in more detail
below, EPA is proposing to determine that ADEM approved a GWMP with an
insufficient number of wells laterally along the downgradient perimeter
of the unit to monitor all potential contaminant pathways. EPA is also
proposing to determine that monitoring wells in the approved plan were
not installed at appropriate depths to ensure that all potential
contaminant pathways were monitored. Finally, EPA is proposing to
determine that the approved groundwater monitoring system fails to
account for preferential pathways beneath the Ash Pond.
(1) Insufficient Lateral Spacing of Compliance Wells To Monitor All
Potential Contaminant Pathways
The majority of the compliance wells along the perimeter of the
Plant Gorgas Ash Pond are spaced hundreds and sometimes thousands of
feet apart. For example, only a single detection monitoring well (GS-
AP-MW-2) was installed near the waste boundary to monitor groundwater
over a large area flowing from the Plant Gorgas Ash Pond along the
northeastern boundary. The lateral distances from GS-AP-MW-2 to the
adjacent compliance wells to the north and south, GS-AP-MW-3, and GS-
AP-MW-1R, respectively, both approach 2,000 feet (as the crow flies).
Furthermore, the waste boundary between the two compliance wells GS-AP-
MW-2 and GS-AP-MW-1R is approximately two miles. This unmonitored two-
mile portion of the waste boundary runs along three sides of an
adjacent offsite 16-acre parcel that appears to include residential
structures. In effect, this leaves a two-mile stretch without any
compliance wells to detect contamination before it migrates off-
site.\86\ See Figure 5A in the 2021 Plant Gorgas Annual GWMCA
Report.\87\
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\86\ Two wells (GS-AP-MW-43H and GS-AP-MW-44HO) are also
situated in the vicinity of the adjacent offsite 16-acre parcel, but
these wells are designed to horizontally delineate the plume of
contamination that has already migrated beyond the unit boundary.
\87\ According to a representative from the Copeland Ferry--
Pumpkin Center Water Authority Publicly Owned Treatment Works, they
serve public drinking water to residents in the vicinity of the Ash
Pond. EPA is also working to confirm whether nearby households are
on public or private water supply.
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This is not an anomaly, and extremely large lateral well spacings
and large lateral gaps in monitoring well coverage are not an isolated
occurrence. Prior to closure, the perimeter of the unit was roughly
14.7 miles in length, and following closure, the perimeter of the
consolidated CCR will be approximately 7.8 miles in lateral extent.\88\
Because
[[Page 55265]]
ADEM approved the groundwater monitoring system in its current form,
and it appears that the monitoring network will change little during
the ongoing closure activities, it is reasonable to evaluate the
lateral well spacing in terms of the current (pre-closure) perimeter,
i.e., 14.7 miles. Over this 14.7-mile unit boundary there are presently
only 30 downgradient compliance wells, indicating an average spacing of
approximately 2,600 feet, or roughly half a mile between monitoring
wells. Prior to 2021, there were only 20 downgradient compliance wells,
indicating an average lateral spacing of downgradient compliance wells
in the lateral dimension was on the order of 3,900 feet apart, or
almost three quarters of a mile.
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\88\ This approach is further supported in view of the fact that
the original footprint, although reconfigured, is still integral to
the overall closure strategy. Further, SSLs have been detected in
the reconfigured northern region, which will require monitoring and/
or corrective action into the future.
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Because wells installed to characterize the release in accordance
with Sec. 257.95(g)(1)(i) are not located on the downgradient waste
boundary and are monitored for different constituents at different
frequencies, these wells are not properly included in an evaluation of
adequacy of the detection and assessment wells installed to comply with
requirements in Sec. 257.91(a). And even if EPA were to consider the
delineation wells as part of the detection and assessment monitoring
systems, that would only bring the total number of monitoring wells to
68, which would equate to one well per every 1,150 feet of boundary.
However, by any reasonable standard, lateral well spacings on the
order of thousands of feet would be excessive. While appropriate
lateral well spacing is site-specific, and varies from site to site,
lateral well spacing appropriate for a site such as the Ash Pond at
Plant Gorgas may be determined by several factors. These include, but
are not limited to, the character, the degree of homogeneity, and
dimensions of the emplaced waste body itself; the nature, variability,
and complexity of the subsurface geology; as well as the dynamics,
complexities, and boundary conditions of the hydraulic flow system into
which the CCR has been emplaced. A greater degree of complexity and
variability concerning these elements would translate to a greater
number of compliance wells in the lateral dimension, i.e., a smaller
inter-well spacing, for the well network to adequately monitor such a
system. Conversely, a well characterized system, based on geological,
hydrogeological, and geotechnical investigations at the site, which has
been demonstrated to be simple, stable, and uniform would allow for a
fewer number of compliance wells to capture the limited inherent
variability. In addition, factors related to resolution and uncertainty
also affect the lateral well spacing appropriate to a given site. In
this regard it should be noted that the Federal regulations indicate
clear expectations regarding expected levels of resolution, which are
generally described as that necessary to ensure that all potential
contaminant pathways in the entire uppermost aquifer are monitored,
including preferential pathways. Uncertainties and data gaps also
equate to the need for greater levels of monitoring than would
otherwise be required to compensate for these deficiencies. In other
words, if characterization data are not available to support a larger
minimum lateral well spacing, a default to a more rigid general
standard is needed, requiring more wells. At the Ash Pond at Plant
Gorgas, a much smaller lateral well spacing is needed to meet the
requirements. This is due to (1) The complexity of the buried CCR; (2)
The low resolution and extreme uncertainties in the characterization of
the groundwater flow system which encompasses the unit; (3) The
demonstrated complexity of the geologic layering in the vertical
dimension; and (4) The presence of significant localized fracturing and
numerous mapped faults which cut through the unit and surrounding
areas. In a general sense, therefore, instead of thousands of feet
apart, monitoring well spacings should have been on the order of
hundreds of feet, except where known features such as narrow buried
erosional stream valleys or fracture zones dictate even tighter lateral
spacing. For example, the lateral spacings between wells MW-9, -10, -
11, and -12 ranges from roughly 700-1,200 feet apart, yet none of these
monitoring wells were located sufficiently close together to intersect
the mapped fracture which cuts through this area of the site. A tighter
well spacing is needed to adequately characterize the site. As another
example, many wells are screened in zones which intersect underground
coal mines. These mine tunnels represent potential preferential
pathways which should have been more intensively monitored. The lateral
and vertical dimensions of these types of underground workings are
knowable and should be factored into decisions concerning appropriate
monitoring well spacings to effectively ensure these preferential
pathways are monitored. Much smaller lateral and vertical wells
spacings are necessary to meet the requirements in this scenario,
instead of wells that are thousands of feet apart.
(2) Insufficient Number of Downgradient Compliance Wells Installed at
Appropriate Depths To Monitor the Entire Aquifer (Inadequate Vertical
Spacing)
EPA is also proposing to determine that ADEM approved a GWMP that
lacked ``a sufficient number of wells, installed at appropriate
locations and depths'' to ensure that all potential contaminant
pathways in the entire uppermost aquifer are monitored. As discussed
above, the uppermost aquifer contains at least four flow systems: (1)
the upper water table; (2) the Pratt Coal seam; (3) the American Coal
seam; and (4) the Lower Pratt/Gillespy Transition zone. A system of
compliance wells that meet the performance standards of Sec.
257.91(a)(2) must be installed in each of them. But none of the four
flow systems contain sufficient numbers of wells to meet these
standards.
Nearly all the compliance wells installed in the three lower flow
systems were screened across the shallow coal seams located between
approximately 250 and 350 ft-MSL, i.e., in the Pratt Coal seam and the
American Coal seam. Of the eight cross sections reviewed,\89\ it
appears that only two downgradient compliance wells were screened below
the coal seams in the Lower Pratt/Gillespy Transition zone (GS-AP-MW-6S
and -6D). These wells are downgradient due to the unit's radial flow at
this depth, and two wells are insufficient to comprehensively monitor
this portion of the uppermost aquifer. First, all the monitoring wells
installed below the coal seams are focused along the western and
northern section of the unit, leaving the northeastern, southwestern,
southern, and eastern sections with little to no data in the aquifer
below the coal seams. Conservatively, this means the lower flow systems
within the Lower Pratt/Gillespy Transition for over half of the pre-
closure extent of the unit (at least 237 acres) are not being
monitored.
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\89\ Anchor QEA. Prepared for Alabama Power Company. Plant
Gorgas Groundwater Remedy Selection Report. December 2021. Figures
5A and 5B in the revised GWMP and Figures 9A thru 16 in the
---------------------------------------------------------------------------
This is further corroborated by the cross-sections in Figures 11A,
14A, 15, and 16 of the Groundwater Remedy Selection Report, which
document the large portions of the uppermost aquifer below the coal
seams where no data
[[Page 55266]]
have been obtained.\90\ According to Figure 14A, there appears to be
only one well cluster (GS-AP-MW-6S/6V/6D) installed below the coal
seams, approximately 900 feet from the edge of the ash pond immediately
downgradient of the current dam. Given the unit's pre-closure size of
474 acres and a vast downgradient waste boundary exceeding fourteen
miles in length, this single well cluster would certainly not monitor
all potential contaminant pathways in this lower flow system.
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\90\ Id at pp 81, 83 of the revised Groundwater Monitoring Plan
and Figures 9A thru 16.
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There are also only 10 wells screened in the upper water table
(i.e., in the unconfined materials above the coal seams in the Cobb
Group). As shown in Figure 6A of the 2022 Semi-Annual GWMCA Report,
entitled Potentiometric Surface Contour Map (Upper) Water Table
Aquifer, February 7, 2022, Plant Gorgas Ash Pond, these 10 water level
monitoring points are installed over hundreds of acres, only 7 of these
are designated as compliance wells, and there is conflicting
information between the Permit Application and the most recent Annual
GWMCA Report from 2022 regarding the stratigraphic layers in which
these compliance wells are screened. For example, the 2022 Annual GWMCA
Report only indicates that two of these 7 wells are screened across the
``shallow water table.'' EPA therefore is proposing to determine that
the compliance monitoring with respect to the shallow unconfined water
table aquifer zone is not adequate to comply with the regulations.
Similarly, based on the 2022 Semi-Annual GWMCA Report, 52 wells
were installed in the Pratt Group as a whole across the entire 274-acre
Ash Pond.\91\ Of these, based on the interpretation of the flow system
provided in the 2022 Semi-Annual GWMCA Report, water levels were
measured at 31 wells installed in Pratt Coal seam,\92\ and water levels
were measured at 21 wells screened in the American Coal seam.\93\
However, the compliance well network listed in Table 1A in the Permit
Application indicates only 15 compliance wells screened in the Pratt
coal seam zone, and only 11 compliance wells screened in the American
Coal seam.
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\91\ Monitoring wells screened in the Nickel Plate coal seam are
included in the Pratt Coal seam category for this discussion.
\92\ Southern Company Services. 2022 Semi-Annual Groundwater
Monitoring and Corrective Action Report, Alabama Power Company,
Plant Gorgas Ash Pond. Prepared for Alabama Power Company. July 31,
2022. Figure 6B, Potentiometric Surface Contour Map, Pratt Aquifer,
February 7, 2022.
\93\ Id at Figure 6C of the same report is entitled
Potentiometric Surface Contour Map, American Aquifer,
---------------------------------------------------------------------------
Lastly, based on the interpretation of the flow system provided in
the 2022 Semi-Annual GWMCA Report, water levels were measured and
plotted for 15 wells to inform a representation of potentiometric
contours for the Base of the Pratt--Gillespy transition zone.\94\
However, these 15 wells do not appear to be screened in equivalent
levels of the transition zone and only 13 of these are listed on Tables
1A (3 Wells), 1B (8 Wells), and 1C (2 wells) in the 2022 Semi-Annual
GWMCA Report. Moreover, not all of 13 wells were included/depicted on
Figure 6B \95\ and only 3 ``Pottsville Fm--Gillespy zone transition''
wells are listed as compliance wells on Table 1A in the Permit
Application. This lack of clarity concerning the characterization and
monitoring of the transition zone between the lower Pratt Group and
Gillespy Group, supports EPA's basic conclusion above, that the base of
the uppermost aquifer has not been determined or sufficiently
characterized vertically (or laterally).
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\94\ Id at inset map on Figure 6B entitled, Generalized
Potentiometric Surface Contour Map--Base of Pratt to Gillespy
Transition (North of Dam).
\95\ Id.
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In summary, installing so few compliance monitoring wells over such
great lateral distances and over such significant vertical intervals
cannot possibly monitor all the potential contaminant pathways at Plant
Gorgas, given the size of the Ash Pond as well as the topographic and
hydrogeologic complexity of the site.
(3) Preferential Pathways Are Not Monitored
Numerous preferential pathways have been documented in the
uppermost aquifer under the Ash Pond. Yet under the approved GWMP, none
of these significant potential contaminant pathways appear to be
adequately monitored, despite the express requirement in Sec.
257.91(a)(2).
The approved GWMP states that, ``Locally, Pratt Coal Group strata
gently dip (0.5[deg] to 1.0[deg]) to the south and south-southwest.
Figure 5A Geologic Cross-Section A-A' and Figure 5B Geologic Cross-
Section B-B' illustrate the geologic layering beneath the site.'' It is
immediately apparent from these cross sections that a simple, nearly
flat series of geologic layers is an overly simplistic representation
of the site. As has been noted in many reports from Alabama Power in
the permit record, the geologic layering is disrupted in many locations
by mappable faults which indicate significant displacement and have
steepened dips resulting in folding in some areas of the subsurface.
Nevertheless, the monitoring network does not include monitoring
wells with screens deliberately targeted to these mapped faults and
associated fractures. Given the presence of these significant fault
zones, some of which have been mapped and delineated within the
aquifer, additional monitoring wells should have been installed to
detect whether CCR contaminants are migrating beyond the unit
boundaries in pathways that follow these fracture lines. As an
illustrative example, as shown on Figures 7A, 7B, 8A and 8B of the 2022
Semi-Annual GWMCA Report, a series of north-northwest striking
fractures with steep dips to the west cut through the unit. One such
fracture is mapped from the region of MW-10R north-northwestward 3600
feet (over half a mile) to the Mulberry Fork and beyond, further to the
north-northwest. Monitoring wells MW-12 and 12V are located hundreds of
feet to the east of the fault and therefore did not intersect it.
Similarly, MW-11 is too far away from the feature and too shallow, so
it also failed to intersect the feature. Ultimately it does not appear
that any monitoring wells effectively monitor this significant
potential contaminant pathway, which is particularly problematic as the
fault appears to intersect the river in the general downgradient
direction and thus has the (unassessed) potential to directly discharge
CCR-related contaminants to the river system. This natural fracture-
controlled ``pipeline'' represents a likely conduit for preferential
groundwater flow which follows the strike of the fracture and thus
represents a significant, unmonitored, potential contaminant pathway.
It is notable that none of these identified fractures are included on
Figure 5, Monitoring Well Location Map Plant Gorgas Ash Pond, of the
same report.
Additional preferential pathways are associated with underground
mine workings which impinge on parts of the unit. Coal mining
operations, including underground workings, are also well documented in
the vicinity of the site, and coal beds have been generally targeted
for most of the monitoring well installations. But while some
monitoring points appear to be screened at the same horizon as these
underground mine workings, their lateral extent in the subsurface
remains unknown, and as such the potential for preferential pathways
which exploit these zones represents a clear data gap. For example, the
geologic cross sections included in the 2021 Plant Gorgas
[[Page 55267]]
Annual GWMCA Report indicate the presence of former mine shafts that
could significantly impact groundwater flow, and therefore warranted
additional characterization and focused monitoring. These pathways were
also documented in the December 2021 Remedy Selection Report, which
ADEM received 3 months prior to its issuance of the Plant Gorgas permit
in February 2022. In addition, according to the cross section in Figure
5A in the revised GWMP and Figure 12A in the Groundwater Remedy
Selection Report, at least one fault that could serve as a potential
preferential pathway for groundwater has been mapped immediately
adjacent to the Ash Pond and penetrates below the coal seams. It is
therefore another significant failure of the approved groundwater
monitoring system that it does not include wells to monitor the
targeted and delineated contaminant pathways that follow coal seams,
underground workings, or other natural and/or man-made features that
can act as preferential pathways for groundwater and contaminant
migration. See 40 CFR 257.91(a)(2). The significance of ADEM's failure
to address this deficiency is illustrated by the numerous and
documented SSIs and SSLs detected in the monitoring wells which are
screened within the coal layers.
In summary EPA is proposing to determine that the groundwater
monitoring network ADEM approved for the Ash Pond at Plant Gorgas falls
far short of the performance standards in Sec. 257.91(a) and (b). The
uppermost aquifer has not been sufficiently characterized or monitored.
In particular, the lower limits of the uppermost aquifer and
hydraulically connected aquifers beneath it have not been defined.
Compliance monitoring wells have not been located at the waste boundary
in most locations. There are an insufficient number of monitoring wells
along the perimeter of the downgradient waste boundary, and at
insufficient depths, to monitor all potential contaminant pathways in
the entire uppermost aquifer, given the potential for radial flow in
deeper aquifer zones. Finally, numerous preferential pathways have not
been monitored.
ADEM's permit does include a permit condition that states:
The Permittee shall install and maintain additional groundwater
monitoring wells as necessary to assess changes in the rate and
extent of any plume of contamination or as otherwise deemed
necessary to maintain compliance with [ADEM Admin. Code] 335-13-15-.
06. A plan in the form of a permit modification request should be
submitted to the Department as required by Section V.D.
However, this condition does not actually require any action that will
bring the groundwater monitoring system into compliance; for example,
by requiring the facility to fully characterize the uppermost aquifer
system or install additional monitoring wells at the waste boundary.
Or, more broadly, it does nothing to compel the facility to meet the
requirements in 40 CFR 257.91(a) and (b).
c. Plant Gorgas Corrective Action Issues
In November 2018, the first SSLs above a groundwater protection
standard were detected at the Gorgas Plant. SSLs were reported for
lithium, arsenic, and molybdenum. The Ash Pond reported SSLs of all
three constituents; the Gypsum Pond, CCR Landfill, and Gypsum Landfills
reported SSLs of lithium only; and the Bottom Ash Landfill reported
SSLs of arsenic. One ACM was developed for all the units at the
facility in June 2019 and revised in February 2020 (``revised
ACM'').\96\ On February 28, 2022, ADEM issued a Final Permit to Alabama
Power for Plant Gorgas Ash Pond, Gypsum Pond, and Bottom Ash Landfill.
---------------------------------------------------------------------------
\96\ Anchor QEA. Assessment of Corrective Measures, Plant
Gorgas. Prepared for Alabama Power Company. June 2019 (Revised:
February 2020).
---------------------------------------------------------------------------
In the RTC for the Gorgas Final Permit,\97\ ADEM states:
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\97\ Alabama Department of Environmental Management. Initial
Permit and Variance, William C. Gorgas Electric Generating Plant,
Permit No. 64-12, Public Commenters. February 28, 2022.
In November of 2019, the Department provided extensive comments to
Alabama Power related to the submitted ACM and proposed final
remedy. The Department's comments addressed many of the concerns
raised by commenters, including the selection of monitored natural
attenuation (MNA) as the final remedy despite providing limited data
to its efficiency as a remedy. To date, Alabama Power has not
submitted a revised ACM, as the facility has been collecting
---------------------------------------------------------------------------
additional data to support a final remedy proposal.
It appears the permit record (Final Permit and RTC) may not reflect
all the relevant information about the status of corrective actions at
Plant Gorgas that was available to ADEM when the permit was issued.
According to Alabama Power ``[a] Groundwater Remedy Selection Report
was prepared and submitted on December 17, 2021, to meet the
requirements of 40 CFR 257.97, ADEM Admin. Code r. 335-13-15-.06(8),
and Part C of ADEM Administrative Order AO 18-096-GW . . .''.\98\ The
remedy the facility selected for the Ash Pond, Gypsum Pond, and Bottom
Ash Landfill consists of closure with waste in place and capping,
permeation grouting at the Ash Pond, and MNA. Additionally, any
comments that may have been provided by ADEM to Alabama Power on the
2020 ACM were not available for review.
---------------------------------------------------------------------------
\98\ Southern Company Services 2022 Annual Groundwater
Monitoring and Corrective Action Report, Alabama Power Company Plant
Gorgas Ash Pond. Prepared for Alabama Power Company. February 1,
2023. p 2.
---------------------------------------------------------------------------
The Plant Gorgas Final Permit contained the same recitation of the
corrective action regulations as the other permits issued by ADEM. As
with the others, incorporating the regulations verbatim in the permit
does not require Alabama Power to achieve compliance with those
requirements at Plant Gorgas. Here as well, it appears that ADEM did
not take into account relevant facts about the status of corrective
action at Plant Gorgas, such as whether the 2020 revised ACM or the
selected remedy submitted to ADEM in December 2021 complied with the
regulatory requirements. Most importantly, ADEM did not determine what
actions are still necessary in light of those facts to achieve
compliance with the regulations and include those actions as
requirements in the Final Permit. Instead, two months later, ADEM
issued a Final Permit that was silent on the adequacy of the revised
ACM and the applicant's selected remedy. Over a year later, it does not
appear that ADEM has evaluated the adequacy of the revised ACM and the
applicant's selected remedy. As a consequence, EPA is proposing to
determine that, by remaining silent, the permit in essence authorized
Alabama Power to continue to pursue a remedy based on the results of an
ACM that does not meet the requirements of Sec. 257.96, even though
the selected remedy does not appear to meet the requirements in Sec.
257.97(b), and the ACM identified other measures that would meet those
requirements.
Delaying a decision on the adequacy of the facility's selected
remedy until some unspecified point after permit issuance \99\
effectively allows Alabama Power to continue operating out of
compliance with the regulations, while operating in compliance with the
permit. Releases continue to migrate off-site during this delay, and in
this case, it appears the contamination may have already migrated off-
site to residential
[[Page 55268]]
property.100 101 The sanctioned delay in implementing an
effective remedy with no schedule for compliance results in a permit
program that is less protective than the Federal regulations.
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\99\ It appears that ADEM has still not evaluated either the
revised 2020 ACM or Alabama Power's selected remedy.
\100\ Alabama Power. Letter to Mr. Taylor. Alabama Power Plant
Gorgas Ash Pond Closure and Groundwater Investigations. July 6,
2020.
\101\ Alabama Power. Letter to Mrs. Salter. Alabama Power Plant
Gorgas Ash Pond Closure and Groundwater Investigations. October 30,
2020.
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EPA is proposing to determine that the Final Permit contains many
of the same issues discussed with respect to the other permits. The
Final Permit does not contain a deadline for correction and resubmittal
of the ACM to address any of the deficiencies ADEM identified in its
2019 comments, or any response to Alabama Power's selected remedy. EPA
has also identified deficiencies in the revised ACM beyond those ADEM
discussed in the RTC.
i. The Plant Gorgas Final Permit Does Not Require Collection of Site
Data Needed To Support Assessments in the ACM
As discussed previously, Sec. 257.95(g)(1) requires a facility to
characterize the nature and extent of the release and any relevant site
conditions that may affect the remedy ultimately selected. The
characterization must be sufficient to support a complete and accurate
assessment of the corrective measures necessary to effectively clean up
all releases from the CCR unit pursuant to Sec. 257.96.
The revised ACM identified MNA as a corrective measure to address
groundwater contamination, in addition to other corrective measures
(e.g., hydraulic control and treatment; in-situ treatment). The revised
ACM delineates releases of lithium, arsenic, and molybdenum but does
not characterize the site conditions that would affect Alabama Power's
selected remedy of MNA. Although the ACM identifies a number of
potential attenuation mechanisms that might be effective for arsenic,
lithium, and molybdenum, the ACM does not demonstrate that any of these
mechanisms occur on site. EPA was unable to locate any data confirming
that any of those potential attenuation mechanisms are occurring at
Plant Gorgas. For example, this could include testing for the presence
and quantity of lithium detected in the aquifer matrix solids to
demonstrate that the constituent is being removed from the groundwater
and immobilized on-site. But no site data were discussed in the ACM.
The subsequent Remedy Selection Report also fails to contain the
necessary site data. Although the Report, like the ACM, identifies a
number of potential attenuation mechanisms that might be occurring on-
site for arsenic, lithium, and molybdenum, the Report does not conclude
that any of these mechanisms occur on-site. Some site data that were
not available in the ACM are discussed in Section 5.3 of the Remedy
Selection Report, but they do not demonstrate that any significant
amount of lithium, molybdenum, or arsenic is being immobilized in the
``solids'' samples,\102\ (e.g., aquifer matrix) or otherwise confirm
the presence of attenuated constituents in the aquatic matrix. The
Report identifies only dispersion and dilution as an MNA mechanism that
currently occurs at Plant Gorgas. Ultimately none of the data presented
support selection of MNA as a primary remedy.
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\102\ Anchor QEA. Prepared for Alabama Power Company. Plant
Gorgas Groundwater Remedy Selection Report. December 2021. Tables 6
and 12 in Appendix D.
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Site data would also be needed to support any assessment of the
performance, reliability, ease of implementation, and the time required
to begin and complete the remedy must also be assessed and supported
with site characterization data and analysis. 40 CFR 257.96(c)(1) and
(2). But the Final Permit issued by ADEM requires neither the
collection of data, or any revisions to the ACM, or any change in the
facility's selected remedy to address these deficiencies.
ii. The Final Permit Does Not Require Submission of a Revised ACM That
Accurately Assesses MNA
In the revised ACM, Alabama Power acknowledges that, ``USEPA (2015)
discourages using dilution and dispersion as primary MNA mechanisms, as
these mechanisms disperse contaminant mass rather than immobilize it.''
\103\ ADEM also raised this as a concern in its 2019 comments on the
original ACM.\104\ However, as noted neither the revised ACM or the
Remedy Selection Report identifies any natural attenuation mechanisms
other than dilution and dispersion that have been demonstrated to be
occurring on-site: ``The performance of MNA requires further
investigation, especially related to the identification of an
attenuating mechanisms, capacity of the Pottsville Formation for
attenuation, and time to achieve GWPS.'' \105\ This investigation was
not completed prior to completion of the ACM. Regardless, Alabama Power
assessed the performance of MNA as ``medium'' based on the dilution and
dispersion (i.e., releases of contaminants) occurring on-site and the
identification of potential attenuation mechanisms.
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\103\ Anchor QEA. Assessment of Corrective Measures, Plant
Gorgas. Prepared for Alabama Power Company. June 2019 (Revised:
February 2020). p. 14.
\104\ Alabama Department of Environmental Management. Response
to CCR Documents Submitted to the Department. Alabama Power Company.
November 14, 2019.
\105\ Anchor QEA. Assessment of Corrective Measures, Plant
Gorgas. Prepared for Alabama Power Company. June 2019 (Revised:
February 2020). p. 17.
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Such a favorable assessment of MNA is contrary to the requirement
in Sec. 257.97(b)(4) that ``[r]emedies must . . . [r]emove from the
environment as much of the contaminated material that was released from
the CCR unit as is feasible.'' As previously discussed, while MNA can
reduce the concentration or mobility of inorganic contaminants in
groundwater if immobilization occurs through adsorption or absorption
to subsurface soils, it does not remove the contaminants from the
environment. MNA, therefore, would not perform well with respect to the
requirement in 40 CFR 257.97(b)(4). This is particularly true in this
circumstance, where Alabama Power has failed to collect the site data
needed to identify whether any naturally occurring attenuation may be
occurring on-site, as well as the mechanism by which it occurs, and to
assess whether site characteristics that control and sustain this
naturally occurring attenuation are sufficient to immobilize the entire
release. Because the revised ACM presents no information that MNA would
meet these requirements, the ACM should have assessed MNA's performance
and reliability as ``low.''
Similarly, in order for MNA through immobilization to be assessed
favorably with respect to its reliability at meeting the other
requirements in Sec. 257.97(b), such as the requirement in Sec.
257.97(b)(2) to attain groundwater protection standards, the chemical
reactions and processes involved that achieve immobilization must be
demonstrated to be present on site and be permanent. Immobilization
that is not permanent could be reversed, causing contaminants to be
released back into groundwater and to migrate off-site. Yet despite the
absence of any data demonstrating immobilization mechanisms to be
present, let alone permanent, the revised ACM assessed the reliability
of MNA through immobilization as ``high.'' This conclusion is
unsupported; since no immobilization mechanisms were
[[Page 55269]]
demonstrated to be present, they could not be known to be reliable.
The revised ACM also fails to consider safety impacts, cross-media
impacts, and control of exposure to any residual contamination in its
assessment of MNA. See 40 CFR 257.96(c)(3). Neither the narrative nor
Table 5 in the 2020 ACM discuss these impacts for MNA. Yet Table 5 in
the 2020 ACM, in the column labeled ``potential impacts of remedy''
nevertheless concludes that the potential impacts from MNA are
``none.'' This conclusion is unsupported by data or analysis. This
conclusion is also inconsistent with other information in the revised
ACM. The Ash Pond and Bottom Ash Landfill are both adjacent to a river.
In the revised ACM in Figure 3, groundwater flow is depicted from the
Ash Pond toward the river. The Bottom Ash Landfill is also near and
upgradient from an adjacent river. As noted, the only MNA that is known
to occur at the site is dilution and dispersion (i.e., the normal
transport associated with groundwater releases.) This means that
contaminants are migrating in groundwater from the Ash Pond to the
river. Migration of contamination from groundwater to surface water is
a cross-media impact. Therefore, the assessment of potential impacts
from the remedy for MNA in Table 5, which includes these cross-media
impacts, should be ``high.''
Conclusions without a supporting assessment or data do not
constitute ``an analysis of the effectiveness of potential control
measures.'' 40 CFR 257.96(c) (emphasis added). In addition, the lack of
data to support the assessments in the revised ACM means it may not
accurately reflect MNA's ``effectiveness in meeting all of the
requirements and objectives'' in Sec. 257.97(b). Inaccurate
assessments in an ACM can ultimately result in selection of a remedy
that will not meet the requirements of Sec. 257.97(b), which is what
appears to be occurring here.
In an ACM, technologies' expected performances are compared with
one another according to how well each alternative meets each
regulatory criterion. The Revised ACM identified MNA as one of several
potential corrective measures to address groundwater contamination
(i.e., hydraulic control and treatment; in-situ treatment). Given both
the absence of any evidence of any attenuation mechanisms occurring at
the Ash Pond, and the conclusion in the revised ACM that the other
alternatives, such as pump and treat, are feasible, there would appear
to be no basis for assessing MNA more favorably than an alternative
that unquestionably removes contaminants from the environment. For the
same reasons, there is no apparent basis for ultimately selecting MNA
as the remedy.
ADEM's Final Permit contains no measures to remedy this, even
though in their 2019 comments on the original ACM, ADEM raised many of
the same issues discussed above. For example, ADEM requested that
Alabama Power update the ACMs to include detailed information for each
requirement. In particular, the comments noted that:
Furthermore, ADEM Admin. Code r. 335-13-15-.06(8)(b)3. and (b)4.
require that the remedy must (1)'' control the source(s) of releases
so as to reduce or eliminate, to the maximum extent feasible,
further releases of constituents in Appendix IV into the
environment'' and (2) '' remove from the environment as much of the
contaminated material that was released from the CCR unit as
feasible . . .''.The ACMs evaluate a number of options, with source
control (by consolidating and capping the CCR units) and monitored
natural attenuation (MNA) proposed as the most effective remedy. The
Department requests a more detailed justification for the proposed
remedies given that source control will not be achieved for an
average of 10 years and that no other mechanism is proposed to
reduce the potential for further releases to the'' maximum extent
feasible'.
EPA was unable to find any evidence that a revised ACM or a more
detailed justification was submitted in response to ADEM's concerns. By
failing to require Alabama Power to take any concrete action to address
these deficiencies, the Final Permit effectively authorizes the
permittee to continue to indefinitely pursue a remedy that ADEM
previously determined had not been demonstrated to meet the
requirements in Sec. 257.97(b). Accordingly, EPA is proposing to
determine that the permit does not require Alabama Power to achieve
compliance with the Federal requirements; and because it allows the
facility to continue to delay implementing a remedy that would meet the
requirements of Sec. 257.97, the alternate State requirement is less
protective.
4. Plant Greene County
EPA reviewed the Final Determination Initial Permit and Variance
for the Alabama Power Company, Greene County Electric Generating Plant
(Plant Greene County Permit), issued by ADEM under Permit No. 32-03 on
December 18, 2020.\106\ The permit summary on Page 1 says,
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\106\ Alabama Department of Environmental Management. Final
Determination Initial Permit and Variance for the Alabama Power
Company, Greene County Electric Generating Plant, issued under
Permit No. 32-03. December 18, 2020.
[t]he Plant Greene County Ash Pond is a CCR surface impoundment
located in Sections 21 and 28, Township 19 North, Range 3 East in
Greene County, Alabama consisting of approximately 559.41 acres with
a disposal area that consists of approximately 477.24 acres. The
permit requires the Permittee to manage CCR in accordance with the
conditions of the permit, ADEM Admin. Code r. 335-13-15, ''
Standards for the Disposal of Coal Combustion Residuals in Landfills
and Surface Impoundments,'' and the approved permit application.
. . .
The Permittee must comply with all conditions of the permit except
to the extent and for the duration such noncompliance is authorized
by a variance granted by ADEM. The first variance requests to
exclude boron as an Appendix IV assessment monitoring constituent.
The second variance requests groundwater protection standards of 6
micrograms per liter ([micro]g/L) for cobalt; 15 [micro]g/L for
lead; 40 [micro]g/L for lithium; and 100 [micro]g/L for molybdenum.
The third variance requests the final grade of the cover system be
less than 5 percent and greater than 25 percent. The fourth variance
being requested is from 335-13-15-.03(6) requiring a 100 foot buffer
from the perimeter of the facility boundary.
As with the other permits evaluated in this proposal, EPA has
identified issues with ADEM's approval of the closure, groundwater
monitoring network, and corrective action at Plant Greene County, which
are discussed below. As previously discussed, EPA focused on only a
subset of the potential issues associated with the permit and limited
its review to information in the permit record (e.g., the Permit
Application) and information publicly available on Alabama Power's CCR
website. This is because the purpose of this review is to determine
whether Alabama's program meets the statutory standard for approval,
not to reach final conclusions about an individual facility's
compliance with the CCR regulations.
a. Plant Greene County Closure Issues
Plant Greene County had not completed closure of the Ash Pond when
ADEM issued the Final Permit in December 2020. But the final permit
ADEM issued looks largely the same as the permits issued to the other
facilities. ADEM incorporated the Alabama CCR regulations by reference
into the Final Permit for Plant Greene County, and it approved and
incorporated the Closure Plan submitted as part of the application into
the Final Permit without modification.\107\ The Final Permit provides:
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\107\ Although the Permit terms are ambiguous, it appears from
the Response to Public Comment that ADEM approved the Closure Plan
submitted as part of the Permit Application.
[[Page 55270]]
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SECTION VII. CLOSURE AND POST-CLOSURE REQUIREMENTS.
A. Closure Timeframe and Notifications. The Permittee shall close
their CCR units as specified in 335-13-15-07(2), this permit and the
Application.
B. Criteria for Closure.
1. Cover. Closure of a CCR landfill, surface impoundment, or any
lateral expansion of a CCR unit must be completed by either leaving
the CCR in place and installing a final cover system or through
removal of the CCR and decontamination of the CCR unit, as described
in 335-13-15-.07(3)(b) through (j). The minimum and maximum final
grade of the final cover system may be less than 5 percent and
greater than 25 percent, as specified in the Permit Application.
(See Section IX.C.)
2. Written Closure Plan. The written closure plan, as part of the
Application, must include, at a minimum, the information specified
in 335-13-15-.07(3)(b)1.(i) through (vi).
3. Initiation of Closure Activities. Except as provided for in 335-
13-15-.07(3)(e)4 and 335-13-15-.07(4), the owner or operator of a
CCR unit must commence closure of the CCR unit no later than the
applicable timeframes specified in either 335-13-15-.07(3)(e)l or 2.
4. Completion of closure activities. Except as provided for in 335-
13-15-.07(3)(f)2, the owner or operator must complete closure of the
CCR unit subject to the requirements in 335-13-15-.07(3)(f)l.(i)
through (ii).
According to the Closure Plan submitted with the Permit
Application, Alabama Power intends to remove CCR from the southern
portion of the Ash Pond and consolidate it within the northern portion
of the existing ash pond.\108\ After the excavation and consolidation
have been completed, the footprint of the remaining waste will occupy
approximately 221 acres. The Plan calls for the 221 acres of
consolidated waste to be closed in place, with a final cover system
consisting of an engineered synthetic turf and geomembrane to be
installed on the consolidated unit. In addition, according to the Plan,
a barrier wall keyed into the low permeability Demopolis Chalk will be
installed around the perimeter of the consolidated CCR material to
create a hydraulic barrier that ``limits the movement of interstitial
water through the constructed interior dike and existing northern
dike.'' \109\ This hydraulic barrier will be connected to the
geomembrane of the final cover system.\110\ According to the Closure
Plan:
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\108\ Alabama Power Company. Revised Closure Permit Application
for the Plant Greene County Ash Pond. April 30, 2020. Appendix 9, p
3, 18-19.
\109\ Id. p.16.
\110\ Additional details regarding the barrier wall system are
provided in the Permit Application in Appendix 6 and Appendix 7,
entitled ``Draft--Construction Quality Assurance Plan.'' Although
the drawings are marked with statements such as ``60 Percent Design
Package'' or ``Issued for 60% Client Review,'' and the Construction
Quality Assurance Plan is marked ``Draft,'' it appears that ADEM
approved these materials with the permit condition directing the
Permittee to close their CCR units ``as specified in the
Application.''
These actions will effectively control the source of CCR
constituents to groundwater by removing free water and some
interstitial water from the ash, reducing the footprint area of the
ash and preventing further infiltration of surface water resulting
from rainfall through the ash. Removal of the free liquid will
reduce the volume of water available to flow from the Ash Pond
during and after closure, while also minimizing the hydraulic head
driving water through the subsurface.\111\
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\111\ Alabama Power Company. Revised Closure Permit Application
for the Plant Greene County Ash Pond. April 30, 2020. Appendix 9, p
19.
In many respects, the outlines of the closure presented in the Plan
could be implemented to be consistent with the Federal requirements;
however, ADEM approved the Plan without requiring Alabama Power to
provide the information necessary to confirm that several critical
closure requirements--which were not addressed or were insufficiently
described--would be met. Specifically, neither the Closure Plan nor
other materials in the Permit Application addressed how the performance
standards in Sec. 257.102(d)(2) will be met with respect to the
saturated CCR that it appears will remain in the base of the
consolidated unit. The Permit could either have specified what the
facility needs to do to meet the requirements, or ADEM could have
required the facility to submit a revised Closure Plan. ADEM did
neither, and as a consequence, there is no binding and enforceable
provision for the facility to comply with these performance standards.
In essence, ADEM has issued a permit that allows the facility to decide
whether to comply with Sec. 257.102(b) and (d)(2), rather than
``requiring each CCR unit to achieve compliance with'' those
provisions. 42 U.S.C. 6945(d)(1).
While it was in operation, the base of the Ash Pond was in
continuous contact with the groundwater beneath the unit. Even now
groundwater continues to saturate the CCR in the unit.\112\ EPA
estimated the amount of saturated CCR remaining in the Ash Pond using
the same methodologies described above for Plants Colbert and Gadsden.
The average groundwater elevation from groundwater monitoring wells in
the vicinity of the Ash Pond between September 2019 and August 2021 is
84.8 ft above MSL. While the base elevation for the unit varies, by
relying on an average base elevation of 83 feet, EPA estimates that, on
average, just under 2 feet in depth of CCR across the entire footprint
of the impoundment is currently in contact with groundwater. This
equates to roughly 640,000 CY of saturated waste. Dewatering and pool
drawdown continue at the site, and when combined with the installation
of the slurry wall, groundwater elevations would be expected to
decrease over time. However, the extent to which the CCR will remain
saturated once closure activities are completed cannot be estimated due
to the lack of information in the relevant documents.
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\112\ Alabama Power Company. Revised Closure Permit Application
for the Plant Greene County Ash Pond. April 30, 2020. GWMP pp 220-
221.
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As discussed previously, the Federal regulations applicable to
surface impoundments closing with waste in place require that ``[f]ree
liquids must be eliminated by removing liquid wastes or solidifying the
remaining waste and waste residues, [and that] remaining wastes must be
stabilized sufficient to support final cover system.'' 40 CFR
257.102(d)(2). But due to the deficiencies in the Closure Plan, it is
not clear that the closure approved by ADEM will meet either standard.
According to the approved Closure Plan, various dewatering
techniques will be employed before and during closure; however, the
Closure Plan appears to limit the use of these techniques to the CCR in
the southern portion of the unit that will be excavated and transported
to the consolidated area, and to the areas under the new dike.\113\ For
example, in the sections specifically discussing dewatering, the
Closure Plan states:
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\113\ Alabama Power Company. Revised Closure Permit Application
for the Plant Greene County Ash Pond. April 30, 2020. Appendix 9, pp
5,7, and 9.
i. Dewatering
Dewatering of the CCR Ponds consists of two phases: decanting of
free water and dewatering of interstitial water within the CCR
material. Dewatering will be required prior to ash excavation and
throughout construction. . . .
Interstitial dewatering refers to the removal of subsurface water
within the saturated CCR material. This dewatering requires lowering
phreatic water levels to improve material handling for excavation
and transport. Removal of interstitial water will likely require
both passive and active methods of drainage.
* * * * *
The CCR material within the subgrade of the proposed interior dike
will be over excavated and a stable, temporary slope formed to the
interior to allow the dike and barrier wall to be constructed.
During this time, the subgrade beneath the new dike will be
dewatered (discussed in a following section).
* * * * *
[[Page 55271]]
As dewatering continues, CCR material will be excavated from the
closure by removal areas and placed and compacted in horizontal
lifts on top of the existing CCR material within the consolidation
area.
As discussed previously, the CCR material will be dewatered in a
systematic fashion prior to and during excavation activities, to
maintain the phreatic surface below the working elevation of removal
operations. For construction of the closed ash pond, it is expected
that the CCR material will be handled multiple times prior to final
placement and closure of the pond. CCR material will be stacked and
dewatered to the proper moisture content prior to placement in the
consolidation area.
(emphasis added).\114\ The Closure Plan lacks the required description
of how--or even whether--Alabama Power intends to dewater the entire
unit. For example, there are inconsistent statements in the Closure
Plan about the scope of the dewatering activities Alabama Power intends
to conduct. In one section, there is a reference to ``dewatering of
wetter ash across the site, especially in the southern end of the
pond.'' But the remainder of the discussion focuses on a technique that
is unlikely to be used on CCR that is not intended to be excavated and
transferred, which suggests that Alabama Power does not intend to fully
dewater all of the CCR in the unit. Specifically, the Closure Plan
states that:
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\114\ Alabama Power Company. Revised Closure Permit Application
for the Plant Greene County Ash Pond. April 30, 2020. Appendix 9, pp
7-8.
Utilization of stacking & casting methods is anticipated. With this
approach, ash with higher moister[sic] content will be excavated and
stacked in piles to allow for gravity drainage. A similar technique
of windrowing may be used throughout the site. This technique
involves spreading the wet ash in thin lifts and rowing/tilling the
ash to allow the moisture to evaporate from the surface.
To expedite interstitial water dewatering and construction
stormwater management, a capillary break drainage system may also be
considered for the ash excavation/placement around the interior
dike. The drainage system will help relieve pore water pressure in
the underlying ash as the weight of earthwork filling is applied.
This is compounded by the Closure Plan's repeated references to the
removal of ``free water,'' rather than the ``free liquids'' the Federal
regulations specify must be eliminated.\115\ For example, on pages 18-
19, under the heading ``f. Achievement of Closure Performance
Standards,'' the Closure Plan states:
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\115\ Alabama Power Company. Revised Closure Permit Application
for the Plant Greene County Ash Pond. April 30, 2020. Appendix 9, pp
5, 7-8, 19.
Free water will be removed, and interstitial water will be lowered
to accomplish the CCR removal from the closure by removal areas and
to close in a consolidated footprint.
* * * * *
These actions will effectively control the source of CCR
constituents to groundwater by removing free water and some
interstitial water from the ash, reducing the footprint area of the
ash and preventing further infiltration of surface water resulting
from rainfall through the ash.
(emphasis added). Alabama Power has defined the term ``free water'' in
other Closure Plans as ``water contained in the CCR unit above the
surface of CCR material.'' \116\ Compare, 40 CFR 257.53 (definition of
``free liquids'').
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\116\ See, e.g., Alabama Power Company. Revised Closure Plan for
the Plant Gorgas Ash Pond. Appendix 11, p 7.
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Moreover, the Closure Plan never refers to the groundwater within
the northern portion of the unit or describes any engineering measures
that will be implemented to remove these liquids. Based on the
information provided, further engineering measures would be necessary
to effectively eliminate these free liquids from the unit prior to
installing the final cover system, required by Sec. 257.102(d)(2)(i).
Absent further data demonstrating that saturated CCR will not be
present in the base of the closed unit prior to the installation of the
final cover system, the permit record does not support a finding that
the remaining wastes will be stabilized sufficiently to support the
final cover system, as required by Sec. 257.102(d)(2)(ii). If the CCR
in the unit is not sufficiently stabilized, e.g., if it has not been
completely drained prior to the installation of the final cover system,
differential settlement of the CCR after installation of the cover
system is possible, especially given the substantial added load from
the consolidation of CCR from the southern portion of the Ash Pond. If
the settlement is great enough it could cause a disruption in the
continuity, and potentially failure, of the final cover system.
Additional information is needed to determine that the permit meets
Federal requirements. This could have been accomplished either by
requiring submission of the information prior to the issuance of the
permit or by including a permit term requiring submission of the
information, along with a clause allowing for further permit conditions
if necessary.
Based on all of the above, EPA is proposing to determine that, by
failing to resolve these issues, ADEM's permit does not require the
Plant Greene County Ash Pond to achieve compliance with the Federal
requirements for closure, or with alternative closure requirements that
are at least as protective as the Federal requirements.
b. Plant Greene County Groundwater Monitoring Issues
Based on EPA's review of the approved groundwater monitoring well
network, EPA is proposing to determine that ADEM approved a groundwater
monitoring system that fails to meet the Federal requirements. As
previously discussed, the Federal regulations specify that a
groundwater monitoring system must be installed that ``consists of a
sufficient number of wells, installed at appropriate locations and
depths, to yield groundwater samples from the uppermost aquifer that
accurately represents the quality of the groundwater passing the waste
boundary of the CCR unit.'' 40 CFR 257.91(a)(2). The regulations
further specify that ``[a]ll potential contaminant pathways must be
monitored.'' Id. But as discussed in more detail below, EPA is
proposing to determine that ADEM approved a groundwater monitoring plan
with an insufficient number of wells laterally along the perimeter of
the unit to monitor all contaminant pathways. EPA is also proposing to
determine that monitoring wells in the approved plan were not installed
at appropriate depths to ensure that all contaminant pathways in the
entire uppermost aquifer were monitored. These are essentially the same
issues previously discussed with respect to Plants Gadsden and Gorgas.
i. Insufficient Number of Downgradient Compliance Wells Installed at
Appropriate Depths To Monitor the Entire Aquifer (Inadequate Vertical
Spacing)
The downgradient well network approved by ADEM was focused
primarily on a narrow subset of the uppermost geologic layers within
what is referred to in the Permit Application as Unit 2: Poorly Graded
Sands With Gravel Lenses. Other interconnected portions of the
uppermost aquifer are not being monitored as discussed below. When
evaluating whether monitoring wells are installed at appropriate depths
(i.e., the adequacy of vertical monitoring well coverage), it is
important to look at cross-sectional views of the entire uppermost
aquifer in the vertical dimension to understand interrelationships of
groundwater monitoring wells, screen depths, and lithological
variations. These points are illustrated (in part) in the geologic
cross-sections on Figures 5A and 5B included on pages 208 and 209 of
the Permit Application, which show that the uppermost aquifer consists
of layers of
[[Page 55272]]
poorly graded sands with gravel lenses (identified as Unit 2), as well
layers of lean clay to sandy clay (identified as Unit 1). These cross
sections and the boring logs that were included in the Permit
Application confirm that the two geologic formations are hydraulically
interconnected and both are therefore the ``uppermost aquifer.'' See,
40 CFR 257.53 (defining uppermost aquifer to include lower
hydraulically connected aquifers). Accordingly, monitoring wells must
be installed in the two formations.
Nearly all of the compliance wells at the waste boundary of the
unit are screened in Unit 2, well below (in some cases over 20 feet
below) the top of the uppermost aquifer; as a consequence there are an
insufficient number of wells across nearly all of Unit 1. More
precisely, EPA found that the groundwater monitoring well network for
the Ash Pond unit has an insufficient number of wells screened in Unit
1 (i.e., a vertical data gap) along at least three sides, as follows:
(1) a 1500-foot section of Unit 1 parallel to the Barge Canal, as shown
on Figure 4A, entitled ``Geologic Cross Section A-A' Plant Greene
County Ash Pond''; (2) a 6000-foot section of Unit 1 along the western
side of the unit, as shown on Figure 4B, entitled ``Geologic Cross
Section B-B' Plant Greene County Ash Pond''; and (3) an approximately
2000-foot section of Unit 1, along the northern side of the unit
between groundwater monitoring wells GC-AP-MW-59-HO and GC-AP-MW-1 as
shown on Figure 4C, entitled ``Geologic Cross Section C-C' Plant Greene
County Ash Pond.'' These figures are found in the 2021 Plant Greene
County Annual GWMCA Report.\117\ EPA was unable to determine if a
similar gap currently exists along the southern side of the Plant
Greene County Ash Pond, because no cross-section extending along the
southern waste boundary of the unit was included in either the 2021
Plant Greene County Annual GWMCA Report or the Permit Application. The
omission of a cross-section in the Permit Application that extends
along the southern side of the Ash Pond is significant because, given
the proximity to the Black Warrior River, which is located immediately
adjacent to the south and southeast of the Ash Pond, additional
potential contaminant pathways that would need to be monitored would
normally be expected to be present.
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\117\ Alabama Power. Plant Greene 2021 Annual Groundwater
Monitoring and Corrective Action Report. January 31, 2022. Two
similar geologic cross sections are found in the Groundwater
Monitoring Plan included in the Permit Application. The two geologic
cross sections were included as Figures 4A, for A-A1, and 4B, for B-
B1; however, no geologic cross section for C--C1 was included in the
Permit Application.
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ii. Insufficient Lateral Spacing of Compliance Wells To Monitor All
Potential Contaminant Pathways
EPA is also proposing to determine that ADEM approved lateral
spacing between wells along the perimeter of the Ash Pond that is
insufficient to meet the performance standards in Sec. 257.91(b).
Monitoring wells used for the detection and assessment monitoring
program are spaced approximately one thousand feet apart with few
exceptions. Large lateral well spacings are particularly problematic to
the east, south and west of the waste boundary of the unit where
groundwater is expected to discharge to surface water. Given the
proximity to the various surface water features, such as the Black
Warrior River and the Barge Canal, the large well spacings make it
likely that potential contaminant pathways from groundwater discharging
to surface water located immediately adjacent to the Ash Pond are not
being monitored. This groundwater to surface water pathway was
acknowledged in the Permit Application with a statement that reads, as
follows: ``Groundwater that migrates downward into the surficial
aquifer will migrate vertically through the Unit 1 clay and then,
primarily laterally (horizontal) and to a lesser extent vertically
along more coarse fractions of the Unit 2 aquifer toward the Black
Warrior River and barge canal.'' \118\
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\118\ Alabama Power Company. Revised Closure Permit Application
for the Plant Greene County Ash Pond. April 30, 2020. PDF pp. 192.
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Based on the concerns discussed above, EPA is proposing to
determine that by approving the deficient downgradient groundwater
monitoring well network in the Permit Application, ADEM's final permit
does not require Alabama Power to achieve compliance with the
performance standards in Sec. 257.91(a)(2), or with an equally
protective alternative.
c. Plant Greene County Corrective Action Issues
In November 2018, SSLs above the groundwater protection standards at
Plant Greene County were reported for arsenic and lithium. An ACM was
prepared in June 2019 (``2019 ACM''). On December 18, 2020, ADEM issued
a final permit to Alabama Power for the Plant Greene County Ash Pond.
In the RTC for the Final Permit, ADEM states:
In November of 2019, the Department provided extensive comments to
Alabama Power related to the submitted ACM and proposed final
remedy. The Department's comments addressed many of the concerns
raised by commenters, including the selection of monitored natural
attenuation (MNA) as the final remedy despite providing limited data
to its efficiency as a remedy. To date, Alabama Power has not
submitted a revised ACM, as the facility has been collecting
additional data to support a final remedy proposal.
The Plant Greene County Final Permit only contained a recitation of
the corrective action regulations, but did not require Alabama Power to
achieve compliance with those requirements. This is because the Final
Permit does not require Alabama Power to take specific actions to
correct the deficiencies in the 2019 ACM, even though, as discussed in
its RTC on the permit, ADEM identified them a year before issuing the
Final Permit. Significantly, ADEM did not determine what actions are
still necessary in light of those facts for Alabama Power to achieve
compliance with the regulations and include those actions as
requirements in the Final Permit. For example, the Final Permit does
not require the permittee to take any particular actions to address
ADEM's comments on the 2019 ACM or with respect to Alabama Power's
proposed remedy, such as specifying the additional data needed to
support the permittee's preferred remedy under a set timetable. As a
consequence, EPA is proposing to determine that the permit authorized
Alabama Power to continue to indefinitely pursue a remedy that appears
not to meet the requirements of Sec. 257.97(b), and that is based on
the results of an ACM that does not meet the requirements of Sec.
257.96.
Whether the 2019 ACM meets the requirements of the regulations, and
what actions Alabama Power must take to remediate groundwater in
compliance with Sec. 257.97 are precisely the types of issues that
must be determined before the permit is issued. This is because, once
the permit is issued, the requirements in the permit become the State
requirements with which the Permittee must comply. 42 U.S.C.
6945(d)(3)(A). And if the permittee is not in compliance with the
regulations, the permit must specify what the permittee is required to
do in order to achieve compliance with those regulations. This is the
role of a permitting authority (i.e., ADEM). Delaying this decision
until after permit issuance effectively allows Alabama Power to
continue operating out of compliance with the regulations, while
operating in compliance with the permit. This results in a permit
program
[[Page 55273]]
that is less protective than the Federal regulations.
As discussed below, EPA is proposing to determine that the Final
Permit fails to require Alabama Power to achieve compliance with
several of the Federal corrective action requirements.
These are many of the same deficiencies that ADEM identified in its
comments on the 2019 ACM, but declined to remedy in the permit issued a
year and a half later.\119\
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\119\ Alabama Department of Environmental Management. Response
to CCR Comments Submitted to the Department, Alabama Power Company.
November 14, 2019. pp 6-7.
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i. The Final Permit Does Not Require Collection of the Data Needed To
Support Assessments in the ACM
As discussed previously, Sec. 257.95(g)(1) requires a facility to
characterize the nature and extent of the release and any relevant site
conditions that may affect the remedy ultimately selected. The
characterization must be sufficient to support a complete and accurate
assessment of the corrective measures necessary to effectively clean up
all releases from the CCR unit pursuant to Sec. 257.96. The 2019 ACM
delineates releases of arsenic, cobalt, and lithium but does not
characterize site conditions that would affect any of the potential
remedies identified in the ACM (e.g., testing for the presence and
quantity of arsenic and lithium detected in soils to demonstrate they
are being removed from the groundwater and immobilized on-site.)
The 2019 ACM identified MNA as a potential corrective measure to
address groundwater contamination, in addition to other corrective
measures (e.g., hydraulic control and treatment; in-situ treatment).
However, Alabama Power failed to collect the site data needed to
identify whether natural attenuation may be occurring on-site, as well
as the mechanism by which it occurs, and to assess whether site
characteristics that control and sustain this naturally occurring
attenuation are sufficient to immobilize the entire release. For
example, in order to accurately assess MNA, site data are needed to
determine whether immobilization occurs on-site through adsorption or
absorption to subsurface soils. In addition, data would be needed to
determine whether the chemical reactions and processes involved that
achieve immobilization are permanent. Immobilization that is not
permanent could be reversed, causing contaminants to be released back
into groundwater and to migrate off-site.
Although the Remedy Selection Report contained some data regarding
the presence of released constituents in soils,\120\ the relative
performance, reliability, ease of implementation, and the time required
to begin and complete the remedy must also be assessed for each
alternative, including MNA. 40 CFR 257.96(c)(1) and (2). These
assessments must be supported with site characterization data and
analysis, but no data were provided in the ACM to support an assessment
of MNA against these criteria, relative to other alternatives, to
support its selection. The Remedy Selection Report discusses site data
in the context of these criteria for MNA only, with no side-by-side
assessments of alternatives based on site data provided. Additionally,
the data discussed in Section 4.3.2 of the Remedy Selection Report do
not demonstrate that any significant amount of lithium or cobalt is
being immobilized in the solids samples.\121\
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\120\ Alabama Power Company. Plant Greene County Groundwater
Remedy Selection Report, September 2021. Appendix D, Tables 6, 9 and
19.
\121\ Id at Appendix D, Tables 6 and 12.
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ii. The Final Permit Does Not Require Submission of a Revised ACM That
Accurately Assesses MNA According to the Criteria in 40 CFR 257.96(c)
No naturally occurring attenuation mechanisms other than dilution
and dispersion were identified at Plant Greene County in the ACM.
Alabama Power acknowledges in the ACM that, ``USEPA (2015) discourages
using dilution and dispersion as primary MNA mechanisms, as these
mechanisms disperse contaminant mass rather than immobilize it.'' \122\
Regardless, Alabama Power assessed the performance of MNA as ``medium''
based on the fact that the aquifer is sandy and dilution and dispersion
(i.e., releases of contaminants) are occurring.
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\122\ Alabama Power Company. Assessment of Corrective Measures
Greene County Ash Pond. June 2019, p. 12
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This favorable assessment of MNA is inconsistent with Sec.
257.97(b)(4), which specifies that ``[r]emedies must . . . remove from
the environment as much of the contaminated material that was released
from the CCR unit as is feasible.'' Neither dilution nor dispersion
removes the contaminants from the environment. Therefore, at this site
MNA would not meet this requirement, since the constituents would
remain in the environment, albeit in a different environment (i.e., the
river rather than the aquifer). Absent information to support a
conclusion that MNA can meet these requirements at this site, MNA
performance and reliability should have been assessed as ``does not
meet.''
Further, in order for MNA through immobilization to be assessed
favorably with respect to its reliability at meeting the other
requirements in Sec. 257.97(b), such as the requirement in Sec.
257.97(b)(2) to attain groundwater protection standards, the chemical
reactions and processes involved that achieve immobilization must be
demonstrated to be permanent. Immobilization that is not permanent
could be reversed, causing contaminants to be released back into
groundwater and to migrate off-site. Assessing the reliability of MNA
through immobilization as ``high'' in the ACM was not supported by
data, since no immobilization mechanisms were identified, they could
not be known to be reliable. Although Section 4.3.2 of the Remedy
Selection Report contained some data regarding the presence of released
constituents in soils, the data do not demonstrate that any significant
amount of lithium or cobalt are being immobilized in the solid
samples,\123\ and therefore these data do not actually support
selection of MNA as a primary remedy for these contaminants.\124\
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\123\ Alabama Power Company. Plant Greene County Groundwater
Remedy Selection Report, September 2021. Appendix D, Tables 6 and
12.
\124\ Some data were provided in the Remedy Selection Report to
indicate arsenic may be immobilized on-site.
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In another section of the ACM, MNA was assessed as easy to
implement because no design or construction would be required. If MNA
occurs through immobilization of constituents in the subsurface that is
not permanent, this would generally require ongoing monitoring as long
as contaminants remain in the soil--indefinitely--in accordance with
Sec. 257.98(a)(1). Since the goal of the remedy would be for
immobilized constituents to remain in the subsurface indefinitely,
monitoring would be needed to demonstrate whether this goal is
achieved. This is a much longer compliance monitoring timeframe than
any other alternative, except possibly in-situ geochemical
manipulation, which means that implementation is not significantly
easier than alternatives that can be completed sooner, such as
hydraulic control and treatment.
EPA is also proposing to determine that the ACM fails to meet the
requirements to consider safety impacts, cross-media impacts, and
control of exposure to any residual contamination in its assessment of
MNA in either the narrative or Table 6. See 40 CFR 257.96(c)(3). Table
6, in the column labeled ``potential impacts of remedy'' assesses the
potential impacts from MNA as ``none.'' This conclusion is
[[Page 55274]]
unsupported by data or analysis. This conclusion is also inconsistent
with information in the ACM. The Ash Pond is bounded on three sides by
adjacent surface water features. In the ACM in Figure 3, groundwater
flow is depicted from the Ash Pond toward surface water features.
Further, as noted Section 4.2.1 of the Groundwater Monitoring Plan,
entitled ``Groundwater Elevations and Flow,'' ``[g]roundwater
elevations in monitoring wells located adjacent or close to the barge
canal and the river appear to demonstrate a temporary reversal of flow
to the groundwater system associated with recent storm events.'' This
temporary reversal of flow indicates a connection between surface water
and groundwater in the vicinity of the Ash Pond.
Because no site data were presented to demonstrate that
immobilization of lithium or cobalt is occurring at Plant Greene, the
only MNA that is known to occur for these two constituents is dilution
and dispersion (i.e., the normal transport associated with groundwater
releases). This means that these contaminants are migrating in
groundwater from the Ash Pond to the river. Migration of contamination
from groundwater to surface water is a cross-media impact. Therefore,
the assessment of potential impacts from the remedy for MNA in Table 6,
which includes these cross-media impacts, should be ``high.''
Conclusions without a supporting assessment or data do not
constitute ``an analysis of the effectiveness of potential control
measures.'' 40 CFR 257.96(c) (emphasis added). In addition, the lack of
data means the ACM does not sufficiently establish MNA's
``effectiveness in meeting all of the requirements and objectives'' in
Sec. 257.97(b). Inaccurate assessments in an ACM can ultimately result
in selection of a remedy that will not meet the requirements of Sec.
257.97(b).
ADEM identified many of these same issues in their comments on the
2019 ACM. For example, on page 6, ADEM states:
ADEM Admin. Code r. 335-13-15-.06(8) contains substantial
requirements that must be evaluated when selecting a remedy, such as
the long- and short-term effectiveness and protectiveness of the
potential remedy, the effectiveness of the remedy in controlling the
source to reduce further releases, among many others. The ACMs
submitted by APCO do not match the level of detail required in the
regulations. Please update the ACMs to include detailed information
for each requirement of this section. Furthermore, ADEM Admin. Code
r. 335-13-15-.06(8)(b)3. and (b)4. require that the remedy must (1)
``control the source(s) of releases so as to reduce or eliminate, to
the maximum extent feasible, further releases of constituents in
Appendix IV into the environment'' and (2) ``remove from the
environment as much of the contaminated material that was released
from the CCR unit as feasible. . .''.
* * * * *
The Department requests a more detailed evaluation of the
effectiveness of MNA, or any other proposed remedy, based on site
specific conditions.
Yet ADEM's Final Permit does not require Alabama Power to take any
actions to remedy any of the deficiencies they identified.
iii. The Permit Does Not Require an Assessment of Source Control
Measures
The permit record contains no assessment of source control
measures. Section 2.5 of the 2019 ACM describes the approved closure
with waste remaining in the Ash Pond but contains no assessment of how
well the closure would control releases. Nor can that information be
found in the Remedy Selection Report, or the Closure Plan.
Moreover, the ACM neither identifies nor assesses any alternative
measures. 40 CFR 257.96 requires that various alternatives for source
control be compared in accordance with the criteria in Sec. 257.96(c).
ADEM raised similar concerns in their comments, which state:
The ACMs evaluate a number of options, with source control (by
consolidating and capping the CCR units) and monitored natural
attenuation (MNA) proposed as the most effective remedy. The
Department requests a more detailed justification for the proposed
remedies given that source control will not be achieved for an
average of 10 years and that no other mechanism is proposed to
reduce the potential for further releases to the ``maximum extent
feasible''.
Yet the permit ADEM subsequently issued does not require any actions to
remedy this deficiency.
5. EPA Conclusion About Alabama's Implementation of the CCR Regulations
Given the systemic problems noted above in ADEM's CCR permits
related to the groundwater monitoring, corrective action and closure
requirements, EPA is proposing to determine that ADEM's implementation
of its permit program is resulting in a State program that is notably
less protective than the Federal CCR regulations. First, ADEM's permits
allow closure with waste in place in unlined surface impoundments,
without requiring any, or sufficient, controls to prevent groundwater
from flowing in and out of CCR in the units indefinitely. In such
circumstances, the permit will allow ongoing contamination of
groundwater from CCR impoundments. Second, ADEM's permits do not
require Permittees to achieve compliance with the groundwater
monitoring regulations. The State-issued permits discussed in this
notice approve groundwater monitoring networks that are insufficient to
accurately determine if a unit is leaking. Finally, ADEM's permits are
inadequate related to the implementation of the corrective action
requirements because they allow facilities to delay effective responses
to contaminant releases that may pose a risk to human health and the
environment. Compounding this problem is the fact that the groundwater
monitoring networks are insufficient and that means there may be
additional unmonitored releases are occurring.
Ultimately, Alabama's CCR permit program Application would not
``require each coal combustion residuals unit located in the State to
achieve compliance with the applicable [Federal or other equally
protective State] criteria.'' 42 U.S.C. 6945(d)(1)(B). Therefore, EPA
is proposing this denial of Alabama's CCR permit program Application.
V. Proposed Action
EPA has preliminarily determined that the Alabama CCR permit
program does not meet the statutory standard for approval. Therefore,
in accordance with 42 U.S.C. 6945(d), EPA is proposing to deny the
Alabama CCR permit program.
Michael S. Regan,
Administrator.
[FR Doc. 2023-17023 Filed 8-11-23; 8:45 am]
BILLING CODE 6560-50-P