Public Health and Environmental Radiation Protection Standards for Yucca Mountain, Nevada, 61256-61289 [E8-23754]
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40 CFR Part 197
[EPA–HQ–OAR–2005–0083; FRL–8724–9]
RIN 2060–AN15
Public Health and Environmental
Radiation Protection Standards for
Yucca Mountain, Nevada
Environmental Protection
Agency (EPA).
ACTION: Final rule.
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AGENCY:
SUMMARY: We, the Environmental
Protection Agency (EPA), are
promulgating amendments to our public
health and safety standards for
radioactive material stored or disposed
of in the potential repository at Yucca
Mountain, Nevada. Congress directed us
to develop these standards and required
us to contract with the National
Academy of Sciences (NAS) to conduct
a study to provide findings and
recommendations on reasonable
standards for protection of the public
health and safety. The health and safety
standards promulgated by EPA are to be
‘‘based upon and consistent with’’ the
findings and recommendations of NAS.
Originally, these standards were
promulgated on June 13, 2001 (66 FR
32074) (the 2001 standards).
On July 9, 2004, the U.S. Court of
Appeals for the District of Columbia
Circuit vacated portions of the 2001
standards concerning the period of time
for which compliance must be
demonstrated. The Court ruled that the
compliance period of 10,000 years was
not ‘‘based upon and consistent with’’
the findings and recommendations of
the NAS and remanded those portions
of the standards to EPA for revision.
These remanded provisions are the
subject of this action.
This final rule incorporates
compliance criteria applicable at
different times for protection of
individuals and in circumstances
involving human intrusion into the
repository. Compliance will be judged
against a standard of 150 microsieverts
per year (µSv/yr) (15 millirem per year
(mrem/yr)) committed effective dose
equivalent (CEDE) at times up to 10,000
years after disposal and against a
standard of 1 millisievert per year (mSv/
yr) (100 mrem/yr) CEDE at times after
10,000 years and up to 1 million years
after disposal. This final rule also
includes several supporting provisions
affecting the projections of expected
disposal system performance prepared
by the Department of Energy (DOE).
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Effective Date: This final rule is
effective on November 14, 2008.
ADDRESSES: EPA has established a
docket for this action under Docket ID
No. EPA–HQ–OAR–2005–0083. All
documents in the docket are listed on
the https://www.regulations.gov Web
site. Although listed in the index, some
information is not publicly available,
e.g., Confidential Business Information
(CBI) or other information whose
disclosure is restricted by statute.
Certain other material, such as
copyrighted material, is not placed on
the Internet and will be publicly
available only in hard copy form.
Publicly available docket materials are
available either electronically through
https://www.regulations.gov, for
purchase or access from sources
identified in the docket (Docket Nos.
EPA–HQ–OAR–2005–0083–0086 and
EPA–HQ–OAR–2005–0083–0087), or in
hard copy at the Air and Radiation
Docket, EPA/DC, EPA Headquarters
West Building, Room 3334, 1301
Constitution Ave., NW., Washington,
DC. The Public Reading Room is open
from 8:30 a.m. to 4:30 p.m., Monday
through Friday, excluding legal
holidays. The telephone number for the
Air and Radiation Docket is (202) 566–
1742.
FOR FURTHER INFORMATION CONTACT: Ray
Clark, Office of Radiation and Indoor
Air, Radiation Protection Division
(6608J), U.S. Environmental Protection
Agency, 1200 Pennsylvania Ave., NW.,
Washington, DC 20460–0001; telephone
number: 202–343–9360; fax number:
202–343–2305; e-mail address:
clark.ray@epa.gov.
SUPPLEMENTARY INFORMATION:
DATES:
ENVIRONMENTAL PROTECTION
AGENCY
I. General Information
A. Does This Action Apply to Me?
DOE is the only entity regulated by
these standards. Our standards affect
NRC only to the extent that, under
Section 801(b) of the EnPA, 42 U.S.C.
10141 n., NRC must modify its licensing
requirements, as necessary, to make
them consistent with our final
standards. Before it may construct the
repository or accept waste at the Yucca
Mountain site and eventually close the
repository, DOE must obtain
authorization for these activities from
NRC. DOE will be subject to NRC’s
modified regulations, which NRC will
implement through its licensing
proceedings.
B. How Can I View Items in the Docket?
1. Information Files. EPA is working
with the Lied Library at the University
of Nevada-Las Vegas (https://
www.library.unlv.edu/about/
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hours.html) and the Amargosa Valley,
Nevada public library (https://
www.amargosalibrary.com) to provide
information files on this rulemaking.
These files are not legal dockets;
however, every effort will be made to
put the same material in them as in the
official public docket in Washington,
DC. The Lied Library information file is
at the Research and Information Desk,
Government Publications Section (702–
895–2200). Hours vary based upon the
academic calendar, so we suggest that
you call ahead to be certain that the
library will be open at the time you
wish to visit. The other information file
is in the Public Library at 829 East Farm
Road in Amargosa Valley, Nevada
(phone 775–372–5340). As of the date of
publication, the hours are Monday and
Thursday (9 a.m.–7 p.m.); Tuesday,
Wednesday, and Friday (9 a.m.–5 p.m.);
and Saturday (9 a.m.-1 p.m.). The
library is closed on Sunday. These
hours can change, so we suggest that
you call ahead to be certain when the
library will be open.
2. Electronic Access. An electronic
version of the public docket is available
through the Federal Docket Management
System at https://www.regulations.gov.
You may use https://
www.regulations.gov to view comments,
access the index listing of the contents
of the official public docket, and to
access those documents in the public
docket that are available electronically.
To access the docket go directly to
https://www.regulations.gov and select
‘‘Advanced Docket Search’’ under
‘‘More Search Options.’’ In the Docket
ID window, type in the docket
identification number EPA–HQ–OAR–
2005–0083 and click on ‘‘Submit.’’
Please be patient since the search could
take several minutes. This will bring
you to the ‘‘Docket Search Results’’
page. From there, you may access the
docket contents (e.g., EPA–HQ–OAR–
2005–0083–0002) by clicking on the
icon in the ‘‘Views’’ column.
C. Can I Access Information by
Telephone or Via the Internet?
Yes. You may call our toll-free
information line (800–331–9477) 24
hours per day. By calling this number,
you may listen to a brief update
describing our rulemaking activities for
Yucca Mountain, leave a message
requesting that we add your name and
address to the Yucca Mountain mailing
list, or request that an EPA staff person
return your call. In addition, we have
established an electronic listserv
through which you can receive
electronic updates of activities related to
this rulemaking. To subscribe to the
listserv, go to https://lists.epa.gov/read/
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all_forums. In the alphabetical list,
locate ‘‘yucca-updates’’ and select
‘‘subscribe’’ at the far right of the screen.
You will be asked to provide your email address and choose a password.
You also can find information and
documents relevant to this rulemaking
on the World Wide Web at https://
www.epa.gov/radiation/yucca. The
proposed rule for today’s final rule
appeared in the Federal Register on
August 22, 2005 (70 FR 49014). We also
recommend that you examine the
preamble and regulatory language for
the earlier proposed and final rules,
which appeared in the Federal Register
on August 27, 1999 (64 FR 46976) and
June 13, 2001 (66 FR 32074),
respectively.
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D. What Documents are Referenced in
This Final Rule?
We refer to a number of documents
that provide supporting information for
our Yucca Mountain standards. All
documents relied upon by EPA in
regulatory decision-making may be
found in our docket (EPA–HQ–OAR–
2005–0083). Other documents, e.g.,
statutes, regulations, and proposed
rules, are readily available from public
sources. The documents below are
referenced most frequently in today’s
final rule.
Item No. (EPA–HQ–OAR–2005–0083–
xxxx).
0076 Technical Bases for Yucca
Mountain Standards (the NAS Report),
National Research Council, National
Academy Press, 1995.
0086 DOE Final Environmental
Impact Statement, DOE/EIS–0250,
February 2002.
0383 ‘‘Geological Disposal of
Radioactive Waste,’’ International
Atomic Energy Agency Final Safety
Requirements (WS–R–4), 2006.
0417 ‘‘Radiation Protection
Recommendations as Applied to the
Disposal of Long-Lived Solid
Radioactive Waste,’’ International
Commission on Radiological Protection
Publication 81, 2000.
0408 ‘‘Regulating the Long-Term
Safety of Geological Disposal: Towards
a Common Understanding of the Main
Objectives and Bases of Safety Criteria,’’
OECD Nuclear Energy Agency, NEA–
6182, 2007.
0421 ‘‘1990 Recommendations of the
International Commission on
Radiological Protection,’’ ICRP
Publication 60.
0423 ‘‘2007 Recommendations of the
International Commission on
Radiological Protection,’’ ICRP
Publication 103.
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0431 Response to Comments
Document for Final Rule, EPA–402–R–
08–008, June 2007.
Acronyms and Abbreviations
We use many acronyms and
abbreviations in this document. These
include:
BID—background information document
CED—committed effective dose
CEDE—committed effective dose equivalent
CFR—Code of Federal Regulations
DOE—U.S. Department of Energy
EIS—Environmental Impact Statement
EnPA—Energy Policy Act of 1992
EPA—U.S. Environmental Protection Agency
FEIS—Final Environmental Impact Statement
FEPs—features, events, and processes
FR—Federal Register
GCD—greater confinement disposal
HLW—high-level radioactive waste
IAEA—International Atomic Energy Agency
ICRP—International Commission on
Radiological Protection
NAS—National Academy of Sciences
NEA—Nuclear Energy Agency
NEI—Nuclear Energy Institute
NRC—U.S. Nuclear Regulatory Commission
NRDC—Natural Resources Defense Council
NTS—Nevada Test Site
NTTAA—National Technology Transfer and
Advancement Act
NWPA—Nuclear Waste Policy Act of 1982,
as amended
NWPAA—Nuclear Waste Policy
Amendments Act of 1987
OECD—Organization for Economic
Cooperation and Development
OMB—Office of Management and Budget
RMEI—reasonably maximally exposed
individual
SSI—Swedish Radiation Protection Authority
SNF—spent nuclear fuel
TRU—transuranic
UK—United Kingdom
UMRA—Unfunded Mandates Reform Act of
1995
U.S.C.—United States Code
WIPP LWA—Waste Isolation Pilot Plant Land
Withdrawal Act of 1992
Outline of This Action
I. What Is the History of This Action?
A. Promulgation of 40 CFR Part 197 in
2001
B. Legal Challenges to 40 CFR Part 197
II. Summary of Proposed Amendments to 40
CFR Part 197 and Public Comments
A. How Did We Propose To Amend Our
2001 Standards?
B. What Factors Did We Consider in
Developing Our Proposal?
C. In Making Our Decisions, How Did We
Incorporate Public Comments on the
Proposed Rule?
D. What Public Comments Did We
Receive?
III. What Final Amendments Are We Issuing
With This Action?
A. What Dose Standards Will Apply?
1. What Is the Dose Standard Between
10,000 Years and 1 Million Years?
2. What Is the Dose Standard for 10,000
Years After Disposal?
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3. How Does Our Final Rule Protect Public
Health and Safety?
4. How Did We Consider Uncertainty and
Reasonable Expectation?
5. How Did We Consider Background
Radiation in Developing the Peak Dose
Standard?
6. How Does Our Rule Protect Future
Generations?
7. What is Geologic Stability and Why Is
it Important?
8. Why Is the Period of Geologic Stability
1 Million Years?
9. How Will NRC Judge Compliance?
10. How Will DOE Calculate the Dose?
B. How Will This Final Rule Affect DOE’s
Performance Assessments?
IV. Statutory and Executive Order Reviews
A. Executive Order 12866: Regulatory
Planning and Review
B. Paperwork Reduction Act
C. Regulatory Flexibility Act
D. Unfunded Mandates Reform Act
E. Executive Order 13132: Federalism
F. Executive Order 13175: Consultation
and Coordination With Indian Tribal
Governments
G. Executive Order 13045: Protection of
Children From Environmental Health &
Safety Risks
H. Executive Order 13211: Actions That
Significantly Affect Energy Supply,
Distribution, or Use
I. National Technology Transfer and
Advancement Act
J. Executive Order 12898: Federal Actions
To Address Environmental Justice in
Minority Populations and Low-income
Populations
K. Congressional Review Act
I. What Is the History of This Action?
Radioactive wastes result from the use
of nuclear fuel and other radioactive
materials. Today, we are revising certain
standards pertaining to spent nuclear
fuel, high-level radioactive waste, and
other radioactive waste (we refer to
these items collectively as ‘‘radioactive
materials’’ or ‘‘waste’’) that may be
stored or disposed of in the Yucca
Mountain repository. When we discuss
storage or disposal in this document in
reference to Yucca Mountain, we note
that, while Public Law 107–200
approved the site at Yucca Mountain for
the development of a repository for the
disposal of spent nuclear fuel and highlevel radioactive waste, no licensing
decision has been made regarding the
acceptability of the proposed Yucca
Mountain facility for storage or disposal
as of the date of this publication. To
save space and to avoid excessive
repetition, we will not describe Yucca
Mountain as a ‘‘potential’’ repository;
however, we intend this meaning to
apply.
Once nuclear reactions have
consumed a certain percentage of the
uranium or other fissionable material in
nuclear reactor fuel, the fuel no longer
is useful for its intended purpose. It
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then is known as ‘‘spent’’ nuclear fuel
(SNF). It is possible to recover specific
radionuclides from SNF through
‘‘reprocessing,’’ which is a process that
dissolves the SNF, thus separating the
radionuclides from one another.
Radionuclides not recovered through
reprocessing become part of the acidic
liquid wastes that the Department of
Energy (DOE) plans to convert into
various types of solid materials. Highlevel radioactive waste (HLW) is the
highly radioactive liquid or solid wastes
that result from reprocessing SNF. The
SNF that does not undergo reprocessing
prior to disposal remains inside the fuel
assembly and becomes the final waste
form for disposal in the repository.
In the United States, SNF and HLW
have been produced since the 1940s,
mainly as a result of commercial power
production and national defense
activities. Since the inception of the
nuclear age, the proper disposal of these
wastes has been the responsibility of the
Federal government. The Nuclear Waste
Policy Act of 1982, as amended (NWPA,
42 U.S.C. Chapter 108) sets forth the
framework for the disposal of SNF and
HLW. In general, DOE is responsible for
siting, constructing, and operating an
underground geologic repository for the
disposal of SNF and HLW and the
Nuclear Regulatory Commission (NRC)
is responsible for licensing the
construction and operation of this
repository, including permanent closure
and decommissioning of the surface
facilities. In making this licensing
decision for the Yucca Mountain
repository, NRC must utilize radiation
protection standards that EPA
establishes pursuant to section 801(a) of
the Energy Policy Act of 1992 (EnPA,
Pub. L. 102–486).1 Thus, today we are
promulgating amendments to our public
health protection standards at 40 CFR
part 197 (which, pursuant to EnPA
section 801(a), apply only to releases of
radioactive material stored or disposed
of at the Yucca Mountain site, rather
than generally applicable). NRC will
amend its regulations to be consistent
with these standards.
On June 3, 2008, pursuant to the
NWPA, as amended, DOE submitted a
license application to NRC seeking a
license to construct the repository. NRC
will determine whether DOE has met
NRC’s requirements, including those
implementing 40 CFR part 197, and
whether to grant or deny authorization
to construct the repository and a license
to receive radioactive material at the
Yucca Mountain site.
1 EnPA, Public Law No. 102–486, 102 Stat. 2776,
42 U.S.C. 10141 n. (1994).
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In 1985, we established generic
standards for the management, storage,
and disposal of SNF, HLW, and
transuranic (TRU) radioactive waste (see
40 CFR part 191, 50 FR 38066,
September 19, 1985), which were
intended to apply to facilities utilized
for the storage or disposal of these
wastes, including Yucca Mountain. In
1987, the U.S. Court of Appeals for the
First Circuit remanded the disposal
standards in 40 CFR part 191 (NRDC v.
EPA, 824 F.2d 1258 (1st Cir. 1987)). We
later amended and reissued those
standards to address issues that the
court raised. Also in 1987, the Nuclear
Waste Policy Amendments Act
(NWPAA, Pub. L. 100–203) amended
the NWPA by, among other actions,
selecting Yucca Mountain, Nevada, as
the only potential site that DOE should
characterize for a geologic repository for
SNF and HLW. In October 1992,
Congress enacted the EnPA and the
Waste Isolation Pilot Plant Land
Withdrawal Act (WIPP LWA, Pub. L.
102–579). These statutes changed our
obligations concerning radiation
standards for the Yucca Mountain
candidate repository. The WIPP LWA:
(1) Reinstated the 40 CFR part 191
disposal standards, except those
portions that were the specific subject of
the remand by the First Circuit;
(2) Required us to issue standards to
replace the portion of the challenged
standards remanded by the court; and
(3) Exempted the Yucca Mountain site
from the 40 CFR part 191 disposal
standards.
We issued the amended 40 CFR part 191
disposal standards, which addressed the
judicial remand, on December 20, 1993
(58 FR 66398).
The EnPA set forth our
responsibilities as they relate to Yucca
Mountain and directed us to set public
health and safety radiation standards for
Yucca Mountain. Specifically, section
801(a)(1) of the EnPA directed us to
‘‘promulgate, by rule, public health and
safety standards for the protection of the
public from releases from radioactive
materials stored or disposed of in the
repository at the Yucca Mountain site.’’
Section 801(a)(2) directed us to contract
with the National Academy of Sciences
(NAS) to conduct a study to provide us
with its findings and recommendations
on reasonable standards for protection
of public health and safety from releases
from the Yucca Mountain disposal
system. Moreover, it provided that our
standards shall be the only such
standards applicable to the Yucca
Mountain site and are to be based upon
and consistent with NAS’s findings and
recommendations. On August 1, 1995,
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NAS released its report, ‘‘Technical
Bases for Yucca Mountain Standards’’
(the NAS Report) (Docket No. EPA–HQ–
OAR–2005–0083–0076).
A. Promulgation of 40 CFR Part 197 in
2001
Pursuant to the EnPA, we developed
standards specifically applicable to
releases from radioactive material stored
or disposed of in the Yucca Mountain
repository. In doing so, we considered
the NAS Report, our generic standards
in 40 CFR part 191, and other relevant
information, precedents, and analyses.
We evaluated 40 CFR part 191
because those standards were developed
to apply to sites selected for storage and
disposal of SNF and HLW. Thus, we
believed that 40 CFR part 191 already
included the major components of
standards needed for any specific site,
such as Yucca Mountain. However, we
recognized that all the components
would not necessarily be directly
transferable to the situation at Yucca
Mountain, and that some modification
might be necessary. We also considered
that some components of the generic
standards would not be carried into sitespecific standards, since not all of the
conditions found among all potential
sites are present at Yucca Mountain. See
66 FR 32076–32078, June 13, 2001
(Docket No. EPA–HQ–OAR–2005–0083–
0042), for a more detailed discussion of
the role of 40 CFR part 191 in
developing 40 CFR part 197.
We also considered the findings and
recommendations of the NAS in
developing standards for Yucca
Mountain. In some cases, provisions of
40 CFR part 191 were already consistent
with NAS’s analysis (e.g., level of
protection for the individual). In other
cases, we used the NAS Report to
modify or draw out parts of 40 CFR part
191 to apply more directly to Yucca
Mountain (e.g., the stylized drilling
scenario for human intrusion). See the
NAS Report for a complete description
of findings and recommendations
(Docket No. EPA–HQ–OAR–2005–0083–
0076).
Because our standards are intended to
apply specifically to the Yucca
Mountain disposal system, we tailored
our approach to consider the
characteristics of the site and the local
populations. Yucca Mountain is in
southwestern Nevada approximately
100 miles northwest of Las Vegas. The
eastern part of the site is on the Nevada
Test Site (NTS). The northwestern part
of the site is on the Nevada Test and
Training Range (referred to in our
proposal as the Nellis Air Force Range).
The southwestern part of the site is on
Bureau of Land Management land. The
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area has a desert climate with
topography typical of the Basin and
Range province. Yucca Mountain is
made of layers of ashfalls from volcanic
eruptions that happened more than 10
million years ago. There are two major
aquifers beneath Yucca Mountain.
Regional ground water in the vicinity of
Yucca Mountain is believed to flow
generally in a south-southeasterly
direction. For more detailed
descriptions of Yucca Mountain’s
geologic and hydrologic characteristics,
and the disposal system, please see
Chapter 7 of the 2001 Background
Information Document (BID) (Docket
No. EPA–HQ–OAR–2005–0083–0050)
and the preamble to the proposed rule
(64 FR 46979–46980, August 27, 1999,
Docket No. EPA–HQ–OAR–2005–0083–
0041).
We proposed the original standards
for Yucca Mountain on August 27, 1999
(64 FR 46976). In response to our
proposal, we received more than 800
public comments and conducted four
public hearings. After evaluating public
comments, we issued final standards (66
FR 32074, June 13, 2001). See the
Response to Comments document from
that rulemaking for more discussion of
comments (Docket No. EPA–HQ–OAR–
2005–0083–0043).
The final standards issued in 2001 as
40 CFR part 197 included the following:
• A standard to protect the public
during management and storage
operations on the Yucca Mountain site;
• An individual-protection standard
to protect the public from releases from
the undisturbed disposal system;
• A human-intrusion standard to
protect the public after disposal from
releases caused by a drilling penetration
into the repository;
• A set of standards to protect ground
water from radionuclide contamination
caused by releases from the disposal
system;
• The requirement that compliance
with the disposal standards be shown
for 10,000 years;
• The requirement that DOE continue
its projections for the individualprotection and human-intrusion
standards beyond 10,000 years to the
time of peak (maximum) dose, and place
those projections in the Environmental
Impact Statement (EIS) for Yucca
Mountain;
• The concept of the Reasonably
Maximally Exposed Individual (RMEI),
defined as a hypothetical person whose
lifestyle is representative of the local
population living today in the Town of
Amargosa Valley, as the individual
against whom the disposal standards
should be assessed; and
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• The concept of a ‘‘controlled area,’’
defined as an area immediately
surrounding the repository whose
geology is considered part of the natural
barrier component of the overall
disposal system, and inside of which
radioactive releases are not regulated.
More detail on these aspects of the
2001 final rule may be found at 66 FR
32074–32134, June 13, 2001, and 70 FR
49019–49020, August 22, 2005.
B. Legal Challenges to 40 CFR Part 197
Various aspects of our standards were
challenged in lawsuits filed with the
U.S. Court of Appeals for the District of
Columbia Circuit in July 2001. These
challenges and the Court’s subsequent
ruling are described briefly here,
emphasizing the aspects leading to
today’s final rule, and in more detail in
the preamble to the proposed rule (70
FR 49014, August 22, 2005).
The State of Nevada, the Natural
Resources Defense Council (NRDC), and
several other petitioners challenged
various aspects of our final standards on
the grounds that they were
insufficiently protective and had not
been adequately justified. The focus of
this challenge was the 10,000-year
compliance period. Nevada and NRDC
claimed that EPA’s promulgation of
numerical standards that applied for
10,000 years after disposal violated the
EnPA because such standards were not
‘‘based upon and consistent with’’ the
findings and recommendations of the
NAS. NAS recommended standards that
would apply to the time of maximum
risk, within the limits imposed by the
long-term geologic stability of the site,
and stated that there is ‘‘no scientific
basis for limiting the time period of the
individual-risk standard to 10,000 years
or any other value.’’ (NAS Report p. 55)
The Nuclear Energy Institute (NEI)
challenged the ground-water protection
standards as unnecessary to protect
public health and safety, contrary to
recommendations of the NAS, and
outside our authority under the EnPA.
The DC Circuit Court’s July 9, 2004
decision dismissed NEI’s challenge, and
all of the challenges by Nevada and
NRDC, except one. On the question of
EPA’s 10,000-year compliance period,
the Court upheld the challenge, ruling
that EPA’s action was not ‘‘based upon
and consistent with’’ the NAS Report,
and that EPA had not sufficiently
justified on policy grounds its decision
to apply compliance standards only to
the first 10,000 years after disposal.
Nuclear Energy Institute v.
Environmental Protection Agency, 373
F.3d 1251 (D.C. Cir. 2004) (NEI ).
The Court concluded that ‘‘we vacate
40 CFR part 197 to the extent that it
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61259
incorporates a 10,000-year compliance
period * * *.’’ (Id. at 1315) The Court
did not address the protectiveness of the
150 µSv/yr (15 mrem/yr) dose standard
applied over the 10,000-year
compliance period, nor was the
protectiveness of the 15 mrem/yr
standard challenged. It ruled only that
the compliance period was not
consistent with or based upon the NAS
findings and recommendations and,
therefore, was contrary to the plain
language of the EnPA.
As the Court noted, NAS stated that
it had found ‘‘no scientific basis for
limiting the time period of the
individual-risk standard to 10,000 years
or any other value,’’ and that
‘‘compliance assessment is feasible
* * * on the time scale of the long-term
stability of the fundamental geologic
regime—a time scale that is on the order
of 106 years at Yucca Mountain.’’ As a
result, and given that ‘‘at least some
potentially important exposures might
not occur until after several hundred
thousand years * * * we recommend
that compliance assessment be
conducted for the time when the
greatest risk occurs.’’ (NAS Report pp.
6–7) Today’s action addresses this
recommendation and the DC Circuit
ruling.
II. Summary of Proposed Amendments
to 40 CFR Part 197 and Public
Comments
The primary goal of our proposal
issued in 2005 was to gather public
comment on the appropriate response to
the Court decision and NAS
recommendation to assess compliance
at the time of maximum dose (risk).
Therefore, our proposed amendments
centered on extending the compliance
period to capture the peak projected
dose from the Yucca Mountain disposal
system ‘‘within the limits imposed by
the long-term stability of the geologic
environment.’’ (NAS Report p. 2) Of
course, establishing a radiological
protection standard to apply at the time
of peak dose is a uniquely challenging
task. Only a small number of countries
have established standards of any kind
for the geologic disposal of SNF and
HLW. Of these, only Switzerland has
established a quantitative standard
applicable for as long as 1 million years,
although we are aware that other
regulatory bodies outside the U.S. are
contemplating the need to establish
some type of regulation addressing these
extremely long time frames. Comments
received in the course of this
rulemaking have been helpful given the
extraordinary technical complexity of
this task.
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A. How Did We Propose To Amend Our
2001 Standards?
We considered carefully the language
and reasoning of the Court’s decision in
revising our 2001 standards. As
originally promulgated in 2001, 40 CFR
part 197 contained four sets of standards
against which compliance would be
assessed. The storage standard applies
to exposures of the general public
during the operational period, when
waste is received at the Yucca Mountain
site, handled in preparation for
emplacement in the repository,
emplaced in the repository, and stored
in the repository until final closure. The
three disposal standards apply to
releases of radionuclides from the
disposal system after final closure, and
include an individual-protection
standard, a human-intrusion standard,
and a set of ground-water protection
standards.
The Court’s ruling vacated only one
aspect of 40 CFR part 197: The 10,000year compliance period applicable to
the disposal standards. Therefore, the
storage standard, which is applicable
only for the period before disposal, is
not affected by the ruling. Further, the
Court recognized that the ground-water
protection standards were issued as an
expression of EPA’s overall groundwater protection policies and were not
among the standards addressed by the
NAS, either in form or purpose (‘‘NAS
treated the compliance-period and
ground-water issues quite differently
* * * NAS made no ‘finding’ or
‘recommendation’ that EPA’s regulation
could fail to be ‘based upon and
consistent with’ ’’ (NEI, 373 F.3d at
1282)). Therefore, we concluded that the
Court’s vacature of the 10,000-year
compliance period, which was
explicitly tied to recommendations
concerning the individual-protection
standard, does not extend to the groundwater provisions. As a result, we did not
propose to amend the ground-water
protection standards. Nothing in today’s
final rule affects those standards.
We proposed to revise only the
individual-protection and humanintrusion standards, along with certain
supporting provisions related to the way
DOE must consider features, events, and
processes (FEPs) in its compliance
analyses (70 FR 49014, August 22,
2005). In addition, we proposed to
adopt updated scientific factors for
calculating doses to show compliance
with the storage, individual-protection,
and human-intrusion standards. We
requested comments only on those
aspects of the individual-protection and
human-intrusion standards which were
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to be amended. Specifically, we
proposed to:
• Extend the compliance period for
the individual-protection and humanintrusion standards to 1 million years
after disposal (closure), consistent with
NAS estimates regarding the ‘‘long-term
stability of the geologic environment’’;
• Retain the dose standard of 150
µSv/yr (hereafter, 15 mrem/yr)
committed effective dose equivalent
(CEDE) for the first 10,000 years after
disposal, as promulgated in 2001;
• Establish a dose standard of 3.5
mSv/yr (hereafter, 350 mrem/yr) CEDE
for the period between 10,000 years and
1 million years;
• Clarify that the arithmetic mean of
the distribution of projected results will
be compared to the dose standard for
the initial 10,000 years, and specify use
of the median of the distribution of
projected results between 10,000 and 1
million years;
• Retain the probability threshold (1
in 10,000 chance of occurring in 10,000
years, or 1 in 100 million chance of
occurring per year) below which ‘‘very
unlikely’’ FEPs may be excluded from
consideration;
• Allow FEPs with a probability of
occurring above the probability
threshold to be excluded if they would
not significantly affect the results of
performance assessments in the initial
10,000 years;
• Require consideration of seismic
and igneous events causing direct
damage to the engineered barrier system
during the 1 million-year period;
• Require consideration of the effects
of increased water flow through the
repository resulting from climate
change, which could be represented by
constant conditions between 10,000 and
1 million years;
• Require consideration of the effects
of general corrosion of the engineered
barriers between 10,000 and 1 million
years; and
• Require use of updated scientific
factors, based on Publications 60 and 72
of the International Commission on
Radiation Protection (ICRP), to calculate
dose for comparison with the storage,
individual-protection, and humanintrusion standards.
B. What Factors Did We Consider in
Developing Our Proposal?
Of great concern in extending the
compliance period to 1 million years is
the increasing uncertainty associated
with numerical projections of
radionuclide releases from the Yucca
Mountain disposal system and
subsequent exposures incurred by the
Reasonably Maximally Exposed
Individual (RMEI). This uncertainty
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affects not only the projections
themselves, but also the interpretation
of the results. There is general
agreement in the international
community that dose projections over
periods as long as 1 million years
cannot be viewed in the same context or
with the same confidence as projections
for periods as ‘‘short’’ as 10,000 years.
As a result, the nature of regulatory
decision-making fundamentally changes
when faced with the prospect of
compliance projections for the next 1
million years. International guidance
from the International Atomic Energy
Agency (IAEA) and Nuclear Energy
Agency (NEA), as well as geologic
disposal programs in other countries,
recognize this difficulty and
accommodate it by viewing longer-term
projections in a more qualitative
manner, to be balanced and
supplemented by other considerations
that would provide confidence in the
long-term safety of the disposal system.
In effect, numerical dose projections are
given less weight in decision-making at
longer times.2 Such approaches
discourage comparison of projections
against a strict compliance limit.
This uncertainty was the overriding
reason for limiting the compliance
period to 10,000 years in our 2001 rule.
We supplemented that 10,000-year
compliance period by requiring DOE to
continue projections through the time of
peak dose, consistent with the approach
favored by the international community.
However, while we believed this
approach was consistent with the NAS
recommendation to assess compliance
at the time of maximum dose (risk) and
the committee’s acknowledgment that
policy considerations would also play a
role in determining the compliance
period, the Court concluded that it was
inconsistent with the NAS
recommendation. We concluded that
the most direct way to address the
Court’s ruling would be to establish a
numeric compliance standard for the
time of peak dose, within the period of
geologic stability at Yucca Mountain,
which NAS judged to be ‘‘on the order
of one million years.’’ (NAS Report p. 2)
In establishing our final standards, we
have considered that the level of
uncertainty increases as the time period
covered by DOE’s performance
2 For example, the ICRP’s most recent
recommendations note that ‘‘both the individual
doses and the size of the exposed population
become increasingly uncertain as time increases.
The Commission is of the opinion that in the
decision-making process, owing to the increasing
uncertainties, giving less weight to very low doses
and to doses received in the distant future could be
considered.’’ (Publication 103, 2007, Docket No.
EPA–HQ–OAR–2005–0083–0423, Paragraph 222)
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assessment increases.3 Therefore, it is
reasonable for us to consider how the
compliance standard itself might also
need to change. Specifically, we do not
believe that extending the 10,000-year
individual-protection standard of 15
mrem/yr to apply for 1 million years
adequately accounts for the
considerations outlined above or
represents a reasonable test of the
disposal system (more extensive
discussion of uncertainty in
performance assessments is in section
III.A.4 of this document, ‘‘How Did We
Consider Uncertainty and Reasonable
Expectation?’’); see also 66 FR 32098.
We turned back to the international
technical literature for advice regarding
appropriate points of comparison for
doses projected over hundreds of
thousands of years. A number of sources
suggested that natural sources of
radioactivity would provide an
appropriate benchmark for such
comparisons. In exploring this approach
further, we found that the variation in
background radiation across the United
States covered a wide range (from
roughly 100 mrem/yr to 1 rem/yr),
primarily because of local variation in
radon exposures. We chose for our
proposal a level of 350 mrem/yr, which
is close to a widely-cited estimate of 300
mrem/yr for the national average
background radiation exposure (NAS
Report Table 2–1), but specifically
represented the difference between
estimated background levels in
Amargosa Valley and the State of
Colorado. This level was proposed for
both the individual-protection and
human-intrusion standards as offering
both a reasonable level of protection and
a sound basis for regulatory decisionmaking when exposures are projected to
occur hundreds of thousands of years
into the future. Selecting such a level
would also provide an indication that
exposures incurred by the RMEI in the
far future from the combination of
natural background radiation and
releases from the Yucca Mountain
disposal system would not exceed
exposures incurred by residents of other
parts of the country today from natural
sources alone. Today’s final rule adopts
a more stringent standard that is not
derived from an analysis of background
radiation, as explained in sections
III.A.1 (‘‘What is the Peak Dose Standard
Between 10,000 and 1 Million Years
After Disposal?’’) and III.A.5 (‘‘How Did
We Consider Background Radiation in
3 ‘‘We recognize that there are significant
uncertainties in the calculations and that these
uncertainties increase as the time at which peak
risk occurs increases.’’ (NAS Report p. 56)
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Developing The Peak Dose Standard?’’)
of this document.
Uncertainty in long-term projections
also influenced our proposal. Given the
probabilistic nature of performance
assessments, it is possible that some
combinations of parameter values will
result in very high doses, even if such
combinations have an extremely low
probability of occurring. Although there
may be only a few results that are very
high, extreme results have the potential
to exert a strong influence on the
arithmetic mean, which could make the
mean less representative of all
performance projections. This
possibility may be increased by the
introduction of additional, and possible
excessive, conservatisms as a way to
account for uncertainties. We expressed
a preference for a statistical measure
that would not be strongly affected by
either very high- or low-end estimates,
believing it appropriate to focus on the
‘‘central tendency’’ of the distribution,
where the bulk of the results might be
expected to be found. We proposed the
median of the distribution as being most
representative of central tendency.
Because it is always located at the point
where half the distribution is higher and
half lower, the median depends only on
the relative nature of the distribution,
rather than the absolute calculated
values. Given our concerns about
specifying a peak dose compliance
value against which performance would
be judged for a period up to 1 million
years, we believed the median might
also provide a reasonable test of longterm performance. Today’s final rule
departs from the proposal by adopting
the arithmetic mean as the statistical
measure of compliance to be applied at
all times, as explained in section III.A.9
of this document (‘‘How Will NRC Judge
Compliance?’’).
Our consideration of FEPs also was
affected to some extent by uncertainty,
as well as by conclusions of the NAS
committee. In our proposal, the overall
probability threshold for inclusion of
FEPs remained the same as in the 2001
rule, which we believe provides a very
inclusive initial screen that captures
both major and minor factors potentially
affecting performance. Uncertainty
plays a role in the sense that very
gradual or infrequent processes and
events may begin to influence
performance only at times in the
hundreds of thousands of years, when
the overall uncertainty of assessments is
increasing. The additional uncertainty
introduced by these slow-acting FEPs
led us to propose the exclusion of FEPs
if they were not significant to the
assessments in the initial 10,000 years.
We believed this would still provide for
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61261
robust assessments that would address
the factors of most importance over the
entire 1 million-year period. We did
consider in our proposal whether
significant FEPs might not be captured
using this approach. In evaluating
whether excluded FEPs might become
more probable or more significant after
10,000 years, and therefore should not
be eliminated, we identified general
corrosion as a FEP that is certain to
occur and represents a significant
failure mechanism at longer times, even
though it is less significant in the initial
10,000 years.
We also consulted the NAS Report for
advice on handling long-term FEPs.
NAS identified three ‘‘modifiers’’ that it
believed could reasonably be included
in assessments: seismic events, igneous
events, and climate change. (NAS
Report p. 91) We developed provisions
addressing these FEPs that incorporated
the views expressed by the NAS. For
seismic and igneous events, we
proposed that DOE focus its attention on
events causing direct damage to the
engineered barriers. We took this
approach because failure of the
engineered barrier system, particularly
the waste packages, is the predominant
factor in determining the timing and
magnitude of the peak dose, and is the
overriding uncertainty in assessing
performance of the disposal system. To
address climate change, we required
DOE to focus on the effects of increased
water flow through the repository,
which is the climatic effect with the
most influence on release and transport
of radionuclides. We determined that
such a focus would provide the basis for
a reasonable test of the disposal system,
and that climate change beyond 10,000
years could be represented by constant
conditions reflecting precipitation levels
that differ from current conditions,
which eliminates unresolvable
speculation regarding the timing,
magnitude, and duration of climatic
cycles over this time frame. We also
directed that NRC establish the exact
nature of future climate characteristics
to be used in performance assessments.
NRC subsequently issued a proposal to
specify a range of values for deep
percolation into the repository, which
DOE would use as another parameter in
its probabilistic performance
assessments. (70 FR 53313, September
8, 2005)
Finally, we proposed to update the
factors used to calculate dose for the
storage, individual-protection, and
human-intrusion standards. Our generic
standards in 40 CFR part 191, and by
inference our Yucca Mountain
standards in 2001, specified the factors
associated with ICRP Publications 26
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and 30 (Docket Nos. EPA–HQ–OAR–
2005–0083–0425 and 0428,
respectively). Since we issued 40 CFR
part 191, ICRP has modified the models
and associated organ-weighting factors
to more accurately calculate dose. See
ICRP Publications 60 and 72 (Docket
Nos. EPA–HQ–OAR–2005–0083–0421
and 0427, respectively). We used this
newer method in 1999 to develop our
Federal Guidance Report 13, ‘‘Cancer
Risk Coefficients from Exposure to
Radionuclides’’ (Docket No. EPA–HQ–
OAR–2005–0083–0072). Where
possible, we believe it is appropriate to
adopt the latest scientific methods.4
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C. In Making Our Final Decisions, How
Did We Incorporate Public Comments
on the Proposed Rule?
Section 801(a)(1) of the EnPA requires
us to set public health and safety
radiation protection standards for Yucca
Mountain by rulemaking. Pursuant to
Section 4 of the Administrative
Procedure Act (APA), regulatory
agencies engaging in informal
rulemaking must provide notice of a
proposed rulemaking, an opportunity
for the public to comment on the
proposed rule, and a general statement
of the basis and purpose of the final
rule.5 The notice of proposed
rulemaking required by the APA must
‘‘disclose in detail the thinking that has
animated the form of the proposed rule
and the data upon which the rule is
based.’’ (Portland Cement Association v.
Ruckelshaus, 486 F. 2d 375, 392–94 (DC
Cir. 1973)) The public thus is enabled to
participate in the process by making
informed comments on the proposal.
This provides us with the benefit of ‘‘an
exchange of views, information, and
criticism between interested persons
and the agency.’’ (Id.)
There are two primary mechanisms by
which we explain the issues raised in
public comments and our reactions to
them. First, we discuss broad or major
comments in the succeeding sections of
this preamble. Second, we are
publishing a document, accompanying
today’s action, entitled ‘‘Response to
Comments’’ (Docket No. EPA–HQ–
OAR–2005–0083–0431). The Response
to Comments document provides more
4 ICRP published its most recent
recommendations in Publication 103, issued in
2007 (Docket No. EPA–HQ–OAR–2005–0083–0423).
EPA has not determined the impact of these
recommendations on its current dose and risk
estimates, but may decide to adopt them in the
future. Today’s final rule will incorporate the ICRP
60 recommendations as consistent with EPA’s
current federal guidance; however, we have
provided some flexibility for use of newer
dosimetry in the future if deemed appropriate by
NRC.
5 5 U.S.C. 553.
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detailed responses to issues addressed
in the preamble. It also addresses all
other significant comments on the
proposal. We gave all the comments we
received, whether written or oral,
consideration in developing the final
rule.
D. What Public Comments Did We
Receive?
The public comment period ended
November 21, 2005. We received more
than 300 individual submittals,
although any particular submittal could
contain many specific comments. We
also received many more submissions as
part of mass comment efforts, in which
organizations encourage commenters to
use prepared texts or comment on
specific aspects of the proposal. All, or
representative, comments are available
electronically through the Federal
Document Management System (FDMS),
available at https://www.regulations.gov.
See the ‘‘General Information’’ section
of this document for instructions on
how to access the electronic docket.
Some submittals may be duplicated in
FDMS, as a commenter may have used
several methods to ensure the comments
were received, such as fax, e-mail, U.S.
mail, or directly through FDMS.
A significant number of comments
addressed the proposed peak dose
standard of 350 mrem/yr, which would
apply between 10,000 and 1 million
years. Most commenters opposed our
proposal, arguing that it is much higher
than any previous standard, is not
protective, is not equitable to future
generations, and is based on
inappropriate use of background
radiation data. Many commenters also
took issue with our proposal to use the
median of the distribution of results as
the statistical measure between 10,000
and 1 million years, viewing this
measure as inconsistent with NAS
recommendations to use the mean.
Commenters also viewed the median as
too ‘‘lax’’ and likely to discount
scenarios that would result in high
exposures. We also received comment
on our proposal concerning the
assessment of FEPs beyond 10,000
years, with some comments expressing
the opinion that we had inappropriately
constrained the analyses, leaving out
potentially significant FEPs. Some
commenters disagreed with our general
premise that uncertainty increases with
assessment time and further disagreed
that we should take uncertainties into
account when considering standards
applicable to the far future. These
specific comments, and our responses to
them, will be discussed in more detail
in section III of this document and in
the Response to Comments document
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associated with this action (Docket No.
EPA–HQ–OAR–2005–0083–0431).
Some commenters also questioned
our conclusion that extending the
compliance period is the appropriate
way to respond to the Court ruling.
These commenters point out that the
Court’s opinion could be interpreted to
permit us to justify the approach taken
in our 2001 standards. They cite
statements by the Court such as ‘‘[i]t
would have been one thing had EPA
taken the Academy’s recommendations
into account and then tailored a
standard that accommodated the
agency’s policy concerns’’ and ‘‘[h]ad
EPA begun with the Academy’s
recommendation to base the compliance
period on peak dosage and then made
adjustments to accommodate policy
considerations not considered by NAS,
this might be a very different case’’ (NEI,
373 F.3d at 1270 and 1273, respectively)
to support the thesis that the Court’s
judgment was based primarily on the
presentation of our case, rather than the
substance. In the commenters’ view, the
Court would have been receptive to our
arguments had they been presented
differently, and the Court provided a
clear ‘‘road map’’ to justify keeping our
original standards in place. In addition,
these and other commenters viewed
extending the compliance period to 1
million years as not justifiable either
scientifically or as a matter of public
policy. We believe that the approach we
are taking is the most appropriate way
to address the concerns raised by the
Court’s decision, particularly given the
weight accorded by the Court to the
NAS technical recommendations
concerning the period of geologic
stability. As we stated in our proposal,
‘‘it is not clear how EPA’s earlier
explanation of its policy concerns might
be reconciled with NAS’s technical
recommendation.’’ (70 FR 49032)
Accordingly, today’s final rule
implements the NAS technical
recommendation with regard to the
length of time for the compliance period
while still accommodating our policy
concerns in the provisions related to the
peak dose standard, and FEPs.
We received some comments that
suggested we should have provided
more or better opportunities for public
participation in our decision making
process. For example, comments
suggested that we should have
rescheduled public hearings, extended
the public comment period, and
provided alternatives to the public
hearing process. We provided numerous
opportunities and avenues for public
participation in the development of
these standards. For example, we held
public hearings in Washington, DC; Las
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Vegas, NV; and Amargosa Valley, NV.
We also opened a 60-day public
comment period and met with key
stakeholders before and during that
time. In response to requests from
stakeholders, we extended the public
comment period by 30 days and held an
additional public hearing in Las Vegas.
We conducted targeted outreach to
Native American tribal groups and have
fully considered all comments received
through December 31, 2005, after the
end of the extended public comment
period. These measures are in full
compliance with the public
participation requirements of the
Administrative Procedure Act.
Several commenters supported our
role in setting standards for Yucca
Mountain. Other commenters thought
that aspects of our standards duplicate
NRC’s implementation role. We believe
the provisions of this rule clearly are
within our authority and they are
central to the concept of a public health
protection standard. We also believe our
standards leave NRC the necessary
flexibility to adapt to changing
conditions at Yucca Mountain or to
impose additional requirements in its
implementation efforts, if NRC deems
them to be necessary.
We also received many general
comments, and others addressing topics
that are outside the scope of our
authority under the EnPA. For example,
several commenters simply expressed
their support for, or opposition to, the
Yucca Mountain repository. Other
comments suggested our standards
should explicitly consider radiation
exposures from all sources because of
the site’s proximity to the Nevada Test
Site (NTS) and other sources of
potential contamination. Also, a number
of commenters suggested that we should
explore alternative methods of waste
disposal, such as neutralizing
radionuclides. Comments also
expressed concern regarding risks of
transporting radioactive materials to
Yucca Mountain. These comments all
raise considerations that are outside the
scope of our authority and this
rulemaking.
Many comments touched on issues
related to our authority and standards,
but outside the limited scope of this
rulemaking. In particular, many
comments urged us to extend the
ground-water protection limits to the
time of peak dose within the 1 millionyear compliance period. Many of these
commenters disagreed with our position
that the ground-water standards were
not the subject of the Court’s ruling, and
that in fact the Court left us with
discretion regarding the content and
application of those standards. Others
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believed that we are obligated to accept
comments on this topic, since we were
proposing not to change the standards.
We stated clearly in our proposal that
we were not soliciting, and would not
consider, comments on this issue.
III. What Final Amendments Are We
Issuing With This Action?
This section describes the provisions
of our final rule, our rationale, and our
response to public comments on various
aspects of our proposal. Today’s final
rule establishes the dose standards
applicable for a period up to 1 million
years after disposal, the statistical
measures used to determine compliance
with those standards, the methods to be
used to calculate the dose, and the
requirements for including features,
events, and processes (FEPs) in the
performance assessments.
A. What Dose Standards Will Apply?
Today’s final rule includes an
individual-protection standard
consisting of two parts, which will
apply over different time frames. The
post-10,000-year public health
protection standard limits the long-term
peak dose to the RMEI from the Yucca
Mountain disposal system to 1 mSv/yr
(100 mrem/yr) committed effective dose
equivalent (CEDE). This post-10,000year (also referred to as the ‘‘peak dose’’)
standard addresses and responds to the
DC Circuit ruling that our 2001
standards, with the compliance period
limited to 10,000 years, were
inconsistent with the recommendations
of the NAS. The post-10,000-year
standard was the focus of our proposal
and will apply after 10,000 years
through the period of geologic stability,
up to 1 million years after disposal. The
other part of the individual-protection
standard, which will apply over the
initial 10,000 years after disposal,
consists of the 150 µSv/yr (15 mrem/yr)
CEDE individual-protection standard
promulgated in 2001 as 40 CFR 197.20.
We believe this approach maintains an
appropriate emphasis on the initial
condition of the repository and its
critical early evolution, including the
period when thermal stresses will be
most significant.6 As the disposal
system evolves, today’s final rule
6 We noted in our 2001 rule: ‘‘Focusing upon a
10,000-year compliance period forces more
emphasis upon those features over which humans
can exert some control, such as repository design
and engineered barriers. Those features, the
geologic barriers, and their interactions define the
waste isolation capability of the disposal system. By
focusing upon an analysis of the features that
humans can influence or dictate at the site, it may
be possible to influence the timing and magnitude
of the peak dose, even over times longer than
10,000 years.’’ (66 FR 32099)
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establishes a peak dose standard for the
period up to 1 million years that is
responsive to the Court’s ruling,
consistent with the NAS
recommendation to establish a
compliance standard for the time of
peak risk, and satisfies our statutory
mandate to protect public health and
safety. The final rule also provides a
reasonable test of disposal system
performance by appropriately
recognizing the relatively more difficult
challenge in treating the uncertainties
associated with projecting performance
to such distant times, and the resulting
lessened level of confidence that can be
derived from such performance
projections.
As we noted in our proposal, there
was no legal challenge to, and the Court
made no ruling on, the protectiveness of
our standards up to 10,000 years.
Further, the Court ruled that we must
address peak dose, but did not state, and
we do not believe intended, that we
could not have additional measures to
bolster the overall protectiveness of the
standard. We believe that promulgating
the post-10,000-year peak dose standard
to protect public health and safety while
retaining a separate individualprotection standard that focuses
attention on the early evolution of the
repository in the pre-10,000-year period
enhances the overall protectiveness of
our rule and is consistent with the
findings and recommendations of the
NAS committee. As the Court noted, the
EnPA requires that EPA ‘‘establish a set
of health and safety standards, at least
one of which must include an EDEbased, individual protection standard’’
(NEI, 373 F.3d at 1281), but does not
restrict us from issuing additional
standards. Thus, as long as we address
the NAS recommendation regarding
peak dose, as we are doing today by
issuing the post-10,000-year standard,
we are not precluded from issuing other,
complementary, standards to apply for a
different compliance period. The
Court’s concern was whether we had
been inconsistent with the NAS
recommendation by not extending the
period of compliance to capture the
peak dose ‘‘within the limits imposed
by the long-term stability of the geologic
environment.’’ (NAS Report p. 2)
Today’s final rule defines the period of
geologic stability for purposes of
compliance as ending at 1 million years
after disposal. We believe our decision
to retain a separate standard applicable
for the first 10,000 years after disposal
during this period, along with ‘‘at least
one * * * EDE-based, individual
protection standard’’ applying to the
peak dose during the period of geologic
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stability between 10,000 years and 1
million years, protects public health and
safety pursuant to the EnPA, complies
with the Court’s decision, falls well
within our policy discretion and is
supported by scientific considerations
concerning the impact of uncertainties
in projecting doses over extremely long
time frames, as discussed in Section
III.A.4 of this document (‘‘How Did We
Consider Uncertainty and Reasonable
Expectation?’’).
The NAS Report recognized the
possible outcome of a rulemaking
establishing separate standards that
apply over different time periods. As
discussed in more detail in Section
III.A.6 (‘‘How Does Our Rule Protect
Future Generations?’’), the committee
contrasted an approach in which ‘‘a
health-based risk standard could be
specified to apply uniformly across time
and generations’’ with ‘‘some other
expression of the principle of
intergenerational equity’’ to be
determined by ‘‘social judgment.’’ (NAS
Report pp. 56–57) The committee also
recognized, as we have just explained,
that ‘‘the scientific basis for analysis
changes with time’’ in potentially
significant ways as the time to peak
dose increases. (NAS Report pp. 30–31)
We also find it useful to consider the
testimony of Mr. Robert Fri, chair of the
NAS committee, before the Senate
Environment and Public Works
Committee on March 1, 2006, in his
personal capacity, wherein he pointed
out that ‘‘the specification of the time
horizon and the selection of the person
to be protected are intimately
connected.’’ As a result, he explained
that retaining the RMEI as the receptor
(which the NAS committee recognized
as more conservative than, but ‘‘broadly
consistent’’ with, its preferred
probabilistic critical group 7) while at
the same time extending the compliance
period ‘‘runs the risk of excessive
conservatism,’’ potentially putting the
rule where the ‘‘committee specifically
did not want to be.’’ He noted that the
committee had considered and rejected
such an approach. (See NAS Report pp.
100–103) Mr. Fri viewed our proposal of
a higher dose limit between 10,000 and
1 million years as a way ‘‘to avoid
becoming overly conservative.’’
Therefore, while he (like the NAS
committee itself) offered no opinion on
the level of the proposed post-10,0007 In discussing an alternative subsistence-farmer
receptor, the committee noted that ‘‘it makes the
most conservative assumption that wherever and
whenever the maximum concentration of
radionuclides occurs in a ground water plume
accessible from the surface, a farmer will be there
to access it.’’ (NAS Report p. 102) We have defined
the RMEI to incorporate this same assumption.
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year standard, he indicated that, in his
opinion, our approach was not in
conflict with the committee’s intention,
and would be closer to the committee’s
overall goal than would applying the 15
mrem/yr standard to the 1 million-year
compliance period. He concluded by
stating ‘‘the committee recognized that
EPA properly had considerable
discretion in applying policy
considerations outside the scope of our
study to the development of the health
standard for Yucca Mountain.’’ (See
generally NAS Report p. 3) See the
hearing transcript at Docket No. EPA–
HQ–OAR–2005–0083–0380 and Mr.
Fri’s prepared testimony at Docket No.
EPA–HQ–OAR–2005–0083–0402. We
believe the decision to establish two
compliance standards falls well within
our policy discretion and in that context
the 10,000-year individual-protection
standard is analogous to our groundwater protection standards, which were
also not addressed by NAS
recommendations.
1. What Is the Peak Dose Standard
Between 10,000 and 1 Million Years
After Disposal?
In establishing a public health and
safety standard applicable at the time of
peak dose, as required by the EnPA and
recommended by the NAS, and after
considering public comments on the
issue, today’s final rule adopts a more
stringent standard than the proposed 3.5
mSv/yr (350 mrem/yr) standard.
Specifically, we are today establishing
an individual-protection standard of 1
mSv/yr (100 mrem/yr) to apply beyond
10,000 years and up to 1 million years
after disposal.
As discussed in more detail later in
this section, NAS expressly refrained
from recommending any specific dose
or risk limit for the compliance
standard, but instead described ‘‘the
spectrum of regulations already
promulgated that imply a level of risk,
all of which are consistent with
recommendations from authoritative
radiation protection bodies’’ for EPA’s
consideration. (NAS Report p. 49)
Further, while NAS stated that a single
standard ‘‘could be specified to apply
uniformly over time and generations,’’ it
also recognized that other approaches
are possible as ‘‘a matter for social
judgment.’’ (NAS Report pp. 56–57)
NAS also recognized that the level of
protection was a matter best left to EPA
to establish through rulemaking: ‘‘We do
not directly recommend a level of
acceptable risk.’’ (NAS Report p. 49)
NAS further noted that, while ‘‘there is
a considerable body of analysis and
informed judgment from which to draw
in formulating a standard for the
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proposed Yucca Mountain repository,’’
‘‘EPA’s process for setting the Yucca
Mountain standard is presumably not
bound by this experience.’’ (NAS Report
p. 39) Thus, the NAS Report contains no
finding or recommendation as to the
dose limit at the time of peak dose in
our Yucca Mountain standards.
In selecting this final standard, we
started with a range of annual fatal
cancer risk (10¥5 to 10¥6) that
encompassed the 15 mrem/yr standard
established in 2001 for the initial 10,000
years after disposal. We also considered
the ‘‘starting range’’ identified by NAS
in determining the appropriate level for
the individual-protection standard to
apply in the time period beyond 10,000
years. (NAS Report p. 49 and Tables 2–
3 and 2–4) For the reasons discussed
below, we determined that it would not
be reasonable to apply a standard within
that starting range for the entire millionyear compliance period. Rather, we
identified dose levels that are protective
of public health and safety and that
reasonably accommodate our policy
concerns regarding the implementation
of a compliance standard for 1 million
years. For the same reasons, the Agency
has determined that it is not reasonable
to apply its traditional risk-management
policies when establishing a compliance
standard applicable for periods beyond
10,000 years and up to 1 million years
(see section III.A.3, ‘‘How Do Our
Standards Protect Public Health and
Safety?’’). EPA does not believe it is
realistic to demand that projections for
such complex systems over this far
future time frame be readily
distinguishable at the level of
incremental risk customarily addressed
by the Agency in situations where
results can be confirmed, modeling is
utilized on a more limited scale, or
institutional controls are more
applicable.
In selecting 100 mrem/yr as the peak
dose standard for the period beyond
10,000 years, we took particular note of
the NAS’s discussion of that dose level:
‘‘Consistent with the current
understanding of the related
consequences, ICRP, NCRP, IAEA,
UNSCEAR, and others have
recommended that radiation doses
above background levels to members of
the public not exceed 1 mSv/yr (100
mrem/yr) effective dose for continuous
or frequent exposure from radiation
sources other than medical exposures.
Countries that have considered national
radiation protection standards in this
area have endorsed the ICRP
recommendation of 1 mSv per year
radiation dose limit above natural
background radiation for members of
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the public.’’ (NAS Report pp. 40–41) We
also note that the 100 mrem/yr level is
included in the range of regulations
offered by NAS for EPA’s consideration.
(NAS Report Table 2–3)
Therefore, as we discussed in our
proposal, a dose level of 100 mrem/yr
level is well-established as protective of
public health under current dose limits,
and, as such, represents a robust public
health protection standard in the
extreme far future. (70 FR 49040) As
noted by NAS, international
organizations such as ICRP, IAEA, and
NEA recommend its use as an overall
public dose limit in planning for
situations where exposures may be
reasonably expected to occur. Although
it had used the concept of public dose
limits previously, ICRP first described
its recommendations for a
comprehensive system of radiation
protection in Publication 60 (‘‘1990
Recommendations of the ICRP’’) (Docket
No. EPA–HQ–OAR–2005–0083–0421).
ICRP considered two referents in
recommending a public dose limit:
health detriment and ‘‘variation in the
existing level of dose from natural
sources.’’ ICRP concluded that estimates
of health detriment ‘‘suggest a value of
the annual dose limit not much above
1 mSv.’’ Similarly, ‘‘[e]xcluding the very
variable exposures to radon, the annual
effective dose from natural sources is
about 1 mSv, with values at high
altitudes above sea level and in some
geological areas of at least twice this. On
the basis of all these considerations, the
Commission recommends an annual
limit on effective dose of 1 mSv.’’
(Paragraphs 190–191) ICRP re-affirmed
this position in its most recent
recommendations: ‘‘For public exposure
in planned exposure situations, the
Commission continues to recommend
that the limit should be expressed as an
effective dose of 1 mSv in a year.’’
(Publication 103, Paragraph 245, Docket
No. EPA–HQ–OAR–2005–0083–0423)
This recommendation as to a 100
mrem/yr public dose limit was adopted
in the 1996 ‘‘International Basic Safety
Standards for Protection Against
Ionizing Radiation and for the Safety of
Radiation Sources,’’ which was jointly
sponsored by IAEA, NEA, the Food and
Agriculture Organization of the United
Nations, the International Labor
Organization, the Pan American Health
Organization, and the World Health
Organization. (IAEA Safety Series 115,
Schedule II, Docket No. EPA–HQ–OAR–
2005–0083–0409) It should also be
noted that the European Union requires
its Member States to incorporate this
100 mrem/yr public dose limit into
national law or regulation (Council
Directive 96/29/EURATOM of 13 May
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1996, Docket No. EPA–HQ–OAR–2005–
0083–0410). Non-EU countries such as
Argentina, Australia, Canada, and Japan
also incorporate this public dose limit
into their systems of regulation, as
shown by their national reports under
the Joint Convention on the Safety of
Spent Fuel Management and on the
Safety of Radioactive Waste
Management (see https://wwwns.iaea.org/conventions/wastejointconvention.htm). The United States
is also a Contracting Party to the Joint
Convention (Docket No. EPA–HQ–
OAR–2005–0083–0393).
Domestically, both NRC and DOE
incorporate the 100 mrem/yr level into
their systems of regulation (10 CFR
20.1301 and DOE Order 5400.5,
respectively), and NCRP also endorses
the ICRP system of protection (NCRP
Report 116, ‘‘Limitation of Exposure to
Ionizing Radiation,’’ Docket No. EPA–
HQ–OAR–2005–0083–0407). In setting
today’s peak dose standard, EPA
acknowledges and concurs in the broad
consensus in the protectiveness of the
100 mrem/yr level and, furthermore,
considers it especially suitable for
application to the extreme far future,
when planning for and projecting public
exposures is much less certain.
For all these reasons, we conclude
that the 100 mrem/yr peak dose
standard we are establishing today for
the period beyond 10,000 years will
protect public health and safety. By
considering international guidance and
examples, we have derived a final peak
dose limit that balances the competing
factors highlighted by NAS and
acknowledged by us as important: the
dual objectives of promulgating a
standard that is protective of the health
and interests of future generations, and
also effectively addressing the effects of
uncertainty on compliance assessment.
Moreover, the 100 mrem/yr level is
comparable to the domestic and
international standards NAS suggested
that EPA consider. (NAS Report p. 49
and Tables 2–3 and 2–4)
Our selection of a 100 mrem/yr
standard is therefore protective and
reasonable in that it effectively
addresses the factors it is necessary to
consider when projecting exposures
very far into the future. By applying this
standard over the entire period of
geologic stability beyond 10,000 years
(up to 1 million years), our approach is
consistent with the NAS
recommendation to have a standard
with compliance measured ‘‘at the time
of peak risk, whenever it occurs, within
the limits imposed by the long-term
stability of the geologic environment,
which is on the order of one million
years.’’ (NAS Report p. 2)
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Although we have not used specific
estimates of background radiation in
determining our final peak dose
standard, as we had proposed, we note
that the 100 mrem/yr level reasonably
comports with such an analysis as well.
For example, it is comparable to outdoor
(unshielded) measurements of cosmic
and terrestrial radiation in Amargosa
Valley. When shielding from buildings
is considered and indoor radon doses
are estimated using a more conservative
conversion factor suggested by some
commenters, 100 mrem/yr is at the low
end of overall background radiation
estimates in Amargosa Valley and
nationally.8 Within the State of Nevada,
the difference in average estimates of
background radiation for counties is
greater than 100 mrem/yr. (Docket No.
EPA–HQ–OAR–2005–0083–0387) This
suggests that 100 mrem/yr can be
considered to be a level such that the
total potential doses incurred by the
RMEI from the combination of
background radiation and releases from
Yucca Mountain will remain below
doses incurred by residents of other
parts of the country from natural
sources alone. See Section III.A.5 of this
document for more discussion of
background radiation (‘‘How Did We
Consider Background Radiation in
Developing the Peak Dose Standard?’’).
Our proposal discussed several factors
that we considered to be important in
setting a dose standard for the time of
peak dose within the period of geologic
stability. We emphasized the
cumulative and increasing uncertainty
in projecting potential doses over great
time periods, and argued against
viewing projected doses as predictions
of disposal system performance. This is
consistent with the position taken by
the NAS committee: ‘‘The results of
compliance analysis should not,
however, be interpreted as accurate
predictions of the expected behavior of
a geologic repository.’’ (NAS Report p.
71)
We also have considered how the role
of quantitative projections in making
compliance decisions must change as
the time covered by those projections
increases to the extreme far future. We
noted that emphasizing incremental
dose increases when such increases may
be overwhelmed by fundamental
uncertainties inappropriately takes
attention away from an evaluation of the
8 NAS cited an estimate of 300 mrem/yr as the
national average for natural background radiation
(cosmic, terrestrial, radon, and radioactive isotopes
internal to the human body). (NAS Report Table 2–
1) This is the best-known estimate of average
natural background in the U.S., but does not use the
more conservative radon dose conversion factor
provided by public comments.
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overall safety of the disposal system,
which may rest equally on other lines of
evidence, such as confidence in the
long-term stability of the site or
reference to natural analogues. In our
view, in order to provide a reasonable
test of the disposal system, the role of
the peak dose standard in the overall
decision of disposal system safety must
be consistent with the relative
confidence that can be placed in
quantitative projections over extremely
long times. We have recognized the
strong consensus in the international
radioactive waste community that dose
projections extending many tens to
hundreds of thousands of years into the
future can best be viewed as qualitative
indicators of disposal system
performance, rather than as firm
predictions that can be compared
against strict numerical compliance
criteria. In fact, international
organizations have treated such
numerical criteria in a more flexible
way and supported their application in
conjunction with other qualitative
considerations in applying them to
regulatory determinations over very
long time frames.9 Further, we agree
9 The 2007 NEA document on ‘‘Consideration of
Timescales in Post-Closure Safety of Geological
Disposal of Radioactive Waste,’’ which is based on
surveys of NEA Member Countries, states
‘‘Calculated values of dose and risk are therefore
viewed in regulations not as predictions but rather
as indicators or measures of protection that are used
to test the capability of the system to provide
isolation of the waste and containment of
radionuclides (the ‘dose’ that is being calculated is
what radio-protectionists refer to as ‘potential
dose’). These indicators are to be evaluated on the
basis of models that include certain stylized
assumptions, in particular regarding the biosphere
and human lifestyle or actions.’’ (Docket No. EPA–
HQ–OAR–2005–0083–0411, p. 38) NEA also notes:
‘‘There is agreement that calculations of dose and
risk in the future are illustrations of possible system
behaviour rather than predictions of outcomes, and
there is consensus that, in the long term, numerical
criteria for radioactive waste disposal should be
considered as references or indicators, addressing
the ultimate safety objectives, rather than as
absolute limits in a legal context.’’ (‘‘Regulating the
Long-Term Safety of Geological Disposal: Towards
a Common Understanding of the Main Objectives
and Bases of Safety Criteria,’’ NEA–6182, Docket
No. EPA–HQ–OAR–2005–0083–0408, p. 24)
Similarly, ICRP Publication 81 contrasts the
approach of ‘‘consideration of quantitative
estimates of dose or risk on the order of 1000 to
10,000 years’’ with ‘‘consideration of quantitative
calculations further into the future making
increasing use of stylized approaches and
considering the time periods when judging the
calculated results. Qualitative arguments could
provide additional information to this judgmental
process.’’ (Docket No. EPA–HQ–OAR–2005–0083–
0417, Paragraph 71) The IAEA consensus document
for geologic disposal (‘‘Safety Requirements for
Geological Disposal of Radioactive Waste,’’ WS–R–
4, 2006) states: ‘‘It is recognized that radiation doses
to individuals in the future can only be estimated
and that the uncertainties associated with these
estimates will increase for times farther into the
future. Care needs to be exercised in using the
criteria beyond the time when the uncertainties
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that confidence in the way the
projections were performed, and the
consideration of supporting qualitative
information, may be more important to
an overall judgment of safety at longer
times.10 However, our task is to
establish a numerical compliance limit,
rather than a qualitative standard or
dose target. Therefore, we believe it is
appropriate in setting that limit to
evaluate and apply the considerations
that have led the international radiation
protection community to view long-term
projections in a more qualitative
manner.
We conclude that a peak dose
standard of 100 mrem/yr for the Yucca
Mountain disposal system for the period
between 10,000 and 1 million years
protects public health and safety.
Setting the standard as we have is also
consistent with the NAS committee’s
decision not to recommend a level for
the final peak standard and EPA’s broad
discretion to establish standards that are
protective while accommodating
technical and policy concerns inherent
in projecting and evaluating potential
events hundreds of thousands of years
into the future. See section III.A.3 of this
document for more discussion of the
protectiveness of our standards (‘‘How
Does Our Final Rule Protect Public
Health and Safety?’’).
The ICRP recommendation for a
public dose limit of 100 mrem/yr relates
to the total exposure to members of the
public from all manmade sources
(excluding occupational, accidental, and
medical, which can be significantly
higher). A number of comments took
issue with our approach and suggestion
that it might be reasonable to
‘‘apportion’’ the entire 100 mrem/yr to
the Yucca Mountain disposal system
because of the lack of other potential
sources in the region, and that this
could be considered consistent with the
NAS recommendation to rely on current
conditions and present knowledge. The
comments expressed the view that such
an approach would be entirely contrary
to the NAS recommendation to apply
apportionment, as well as to the
principle of apportionment itself, which
recognizes the potential for new or
become so large that the criteria may no longer
serve as a reasonable basis for decisionmaking.’’
(Docket No. EPA–HQ–OAR–2005–0083–0383,
Paragraph 2.12)
10 Such considerations are not unusual in other
applications. For example, in making plans based
on weather forecasts, one can expect the next-day
forecast to be fairly accurate. However, one has to
recognize that the same degree of accuracy cannot
be expected from longer-range forecasts. In that
case, one would want to have confidence that the
forecast is based upon the most current scientific
understanding of weather patterns.
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additional sources of exposure to be
developed.
NAS made no recommendation or
finding regarding apportionment. In its
discussion of apportionment, NAS
noted that the concept had been widely
adopted (NAS Report pp. 40–41). NAS
also noted that ‘‘guidance to date has
been for expected exposures from
routine practices. There is little
guidance on potential exposures in the
far distant future.’’ (NAS Report p. 41).
NAS made no specific recommendation
that EPA apply the concept to Yucca
Mountain, let alone how the concept
should be applied.
Further, given our statutory obligation
under the EnPA to establish a sitespecific standard, allocating 100 mrem/
yr to a single source at the time of peak
dose is reasonable because other
contributors currently in the Yucca
Mountain area are negligible by
comparison (FEIS, DOE/EIS–0250,
section 8.3.2, Docket No. EPA–HQ–
OAR–2005–0083–0086). By relying on
current conditions, as recommended by
NAS, rather than speculating on
potential future sources of exposure to
the local population, it is reasonable for
EPA to allocate the entire 100 mrem/yr
to the Yucca Mountain disposal system.
By assuming that current conditions
will apply in the future, we are applying
an approach routinely applied
internationally, as well as by EPA in its
WIPP compliance criteria (the ‘‘future
states’’ assumption at 40 CFR 194.25).11
EPA’s application of the concept of
apportionment is, moreover, reasonable.
We addressed the apportionment
approach in conjunction with our
10,000-year standard of 15 mrem/yr as
consistent with EPA’s overall risk
management approach and past actions.
However, we do not agree that it is
either required or reasonable to follow
the apportionment approach over
hundreds of thousands of years, when
the level of uncertainty in dose
projections is significantly increased
and the ability to project the
performance of engineered barriers and
the overall disposal system with a high
degree of certainty decreases. This
position is consistent with general
11 For example, IAEA notes that in modeling over
longer time frames, ‘‘The emphasis of assessment
should therefore be changed so that the calculations
relating to the near-surface zone and human activity
are simplified by assuming present day
communities under present conditions.’’ (TECDOC–
767, Docket No. EPA–HQ–OAR–2005–0083–0044,
p. 19) The French Basic Safety Rule III.2.f specifies
that ‘‘The characteristics of man will be considered
to be constant (sensitivity to radiation, nature of
food, contingency of life, and general knowledge
without assuming scientific progress, particularly in
the technical and medical fields).’’ (Docket No.
EPA–HQ–OAR–2005–0083–0389, Section 3.2)
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international practice and guidance, in
which regulatory judgments rely less on
compliance with quantitative standards
and more on other qualitative factors
supporting the overall safety case. Thus,
for example, IAEA recognizes in the
consensus document ‘‘Safety
Requirements for Geological Disposal of
Radioactive Waste’’ (WS–R–4, Docket
No. EPA–HQ–OAR–2005–0083–0383)
the general agreement of the geologic
disposal community that, while
apportionment is pertinent to geologic
disposal, it cannot be assumed to apply
indefinitely.12 Moreover, IAEA reaches
this conclusion on the basis of
uncertainty in projecting exposure from
a specific long-term source, without
regard to the presumed knowledge, or
lack thereof, of other potential sources
of exposure. We believe our approach is
consistent with the long-held
international view of 10,000 years
generally as a demarcation point prior to
which quantitative dose projections can
be reasonably well-managed, but
beyond which those projections become
progressively more uncertain and less
valuable.13 In our view, it is preferable
12 In describing criteria relevant to
apportionment, IAEA states: ‘‘It is recognized that
radiation doses to individuals in the future can only
be estimated and that the uncertainties associated
with these estimates will increase for times farther
into the future. Care needs to be exercised in using
the criteria beyond the time when the uncertainties
become so large that the criteria may no longer
serve as a reasonable basis for decision making.’’
(Paragraph 2.12, emphasis added) Similarly, NEA
cites IAEA and ICRP in noting that ‘‘Generally
speaking, these documents recommend that the
same criteria should be used as are applied for
radiation protection from current practices. These
documents also recognise, however, that such
criteria cannot be applied in the same way for the
distant future as they are for current practices.’’
(NEA–6182, Docket No. EPA–HQ–OAR–2005–
w0083–0408, p. 19, emphasis added)
13 ICRP clearly expresses this view in Publication
81: ‘‘To evaluate the performance of waste disposal
systems over long time scales, one approach is the
consideration of quantitative estimates of dose or
risk on the order of 1000 to 10,000 years. This
approach focuses on that period when the
calculation of doses most directly relates to health
detriment and also recognises the possibility that
over longer time frames the risks associated with
cataclysmic geologic changes such as glaciation and
tectonic movements may obscure risks associated
with the disposal system. Another approach is the
consideration of quantitative calculations further
into the future making increased use of stylised
approaches and considering the time periods when
judging the calculated results. Qualitative
arguments could provide additional information to
this judgmental process.’’ (Docket No. EPA–HQ–
OAR–2005–0083–0417, Paragraph 71) Similarly,
IAEA suggests that within 10,000 years, ‘‘While it
is recognized that considerable uncertainty can
exist during this time period, it is still reasonable
to attempt to make quantitative estimates of the
indicators to be used.’’ However, beyond that time,
‘‘While it may be possible to make general
predictions about geological conditions, the range
of possible biospheric conditions and human
behaviour is too wide to allow reliable modeling
* * * Such calculations can therefore only be
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to follow this well-established
precedent rather than to attempt to
define a different transition point based
on the level and timing of uncertainty
in dose projections. As discussed in
more detail later in this section,
countries that have established dose or
risk standards for geologic disposal have
typically applied them for 10,000 years
or less, suggesting that this is a period
of time within which standards
comparable to those applied to current
practices can ‘‘serve as a reasonable
basis for decision making.’’ Beyond that
time, the initial ‘‘criteria,’’ or dose
standards, are viewed more qualitatively
or entirely different criteria that are not
expressed in terms of risk or dose are
applied.14
Moreover, we note that under 10 CFR
20.1301, NRC requires that licensees
conduct operations so that the total
effective dose equivalent to individual
members of the public from ‘‘the
licensed operation’’ does not exceed 100
mrem/yr. Thus, this regulatory limit
applies to individual licensees operating
today, without reference to other
potential sources of exposure to the
public. Of course, some types of NRC
licensees, such as fuel cycle facilities
subject to our standards in 40 CFR part
190, must meet dose constraints lower
than the 100 mrem/yr limit.
Nonetheless, 100 mrem/yr is the public
dose limit from licensed operations
imposed in NRC regulations.
We disagree with those comments
generally questioning both the legality
and the protectiveness of our proposal
to establish a long-term standard higher
than 15 mrem/yr. As described
previously in section III.A (‘‘What Dose
Standards Will Apply?’’), commenters
stated that the NAS Report and Court
decision required us to retain a single
dose standard (i.e., 15 mrem/yr) for the
entire 1 million-year compliance period,
viewed as illustrative and the ‘doses’ as indicative.’’
(‘‘Safety Indicators in Different Time Frames for the
Safety Assessment of Underground Radioactive
Waste Repositories,’’ TECDOC–767, Docket No.
EPA–HQ–OAR–2005–0083–0044, pp. 18–19)
14 France applies a dose standard for the first
10,000 years that ‘‘will be applied for determining
the acceptability of the radiological consequences.’’
However, at later times, ‘‘the same [25 mrem/yr]
limit shall be used as a reference value.’’ (Basic
Safety Rule III.2.f, Section 3.2.1, Docket No. EPA–
HQ–OAR–2005–0083–0389, emphasis added)
Sweden specifies quantitative analyses to be judged
against a numerical standard for the first 1,000
years, but requires examination of ‘‘various possible
sequences for the development of the repository’s
properties, its environment and the biosphere’’ after
that time. (SSI FS 1998:1, Docket EPA–HQ–OAR–
2005–0083–0047) Similarly, Finland applies a dose
standard for ‘‘at least several thousands of years,’’
but when ‘‘human exposure’’ is no longer
‘‘adequately predictable,’’ an activity release
standard is in place. (YVL 8.4, Docket EPA–HQ–
OAR–2005–0083–0392)
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equivalent to the period of geologic
stability defined in our rule.
Commenters pointed out that the
proposed level was well above the range
identified by NAS as a starting point for
our rulemaking, and therefore stated
that only the 15 mrem/yr level could be
considered consistent with the
committee’s recommendation.
Similarly, some commenters interpreted
the Court ruling to require us to adjust
the time period covered by the existing
15 mrem/yr standard, which was not
challenged. We do not believe this
interpretation to be correct. It should be
emphasized that NAS identified a range
of risks represented by current national
and international standards, ‘‘all of
which are consistent with
recommendations from authoritative
radiation protection bodies,’’ suggested
only a ‘‘reasonable starting point’’ for
our rulemaking, and that none of the
regulatory precedents considered by
NAS applied for periods approaching 1
million years. (NAS Report pp. 5 and
49, respectively) In fact, NAS explicitly
declined to recommend a level of
protection, recognizing that this was a
matter best left to EPA to establish
through rulemaking: ‘‘We have not
recommended what levels of risk are
acceptable * * * The specific level of
acceptable risk cannot be identified by
scientific analysis, but must rather be
the result of a societal decision-making
process. Because we have no particular
authority or expertise for judging the
outcome of a properly constructed
social decision-making process on
acceptable risk, we have not attempted
to make recommendations on this
important question.’’ (NAS Report p. 20)
Indeed, NAS explicitly acknowledged
‘‘that determining what risk level is
acceptable is not ultimately a question
of science but of public policy.’’ (NAS
Report p. 5) Further, NAS noted that the
final outcome of the rulemaking might
diverge substantially from the starting
point suggested by NAS: ‘‘Finally we
have identified several instances where
science cannot provide all of the
guidance necessary to resolve an issue
* * * In these cases, we have tried to
suggest positions that could be used by
the responsible agency in formulating a
proposed rule. Other starting positions
are possible, and of course the final rule
could differ markedly from any of
them.’’ (NAS Report p. 3, emphasis
added) Thus, we agree with NAS that
the selection of a level for the peak dose
standard is one of the regulatory policy
issues left to EPA’s discretion by the
EnPA. As stated earlier, we find that the
annual risk associated with the final
peak dose standard of 100 mrem/yr is
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protective of public health and
comparable to the domestic and
international standards NAS suggested
that EPA consider, particularly when
considering the extended time frames
under consideration for this rulemaking.
(NAS Report p. 49 and Tables 2–3 and
2–4)
We also find it instructive to consider
again the personal Senate testimony of
NAS committee chair Robert Fri, as
described in Section III.A (‘‘What Dose
Limits Will Apply?’’) (Docket Nos. EPA–
HQ–OAR–2005–0083–0380 and 0402).
Mr. Fri noted that simply extending the
compliance period in our 2001 rule to
1 million years ‘‘runs the risk of
excessive conservatism’’ and could
place our standard where the
‘‘committee specifically did not want to
be.’’ He recognized that a higher
standard at the time of peak dose would
be one way to reduce that conservatism.
Mr. Fri did not address the consistency
of our proposed dose level with the
NAS findings and recommendations;
however, he indicated that, in his view,
retaining the 15 mrem/yr standard at the
time of peak dose would not be
consistent with those findings and
recommendations if other aspects of our
rule remained unchanged (specifically,
the choice of receptor). We find this
perspective noteworthy, in that it
suggests that there are circumstances in
which applying 15 mrem/yr throughout
the 1 million-year compliance period
could result in a standard contrary to
the committee’s overall goals, which
emphasized the use of ‘‘cautious, but
reasonable’’ assumptions and care in the
use of ‘‘pessimistic scenarios and
parameter values.’’ (NAS Report pp. 100
and 79, respectively)
Further, we do not believe the Court’s
decision provides direction
independent of the NAS Report; rather,
the decision requires only that we
ensure that our standards are consistent
with the NAS committee’s findings and
recommendations, as required by the
EnPA.
In considering appropriate dose
standards for periods approaching 1
million years, we also considered the
development of our generic standards in
40 CFR part 191. In both our 1985 and
1993 rulemakings establishing those
generic standards, we emphasized that
the 10,000-year compliance period for
both the containment requirements and
individual-protection limit would lead
to a combination of site characteristics
and engineered barriers that would be
capable of providing containment and
isolation of the waste for these long
periods of time. We did not, however,
anticipate that such performance could
be maintained indefinitely. Our generic
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technical analyses, in fact, suggested
that significant releases and doses to
individuals could result at later times,
depending on the characteristics of the
site in question and the presumed
location of the receptor. (See 58 FR
66401, December 20, 1993)
We note that sites whose natural
features alone did not provide total
containment were not necessarily
considered unsuitable, but we
recognized that in those instances, the
focus would have to be on ‘‘the design
of more robust engineered barrier
systems capable of significantly
impeding radionuclide releases.’’ We
believe that it is unrealistic to assume
that these sites would then exhibit
better performance after the failure of
those barriers than they would in the
initial 10,000-year period.
Consequently, we believe that the
potential for doses higher than 15
mrem/yr to individuals in the far future
has always been implicit in the concept
of geologic disposal. Over time, the
initial static system consisting of intact
waste packages and other engineered
barriers in the natural geologic setting
gives way to a more dynamic system in
which episodic and gradual processes
combine to transport radionuclides to
the accessible environment. The
sequence and timing of barrier failures
strongly influence, and introduce
considerable uncertainty into, the
timing and magnitude of projected
doses over the 1 million-year period.
The range of projected doses widens
considerably as the containment
capability of the engineered barriers
diminishes. Interpreting the safety of the
disposal system for regulatory purposes,
in our judgment, involves more than
comparison of projected doses to a
regulatory standard, and a single
standard applicable to the initial static
system would not adequately capture
the essential nature of a system that will
evolve over 1 million years.
In developing our final standards, we
have given much attention to guidance
from international organizations and
examples from specific national
programs. In general, we find few
similarities in the details of the
international approaches that are
directly applicable, and no clear basis
for comparing the different approaches.
At the same time, we did find broad
points of similarity in the overall
approach to long-term projections, and
referred in our proposal to organizations
such as IAEA and NEA, as well as
specific countries, such as Sweden. The
more typical approach internationally is
to require compliance with quantitative
performance assessment for only a
limited period of time (in some cases,
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less than 10,000 years). Longer-term
dose projections may be compared to
dose or risk targets or reference levels,
but are viewed more as qualitative
indicators of performance than as
‘‘accurate predictions of the expected
behavior of a geologic repository’’ (NAS
Report p. 71), to be weighed in
conjunction with other qualitative
arguments for confidence in the overall
safety of the facility. At longer times, the
weight given to quantitative projections
typically decreases.15 More detailed
discussion of specific international
approaches may be found in Section 4
of the Response to Comments document
for this final rule (Docket No. EPA–HQ–
OAR–2005–0083–0431).
15 The standard issued by the Swedish Radiation
Protection Authority (SSI, formerly the Swedish
Radiation Protection Institute) (SSI FS 1998:1,
‘‘Regulations on the Protection of Human Health
and the Environment in Connection with the Final
Management of Spent Nuclear Fuel and Nuclear
Waste,’’ Docket EPA–HQ–OAR–2005–0083–0047)
includes a numerical standard during the initial
period after disposal and adopts a more qualitative
approach at later times. Specifically, for the first
1,000 years following closure of a repository, ‘‘the
assessment of the repository’s protective capability
shall be based on quantitative analyses of the
impact on human health and the environment.’’
(Section 11) Thus, initially the performance
projections may be used to make decisions
regarding the protectiveness of the disposal system.
However, beyond the first thousand years, ‘‘the
assessment of the repository’s protective capability
shall be based on various possible sequences for the
development of the repository’s properties, its
environment and the biosphere.’’ (Section 12)
Similarly, the Finnish Radiation and Nuclear Safety
Authority’s (STUK) regulations for ‘‘Long-term
Safety of Disposal of Spent Nuclear Fuel’’ (YVL 8.4,
May 2001, Docket EPA–HQ–OAR–2005–0083–
0392) include two primary protection standards.
The first is an individual-protection standard of 10
mrem/yr (0.1 mSv/yr), which applies to ‘‘an
assessment period that is adequately predictable
with respect to assessments of human exposure but
that shall be extended to at least several thousands
of years.’’ (Section 2.2) The second protection
standard, which is implied to cover periods beyond
the time for which ‘‘human exposure’’ is
‘‘adequately predictable,’’ is a radionuclide release
standard similar to that included in 40 CFR part 191
and applied at WIPP. We also refer readers to the
French standard (Basic Safety Rule No. III.2.f,
‘‘Disposal of Radioactive Waste in Deep Geological
Formations,’’ 1991, Docket No. EPA–HQ–OAR–
2005–0083–0389). For the initial period, which is
to last ‘‘at least 10,000 years * * * The limit of [25
mrem/yr] will be applied for determining the
acceptability of the radiological consequences.’’
However, ‘‘[b]eyond this period’’ when
‘‘uncertainty concerning the evolution of the
repository increases progressively with time * * *
Quantified estimates of the individual dose
estimates must then be made. These may be
supplemented, by more qualitative assessments of
the results of these estimates, as regards the
geological barrier evolution factors, so as to verify
that the release of the radionuclides does not result
in an unacceptable individual dose. In this
verification, the same [25 mrem/yr] limit shall be
used as a reference value.’’ (Section 3.2.1, emphasis
added)
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2. What is the Dose Standard for 10,000
Years After Disposal?
Section 801(a)(1) of the EnPA directs
us to ‘‘promulgate, by rule, public
health and safety standards’’ that
‘‘prescribe the maximum annual
effective dose equivalent to individual
members of the public’’ from releases of
radioactive material from the Yucca
Mountain repository. Promulgation of
the standard described in section III.A.1
of this document, which will apply
beyond 10,000 years and up to 1 million
years, fulfills this statutory direction.
Today’s final rule also retains the
standard promulgated in 2001 as
§ 197.20, which requires that DOE
demonstrate a reasonable expectation
that the RMEI will not incur annual
doses greater than 15 mrem from
releases of radionuclides from the Yucca
Mountain disposal system for 10,000
years after disposal. We believe this is
an appropriate exercise of our policy
discretion, protective of public health
and safety, and consistent with our
generic standards at 40 CFR part 191
(now applied to the WIPP) and other
applications in both our regulations for
hazardous materials and internationally
for radioactive waste. Further, this dose
level is also within the range of risks
identified by NAS as consistent with
current national and international
regulations. (NAS Report p. 49, Tables
2–3 and 2–3) Moreover, the 15 mrem/yr
standard for 10,000 years is consistent
with EPA’s overall risk management
policies 16 and serves as a logical
foundation for us to incorporate
concerns regarding far future projections
(such as the specifications regarding
seismic, igneous, and climatic events
and processes discussed in section III.B
of this document).
As we stated in our proposal, an
important reason for retaining a
standard applicable for the first 10,000
years is to address the possibility,
however unlikely, that significant doses
could occur within 10,000 years, even if
the peak dose occurs significantly later,
as NAS believed likely. (NAS Report p.
2) We received some comments
suggesting that DOE’s estimates of waste
package performance are overly
optimistic and that significant early
package failures are possible, if not to be
expected. Some commenters incorrectly
argued that we had inappropriately
‘‘ratified’’ DOE’s projections of waste
package performance and our proposal
‘‘would provide essentially no
protection for the period before 10,000
years,’’ because early failure of a system
16 The
annual fatal cancer risk of 15 mrem is 8.6
× 10¥6, based on a conversion factor of 5.75 × 10¥4
fatal cancers per rem.
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licensed against a post-10,000-year dose
standard in excess of 15 mrem/yr would
have greater consequences than would
early failure of a system licensed against
a 15 mrem/yr standard that applied at
all times. We recognize that DOE’s
estimates of waste package integrity rely
heavily on extrapolations of laboratory
testing data, which involve significant
uncertainties, especially when
considering time frames well in excess
of all practical experience. It is not
possible to claim unequivocally that no
information will come to light that
might cause a reassessment of the
containers’ behavior and its effect on
disposal system performance. However,
while DOE must defend its estimates in
licensing, our rulemaking is not
dependent on resolution of this issue.
DOE will have to demonstrate that there
is a reasonable expectation that the dose
to the RMEI will not exceed 15 mrem/
yr in the first 10,000 years after closure.
Thus, the addition of the peak dose
standard in no way weakens the
protection provided by our 2001
standards, since disposal system
performance must still be assessed
against the 15 mrem/yr limit during the
relevant time period.
In fact, the reverse is true. The peak
dose standard adds a new level of
public health protection for the post10,000-year period that was not defined
in our 2001 standards. It may in fact be
highly unlikely, if not impossible, for
projected doses to exceed (or even
approach) 15 mrem/yr within the first
10,000 years without also exceeding 100
mrem/yr at some other time during the
compliance period (see section III.A.4,
‘‘How Did We Consider Uncertainty and
Reasonable Expectation?’’). In that case,
the peak dose standard of 100 mrem/yr
alone would provide the necessary
public health protection at all times
during the compliance period. The
10,000-year standard would not, then,
control projected doses during that
period but would instead represent an
explicit statement of the level of
performance that is required to be
achieved by the peak dose standard in
that initial period. We believe it is
important to structure our regulations to
make it clear that the standard of
protection at Yucca Mountain would
not be less than that provided for WIPP
or the Greater Confinement Disposal
facility (GCD).17
17 GCD
is a group of 120-feet deep boreholes,
located within the Nevada Test Site, which contain
disposed transuranic wastes.
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3. How Do Our Standards Protect Public
Health and Safety?
The peak dose standard we are
establishing today, 1 mSv/yr (100
mrem/yr), will protect public health and
safety for the period beyond 10,000
years and up to 1 million years. This
standard is consistent with the public
dose limit recommended by ICRP and
widely adopted internationally and
nationally. Section 801(a)(1) of the
EnPA directs us to ‘‘promulgate, by rule,
public health and safety standards’’ that
‘‘prescribe the maximum annual
effective dose equivalent to individual
members of the public’’ from releases of
radioactive material from the Yucca
Mountain repository. In promulgating
these standards, we have given special
consideration to the EnPA mandate that
our standards be ‘‘based upon and
consistent with’’ the recommendations
of the NAS, which included setting a
‘‘health-based individual standard’’
‘‘that sets a limit on risk to individuals
of adverse health effects.’’ (NAS Report
pp. 65 and 4) We understand this to
mean that we should select the standard
based, in part, on the level of risk,
although NAS declined to recommend
such a level. (NAS Report p. 49) We
have chosen to express the standard in
terms of dose, for the reasons described
in our 2001 final rulemaking (66 FR
32085–32086). In that rulemaking, we
did consider both the NAS views on risk
and EPA policies and precedents in
establishing the dose standard. The risk
associated with the 15 mrem/yr
standard applicable for the initial
10,000-year period is consistent with
both the Agency’s overall risk
management policies and the suggested
NAS ‘‘starting point’’ (NAS Report p.
49) The nominal annual risk associated
with the final peak dose standard of 100
mrem/yr, 5.75 × 10¥5, is comparable to
the range of risks represented by
domestic and international standards
that NAS suggested for EPA to
consider.18 This is a protective level of
risk given the extremely long time
frames contemplated for this standard,
and reasonable in that it effectively
addresses the associated uncertainty in
projecting doses for up to 1 million
years. Given this fact and the broad
consensus regarding 100 mrem/yr as a
protective public dose limit, EPA finds
that the dose standard of 100 mrem/yr,
with its associated risk, is protective of
the RMEI over the period from 10,000
18 This document focuses on annual risk rather
than lifetime risk because NAS identified annual
risk as the appropriate metric, although it did not
recommend a particular risk level.
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years to 1 million years, as required by
the EnPA.
The Agency believes it important to
emphasize two aspects of this decision.
First, modeling of a complex system
such as the Yucca Mountain disposal
system over such time frames involves
significant uncertainties in both the
knowledge of characteristics of the site
and the conceptual representation of the
processes contributing to release and
transport of radionuclides. The NAS
recommendation has extended the
application of regulatory judgment
beyond the period when substantially
complete containment might reasonably
be provided, and through a period
during which complete loss of
containment cannot be discounted. The
sequence and timing of scenarios
resulting in waste package failure are
highly dependent on initial assumptions
and are the most significant factors in
estimating the timing and magnitude of
doses to the RMEI. Dose projections
involve extrapolation of assumptions,
models, and data over time periods
much longer than those considered in
other regulatory contexts. Such
projections therefore cannot be
confirmed in the usual sense (i.e.,
through measurements or monitoring),
nor is it expected that long-term
maintenance of the repository will be
performed. Such considerations lead us
to conclude that it would not be realistic
to demand that projections from such
complex systems be readily
distinguishable from one another at the
level of incremental risk customarily
addressed by the Agency in situations
where results can be confirmed,
modeling is utilized on a more limited
scale, or institutional controls are more
applicable.
The Agency’s second concern is the
correlation of risk with health
detriment. NAS specifically framed its
recommendation to establish a risk
standard in the context of health effects.
(NAS Report pp. 4 and 65) In doing so,
it explicitly extended the traditional
reliance on ‘‘present knowledge’’ in the
framing of performance assessments to
assume that future societies would not
have eliminated radiation cancer
risks.19 (NAS Report p. 100) However,
19 Dose can be converted to risk by use of either
radionuclide-specific or overall conversion factors.
The NAS committee referred only to overall
conversions (i.e., risk per rem), which is the typical
approach applied to dose standards when the
specific mix of radionuclides is not well-defined in
advance. The committee saw the direct use of risk
as an advantage if the relationship should change
in the future through new research on low-dose
health effects, because the underlying risk could be
viewed as representing the level of societal
acceptance of health impacts, which the committee
saw as less likely to change, whereas dose could
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the reliance on risk to express the
results of long-term safety assessments
has been approached more cautiously,
and it has primarily been viewed as a
mechanism to incorporate the
likelihood of scenarios affecting
potential exposures, rather than as a
direct measure of health impacts or as
a firm compliance criterion.20
Risk correlations are highly
dependent on population characteristics
and baseline cancer rates, which change
over time with dietary, lifestyle,
medical, industrial, environmental,
demographic, and other contributing
factors. ICRP has expressed caution that
‘‘[d]oses and risks, as measures of health
detriment, cannot be forecast with any
certainty for periods beyond around
several hundreds of years into the future
* * * Such estimates must not be
regarded as predictions of future health
detriment.’’ However, ICRP has also
suggested that it is not unreasonable for
shorter-term assessments to relate dose
or risk to health effects: ‘‘To evaluate the
performance of waste disposal systems
over long time scales, one approach is
the consideration of quantitative
estimates of dose or risk on the order of
1000 to 10,000 years. This approach
focuses on that period when the
calculation of doses most directly
relates to health detriment * * *’’ (ICRP
Publication 81, ‘‘Radiation Protection
Recommendations as Applied to the
Disposal of Long-Lived Radioactive
Waste,’’ Docket No. EPA–HQ–OAR–
2005–0083–0417, Paragraphs 41 and 71,
respectively) Thus, the Agency finds
become further removed from this level of societal
acceptance. (NAS Report p. 64) In fact, we use a
conversion factor slightly higher than that cited by
the NAS committee (5.75 × 10¥4 fatal cancers per
rem, compared to the committee’s figure of 5 × 10¥4
per rem). See 66 FR 32080–32081, for more
discussion of health risks from ionizing radiation.
20 For example, a 2007 NEA document on
‘‘Consideration of Timescales in Post-Closure Safety
of Geological Disposal of Radioactive Waste’’ (NEA/
RWMC/IGSC/(2006)3), which was based on surveys
of Member Countries, points out that ‘‘In evaluating
compliance with regulatory criteria, or in
formulating these criteria, extreme scenarios or
parameter distributions can generally be assigned
less weight. This is, for example, inherent in criteria
expressed in terms of risk.’’ (Docket No. EPA–HQ–
OAR–2005–0083–0411, p. 38) Similarly, the UK
Environment Agency has stated: ‘‘In the 1995 White
Paper, the Government stated that reliance cannot
be placed exclusively on estimates of risk to
determine whether the facility is safe. Whilst such
calculations can inform a judgement on the safety
of the facility, other technical factors, including
some of a more qualitative nature, will also need
to be considered. The Government therefore
considers it inappropriate to rely on a specified risk
limit or risk constraint as an acceptance criterion
for a disposal facility after control is withdrawn. It
is, however, considered appropriate to apply a risk
target in the design process.’’ (Guidelines for
Authorisation of Disposal Facilities for Low- and
Intermediate-Level Radioactive Waste, Docket No.
EPA–HQ–OAR–2005–0083–0063, Paragraph 6.14)
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that its requirements for the
probabilistic calculation of doses
effectively incorporates the issue of risk
as it has customarily been considered in
long-term safety assessments. Further,
the Agency believes its decision to view
the 10,000-year standard within its
traditional risk-management framework
is reasonable and consistent with views
on shorter-term safety assessments.
The nominal annual risk level for fatal
cancer associated with the 100 mrem/yr
dose standard is 5.75 × 10¥5. This is
comparable to the range of risks
represented by national and
international regulations identified by
NAS for EPA to consider, and is
premised on a dose level the NAS has
addressed favorably as a matter of
international regulatory consensus (NAS
Report pp. 40–41, Tables 2–3 and 2–4).
Considering that this standard will
apply for up to 1 million years, we
believe this represents a level of risk
that will protect public health and
safety in the far future. However, for the
reasons described above, we do not
believe it is appropriate to view the
standard through a strict risk
perspective, and caution against doing
so. Further, even if the risk correlations
could be assumed valid over such times,
the nominal risk represented by
projected doses may be a reflection of
the uncertainties inherent in such
projections, and therefore overstated.
ICRP states, for example, that ‘‘as the
time frame increases, some allowance
should be made for assessed dose or risk
exceeding the dose or risk constraint
* * * This must not be misinterpreted
as a reduction in the protection of future
generations, and, hence, as a
contradiction of the principle of equity
of protection, but rather as an adequate
consideration of the uncertainties
associated with the calculated results.’’
(ICRP Publication 81, Docket No. EPA–
HQ–OAR–2005–0083–0417, Paragraph
77).
As a result of these considerations, for
a standard covering periods up to 1
million years, the Agency believes it is
more appropriate to view protectiveness
from a broader perspective. This
perspective must include consideration
of the modeling issues discussed earlier,
as well as be cognizant of the regulatory
context in which dose projections will
be presented. NRC’s judgment of
‘‘reasonable expectation’’ will not rely
on a simple comparison of the mean
projected dose with the regulatory
standard, but will encompass the data,
assumptions, and models underlying
those projections, including the sources
and treatment of uncertainties and
conservatisms. We are also mindful that
the post-10,000-year peak dose standard
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covers an extremely wide time window,
far beyond that for any previous
regulatory situation in this country, and
that a peak mean dose could be
projected to occur at any point within
that time span. Where the precision and
predictive capabilities of performance
assessment models diminish over such
long times, we believe it is appropriate
that NRC ‘‘weigh how the scientific
basis for analysis changes with time’’ in
reaching its judgment (NAS Report pp.
30–31).
In that context, the 100 mrem/yr
public dose limit recommended by ICRP
and widely adopted by national and
international organizations and
government agencies represents a key
element of radiation protection practice
that can be applied to the estimation of
potential future exposures. It provides a
standard for public protection today
and, by extension in the far future. This
judgment reflects our view that the
selected level must take into account
larger, less quantifiable factors such as
the uncertainties involved in projecting
doses over 1 million years and the
meaning that can be assigned to such
projections (both in terms of their value
as predictions of expected behavior of
the disposal system and in their
correlation with health effects), as well
as the relative importance they should
assume, in a regulatory context. Having
considered these factors, we conclude
that the post-10,000-year dose standard
of 100 mrem/yr is protective of the
RMEI. It must also be emphasized that
the 100 mrem/yr level applies to the
RMEI, who is described as a person
whose location, lifestyle, and
characteristics cause that person to be
subject to doses at the high end of the
local population. As a result, the RMEI
is among the most highly exposed
members of the public. Most residents
in the vicinity of Yucca Mountain
would receive much lower doses from
the disposal system than the RMEI, if
any dose at all.
Taken together, the dual standards
provide a reasonable test of the disposal
system that appropriately combines
protectiveness with recognition of the
limitations of modeling in predicting
the evolution of that system over
hundreds of thousands of years. The
10,000-year standard is solidly
grounded in the Agency’s riskmanagement framework and prior
practice for geologic disposal facilities.
The longer-term peak dose standard is
widely-accepted domestically and
internationally as protective of public
health and safety, reasonable in its
recognition of the regulatory context,
and fulfills our EnPA mandate by
extending to the time of peak dose up
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to 1 million years. However, the Agency
also emphasizes the site-specific nature
of this rulemaking, which should not be
viewed as a precedent for other
regulatory situations, but as a reasoned
response to unique circumstances
involving issuance of a compliance
standard applicable for periods up to 1
million years after disposal.
4. How Did We Consider Uncertainty
and Reasonable Expectation?
In establishing our final standards
pursuant to the EnPA, we have
considered two important statements
from the NAS committee: (1) ‘‘We
recognize that there are significant
uncertainties in the supporting
calculations and that the uncertainties
increase as the time at which peak risk
occurs increases’’ and (2) ‘‘No analysis
of compliance will ever constitute an
absolute proof; the objective instead is
a reasonable level of confidence in
analyses that indicates whether limits
established by the standard will be
exceeded.’’ (NAS Report pp. 56 and 71,
respectively) We have been mindful of
these statements, as well as the fact that
NAS deferred to our judgment in setting
the level of the final compliance
standard, as indicating that there are
limits to the ability of science to provide
definitive answers. ‘‘When all
reasonable steps have been taken to
reduce technical uncertainty * * *
there still remains a residual,
unquantifiable uncertainty * * * The
only defense against it is to rely on
informed judgment.’’ (NAS Report p. 80)
We believe we have appropriately
considered the NAS views in
establishing 1 mSv/yr (100 mrem/yr) as
the individual-protection standard for
the period beyond 10,000 years and up
to 1 million years. In order to approve
DOE’s license application, NRC must
determine, at a minimum, that there is
a reasonable expectation that standard
will be met (as well as determine
compliance with other NRC
requirements, such as a multiple-barrier
system). The primary indicator of
compliance with the individualprotection standard is the mean of the
distribution of projected doses
presented by DOE (see Section III.A.9 of
this document, ‘‘How Will NRC
Determine Compliance?’’). However,
NRC’s compliance determination will
consist of more than a simple
comparison of the mean of projected
doses with the dose standard. Rather, as
stated in 40 CFR 197.14, NRC will reach
its determination ‘‘based upon the full
record before it.’’ Regardless of whether
the mean of projected doses is well
below the dose standard or not, NRC
will examine the assumptions, data,
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models, and other aspects of DOE’s
projections to ensure that it has an
understanding of those projections
sufficient to reach a ‘‘reasonable
expectation’’ as to their compliance
with the standard (40 CFR 197.13).
While applying the principles of
reasonable expectation at all times, NRC
may also use its judgment as to whether
it would apply the concept in exactly
the same way for times as long as 1
million years as it would for much
shorter times. A key element of
reasonable expectation is that it
‘‘accounts for the inherently greater
uncertainties in making long-term
projections of the performance of the
Yucca Mountain disposal system’’
(§ 197.14(b)), we would consider it
logical as well as practical for NRC, in
reaching its compliance decision, to
evaluate the sources and effects of
uncertainties in DOE’s analyses, as well
as DOE’s treatment of them.21
Uncertainties can influence
performance assessments in a number of
ways. Some sources of uncertainty can
be addressed, or at least accounted for,
while in other areas our knowledge may
be too limited to even characterize the
uncertainty, much less explicitly
account for it. Sources of uncertainty are
often discussed in broad categories such
as ‘‘data’’ or ‘‘model’’ uncertainty,
although these can take on various
forms within those broader categories
that create individual challenges.22
NAS supported the use of
probabilistic modeling as one way to
address the effects of uncertainty.
However, NAS noted that this process
itself can involve significant
uncertainties in defining the parameter
value distributions from which the
probabilistic selections would be made.
(NAS Report pp. 78–79) As a result,
interpretation of probabilistic results,
which illustrate uncertainty through the
distribution of calculated values, may
21 ICRP Publication 81: ‘‘Demonstration of
compliance with the radiological criteria is not as
simple as a straightforward comparison of
calculated dose or risk with the constraints, but
requires a certain latitude of judgement.’’ (Docket
No. EPA–HQ–OAR–2005–0083–0417, Paragraph 86)
22 For example, ‘‘data’’ uncertainty can cover
broad issues such as whether sufficient data are
available, whether the right kind of data are
available, whether the data are of sufficient quality,
and whether the available data adequately capture
what NAS referred to as ‘‘the difficulties in spatial
interpolation of site characteristics’’ which ‘‘will be
present at all times’’ (NAS Report p. 72). Similarly,
‘‘model’’ uncertainty includes not only whether the
processes acting on the site have been correctly
represented mathematically and coupled with each
other, but also whether the basic understanding of
which processes operate, whether there are
competing mechanisms that must be considered
(e.g., for corrosion or ground-water flow), and the
extent to which and conditions under which one
mechanism is dominant.
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also be affected by this underlying
uncertainty, which may not be fully
appreciated or understood.
Selecting an appropriate dose limit for
periods up to 1 million years must also
consider the ability of performance
assessments, and those who interpret
them, to distinguish between differing
repository designs, as well as different
conceptualizations of total system
performance over very long time frames.
We have described the general view that
the predictive capabilities of
performance assessments diminish as
the time periods covered by the
assessments increase. It is also
important to understand that, while
mathematical calculations can result in
very precise estimates of dose (to
multiple significant digits), this
precision is misleading in its
presentation of the approximate
outcomes of multiple interacting
processes. We believe it is not
appropriate to imply that there is a clear
and immutable difference between two
projections of dose, when it is
understood that neither on its own is an
unqualified representation of reality.
Such representations may promise more
than can be delivered by the model’s
ability to ‘‘slice it thin.’’ 23 In our view,
it makes little sense to assert that a 15
mrem/yr dose limit for the period
within 10,000 years is more
‘‘protective’’ than a higher limit much
later in time if, in the time frame of
hundreds of thousands of years, the
uncertainties in projecting disposal
system performance cannot easily make
23 This problem is not specific to quantitative
performance assessment. Similar issues have been
identified in analysis of different policy options for
energy or other areas associated with technological
risk. It has been noted that ‘‘The results of
individual risk assessment studies are often
reported with formidable precision, expressed as
discrete numbers (rather than ranges) and presented
to two, three and even four significant figures. Yet
* * * such precision seems entirely to
misrepresent the accuracy of this style of appraisal
taken as a whole * * * the problem does not tend
to be driven by any single factor in analysis, nor is
it a simple matter of some studies being more
‘accurate’ or ‘reasonable’ than others in any
definitive sense. The manifest variability * * * is
rather a simple reflection of * * * the adoption of
different (but equally scientifically valid)
assumptions and priorities concerning the
multitude of different dimensions of risk. Where
[different options cannot be clearly distinguished]
in any absolute sense, then the value of appraisal
lies in exposing the relationships between different
assumptions in analysis and the associate pictures
of the relative importance of different options. It is
better to be roughly accurate in this task of mapping
the social and methodological contextdependencies than it is to be precisely wrong in
spurious aspirations to a one-dimensional
quantitative expression of technological risk.’’ (‘‘On
Science and Precaution in the Management of
Technological Risk,’’ Volume 1, Institute for
Prospective Technical Studies, 1999, Docket No.
EPA–HQ–OAR–2005–0083–0413, pp 13–16,
emphasis in original)
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distinctions at such incremental
levels.24
In responding to comments on this
issue, we considered how it might be
possible to demonstrate the increase in
projected uncertainties and provide a
quantitative estimate of the degree of
increased uncertainty that might be
encountered as a result of variation in
parameter values. To examine the longterm propagation of uncertainty in dose
projections, we used a simplified Yucca
Mountain site performance assessment
model and constructed a hypothetical
disposal system that would produce a
mean dose to the RMEI of 15 mrem/yr
at 10,000 years. That is, we estimated
the number of waste package failures
that would be necessary to produce a
disposal system operating at the ‘‘edge
of compliance’’ at 10,000 years. This
disposal system, which would still meet
the performance standard at 10,000
years, was the reference base case for
our uncertainty analyses. The number of
‘‘failed’’ waste packages needed to
produce the reference case dose (a mean
of 15 mrem/yr at 10,000 years) was
calculated using the simplified site
model and parameters used in the DOE
model, and assumed some components
of the engineered barrier did not
function to provide containment (i.e.,
the titanium drip shields designed to
divert water from the waste packages, as
well as other components of the
engineered barrier system, were
removed from the model).25 Further,
upon ‘‘failure’’ of a waste package, the
entire inventory of that package was
assumed to be available for dissolution
and transport, subject to solubility
limits applied to each radionuclide.
To assess the progressive effects of
uncertainty, the number of ‘‘failed’’
packages was limited to the number
necessary to produce 15 mrem/yr at
10,000 years, and the hypothetical site
24 One might compare this situation to finding
two proximate, but distinct, locations on a road
map. In the first instance, the scale on the map is
such that all individual roads and landmarks (e.g.,
schools, churches, libraries) can be seen. One can
easily locate each site and circle it. Now consider
a map of the same size, in which the scale is much
smaller, showing only major thoroughfares and
main local roads. One would still be able to
approximate the desired location(s), but any
attempt to circle them would likely encompass both
(and may be deliberately larger to ensure that both
are captured). Thus, the ability to distinguish the
two locations hinges on the scale and detail of the
map in question. The change in ‘‘scale’’ for our
rulemaking is the extension of the compliance
period to 1 million years.
25 Although it employed site parameter value
distributions used by DOE, the model used in this
analysis was simplified and ‘‘forced’’ to the
boundary condition of a 15 mrem/yr mean dose at
10,000 years. This analysis should in no way be
compared to the modeling conducted to support
DOE’s license application.
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model was used to make dose
projections from 10,000 years (the
reference base case) through the period
of peak dose within the period of
geologic stability. Thus, the system
established as a starting point for the
peak dose projections was one in which
some degree of release and transport to
the RMEI had already taken place
within the initial 10,000 years,
providing a basis for judging how the
continuation of these processes would
change the results over time. These
analyses examined the effects of
uncertainties from the natural barrier
portion of the disposal system, since
additional waste package failures were
not considered.26 It should be
recognized that the base case was
determined using probabilistic methods,
so the results at 10,000 years already
showed some effects of uncertainty, as
indicated by the range of projected
doses with the mean at 15 mrem/yr.
We found that the uncertainty in dose
projections, from the base case (at
10,000 years) to peak dose (as measured
by the spread in dose estimates between
the 5th and 95th percentiles at these
times), increased by approximately two
orders of magnitude. These results
showed quantitatively that uncertainty
in performance projections does
increase with time for the Yucca
Mountain system, and supports the
premise that increasing uncertainty
reduces the degree of confidence that
can be assumed for very long-term
performance assessments. We believe
this supports the premise, discussed
earlier, that increasing uncertainty in
dose projections over very long time
periods lessens the ability of
performance assessment modeling to
meaningfully distinguish among
alternative (and equally ‘‘likely’’)
‘‘futures’’ represented by individual
model simulations, and ultimately to
distinguish among alternate models and
assumptions for site performance
assessments. More detail on the site
model we used, parameter databases,
sensitivity analyses and discussion of
the results, is provided in the technical
reports describing this work (Docket No.
EPA–HQ–OAR–2005–0083–0386).
NRC must reach a determination of
compliance based on the specific case
presented by DOE. In order to conclude
that there is a reasonable expectation
that the Yucca Mountain disposal
system will comply with our standard of
100 mrem/yr, NRC must understand the
technical basis for DOE’s projections,
26 We considered release of radionuclides from
the waste form as a natural process dependent on
solubility parameters. The waste form itself (spent
fuel assemblies or vitrified HLW) is often
considered part of the engineered barrier system.
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including the inherent uncertainties. We
believe it is appropriate for NRC to
examine uncertainty in its licensing
review in order to achieve the necessary
level of confidence in DOE’s
understanding and depiction of the
disposal system. Ultimately, in reaching
its compliance determination, it is
incumbent upon NRC to clearly state
what it can or cannot conclude from the
performance assessment results, within
the limits of science.
5. How Did We Consider Background
Radiation In Developing the Peak Dose
Standard?
We are not adopting the proposed 3.5
mSv/yr (350 mrem/yr) level as the
compliance standard for the period
beyond 10,000 years, nor have we
adopted the reasoning used to support
the proposed standard (i.e.,
considerations of specific background
radiation estimates) to the selection of
the 100 mrem/yr level. We received
significant comment on this aspect of
our proposal, much of it taking issue
with the concept of using background
radiation as an indicator of ‘‘safe’’ levels
of exposure from an engineered facility.
We also received additional information
that provided insights into and refined
our consideration of background
radiation. For example, commenters
referred to monitoring data collected by
the Desert Research Institute indicating
that the unshielded (outdoor)
background radiation from cosmic and
terrestrial sources in Amargosa Valley is
roughly 110 mrem/yr. Commenters also
informed us that roughly 90% of the
population in Amargosa Valley lives in
mobile homes, which has implications
for indoor radon exposures. Other
commenters supported the use of a
different factor for converting radon
concentrations into dose.
In considering these comments, as
well as those taking issue with the
overall premise described in the
proposal, we found the relatively simple
approach used in the proposal evolving
into a more complex undertaking
requiring numerous decisions where
science did not provide a definitive
answer. Addressing indoor radon
estimates presented the greatest
challenge, as indoor radon represented
the highest proportion of overall
background radiation. Complicating
factors included multiple ways of
calculating radon dose, the prevalence
of mobile homes in Amargosa Valley,
limited data sets primarily from the
early 1990s, and data for individual
counties in a different format than statewide data. We concluded that there was
no generally agreed-upon approach in
the context of Amargosa Valley for
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incorporating indoor radon exposures
into an analysis of background radiation
that would lead to a regulatory standard,
particularly given the fact that many
commenters viewed the entire concept
as arbitrary. Accordingly, we have
decided not to adopt a standard derived
from an analysis of background
radiation estimates at specific locations
or the differences between background
radiation estimates at different
locations.
We continue to believe that references
to natural sources of radiation can
provide useful insights. IAEA has
observed that ‘‘[i]n very long time
frames * * * uncertainties could
become much larger and calculated
doses may exceed the dose constraint.
Comparison of the doses with doses
from naturally occurring radionuclides
may provide a useful indication of the
significance of such cases’’. (IAEA WS–
R–4, Docket No. EPA–HQ–OAR–2005–
0083–0383, Paragraph A.8) We note that
the 100 mrem/yr level reasonably
comports with such an analysis as well.
For example, as noted above, 100 mrem/
yr is roughly the value reported by the
Desert Research Institute for cosmic and
terrestrial radiation at Amargosa Valley
(unshielded). When shielding from
buildings is considered and indoor
radon doses are estimated using a more
conservative conversion factor
suggested by some commenters, 100
mrem/yr is at the low end of overall
background radiation estimates in
Amargosa Valley and nationally. Within
the State of Nevada, the difference in
average estimates of background
radiation for counties is greater than 100
mrem/yr. (Docket No. EPA–HQ–OAR–
2005–0083–0387) As previously stated,
this suggests that 100 mrem/yr can be
considered to be a level such that the
total potential doses incurred by the
RMEI from the combination of
background radiation and releases from
Yucca Mountain will remain below
doses incurred by residents of other
parts of the country from natural
sources alone.27 It may also be noted
that the 100 mrem/yr public dose limit
recommended by ICRP is itself related
to background radiation, so indirectly
our peak dose standard does incorporate
the concept of variations in background
27 It could also be considered consistent with the
NEA statement that ‘‘[w]hat can be aimed at,
however, is to leave future generations an
environment that is protected to a degree acceptable
to our own generation. It is also relevant to observe
that this level of protection will ensure that any
radiological impacts due to disposal will not raise
levels of radiation above the range that typically
occurs naturally.’’ (‘‘The Handling of Timescales in
Assessing Post-Closure Safety: Lessons Learnt from
the April 2002 Workshop in Paris, France,’’ p. 9,
Docket No. EPA–HQ–OAR–2005–0083–0046)
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radiation.28 However, in the absence of
compelling reasons for selecting specific
background radiation estimates and
points of comparison, we conclude that
comparing background radiation
estimates from specific locations does
not provide a clear or sufficient basis for
a regulatory compliance standard
applicable to the Yucca Mountain
disposal system. Discussion of specific
issues raised in public comments is in
Section 3 of the Response to Comments
document.
6. How Does Our Rule Protect Future
Generations?
Because of its long lifetime, high
hazard, and potential for misuse, SNF
and HLW present special challenges to
those charged with protecting the
health, safety, and security of the public
and the environment. Geologic disposal
has long been viewed by policymakers
as the management option that best
addresses all of these concerns.29 In the
United States, geologic disposal was
first endorsed by the NAS in 1957 (‘‘The
Disposal of Radioactive Waste on
Land’’) and established as national
policy in the Nuclear Waste Policy Act
of 1982.
However, the fact that geologic
disposal has potentially significant
28 ‘‘This natural background may not be harmless
* * * but the variations from place to place
(excluding the large variations in the dose from
radon in dwellings) can hardly be called
unacceptable * * * Excluding the very variable
exposures to radon, the annual effective dose from
natural sources is about 1 mSv, with values at high
altitudes above sea level and in some geological
areas of at least twice this. On the basis of all these
considerations, the Commission recommends an
annual limit on effective dose of 1 mSv.’’ (ICRP
Publication 60, Docket No. EPA–HQ–OAR–2005–
0083–0421, Paragraphs 190–191)
29 In its 1995 Collective Opinion, the NEA
Radioactive Waste Management Committee
concludes that ‘‘from an ethical standpoint,
including long-term safety considerations, our
responsibilities to future generations are better
discharged by a strategy of final disposal than by
reliance on stores which require surveillance,
bequeath long-term responsibilities of care, and
may in due course be neglected by future societies
whose structural stability should not be presumed’’
and ‘‘after consideration of the options for
achieving the required degree of isolation of such
wastes from the biosphere, geological disposal is
currently the most favoured strategy,’’ whereby ‘‘it
is justified, both environmentally and ethically, to
continue development of geological repositories for
those long-lived radioactive wastes which should
be isolated from the biosphere for more than a few
hundred years.’’ (‘‘The Environmental and Ethical
Basis of Geological Disposal of Long-Lived
Radioactive Wastes,’’ Docket No. EPA–HQ–OAR–
2005–0083–0412, pp. 5–6) Similarly, the NAS
Board on Radioactive Waste Management stated:
‘‘There is a strong worldwide consensus that the
best, safest long-term option for dealing with HLW
is geological isolation.’’ (‘‘Rethinking High-Level
Radioactive Waste Disposal: A Position Statement
of the Board on Radioactive Waste Management,’’
1990, Docket No. EPA–HQ–OAR–2005–0083–0420,
p. 2)
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impacts over times far in excess of
recorded human history naturally raises
concerns as to how the welfare of
people living far in the future can and
should be taken into account when
societal institutions may no longer exist
to provide oversight of a disposal
facility.30
In considering how our standards
reflect these intergenerational issues, we
considered the guidance offered by the
NAS committee. (See 70 FR 49036) In
citing NRC and IAEA sources on the
question of intergenerational equity,
NAS wrote:
A health-based risk standard could be
specified to apply uniformly over time and
generations. Such an approach would be
consistent with the principle of
intergenerational equity that requires that the
risks to future generations be no greater than
the risks that would be accepted today.
Whether to adopt this or some other
expression of the principle of
intergenerational equity is a matter for social
judgment.
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NAS Report pp. 56–57, emphasis added.
We generally agree with the NAS
statement. A single dose standard
applicable at all times would typically
be consistent with a close reading of the
principle of intergenerational equity as
stated by NAS. However, NAS clearly
acknowledges that ‘‘some other’’
approach could also be consistent with
that principle. We believe it is
reasonable to conclude that ‘‘some
other’’ approach must include situations
where it may not be reasonable to apply
the same dose standard at all times
because of the extremely long
compliance period. We believe
establishing a peak dose standard for the
Yucca Mountain disposal system is a
situation in which ‘‘some other
expression of intergenerational equity’’
is more appropriate than is applying a
single dose standard of 15 mrem/yr
throughout the compliance period. The
rulemaking process we are following is
the accepted way for ‘‘social judgment’’
to be incorporated into regulations.
NAS made no recommendation
regarding the appropriate expression of
intergenerational equity, just as it made
no recommendation regarding the level
30 NEA states: ‘‘The design and implementation of
a repository involves balancing of risks and
responsibilities between generations. The
obligations of the present generation toward the
future are complex, involving not only issues of
safety and protection but also of freedom of choice
and of the accompanying burden of responsibility,
and of the need to transfer knowledge and
resources. Our capacity to deliver these obligations
diminishes with distance in time, which
complicates the setting of criteria to be used today
in order to demonstrate that obligations to the
future will be met.’’ NEA–6182, Docket No. EPA–
HQ–OAR–2005–0083–0408, p. 25)
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of the final peak compliance standard.
Rather, NAS acknowledged EPA’s wide
latitude to exercise its policy judgment.
We emphasize that we do not
question whether there is an obligation
to future generations, but we believe
there is no consensus regarding the
nature of that obligation, for how long
it applies, whether it changes over time,
or how it can be discharged. Regarding
radioactive waste management and
geologic disposal, there is general
agreement that assurances can be
provided that the protections offered
will be similar to those applied to
current activities for periods
approximating 10,000 years, which is a
very long time. It also is generally
accepted that engineered barriers cannot
be relied upon indefinitely, and that
projected doses may eventually exceed
the initial regulatory levels. The
question of equity is also raised by the
fact that the repository is part of a
passive disposal system that may
provide complete containment for
hundreds of generations without their
knowledge, but present the greatest risks
to equally unsuspecting generations
beyond that time. However, it is unclear
as to exactly how such long-term
projected doses should be factored into
a judgment of facility safety, if we are
not confident they can be interpreted in
the same way at all times.31 We are
establishing today a standard consistent
with a public dose limit of 100 mrem/
yr that is deemed protective today as a
matter of international consensus,
which would not affect the quality of
life for future generations, even those
hundreds of thousands of years distant.
We believe this is a reasonable level of
commitment for such long times, given
the complexities of the situation and
what we see as our responsibility to
establish a level of compliance, not a
soft target or reference level that could
be exceeded for unspecified reasons and
by unspecified amounts.
In conclusion, EPA acknowledges and
remains committed to the principles of
intergenerational equity. However, we
do not interpret these principles as
requiring that the same compliance
standard must apply at all times. Such
an approach is overly simplistic in the
31 NEA–6182: ‘‘National programmes which have
already established such criteria have generally
found it possible to make cautious, but reasonable
assumptions to extend the use of radiological limits
already applied to contemporary activities for
several thousands of years. The greater challenge
lies in setting criteria for very long time frames,
extending to a million years and beyond, for which
safety analyses must account for high uncertainty
and for which the understanding of the needs and
impacts on future generations become increasingly
speculative.’’ (Docket No. EPA–HQ–OAR–2005–
0083–0408, pp. 20–21).
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circumstances and ignores the
complexities involved in establishing
radiological protection standards for
periods approaching 1 million years. We
believe that peak dose limits over such
periods should be viewed as
qualitatively different from limits
applied at earlier times; in other words,
the basis for judgment at different times
is not the same. As a matter of public
policy, a commitment to protect future
generations over the next 10,000 years at
levels consistent with standards applied
for the current generation, and to protect
more distant generations at levels
consistent with the overall public dose
limits deemed protective today and
adopted nationally and internationally,
protects public health and the
environment across generations in a
manner that comports with the objective
of intergenerational equity. Under this
approach, future generations will not
face undue burdens or the irreversible
loss of reasonable options arising from
a decision by the current generation to
pursue a policy of geologic disposal at
Yucca Mountain, nor will the
compliance demonstration demand
more than can be provided by scientific
analysis. The standards applicable to
both time frames are protective of public
health and safety and will offer
comparable, if not identical, protections
to the affected generations. See section
9 of the Response to Comments
document for more detailed discussion
of these issues.
7. What is Geologic Stability and Why
is it Important?
Underlying the NAS recommendation
to assess compliance at the time of
maximum risk is the concept of geologic
stability (i.e., peak dose should be
assessed ‘‘within the limits imposed by
the long-term stability of the geologic
environment,’’ NAS Report p. 2). NAS
viewed this as an important
consideration in assessing performance,
both analytically and in regulatory
review. Indeed, NAS discussed two
important kinds of uncertainty in
describing this concept, which are
spatial and temporal uncertainty. The
committee concluded that spatial
uncertainties will always exist no matter
what time frame is used for the
performance assessments. Temporal
uncertainties, on the other hand, will
vary over different time frames, and the
presence of such uncertainties indicates
the advisability of defining a ‘‘period of
geologic stability,’’ during which
performance projections can be made
with some degree of confidence. For
time periods where conditions at the
site would change dramatically in a
relatively short time, projections of site
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conditions would be highly speculative,
and consequently performance
assessments would have very limited if
any validity. It is important to
understand that ‘‘stable’’ in this context
is not synonymous with ‘‘static and
unchanging.’’ Rather, NAS recognized
that many ‘‘physical and geologic
processes’’ are characteristic of any site
and have the potential to affect
performance of the disposal system.
NAS concluded that these processes
could be evaluated as long as ‘‘the
geologic system is relatively stable and
varies in a boundable manner’’ (NAS
Report p. 9). Thus, the site itself could
be anticipated to change over time, but
in relatively narrow ways that can be
defined (‘‘bounded’’). Implicit in the
NAS recommendation is the idea that
the maximum risk might occur outside
the period of geologic stability, but
assessments performed at that time
would have little credibility and would
not be a legitimate basis for regulatory
decisions: ‘‘After the geologic
environment has changed, of course, the
scientific basis for performance
assessment is substantially eroded and
little useful information can be
developed.’’ (NAS Report p. 72)
NAS judged this period of ‘‘long-term
stability’’ to be ‘‘on the order of one
million years.’’ (NAS Report p. 2) We
describe in section III.A.8 (‘‘Why is the
Period of Geologic Stability 1 Million
Years?’’) the policy judgment on our
part to explicitly equate the period of
geologic stability with 1 million years.
More important, however, is to
understand the relationship among the
regulatory definition, the physical
reality of the site, and the performance
assessment models. In reaching its
conclusion, NAS considered
information available on the site
properties and the processes as they
currently operate. This provides a basis
for understanding how the site
functions today, but would not be
sufficient to project that understanding
for periods of millions of years into the
future. To do that, NAS also considered
information obtained through studies of
the geologic record at the site, to see if
evidence existed for times when
processes were either fundamentally
different or they operated at different
rates. This is similar to our
recommendation that DOE consider at
least the last two million years (the
Quaternary period) in characterizing
FEPs. In fact, examination of the
Quaternary geologic record is an
important component in understanding
the evolution of the geologic setting over
time. NAS expressed confidence that
neither the processes active at the site,
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nor the site itself, had changed in
fundamental ways over the Quaternary
Period and longer, and probably would
continue to behave much as it does
today for the next million years. NAS
therefore suggested that geologic
conditions could be bounded with
reasonable confidence for periods ‘‘on
the order of one million years.’’ (NAS
Report p. 2)
Models used to assess performance
need to incorporate a description of the
bounds under which the model can be
considered valid, so as to avoid
physically impossible situations, as well
as assure that the conceptual models
upon which the performance
assessments are based reasonably
represent the way the site is expected to
behave over the period of stability. They
must be defined so that significant
changes to the properties of the site and
physical and geologic processes are not
projected inadvertently to create
conditions of ‘‘geologic instability.’’
That is, they must avoid crossing over
into sets of conditions that would in
reality not be a geologically stable
situation, or are outside the bounds
under which the model can be
considered valid. Here again the
examination of the geologic record at
the site provides the means of
constructing the models to adequately
make simulations of future performance
that reflect the range of potential
expected conditions at the site over the
regulatory compliance period.
Parameter value distributions used in
the simulations, which are the
fundamental input information used to
make the dose assessments, should not
be limited only to data collected for the
present situation at the site, but should
consider how those parameter values
could change over the period of
stability. Expert judgment, where
appropriate, based upon site-specific
information and broader understanding
of how these processes operate in
general, plays an important role in
defining such modeling input data.
The geologic record is the primary
source of information on the question of
geologic stability and was considered by
NAS in reaching its conclusions about
the geologic stability period. We believe
that the geologic record at the site
clearly supports the position that the
site will be stable over the course of the
next million years. Conclusions based
on extrapolation beyond what can be
supported in the geologic record should
be avoided.
8. Why is the Period of Geologic
Stability 1 Million Years?
Today’s final rule includes a
compliance period of 1 million years,
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over which DOE must project
performance and demonstrate
compliance with the individualprotection and human-intrusion
standards. As discussed at length in our
proposal and more briefly in Sections I
and II of this document, our rulemaking
is in response to the DC Circuit decision
vacating the 10,000-year compliance
period in our 2001 rule. The Court
concluded that the 10,000-year
compliance period was not based upon
and consistent with the NAS
recommendations, as the EnPA
required. NAS recommended ‘‘that
compliance with the standard be
assessed at the time of peak risk,
whenever it occurs, within the limits
imposed by the long-term stability of the
geologic environment, which is on the
order of one million years.’’ (NAS
Report p. 2) NAS found that
‘‘compliance assessment is feasible for
most physical and geologic aspects of
repository performance on the time
scale of the long-term stability of the
fundamental geologic regime,’’ and
accordingly ‘‘there is no scientific basis
for limiting the time period of an
individual-risk standard.’’ (NAS Report
p. 6) As a matter of policy, we believe
it is appropriate and necessary to define
a compliance period within which our
standards apply. This section discusses
the considerations that led us to
conclude that a compliance period of 1
million years is appropriate from a
policy perspective and consistent with
NAS statements regarding geologic
stability at Yucca Mountain.
As discussed in section III.A.7 (‘‘What
is Geologic Stability and Why is it
Important?’’), the NAS introduced the
concept of geologic stability in its report
and referred to it repeatedly in its
discussions (NAS Report, e.g., pp. 9, 55,
69, 71, and 72). In discussing the
physical properties and geologic
processes leading to the transport of
radionuclides away from the repository,
the NAS committee concluded ‘‘that
these physical and geologic processes
are sufficiently quantifiable and the
related uncertainties sufficiently
boundable that the performance can be
assessed over time frames during which
the geologic system is relatively stable
or varies in a boundable manner.’’ (NAS
Report p. 9) While variation of site
characteristics over time produces some
uncertainty, NAS believed that such
changes could be bounded during the
period of geologic stability of the site,
i.e., as long as the conditions do not
change significantly. (NAS Report pp.
72, 77) NAS also noted that ‘‘[a]fter the
geologic environment has changed, of
course, the scientific basis for
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performance assessment is substantially
eroded and little useful information can
be developed.’’ (NAS Report p. 72)
While NAS made no additional
qualification on what constituted
‘‘significant’’ changes, it made
numerous references in its report to a
stability period for the site ‘‘on the order
of one million years.’’ The committee
concluded that during this period it
would be feasible to make projections of
repository site conditions. We concur
and believe that assessments can be
made and bounded where uncertainty
exists, and consequently performance
assessments can be developed with
adequate confidence for regulatory
decision-making within the context of
the requirements adopted in today’s
final rule. We discuss some additional
qualifications to this proposition in the
remainder of this section.
While the NAS characterized the
length of the geologic stability period in
loose terms (‘‘on the order of’’), we
believe it is appropriate to fix the
stability period duration as a matter of
regulatory policy. We find support on
this point from NAS: ‘‘It is important,
therefore, that the ‘rules’ for the
compliance assessment be established
in advance of the licensing process.’’
(NAS Report p. 73). We believe,
therefore, as a matter of regulatory
philosophy and policy, that a relatively
loosely defined stability period ‘‘on the
order of’’ one million years is not
sufficiently specific for regulatory
purposes, i.e., implementing our
standards and reaching a compliance
decision. Indeed, NAS clearly
considered that the compliance period
could be one of the ‘‘rules’’ that should
be established for compliance
assessments. (NAS Report p. 56) Some
commenters suggested that the period of
geologic stability could be longer (or
interpreted ‘‘on the order of one million
years’’ as possibly as long as ten million
years), and said our rule should allow
consideration of longer timescales if
justified by considerations of geologic
stability. The actual period of geologic
stability at Yucca Mountain is
unknowable, and we disagree that an
open-ended compliance standard is
justified over such time frames. We
believe that the applicant (DOE) and the
compliance decision-maker (NRC) must
have definitive markers to judge when
compliance is demonstrated, and that a
loosely defined time frame does not
provide such a marker for
implementation of our standards in a
licensing process. We believe that the
geologic stability period of 1 million
years that we have defined provides the
necessary marker, and is within our
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discretion to set as a matter of policy.
(See generally NAS Report p. 3) To do
otherwise we believe would leave the
licensing process in a potentially
untenable situation of dealing with
possibly endless debate over exactly
when a peak dose occurs in relation to
a compliance period time limit. Such
debate can arise because of the inherent
uncertainty that exists in characterizing
the complex processes and variables
involved in projecting performance of
the disposal system over very long
periods of time. As the NAS explained,
‘‘although the selection of a time period
of applicability has scientific elements,
it also has policy aspects we have not
addressed.’’ (NAS Report p. 56)
As commenters have pointed out, the
rate of waste package failure is a
dominant factor in determining when
the peak dose for a probabilistic
assessment will occur. With all the
parameters (and the uncertainty in their
values over time) involved in a total
system performance assessment, as well
as the assumptions necessary to select
processes involved in projecting
performance, it is quite possible that
significant debate could result in the
licensing process over selection of the
parameter values and the resulting
timing of the peak dose results. We do
not believe such debate is constructive
because it would not advance the goal
of providing a reasonable test of the
disposal system. We also believe that
the 1 million year stability period
provides the needed definitive marker
for judging the time over which the
standards apply and is an appropriate
exercise of our policy discretion.
Throughout our proposal and in this
final rule we have cited a significant
number of international references to
support policy judgments such as the
one discussed here. Readers may recall
that we cited such references suggesting
that dose projections beyond 1 million
years have little credibility and believe
that we used those arguments to justify
proposing the 1 million-year
compliance period (70 FR 49036,
August 22, 2005). We did not explicitly
discuss in the proposal our reasons for
selecting 1 million years as the
compliance period and equating it to the
period of geologic stability, other than
references to the NAS language that it is
‘‘on the order of’’ 1 million years.
However, these sources do generally
reflect widespread acceptance of the
proposition that quantitative
performance projections at very long
time frames have limited utility for
regulatory decision-making, and that 1
million years may be a reasonable
reference point beyond which such
projections either should not be
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required or should be considered only
in their broadest sense.32 Further, while
it should be clear that we agree with the
thrust of those international sources
regarding the effects of uncertainty on
long-term dose projections and the
relative level of confidence that can be
placed in them for decision-making, we
believe the post-10,000-year peak dose
standard in today’s final rule
appropriately accommodates those
considerations and is protective of
public health, meaningful,
implementable, and provides a
reasonable test of the disposal system
that is consistent with the NAS Report,
DC Circuit decision, and the principles
of reasonable expectation.
To support these general policy
arguments, which would lead us to
consider a time period of approximately
1 million years as an appropriate
regulatory time frame, it is necessary to
address NAS’s scientific judgments.
While NAS did not define with
precision the period of time that the
geologic environment likely would
remain stable, for purposes of our
regulation we believe scientific
information can be relied upon to
support a firm definition of that period
as ending at 1 million years after
disposal. Further, we believe that
equating a specific time period with the
‘‘period of geologic stability’’ is a sitespecific decision, as NAS’s statements
regarding geologic stability were wholly
in the context of Yucca Mountain. (See,
for example, NAS Report p. 69: ‘‘The
time scales of long term geologic
32 For example, in general guidance documents,
the IAEA has stated that ‘‘little credibility can be
attached to assessments beyond 106 years.’’ (‘‘Safety
Indicators in Different Time Frames for the Safety
Assessment of Underground Radioactive Waste
Repositories,’’ IAEA–TECDOC–767, p. 19, 1994,
Docket No. EPA–HQ–OAR–2005–0083–0044) In its
final 2006 Safety Requirements for Geological
Disposal of Radioactive Waste, IAEA also states,
‘‘Care needs to be exercised in using the criteria
beyond the time where the uncertainties become so
large that the criteria may no longer serve as a
reasonable basis for decision making.’’ (Docket No.
EPA–HQ–OAR–2005–0083–0383, page 11,
paragraph 2.12) As a country-specific example, final
guidelines from the Swedish Radiation Protection
Authority state that ‘‘the risk analysis should be
extended in time as long as it provides important
information about the possibility of improving the
protective capability of the repository, although at
the longest for a time period of one million years.’’
(Docket No. EPA–HQ–OAR–2005–0083–0388) Also,
in an example where the official guidelines specify
a risk target that is of undefined duration, the
United Kingdom’s National Radiological Protection
Board has stated that ‘‘[o]ne million years is * * *
the timescale over which stable geological
formations can be expected to remain relatively
unchanged,’’ while concluding that the scientific
basis for risk calculations past one million years is
‘‘highly questionable.’’ (‘‘Board Statement on
Radiological Protection Objectives for the Landbased Disposal of Solid Radioactive Wastes,’’ 1992
Documents of the NRPB, Volume 3, No. 3, p. 15,
Docket No. EPA–HQ–OAR–2005–0083–0416)
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processes at Yucca Mountain are on the
order of 106 years’’; and NAS Report p.
85: ‘‘The geologic record suggests this
time frame is on the order of about 106
years.’’) Therefore, we have considered
how the natural processes and
characteristics at the Yucca Mountain
site would support defining the period
of geologic stability as ending at a
specified time after disposal. In
considering the natural setting, many
comments expressed the view that the
site’s natural characteristics are so
conducive to rapid release and transport
of radionuclides, only the waste
packages and other engineered barriers
would make it possible for significant
doses to be delayed much beyond
10,000 years. We believe it is therefore
also appropriate to consider the geologic
stability period from the perspective of
a reasonable length of time for
significant events to act on the waste
packages and engineered barriers, and
ultimately lead to release of
radionuclides. Natural processes and
events would contribute to both the
package failures and to the subsequent
transport of radionuclides, even if such
failures occur relatively late in the
period under consideration.
A consideration of the geologic
history of the site, in the areas of
igneous and seismic activity, also
supports a 1 million year stability
period. Information compiled by NRC
(Docket No. EPA–HQ–OAR–2005–0083–
0373) concerning basaltic igneous
activity around the site shows that this
type of activity has been the only
activity around the site through the
Pliocene (beginning roughly 5.4 million
years ago), and that the volume of
eruptive activity (both tuff and basaltic
material) has decreased continually over
the last 10 million years (Coleman et al.,
2004, Docket No. EPA–HQ–OAR–2005–
0083–0378). From the identification of
surface features as well as indicators of
buried remnants of past volcanic
activity, the episodes of basaltic activity
around the site can be shown to have
occurred in clusters of events around 1
million and 4 million years ago (Hill,
2004, Docket No. EPA–HQ–OAR–2005–
0083–0373). The occurrence of these
clusters indicates that the nature and
extent of past volcanic activity can be
reasonably well characterized and that
annual probabilities for such events can
be reasonably estimated from the
geologic record around the site. Annual
probabilities of volcanic disruptions to
the repository have been estimated by
various investigators, and range from as
high as 10¥6 to as low as 5.4 × 10¥10
(Coleman et al., 2004, Docket No. EPA–
HQ–OAR–2005–0083–0378).
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Further, while geologic stability may
be viewed as being affected primarily by
large-scale events, accumulations of
small-scale changes over very long time
periods also have the potential to alter
the geologic setting and affect the
technical basis for performance
assessments. Tectonic events have such
a potential at Yucca Mountain. Rates of
displacement on the nearest potentially
significant fault in the region average
about 0.02 mm/yr. (DOE, Science &
Engineering Report, 2002, p. 4–409,
Docket No. EPA–HQ–OAR–2005–0083–
0069) This means that in 10,000 years,
there could be 20 cm (0.65 ft) of
displacement, a relatively small change
not likely to affect performance of the
geologic system. However, in 1 million
years, the same rate of movement results
in 20 m (65 ft) of displacement on the
fault. Using the larger estimates of
movement within the range of potential
movement, displacement could be as
much as 30 m (100 ft) over 1 million
years. Such changes in the geologic
setting at Yucca Mountain have the
potential to erode the scientific basis for
performance assessment and possibly to
affect the quality of the information the
assessment can provide to decisionmakers.
NAS also stated that ‘‘we see no
technical basis for limiting the period of
concern to a period that is short
compared to the time of peak risk or the
anticipated travel time.’’ (NAS Report p.
56) This statement suggests that the
stability period must be long enough to
allow FEPs that pass the probability and
significance screens to demonstrate
their effects, if any, on the results of the
performance assessments, even from
waste package failures occurring
relatively late in the period. In contrast
to the accumulated small-scale changes
discussed above, larger-scale seismic
events are more likely to contribute
directly to radionuclide releases through
the effects of ground motion. Strong
seismic events could damage waste
package integrity by causing
emplacement drift collapse or vigorous
shaking of the packages themselves.
Earthquake recurrence intervals for the
site indicate that strong events could
reasonably be assumed to test waste
package integrity at various times
within the 1 million-year period (Docket
No. EPA–HQ–OAR–2005–0083–0374
and 0379). In addition, we note that
estimates of ground water travel time
from the repository to the RMEI location
are on the order of thousands of years
(see the BID for the 2001 final rule,
Docket No. EPA–HQ–OAR–2005–0083–
0050). At these rates, the effects of
disruptive volcanic and seismic effects
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on releases would not be delayed from
reaching the RMEI location during the
stability period, e.g., added releases
from a low probability seismic event at
800,000 years would have ample time to
be captured by the performance
assessments. Based on these
considerations, the 1 million-year
period is a sufficiently long time frame
to evaluate the potential consequences
of both gradual processes and disruptive
events on disposal system performance.
In summary, for regulatory policy as
well as site-specific scientific
considerations, we believe that fixing
the period of geologic stability for
compliance assessments at 1 million
years provides a reasonable test for the
disposal system performance. We
believe a fixed time period is necessary
both to provide a definitive marker for
compliance decision-making and to
prevent unbounded speculation
surrounding the factors affecting
engineered barrier performance and the
ultimate timing of peak dose
projections. Examination of site
characteristics indicates that the
influences of natural processes and
events on release and transport of
radionuclides would be demonstrated
even for waste package failures
occurring relatively late in the period.
We believe that setting a 1 million year
limit is a cautious but reasonable
approach consistent with the NAS
position on bounding performance
assessments for uncertain elements
affecting disposal system performance.
Finally, explicitly defining the period
during which our standards apply will
focus attention on times for which the
geologic setting and associated
processes are more quantifiable and
boundable, rather than entering debate
on disposal system performance in time
periods where the fundamental geologic
regime may have sufficiently changed so
that the ‘‘scientific basis for
performance assessment is substantially
eroded and little useful information can
be developed.’’ (NAS Report p. 72)
9. How Will NRC Judge Compliance?
Today’s final rule directs NRC to use
the arithmetic mean of the distribution
of projected doses to determine
compliance with both the 150 µSv/yr
(15 mrem/yr) dose standard applicable
for the first 10,000 years after closure
and the 1 mSv/yr (100 mrem/yr) peak
dose standard applicable between
10,000 and 1 million years after closure.
In reaching this decision, we considered
comments raising legal, technical, and
policy points. Foremost among these
were comments focusing on a statement
by the NAS committee: ‘‘We
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recommend that the mean values of
calculations be the basis for comparison
with our recommended standards.’’
(NAS Report p. 123)
After considering public comments,
the NAS Report, and the DC Circuit
decision, we conclude that the use of
the arithmetic mean to determine
compliance at all times, without
conditions or restrictions, is
straightforward and clearly consistent
with the NAS recommendation,
pursuant to the EnPA. Consistent with
our proposal, we are specifying that the
‘‘mean’’ to be used is the arithmetic
mean, as this is consistent with the
intent of 40 CFR part 191 and its
implementation at WIPP. See section 7
of the Response to Comments document
for more discussion of the points raised
in public comments.
10. How Will DOE Calculate the Dose?
Today’s final rule requires DOE to
calculate the annual committed effective
dose equivalent (CEDE) for comparison
to the storage, individual-protection,
and human-intrusion standards using
the radiation- and organ-weighting
factors in ICRP Publication 60 (‘‘1990
Recommendations of the ICRP’’), rather
than those in ICRP Publication 26
(‘‘1977 Recommendations of the ICRP’’).
As we described in our proposal, this
action will incorporate updated
scientific factors necessary for the
calculation, but will not change the
underlying methodology. We explained
in some detail the use of the terms
‘‘effective dose equivalent’’ and
‘‘effective dose’’ in the EnPA, the DC
Circuit decision, the ICRP publications,
and our previous actions to support our
position that use of the weighting
factors in ICRP 60 (and its follow-on
implementing Publication 72) is
consistent with calculation of effective
dose equivalent, as required by the
EnPA. (70 FR 49046–49047)
We received some comment
disagreeing with our conclusion that use
of the term ‘‘effective dose equivalent’’
is consistent with the use of the ICRP 60
weighting factors. As we discussed in
our proposal, we believe a close reading
of ICRP 60 supports our interpretation
that effective dose equivalent and
effective dose are synonymous concepts.
ICRP defined two weighting factors in
ICRP 26, the radiation quality factor, Q,
and the tissue weighting factor, WT. In
ICRP 60, the quality factor was replaced
by the radiation weighting factor, WR,
with the same values assigned to alpha,
beta, and gamma radiation. In ICRP 26,
the tissue weighting factor was
presented as a rigid construct with
defined values for specific organs. In
ICRP 60, the tissue weighting factor was
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redefined as a set of recommended
values for an expanded set of organs
(which could be modified in cases
where scientific information was
available to support using alternative
factors), and it was explained that the
attributes of the tissue weighting factor
include the components of detriment
cited by the comments (fatal and nonfatal cancers, length of life lost, and
hereditary effects). However, ICRP made
a clear distinction between its renaming
of the doubly weighted dose quantity
from ‘‘effective dose equivalent’’ (ede) to
‘‘effective dose’’ (E) and its redefining of
WT. The association of effective dose
equivalent with the ICRP 26 tissue
weighting factors is thus coincidental
but not required. We cited ICRP to that
effect in our proposal:
The weighted equivalent dose (a doubly
weighted absorbed dose) has previously been
called the effective dose equivalent but this
name is unnecessarily cumbersome,
especially in more complex combinations
such as collective committed effective dose
equivalent. The Commission has now
decided to use the simpler name effective
dose, E. The introduction of the name
effective dose is associated with the change
to equivalent dose, but has no connection
with changes in the number or magnitude of
the tissue weighting factors * * *
ICRP Publication 60, p. 7, paragraph 27,
Docket No. EPA–HQ–OAR–2005–0083–
0421, emphasis added.
Similarly, ICRP also states:
The values of both the radiation and tissue
weighting factors depend on our current
knowledge of radiobiology and may change
from time to time. Indeed, new values are
adopted in these recommendations * * *. It
is appropriate to treat as additive the
weighted quantities used by the Commission
but assessed at different times, despite the
use of different values of weighting factors.
The Commission does not recommend that
any attempt be made to correct earlier values.
It is also appropriate to add values of dose
equivalent to equivalent dose and values of
effective dose equivalent to effective dose
without any adjustments.
ICRP Publication 60, p. 9, paragraph 31,
Docket No. EPA–HQ–OAR–2005–0083–
0421, emphases added.
In summary, we believe the intent of
Congress in specifying effective dose
equivalent is that the Yucca Mountain
standards be based on a doubly
weighted dose quantity, not that the
assessment of that quantity be tied to
factors developed at a particular time,
when newer science indicates those
factors should be updated. We use
effective dose equivalent for consistency
with the terminology used in the EnPA,
but are adopting in today’s final rule the
current recommended values for WT.
Our approach is thus fully consistent
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with both the current ICRP
recommendations and the EnPA.
Today’s final rule does incorporate a
change to the proposed definition of
‘‘effective dose equivalent’’ in § 197.2 to
make it consistent with language in
Appendix A regarding the potential use
of future ICRP recommendations. We
received some comments suggesting that
the appendix should not include
specific weighting factors, but state only
that doses are to be calculated in
accordance with the methods of ICRP
60/72. The commenter believes this is
appropriate because NRC’s proposed
licensing requirements included the
tissue weighting factors, but not the
radiation weighting factors. Further, the
commenter points out that dose
coefficients in ICRP 72 (and Federal
Guidance Report 13) consider a
somewhat different set of organs than do
the tissue weighting factors. We prefer
not to adopt the commenter’s
suggestion, which we believe could lead
to questions regarding the appropriate
factors to use. We note that ICRP 60,
unlike ICRP 26, is not tied to a specific
set of weighting factors, and allows for
the possibility that users will substitute
their own preferred set of factors.
Stating only that the methods of ICRP
60/72 be used to calculate dose, without
the additional stipulations in the
appendix, would not provide sufficient
clarity on this point. Therefore, we are
adding language to the definition in
§ 197.2 to the effect that NRC can direct
that other weighting factors be used to
calculate dose, consistent with the
conditions presented in Appendix A.
We believe this will effectively address
the commenter’s concern.
B. How Will This Final Rule Affect
DOE’s Performance Assessments?
Today’s final rule requires DOE to
demonstrate compliance with the
individual-protection standard through
use of performance assessment. A
performance assessment is developed by
first compiling lists of features
(characteristics of the disposal system,
including both natural and engineered
barriers), events (discrete and episodic
occurrences at the site), and processes
(continuing activity, gradual or more
rapid, and which may occur over
intervals of time) anticipated to be
active during the compliance period of
the disposal system. These items are
collectively referred to as ‘‘FEPs’’
(features, events, and processes). Once
FEPs are identified, they are evaluated
for their probability of occurrence (i.e.,
how likely they are to occur during the
compliance period) and their effect on
the results of the performance
assessment (i.e., do they significantly
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affect projected doses from the disposal
system during the first 10,000 years after
disposal). Addressing these aspects of
performance assessment for a
compliance period of 1 million years
was a central aspect of our proposal and
is the focus of this section.
After considering public comments,
we are retaining § 197.36 as proposed,
with two modifications. First, the
probability threshold for FEPs to be
considered for inclusion in performance
assessments conducted to show
compliance with § 197.20(a)(1) is now
stated as an annual probability of 1 in
100 million (10¥8 per year).33 Because
the same FEPs included in these
performance assessments will also be
included in performance assessments
conducted to show compliance with
§ 197.20(a)(2), the same probability
threshold applies in all cases. Second,
we are adding a provision to address a
potential effect of seismicity on
hydrology that was identified by NAS.
The final rule now requires the potential
effects of a rise in the ground-water
table as a result of seismicity to be
considered. If NRC determines such
effects to be significant to the results of
the performance assessment, it shall
specify the extent of the rise for DOE to
assess.
Our 2001 rule set forth three basic
criteria for evaluating FEPs for their
potential effects on site performance
and their incorporation into the
scenarios used for compliance
performance assessments (§ 197.36).
These criteria retained the same
limitations originally established in 40
CFR part 191, which were developed to
apply to any potential repository for
spent nuclear fuel, high-level waste, or
transuranic radioactive waste. We
believe that approach remains
reasonable for the site-specific Yucca
Mountain standards, and we believe it
is desirable to maintain consistency
between the two regulations for geologic
repositories in the basic criteria for
evaluating FEPs. The criteria for
evaluating FEPs are:
• A probability threshold below
which FEPs are considered ‘‘very
unlikely’’ and need not be included in
performance assessments;
• A provision allowing FEPs above
the probability threshold to be excluded
from the analyses if they would not
significantly change the results of
performance assessments; and
33 Only FEPs with an annual probability greater
than or equal to 10¥5 need to be considered in
performance assessments to show compliance with
§§ 197.25(b) and 197.30. FEPs below this
probability threshold, but still above 10¥8 per year,
are defined by NRC as ‘‘unlikely’’.
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• An additional stipulation that in
addition to ‘‘very unlikely’’ FEPs,
‘‘unlikely’’ FEPs need not be considered
in performance assessments conducted
to show compliance with the humanintrusion and ground-water protection
standards.
As an initial step, a wide-ranging set
of FEPs that potentially could affect
disposal system performance is
identified. The term ‘‘potentially’’ is key
here, because at this early stage, the list
is deliberately broad, focusing more on
‘‘what could happen’’ rather than ‘‘what
is likely to happen at Yucca Mountain.’’
Under the 2001 rule, each of these FEPs
is then examined to determine whether
it should be included in an assessment
of disposal system performance over a
10,000-year period by evaluating the
probability of occurrence at Yucca
Mountain and, as appropriate, the
effects of the FEP on the results of the
performance assessment. Based on these
evaluations, a FEP may be excluded
from the assessment of disposal system
performance on the basis of probability,
or if the results of the performance
assessments would not be changed
significantly by its exclusion.
We included in our proposal
provisions describing how FEPs should
be incorporated into assessments of
disposal system performance during the
period of geologic stability, defined as
ending at 1 million years after closure.
Our purpose was to build upon the
provisions applicable to the 10,000-year
compliance period in our 2001 rule to
address the complexities introduced by
extending the compliance period to 1
million years. In general, the database of
FEPs applicable to Yucca Mountain
should be the same, regardless of the
period covered by the assessments. In
developing our proposal, however, we
considered how these general
provisions might change when the
compliance period extends to 1 million
years. We also proposed specific
provisions to address climate change,
seismicity, and igneous events, which
were identified by NAS as potential
‘‘modifiers’’ whose effects could be
bounded within the period of geologic
stability.
Some commenters questioned
whether our authority to establish
public health protection standards for
Yucca Mountain extended to specifying
how FEPs must be considered,
contending that this function properly
lies with the implementing authority
(NRC). We disagree. While NRC clearly
has authority to specify such provisions,
it is also within our purview to stipulate
such conditions as are necessary to
place our regulations in context and
ensure they are implemented as we
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intended. For analyses covering 1
million years, it is important to focus on
those factors most affecting
performance, if necessary by excluding
other aspects that are more likely to
have little or no significance. We believe
this approach is consistent with the
direction from NAS. NAS was charged
with providing advice to EPA on
‘‘reasonable standards for protection of
public health and safety’’ (EnPA section
801(a)(2)). NAS provided its findings
and recommendations in the context of
standards to be developed by EPA,
including discussion of FEPs, for
example: ‘‘the radiological health risk
from volcanism can and should be
subject to the overall health risk
standard to be required for a repository
at Yucca Mountain.’’ (NAS Report p. 95)
Further, NAS discussed the question of
uncertainty in quantifying physical and
chemical processes and their operation
over long time periods and the
inevitability of ‘‘residual, unquantifiable
uncertainty,’’ stating ‘‘[t]he only defense
against it is to rely on informed
judgment.’’ (NAS Report p. 80)
Therefore, we believe it appropriate to
specify, where necessary, additional
provisions for the treatment of FEPs in
disposal system assessments to avoid
boundless speculation. We have
explained our understanding of the
proper use of bounding performance
scenarios, and we believe we are
consistent with the NAS on this point.
Bounding assessments addressing
uncertainty in understanding the longterm behavior of the site should be
constructed using informed judgment,
not speculative assumptions without
credible supporting evidence.
Two of the criteria for evaluating
FEPs, probability and significance of the
impacts on performance assessments,
are of primary importance in
considering how the provisions
applicable to the 10,000-year period
might change when the compliance
period is extended to 1 million years. In
the proposed rule, we concluded that
the 10,000-year FEPs screening could
serve as an adequate basis for longerterm assessments because it is
sufficiently inclusive to be appropriate
for the entire 1 million-year compliance
period, while at the same time
reasonably bounding the scenarios that
must be considered over the longer time
frame. We thought our statements in the
preamble on this point were sufficiently
clear, but we understand that the way
we structured § 197.36 of the proposal,
essentially separating the two time
periods, may have caused some
confusion. For example, we did not
intend to indicate or imply that the
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post-closure performance assessments
would consist of two separate and
dramatically different calculations, with
each having distinctly different scenario
construction, parameter value
distributions, or other attributes.
Regardless of the standard against
which compliance is being judged, the
probability of occurrence and the
significance of the impacts on
performance assessment are the two
primary criteria for including a FEP in
the compliance analysis. The screening
for FEPs is done for the 10,000-year
performance assessment and then used
with certain additions set forth in the
rule for the 1 million-year peak dose
performance assessment. The initial
screening provides a database of FEPs,
which is then used for both the 10,000year and post-10,000-year peak dose
analyses, with some additional
stipulations for the period beyond
10,000 years. The discussion that
follows addresses each of these
screening criteria in turn.
Probability
In the proposed standards, we defined
the probability threshold for ‘‘very
unlikely’’ FEPs as a 1 in 10,000 chance
of occurrence within 10,000 years, or
roughly a 1 in 100 million (10¥8)
chance per year of occurring. In today’s
final rule, the probability threshold is
now stated only as an annual
probability of 1 in 100 million (10¥8).
We believe it is appropriate to clarify
that FEPs have associated probabilities
of occurrence that generally do not
change over time. That is, the database
of FEPs deemed sufficiently probable
would serve equally well as the basis for
assessments covering 1,000, 10,000,
100,000, or 1 million years. These
probabilities of occurrence are
established by examining the geologic
record and considering potential
mechanisms for components of the
repository and its natural setting to
undergo changes. FEPs with a
probability of occurrence greater than 1
chance in 100 million per year should
be considered for inclusion in the
performance assessments to show
compliance with the 10,000-year
individual-protection standard, and the
same FEPs included in those
assessments should be used to develop
the performance assessment scenarios to
be analyzed for the peak dose
performance assessments between
10,000 and 1 million years. We believe
that this is an inclusive threshold level
that fully considers a range of lowprobability FEPs, while at the same time
limiting speculation over highly
improbable FEPs. We believe the
probability screening threshold provides
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the foundation for a reasonable test of
the disposal system, as discussed
further below.
Although we discussed the meaning
of the probability threshold in some
detail in our proposal, we emphasize it
again as the foundation for constructing
the performance assessment. A 1 in 100
million annual probability of
occurrence, when considered over a
10,000-year period, includes FEPs with
a cumulative chance of occurring of one
one-hundredth of one percent (0.01%).
Similarly, over 1 million years, the
cumulative probability increases to only
a one percent (1%) chance of occurrence
within that time frame. We believe that
the database of information necessary to
assess FEPs at this low probability is the
same as that necessary for examining
their importance over the entire 1
million-year compliance period. We
believe this probability criterion leads to
an inclusive set of potential FEPs for
both the 10,000-year and peak dose
assessments, and in our view would
support a reasonable test of the disposal
system that encompasses the climate
change, seismic, igneous, and corrosion
scenarios specified in our proposal.
In our proposed rule, we concluded
that the 10,000-year FEPs screening
could serve as an adequate basis for
longer-term assessments because it is
sufficiently inclusive to be appropriate
for use in developing performance
scenarios applicable to the entire 1
million-year compliance period. That is,
we did not propose to require DOE to
consider FEPs with an annual
probability lower than 10¥8 to
accommodate the lengthened
compliance period. We believe
excluding FEPs with less than a 1%
chance of occurrence in 1 million years
is consistent with the principles of
reasonable expectation. We believe that
lowering the annual probability level
below 10¥8 would allow for speculative
scenarios to be considered in the peak
dose performance assessment, which
would be neither reasonable nor
justifiable, as explained below.
Some commenters disagreed, stating
that, because we are extending the
compliance period by a factor of 100,
the probability threshold for excluding
FEPs should also be extended by a
factor of 100, resulting in a threshold of
1 chance in 10 billion of occurrence per
year. Similarly, we received some
comments questioning altogether the
need for or validity of a probability
threshold. The comments suggest that,
because the effects are weighted by the
probability of occurrence, any potential
FEP, no matter how unlikely, should be
characterized and assessed because its
influence will be mitigated by its low
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probability. They cite NAS to the effect
that ‘‘all these scenarios need to be
quantified’’ with respect to probability
and consequence. (NAS Report p. 72)
Therefore, the commenters conclude
that our concerns about introducing
excessive speculation are unfounded.
We disagree. We addressed this topic in
our proposal, in the expectation that we
would be encouraged to adjust the
probability threshold by two orders of
magnitude (i.e., widening the
probability range by a factor of 100) to
account for the similarly lengthened
compliance period. We believe that
simply extending the approach of using
a one in 10,000 probability over a 1
million-year period to give 1 in 10
billion chance per year of occurring
(10¥10) would result in the inclusion of
FEPs that are so speculative as to be
unreasonable (70 FR 49052). Nor do we
believe it would be consistent with
NAS’s view that the overall goal was ‘‘to
define a standard that specifies a high
level of protection but that does not rule
out an adequately sited and welldesigned repository because of highly
improbable events.’’ (NAS Report p. 28)
Further, NAS itself suggested situations
in which scenarios need not be
quantified. NAS discusses, in the
context of volcanism, a 10¥8 annual
probability of occurrence as a level that
‘‘might be sufficiently low to constitute
a negligible risk’’ below which ‘‘it might
not be necessary to consider’’ how the
event might contribute to releases from
the disposal system. (NAS Report p. 95)
We believe this example is instructive,
given that volcanism is the single
scenario resulting in direct release of
radioactive material from the repository
into the biosphere, resulting in
relatively immediate exposures. We
believe it is reasonable to extend the
concept expressed by NAS as
‘‘negligible risk’’ to FEPs whose
influences are seen in the gradual
release and transport of radionuclides
over long periods of time. Therefore, we
believe that lowering the probability
threshold, or eliminating it altogether,
would be inconsistent with the
important NAS cautions to focus
assessment efforts on FEPs that can be
bounded within the limits of geologic
stability.
In our view, were we to lower or
eliminate the probability threshold, it
would be necessary to consider and
describe FEPs that might have been
present or occurred only the initial
years of the planet’s existence.
Similarly, FEPs with an annual
probability of 10¥10 may be only
hypothetical, since the age of the Earth
is generally considered to be ‘‘only’’ 4.6
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× 109 years, suggesting that these FEPs
may have less than a 50% chance of
occurring within the entire history of
the Earth. Indeed, the volcanic rocks
comprising Yucca Mountain and its
surroundings are only on the order of
10–12 million years old (∼107 years). In
determining the probability of particular
FEPs, the geologic record at the site is
the source of information to identify
what FEPs have occurred at the site in
the past and may occur in the future
(through the period of geologic
stability). Since the host rock formations
at the site are only about 10 million
years old, an annual probability cut-off
of 10¥10 would mean that probability
estimates for some FEPs would have to
be made in spite of the fact that there
is no evidence for their occurrence at
the site in the past. As it is, the 10¥8
probability threshold presents a
significant challenge to characterize
FEPs with some degree of confidence,
given the limits of today’s science and
technology. ICRP makes a similar point
in its 2007 recommendations: ‘‘The use
of probability assessment is limited by
the extent that unlikely events can be
forecast. In circumstances where
accidents can occur as a result of a wide
spectrum of initiating events, caution
should be exercised over any estimate of
overall probabilities because of the
serious uncertainty of predicting the
existence of all the unlikely initiating
events.’’ (Publication 103, Docket No.
EPA–HQ–OAR–2005–0083–0423,
paragraph 269) (Note that this
discussion is in the context of
‘‘potential’’ exposures, which include
releases that may occur in the far future
from disposal facilities. Therefore, the
term ‘‘accidents’’ should not be taken as
limited to operational activities.)
Overall, we believe events with a lower
annual probability than 10¥8 would
introduce speculation beyond what is
appropriate to define a reasonable test of
disposal system performance.
We also received comments stating
that maintaining the probability
screening criteria for the extended
compliance period undermines our
arguments for increasing uncertainty. To
the contrary, we believe the physical
meaning of the probability threshold
(0.01% chance of occurrence within
10,000 years, but a 1% chance within 1
million years) appropriately
incorporates the concept of uncertainty
increasing with time, while still
applying a substantially conservative
screening criterion.
We believe that the guidance we have
provided for executing a FEPs
evaluation and screening process
assures that it is executed in a thorough
manner. For example, we have stated
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that the geologic record through the
Quaternary Period (a period extending
back approximately 2 million years from
today) at and around the site should be
examined to identify relevant FEPs.
While we believe that the Quaternary
Period offers the most reliable data for
identifying and characterizing site
geologic FEPs, we do not believe that
evidence preserved in older portions of
the geologic record should be ignored in
the FEPs identification process. We did
not mean to imply that DOE need only
consider the previous 10,000 years
when developing evidence for the
probability of occurrence of future
events. Rather, our statements regarding
the Quaternary Period as an appropriate
geologic record were intended to
confirm that, where available, reliable
geologic records for earlier time periods
should be consulted. For example,
determining the probability of seismic
and igneous events would make use of
the geologic record at the site for as far
back in time as reliable estimates of past
events can be made so that defensible
probability estimates can be made. We
believe the Quaternary Period offers the
best information to quantify the
probabilities and consequences of
geologic FEPs relevant to site
performance. However, we did not
intend that significant information
about FEPs be ignored simply because
that information appears in the geologic
record at the site prior to the Quaternary
Period.
In fact, a longer portion of the
geologic record has been examined by
DOE and NRC in developing FEP
probabilities. For example, to determine
the nature and frequency of volcanic
activity around Yucca Mountain,
volcanic activity around the site through
the Quaternary Period was extensively
examined, as well as volcanic activity
prior to that time (ACNW Workshop on
Volcanism at Yucca Mountain,
September 22, 2004—Docket No. EPA–
HQ–OAR–2005–0083–0373 and 0378).
We believe that the information
necessary to evaluate FEPs against the
probability threshold we established
(10¥8 annual probability) will be
extensive, and that increasing the
compliance period from 10,000 to 1
million years does not require that
additional studies be performed beyond
those necessary to derive the FEPs
probabilities under the screening
process done for the 10,000-year time
frame assessments. As we have noted
previously, the probabilities for
individual FEPs are determined once,
and the same probabilities are used in
both the 10,000-year and 1 million-year
assessments.
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61281
On this last point, we stress that the
revised § 197.36(a) issued today should
not be interpreted as compelling DOE to
extend the databases for its technical
justifications. We are restating the
probability screening criterion, not
recasting the entire framework for the
analysis. We recognize that in any
licensing process the burden of proof is
on the applicant to demonstrate that the
necessary factors and influences have
been evaluated. It must also be
recognized that there will always be
limits to the ability of science and
technology to characterize FEPs and
their effects on the disposal system.
However, NAS has stated that many of
these processes and their uncertainties
are boundable. In our judgment, given
the capabilities of today’s science and
technology, it would be contrary to the
principle of reasonable expectation to
require DOE to demonstrate the same
level of confidence in assessments
covering 1 million years as it would for
a much shorter 10,000-year analysis.
Similarly, we believe that this
clarification does not create the prospect
of speculative scenarios of very low
probability (from combinations of FEPs)
being proposed, thereby opening the
performance assessments to unbounded
speculation. For example, if two low
probability independent FEPs were
proposed to occur simultaneously
because of the longer time horizon
under consideration, the probability of
that combination would be the product
of their respective probabilities. In other
words, the probability of the combined
FEPs occurring during the same year
will be much lower, by possibly orders
of magnitude, than the probability of
either FEP occurring individually.
Therefore, since the contributions of
various FEPs (or scenarios) to the dose
assessments is the product of their
respective probabilities and
consequences, the consequence of the
combined FEPs would need to be
inversely proportionally higher,
typically by orders of magnitude, than
the combined consequences of the
individual FEPs considered separately,
in order to make a significant change in
the overall dose assessment.
We did receive some comment
suggesting that we had inappropriately
excluded the type of volcanic events
that created the Yucca Mountain tuff
some 12 to 14 million years ago, instead
focusing on the past several million
years. However, as we stated in our
proposal, the geologic record of the past
several million years in the area around
the site indicates that basaltic volcanism
is the type of volcanism that has
occurred recently and has the potential
to recur in the future. The earlier events
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were of a much different, cataclysmic
nature, producing rock units more than
6000 ft (1800 m) thick. The type of
volcanic activity that created Yucca
Mountain and the surrounding area has
not recurred over the approximately 10
million years since the deposits were
originally laid down and is extremely
unlikely to occur within the next 1
million years (Docket No. EPA–HQ–
OAR–2005–0083–0050, pp. 7–42
through 7–49). Further, we question
whether such cataclysmic events could
be reasonably considered to fall within
the bounds of geologic stability as
envisioned by NAS. Inclusion of such
events in the peak dose assessment up
to 1 million years would be inconsistent
with the intent of the NAS when it
noted that long-term performance can be
assessed (because physical and geologic
processes are sufficiently quantifiable,
and the related uncertainties sufficiently
boundable) when the geologic system is
relatively stable or varies in a boundable
manner. (NAS Report p. 9) However,
NAS noted that ‘‘[a]fter the geologic
environment has changed, of course, the
scientific basis for performance
assessment is substantially eroded and
little useful information can be
developed.’’ (NAS Report p. 72) We
believe that volcanism of that
magnitude would result in fundamental
change of the geologic environment and
would not represent a reasonable test of
the disposal system. Therefore, we
continue to see no basis for requiring
this type of event be included in the
performance assessment.
Some may view our approach using a
single probability threshold for
determining which FEPs should be
considered for inclusion in the
performance assessments as
inconsistent with the application of
different dose standards for the initial
10,000 years and the period up to 1
million years. We do not see an
inconsistency primarily because the
nature and effects of uncertainty on
event probability and dose projections
are dissimilar. The overall uncertainty
in projecting doses using a model
simulating the complex interplay of the
disposal system components over long
times, each of which has inherent
uncertainties in their characteristics,
and the associated difficulty in relying
on such projections for regulatory
decisions, should not be confused with
the uncertainty implied in assigning a
probability of occurrence to a particular
FEP, which in many cases derives from
an examination of the geologic record at
the site. We have noted the difficulty in
extrapolating performance to very long
times, and believe it is appropriate to
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address this difficulty by establishing a
somewhat higher, but still protective,
dose limit for the period beyond 10,000
years. FEP probabilities are assigned
based on observations that may cover
long periods of time, such as for
geologic processes, or from laboratory
testing and the extrapolation of such
results to conditions that may exist in
the distant future, such as for corrosion
processes. In today’s final rule, the FEP
probability threshold that must be
considered in developing performance
assessments represents a policy
judgment about how such events should
be addressed in order to meet the
regulatory challenge recognized by
NAS, supported by technical reasoning
about the nature of the site database for
identifying and characterizing FEPs.
Significance
The second criterion for evaluating
FEPs, the evaluation of the significance
of the impacts on performance
assessment, allows FEPs above the
probability threshold to be excluded
from the analyses if they would not
significantly change the results of
performance assessments. In other
words, this evaluation is intended to
identify those FEPs whose projected
probability would otherwise make them
candidates for inclusion in the
performance assessment, but whose
effect on repository performance
(however probable) can be demonstrated
not to be significant. We are retaining
the provisions presented in the
proposed rule related to screening FEPs
for their effects on the performance
assessment results, and, for the reasons
discussed below, are adding an
additional provision regarding the
analysis of seismic FEPs in § 197.36(c).
Today’s final rule continues to focus
on seismic and igneous events that
cause direct damage to the engineered
barrier system (e.g., repository drifts and
waste packages). Regardless of other
effects of these events on the disposal
system, the timing and degree of waste
package degradation has a significant
effect on peak dose. The longevity of
waste packages, when considering
periods of hundreds of thousands of
years, is uncertain and dependent on a
number of factors. Therefore, the aspect
of primary interest in evaluating seismic
and igneous FEPs is their potential to
breach waste packages and make
radioactive material available for
transport by infiltrating water (or, in the
case of volcanic events, for direct
release into the biosphere).
We believe that the use of the
significance criterion of § 197.36(a)
would assure a reasonable test of
disposal system performance through
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the period of geologic stability. We
recognize that setting forth the
significance screening criterion in
§ 197.36(a) of our proposal as pertaining
to the 10,000-year period could be
construed as creating a situation in
which important long-term processes
could be excluded altogether from the
analysis if they were not significant in
the earlier period. However, we do not
believe it is reasonable to interpret the
significance criterion in this way. We
have taken specific steps to ensure that
significant long-term FEPs will be
considered in the assessments.
Consistent with NAS, we have
addressed the long-term effects of
seismic, igneous, and climatic FEPs. In
addition, as described below, we have
directed that the effects of general
corrosion on the engineered barrier
system be evaluated. Further, contrary
to some comments, we explicitly
required that FEPs included in the
10,000-year analysis must continue to
be included for the longer-term (10,000
years to 1 million years) assessment.
That is, FEPs included in the initial
10,000-year assessments will continue
to operate throughout the period of
geologic stability. These FEPs are
already identified as appropriate for
inclusion, and include fundamental
physical and geologic processes that
play roles in the release and transport of
radionuclides, regardless of the time
period covered by the assessment.
As noted above, to further bolster the
significance screening criterion, in our
proposal we considered whether it
might be possible that FEPs eliminated
from consideration during the first
10,000 years should be included in the
longer-term assessment if they would
have a significant bearing on
performance at later times, even if they
could legitimately be dismissed for the
initial 10,000-year period. We focused
our attention on FEPs affecting the
engineered barriers since, as noted
above, waste package failure is the
dominant factor in the timing and
magnitude of the peak dose, and is the
primary reason for considering time
frames up to 1 million years. To
illustrate one consideration, thermal
conditions in the repository change
dramatically within the initial 10,000year period, affecting the relative
importance of some FEPs during and
after the thermal pulse. However, FEPs
involved in release and transport of
radionuclides would generally be the
same, regardless of when the waste
package fails. Further, while FEPs
associated with the natural
characteristics of the site are active
today or can be observed in the geologic
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record, FEPs related to engineered
barrier longevity involve extrapolation
of shorter-term testing data. The degree
to which natural FEPs can contribute to
the breaching of waste packages is
dependent to a large extent on the
condition of those packages over time,
making FEPs specific to the engineered
barriers of particular importance. We
took this approach for two reasons.
First, we needed to clearly outline the
reasons why a FEP that could be
excluded on the basis of significance
from the performance assessments for
the initial 10,000-year period might
potentially need to be re-considered for
the lengthened compliance period.
Second, we wanted to further our goal
of issuing an implementable standard by
limiting potentially unconstrained
speculation over the longer compliance
period. By discussing the considerations
involved in evaluating FEPs that could
be previously excluded, we hoped to lay
out clearly the reasoning that could be
used to justify inclusion of additional
FEPs beyond those identified by the
NAS committee.
We explicitly addressed general
corrosion of the waste packages and
other engineered barriers in our
proposal because it is likely to be a
significant degradation process at later
times. We identified this FEP as being
significant at times greater than 10,000
years because we believe it is the
principal process FEP that could lead to
‘‘gross breaching’’ of the waste package
over those extended time frames.
Processes and events that could lead to
‘‘gross breaching’’ are of greatest
significance to long term performance
because, as noted by the NAS,
‘‘canisters are likely to fail initially at
small local openings through which
water might enter, but out of which the
diffusion of dissolved wastes will be
slow until the canister is grossly
breached.’’ (NAS Report p. 86) It is the
time of ‘‘gross breaching’’ that
determines the time of more rapid
release of dissolved wastes from the
repository and hence may have a
significant effect on the time and
magnitude of the peak dose within 1
million years. Although the general
corrosion process is slow, tends to
decrease with decreasing temperature,
and may not lead to significant releases
for the first 10,000 years (depending on
DOE’s design of the waste package), we
believe this FEP could be significant
enough over the long term to require
inclusion in the assessment of
performance during the time of geologic
stability, regardless of the screening
decision in the first 10,000 years.
Further, consideration of the
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uncertainties involved in extrapolating
general corrosion data for the proposed
waste package materials supports the
inclusion of this potentially highly
significant process (‘‘Assumptions,
Conservatisms, and Uncertainties in
Yucca Mountain Performance
Assessments,’’ Docket No. EPA–HQ–
OAR–2005–0083–0085, section 5.4.1).
Therefore, we believe that general
corrosion, in addition to those FEPs
related to seismicity, igneous activity
and climate change identified by NAS,
requires explicit inclusion in the
assessments during the time of geologic
stability.
We did, as one commenter pointed
out, consider providing NRC more
latitude to identify FEPs if they would
significantly affect the peak dose. After
further consideration, we decided
against this approach, believing the
provisions outlined above and the
specification of general corrosion would
adequately address this situation,
provide a reasonable test of disposal
system performance, and give DOE the
necessary assurance that the important
factors have been explicitly identified in
the rule. As we noted above, we
identified general corrosion of
engineered barriers as a FEP potentially
significant to the peak dose, and
specified its inclusion because it is
likely to be a significant degradation
process at later times. Similarly,
consistent with the NAS
recommendations, we have specified
the inclusion of climate change,
seismicity, and igneous scenarios. We
view the requirement to include general
corrosion, as well as the climate,
seismic, and igneous scenarios
identified by NAS, as leading to an
effective and extensive assessment,
which can fairly be represented as a
reasonable test of the disposal system.
As we discussed in our proposal, the
search for additional FEPs that might be
significant at some point beyond 10,000
years can rapidly become highly
speculative and limited in benefit.
Therefore, we continue to believe that
our approach represents ‘‘informed
judgment’’ and a reasonable test of
repository performance over time frames
as long as 1 million years for the Yucca
Mountain disposal system.
We also note that DOE submitted, as
part of its comments on the proposed
rule, the results of analyses based on a
simplified peak dose model (Docket No.
EPA–HQ–OAR–2005–0083–0352,
Appendix 1). DOE states that it had
compiled a database of FEPs,
independent of compliance period, and
evaluated them for inclusion in a
10,000-year analysis. DOE
‘‘subsequently re-evaluated the FEPs
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over the period beyond 10,000 years’’
and concluded that those FEPs excluded
on the basis of significance within
10,000 years would also not have
significant effects on performance
projections beyond 10,000 years. DOE
reached its conclusion both for FEPs
excluded ‘‘on a low consequence basis
that is not affected by time’’ and for
‘‘gradual and continuing processes’’ that
‘‘are time dependent.’’
Also as part of its comments, DOE
submitted an analysis that identified
three reasons why gradual and/or
infrequent FEPs excluded on the basis
of significance within 10,000 years
would also not have significant effects
on performance projections beyond
10,000 years: (1) An excluded FEP was
determined to be of secondary
importance to the primary significant
degradation FEP, which was included in
the analysis; (2) the inclusion of the FEP
would tend to lower the peak dose
during the time of geologic stability
because it resulted in earlier and more
diffuse releases (hence the exclusion of
the FEP would be conservative from a
peak dose perspective); or (3) the FEP is
correlated in some way with
temperature (e.g., in the rate with which
it operates), so it would be less
significant at later times due to the
lower temperature in the repository over
time. (Docket No. EPA–HQ–OAR–2005–
0083–0352, Appendix 1, section 6.1 and
Table 24) DOE considered FEPs of this
nature associated with both the
engineered and natural barrier systems.
DOE concluded, for example, that some
longer-term processes, such as general
corrosion, may contribute to waste
package failure, and disruptive seismic
events may contribute to rockfall and
other physical mechanisms leading to
release.
We also considered public comments
on this topic. Most commenters who
disagreed with our proposal cited the
limited data available on various
corrosion mechanisms that could affect
the waste packages. Many of these
commenters seem to believe that we
have excluded all corrosion
mechanisms except general corrosion.
This is not the case. We have explicitly
directed that general corrosion be
considered because it is likely to be the
most significant such process at longer
times; however, other corrosion
mechanisms (such as localized
corrosion) are more likely in the early
period after disposal when temperatures
inside the repository are high. If DOE
determines these processes to be
insignificant within 10,000 years, they
are not likely to be more significant than
general corrosion at later times. If they
are included in the 10,000-year analysis,
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they must be included in the longerterm assessments. One commenter
highlighted our discussion of criticality
as excluding one of the ‘‘most
worrisome threats to the repository’’
over the long term. We cited an NRC
technical study to support our
conclusion that such an event is
unlikely to be significant to the results
of the assessments. Further, the DOE
reference cited above concludes that all
criticality scenarios fall below the
probability screening threshold. An
alternative view on the FEPs screening
process was expressed in a report by the
Electric Power Research Institute (EPRI):
‘‘Thus, the current EPA screening limit
is very conservative compared to the
[Negligible Incremental Dose] level
suggested by [NAS]. It is likely that
there are many FEPs that DOE has
already included in their analysis using
the EPA approach that would not have
been included if the [NAS]recommended approach had been
followed. Given that many additional
FEPs are already included, it should be
unnecessary to include any additional
FEPs if the regulatory compliance
period is extended beyond 10,000
years.’’ (‘‘Yucca Mountain Licensing
Standard Options for Very Long Time
Frames,’’ April 2005, pp. 3–5 and 3–6,
Docket No. EPA–HQ–OAR–2005–0083–
0087) Taking all of this information into
account, we continue to believe it is
reasonable that, with the exception of
the specific FEPs identified in 197.36(c),
a FEP determined to be insignificant in
the first 10,000 years may continue to be
excluded in the post-10,000-year
analyses.
As we noted above, we are modifying
the proposed rule regarding the
provisions related to seismic events in
§ 197.36(c). We noted in our proposal
the NAS statement that ‘‘[w]ith respect
to the effects of seismicity on the
hydrologic regime, the possibility of
adverse effects due to displacements
along existing fractures cannot be
overlooked’’ but that ‘‘such
displacements have an equal probability
of favorably changing the hydrologic
regime.’’ (NAS Report p. 93). We argued
that these effects would likely be
minimal given the many small-scale
changes that would be possible in the
connectivity of the fracture networks,
and that these effects would likely be
small compared to the effects of climate
change on the hydrologic behavior of
the disposal system. We did not mean
to imply that the seismic and climate
events would involve the same
hydrologic characteristics and processes
or produce the same effects on the
ground-water flow regime, but that the
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effects of one were likely to outweigh
the effects of the other. While we still
believe that is likely, we have
concluded, after further consideration,
that the issue of hydrologic effects
resulting from seismic events needs to
be examined in sufficient detail to
address the point made by NAS. We
believe the effects of fault displacement
on the hydrologic regime will be
adequately addressed by the variation in
parameters such as hydraulic
conductivity (i.e., evaluating reasonable
variation in ground-water flow
parameter values, whether seismicallyinduced or not, will illustrate the range
of effects that might result from
seismicity). However, NAS also
identified another seismic effect on
hydrology, namely the potential for
transient rise in the ground-water table.
In this instance, NAS did not simply
state that such potential could be
bounded, but noted site-specific studies
suggesting ‘‘a probable maximum
transient rise on the order of 20 m or
less.’’ (NAS Report p. 94) Therefore, we
now require that the effects of a rise in
the ground-water table as a result of
seismicity be considered. We are not
specifying the extent of the rise to be
considered, but leave that conclusion to
be determined by NRC. NRC may
choose to estimate the magnitude of
ground-water table rise itself, or require
DOE to include such estimates in its
license application. In this case,
however, we are also allowing NRC to
make a judgment as to whether such a
rise in ground water would be
significant to the results of the
performance assessment. If NRC
determines that such a reasonably
bounded scenario would not be
significant, DOE would not be required
to evaluate its effects.
We believe deferring to NRC on this
point is the appropriate approach. The
above quote from page 93 of the NAS
Report makes it clear that changes to the
hydrologic regime from seismic events
would be equally likely to enhance or
reduce transport of radionuclides.
However, it would seem unlikely for
changes to occur that would all combine
to enhance transport to the saturated
zone and then through the controlled
area, such that concentrations of
radionuclides at the RMEI location
would be significantly increased. It
seems more likely that localized
changes would occur, which in sum
would not significantly increase overall
transport of radionuclides. Further, as
noted above, we believe these
seismically-induced changes are likely
to be approximated by the normal
variation in flow parameters. Changes in
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the hydrologic system from climate
change (e.g., increases in infiltration) are
expected to be quantitatively more
significant than such changes resulting
from seismic activity. We believe NRC
is better positioned to make judgments
regarding the significance and extent of
such changes. We note that a dozen
years of site characterization, scientific
study, and performance assessments
have been conducted since the NAS
Report in 1995. NRC has conducted its
own analyses as well as participated in
ongoing technical exchanges with DOE
over this period. We view deferring to
NRC’s judgment in this case as
comparable to the approach we have
taken with climate change. In that
instance, we outlined the primary issues
and overall approach, but specified that
NRC would establish the details
required to implement our standard.
Finally, we are retaining the provision
related to climate change as it was
proposed. We believe this is a
reasonable approach, which allows NRC
to characterize climate change beyond
10,000 years using constant conditions.
This approach has the advantage of
avoiding speculation regarding the
timing and magnitude of climatic
cycles, while addressing the important
aspects of climate change. We received
some comments that appear to have
misinterpreted our proposal. Some
comments suggested that our citation of
the NAS statement to the effect that
‘‘climate changes on the time scale of
hundreds of years would probably have
little if any effect on repository
performance’’ (NAS Report p. 92) as
implying that we are ‘‘ignoring longerterm changes’’ such as ‘‘glacial periods
covering thousands of years.’’ This
represents a fundamental
misunderstanding of our proposal,
which would allow the future climate to
be represented by what is essentially a
glacial transition period lasting 990,000
years, but in any event placed no limits
on the duration of periods of increased
precipitation. Similarly, some
commenters expressed the view that we
‘‘required’’ the future climate to be
represented by constant conditions, or
that we were suggesting that a single
climate be used in all realizations. On
the contrary, we cited the NAS
conclusion that ‘‘a doubling of the
effective wetness’’ might be significant
as one justification for stating that it
would be reasonable to represent farfuture climate by constant conditions.
Today’s final rule, consistent with our
proposal, leaves it to NRC to determine
the parameter values that would define
the future climate, including influential
parameters other than precipitation,
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such as temperature. Our specification
of the outcome of ‘‘increased water flow
through the repository’’ provides NRC
with the flexibility to specify basic
parameters, such as precipitation and
temperature, that must be assumed by
DOE, or to derive estimates of water
flow directly. This is consistent with
our current belief that the dominant
mechanisms and flow paths for water to
move from the surface through the
repository and beyond should be
determined by NRC rather than EPA.
Further, we anticipated that ‘‘constant
climate conditions’’ would be used as
another parameter in the probabilistic
assessment. That is, each realization
would select its constant conditions
from among a distribution of such
conditions developed to reflect
estimates of different future climate
states. This is exactly the approach that
NRC has taken in its proposal, i.e., that
a range of deep percolation values be
used (70 FR 53313–53320, September 8,
2005).
Some commenters disagreed with the
approach of specifying constant climate
conditions leading to a higher rate of
water flow through the repository,
stating that the ‘‘non-linear’’ nature of
the disposal system would be more
sensitive to a dynamic, cyclical
representation of climate. This is not
necessarily true, as the effects on the
disposal system would be highly
affected by the timing of waste package
failures (e.g., whether they fail during a
wetter or drier cycle). Some comments
cite recent climate research suggesting
that anthropogenic climate influences
will postpone the next glacial cycle by
roughly 500,000 years, or that today’s
climate at Yucca Mountain will actually
be more representative of future
climates than would the wetter
conditions known to have occurred in
the past. We believe that our final rule’s
approach to climate change provides a
reasonable approach to address a point
of fundamental uncertainty regarding
long-term climate change and its role in
the performance assessments, an
uncertainty that cannot be removed by
additional research into past climate
cycles or modeling of present or future
climate behavior. We refer to NAS on
this point: ‘‘Although the typical nature
of past climate changes is well known,
it is obviously impossible to predict in
detail either the nature or the timing of
future climate change.’’ (NAS Report p.
77, emphasis added) Although
continuing research will provide better
understanding of past climate
fluctuations, we believe that predicting
with high confidence the timing and
extent of climate fluctuations into the
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far future will remain an unrealistic
goal. We believe that the understanding
of past climate fluctuations and their
potential effects on the Yucca Mountain
hydrologic system is valuable
information and should be applied to
define the climate-related parameter
values. As noted above, NRC has used
such information to propose climaterelated parameter values, which DOE
will use to project the behavior of
hydrologic processes at the site. We
believe that this approach to treatment
of a ‘‘residual, unquantifiable
uncertainty’’ by the application of
‘‘informed judgment’’ is consistent with
NAS guidance. (NAS Report p. 80)
IV. Statutory and Executive Order
Reviews
A. Executive Order 12866: Regulatory
Planning and Review
Under Executive Order 12866 (58 FR
51735, October 4, 1993), this action is a
‘‘significant regulatory action’’ because
it raises novel legal or policy issues
arising out of the specific legal mandate
of section 801 of the Energy Policy Act
of 1992. Accordingly, EPA submitted
this action to the Office of Management
and Budget for review under Executive
Order 12866 and any changes made in
response to OMB recommendations
have been documented in the docket for
this action.
B. Paperwork Reduction Act
This action does not impose an
information collection burden under the
provisions of the Paperwork Reduction
Act, 44 U.S.C. 3501 et seq. Burden is
defined at 5 CFR 1320.3(b). We have
determined that this rule contains no
information collection requirements
within the scope of the Paperwork
Reduction Act. This final rule
establishes requirements that apply only
to DOE.
C. Regulatory Flexibility Act
The Regulatory Flexibility Act (RFA)
generally requires an agency to prepare
a regulatory flexibility analysis of any
rule subject to notice and comment
rulemaking requirements under the
Administrative Procedure Act or any
other statute unless the agency certifies
that the rule will not have a significant
economic impact on a substantial
number of small entities. Small entities
include small businesses, small
organizations, and small governmental
jurisdictions.
For purposes of assessing the impacts
of today’s rule on small entities, small
entity is defined as: (1) A small business
as defined by the Small Business
Administration’s (SBA) regulations at 13
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CFR 121.201; (2) a small governmental
jurisdiction that is a government of a
city, county, town, school district or
special district with a population of less
than 50,000; and (3) a small
organization that is any not-for-profit
enterprise which is independently
owned and operated and is not
dominant in its field.
After considering the economic
impacts of today’s final rule on small
entities, I certify that this action will not
have a significant economic impact
upon a substantial number of small
entities. This final rule will not impose
any requirements on small entities. This
final rule establishes requirements that
apply only to DOE.
D. Unfunded Mandates Reform Act
Title II of the Unfunded Mandates
Reform Act of 1995 (UMRA), Public
Law 104–4, establishes requirements for
Federal agencies to assess the effects of
their regulatory actions on State, local,
and tribal governments and the private
sector. Under section 202 of the UMRA,
EPA generally must prepare a written
statement, including a cost-benefit
analysis, for proposed and final rules
with ‘‘Federal mandates’’ that may
result in expenditures to State, local,
and tribal governments, in the aggregate,
or to the private sector, of $100 million
or more in any one year. Before
promulgating an EPA rule for which a
written statement is needed, section 205
of the UMRA generally requires EPA to
identify and consider a reasonable
number of regulatory alternatives and
adopt the least costly, most costeffective or least burdensome alternative
that achieves the objectives of the rule.
The provisions of section 205 do not
apply when they are inconsistent with
applicable law. Moreover, section 205
allows EPA to adopt an alternative other
than the least costly, most cost-effective
or least burdensome alternative if the
Administrator publishes with the final
rule an explanation why that alternative
was not adopted. Before EPA establishes
any regulatory requirements that may
significantly or uniquely affect small
governments, including tribal
governments, it must have developed
under section 203 of the UMRA a small
government agency plan. The plan must
provide for notifying potentially
affected small governments, enabling
officials of affected small governments
to have meaningful and timely input in
the development of EPA regulatory
proposals with significant Federal
intergovernmental mandates, and
informing, educating, and advising
small governments on compliance with
the regulatory requirements.
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Today’s final rule contains no Federal
mandates (under the regulatory
provisions of Title II of UMRA) for
State, local, or tribal governments or the
private sector. This final rule
implements requirements specifically
set forth by the Congress in section 801
of the EnPA and establishes radiological
protection standards applicable solely
and exclusively to the Department of
Energy’s potential storage and disposal
facility at Yucca Mountain. The rule
imposes no enforceable duty on any
State, local or tribal governments or the
private sector. Thus, today’s rule is not
subject to the requirements of sections
202 and 205 of UMRA.
EPA has determined that this rule
contains no regulatory requirements that
might significantly or uniquely affect
small governments. This final rule
implements requirements specifically
set forth by the Congress in section 801
of the EnPA and establishes radiological
protection standards applicable solely
and exclusively to the Department of
Energy’s potential storage and disposal
facility at Yucca Mountain. The rule
imposes no enforceable duty on any
small governments. Thus, today’s rule is
not subject to the requirements of
section 203 of UMRA.
E. Executive Order 13132: Federalism
Executive Order 13132, entitled
‘‘Federalism’’ (64 FR 43255, August 10,
1999), requires EPA to develop an
accountable process to ensure
‘‘meaningful and timely input by State
and local officials in the development of
regulatory policies that have federalism
implications.’’ ‘‘Policies that have
federalism implications’’ is defined in
the Executive Order to include
regulations that have ‘‘substantial direct
effects on the States, on the relationship
between the national government and
the States, or on the distribution of
power and responsibilities among the
various levels of government.’’
This final rule does not have
federalism implications. It will not have
substantial direct effects on the States,
on the relationship between the national
government and the States, or on the
distribution of power and
responsibilities among the various
levels of government, as specified in
Executive Order 13132. This final rule
implements requirements specifically
set forth by the Congress in section 801
of the EnPA and establishes radiological
protection standards applicable solely
and exclusively to the Department of
Energy’s potential storage and disposal
facility at Yucca Mountain. Thus,
Executive Order 13132 does not apply
to this rule. In the spirit of Executive
Order 13132, and consistent with EPA
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policy to promote communications
between EPA and State and local
governments, EPA specifically solicited
comment on the proposed rule from
State and local officials.
F. Executive Order 13175: Consultation
and Coordination With Indian Tribal
Governments
Executive Order 13175, entitled
‘‘Consultation and Coordination with
Indian Tribal Governments’’ (65 FR
67249, November 9, 2000), requires EPA
to develop an accountable process to
ensure ‘‘meaningful and timely input by
tribal officials in the development of
regulatory policies that have tribal
implications.’’ This final rule does not
have tribal implications, as specified in
Executive Order 13175. This final rule
will regulate only DOE on land owned
by the Federal government. The rule
does not have substantial direct effects
on one or more Indian tribes, on the
relationship between the Federal
Government and Indian tribes, or on the
distribution of power and
responsibilities between the Federal
Government and Indian tribes. Thus,
Executive Order 13175 does not apply
to this rule.
Although Executive Order 13175 does
not apply to this rule, EPA specifically
solicited additional comment on this
proposed rule from tribal officials and
consulted with tribal officials in
developing this rule. EPA directly
contacted more than 20 tribal
governments and conducted three
conference calls with members of tribal
governments. In recognition of the
importance of government-togovernment consultation with tribes and
the significance of tribal governments as
sovereign nations, EPA extended the
public comment period for tribal
governments to December 31, 2005.
Comments related to tribal issues, and
our responses to them, may be found in
Section 13 of the Response to Comments
document associated with this final rule
(docket ref).
G. Executive Order 13045: Protection of
Children From Environmental Health &
Safety Risks
This final rule is not subject to
Executive Order 13045 because it is not
economically significant as defined in
Executive Order 12866, and because the
Agency does not have reason to believe
the environmental health risks or safety
risks addressed by this action present a
disproportionate risk to children.
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H. Executive Order 13211: Actions That
Significantly Affect Energy Supply,
Distribution, or Use
This action is not a ‘‘significant
energy action’’ as defined in Executive
Order 13211 (66 FR 28355 (May 22,
2001)), because it is not likely to have
a significant adverse effect on the
supply, distribution, or use of energy.
This final rule will apply only to DOE.
Construction, operation, and closure of
the repository at Yucca Mountain would
fulfill the Federal government’s
commitment to manage the final
disposition of spent nuclear fuel from
commercial power reactors. However,
there is no direct link between operation
of the repository and an increased use
of nuclear power. Other economic,
technical, and policy factors will
influence the extent to which nuclear
energy is utilized.
I. National Technology Transfer and
Advancement Act
Section 12(d) of the National
Technology Transfer and Advancement
Act of 1995 (‘‘NTTAA’’), Public Law No.
104–113, 12(d) (15 U.S.C. 272 note)
directs EPA to use voluntary consensus
standards in its regulatory activities
unless to do so would be inconsistent
with applicable law or otherwise
impractical. Voluntary consensus
standards are technical standards (e.g.,
materials specifications, test methods,
sampling procedures, and business
practices) that are developed or adopted
by voluntary consensus standards
bodies. NTTAA directs EPA to provide
Congress, through OMB, explanations
when the Agency decides not to use
available and applicable voluntary
consensus standards.
This rulemaking involves technical
standards. Therefore, the Agency
conducted a search to identify
potentially applicable voluntary
consensus standards. In our original
1999 proposal (64 FR 46976), we
requested public comment on
potentially applicable voluntary
consensus standards that would be
appropriate for inclusion in the Yucca
Mountain rule. However, we identified
no such standards, and none were
brought to our attention in comments.
Therefore, the standards promulgated in
2001 and today’s final revisions are sitespecific and developed solely for
application to the Yucca Mountain
disposal facility.
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Radionuclides, Uranium, Waste
treatment and disposal, Spent nuclear
fuel, High-level radioactive waste.
J. Executive Order 12898: Federal
Actions To Address Environmental
Justice in Minority Populations and
Low-income Populations
Executive Order (EO) 12898 (59 FR
7629 (Feb. 16, 1994)) establishes federal
executive policy on environmental
justice. Its main provision directs
federal agencies, to the greatest extent
practicable and permitted by law, to
make environmental justice part of their
mission by identifying and addressing,
as appropriate, disproportionately high
and adverse human health or
environmental effects of their programs,
policies, and activities on minority
populations and low-income
populations in the United States.
EPA lacks the discretionary authority
to address environmental justice in this
final rulemaking. This final rule
implements requirements specifically
set forth by the Congress in section 801
of the EnPA and establishes radiological
protection standards applicable solely
and exclusively to the Department of
Energy’s potential storage and disposal
facility at Yucca Mountain. Section
801(a)(1) of the EnPA directs EPA to
‘‘promulgate, by rule, public health and
safety standards’’ that ‘‘ prescribe the
maximum annual effective dose
equivalent to individual members of the
public’’ from releases of radioactive
material from the Yucca Mountain
repository. This final rule fulfills this
statutory direction.
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K. Congressional Review Act
The Congressional Review Act, 5
U.S.C. 801 et seq., as added by the Small
Business Regulatory Enforcement
Fairness Act of 1996, generally provides
that before a rule may take effect, the
agency promulgating the rule must
submit a rule report, which includes a
copy of the rule, to each House of the
Congress and to the Comptroller General
of the United States. Section 804
exempts from section 801 the following
types of rules: (1) Rules of particular
applicability; (2) rules relating to agency
management or personnel; and (3) rules
of agency organization, procedure, or
practice that do not substantially affect
the rights or obligations of non-agency
parties. 5 U.S.C. 804(3). EPA is not
required to submit a rule report
regarding today’s action under section
801 because this is a rule of particular
applicability. This final rule will apply
only to DOE, and is issued by EPA in
response to direction from Congress in
the EnPA.
List of Subjects in 40 CFR Part 197
Environmental protection, Nuclear
energy, Radiation protection,
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Dated: September 30, 2008.
Stephen L. Johnson,
Administrator.
40 CFR part 197 is amended as
follows:
■
PART 197—PUBLIC HEALTH AND
ENVIRONMENTAL RADIATION
PROTECTION STANDARDS FOR
YUCCA MOUNTAIN, NEVADA
1. The authority citation for part 197
continues to read as follows:
■
Authority: Sec. 801, Pub. L. 102–486, 106
Stat. 2921, 42 U.S.C. 10141n.
Subpart A—Public Health and
Environmental Standards for Storage
2. Section 197.2 is amended by
revising the definition of ‘‘Effective dose
equivalent’’ to read as follows:
■
§ 197.2
A?
What definitions apply in Subpart
*
*
*
*
*
Effective dose equivalent means the
sum of the products of the dose
equivalent received by specified tissues
following an exposure of, or an intake
of radionuclides into, specified tissues
of the body, multiplied by appropriate
weighting factors. Annual committed
effective dose equivalents shall be
calculated using weighting factors in
appendix A of this part, unless
otherwise directed by NRC in
accordance with the introduction to
appendix A of this part.
*
*
*
*
*
Subpart B—Public Health and
Environmental Standards for Disposal
3. Section 197.12 is amended by
revising paragraph (1) of the definition
of ‘‘Performance assessment’’ and the
definition of ‘‘Period of geologic
stability’’ to read as follows:
■
§ 197.12
B?
What definitions apply in Subpart
*
*
*
*
*
Performance assessment means an
analysis that:
(1) Identifies the features, events,
processes, (except human intrusion),
and sequences of events and processes
(except human intrusion) that might
affect the Yucca Mountain disposal
system and their probabilities of
occurring;
*
*
*
*
*
Period of geologic stability means the
time during which the variability of
geologic characteristics and their future
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61287
behavior in and around the Yucca
Mountain site can be bounded, that is,
they can be projected within a
reasonable range of possibilities. This
period is defined to end at 1 million
years after disposal.
*
*
*
*
*
■ 4. Section 197.13 is revised to read as
follows:
§ 197.13
How is Subpart B implemented?
The NRC implements this subpart B.
The DOE must demonstrate to NRC that
there is a reasonable expectation of
compliance with this subpart before
NRC may issue a license.
(a) The NRC will determine
compliance, based upon the arithmetic
mean of the projected doses from DOE’s
performance assessments for the period
within 1 million years after disposal,
with:
(1) Sections 197.20(a)(1) and
197.20(a)(2) of this subpart; and
(2) Sections 197.25(b)(1), 197.25(b)(2),
and 197.30 of this subpart, if
performance assessment is used to
demonstrate compliance with either or
both of these sections.
(b) [Reserved]
■ 5. Section 197.15 is revised to read as
follows:
§ 197.15 How must DOE take into account
the changes that will occur during the
period of geologic stability?
The DOE should not project changes
in society, the biosphere (other than
climate), human biology, or increases or
decreases of human knowledge or
technology. In all analyses done to
demonstrate compliance with this part,
DOE must assume that all of those
factors remain constant as they are at
the time of license application
submission to NRC. However, DOE must
vary factors related to the geology,
hydrology, and climate based upon
cautious, but reasonable assumptions of
the changes in these factors that could
affect the Yucca Mountain disposal
system during the period of geologic
stability, consistent with the
requirements for performance
assessments specified at § 197.36.
■ 6. Section 197.20 is revised to read as
follows:
§ 197.20
What standard must DOE meet?
(a) The DOE must demonstrate, using
performance assessment, that there is a
reasonable expectation that the
reasonably maximally exposed
individual receives no more than the
following annual committed effective
dose equivalent from releases from the
undisturbed Yucca Mountain disposal
system:
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Federal Register / Vol. 73, No. 200 / Wednesday, October 15, 2008 / Rules and Regulations
§ 197.25
What standard must DOE meet?
(a) The DOE must determine the
earliest time after disposal that the
waste package would degrade
sufficiently that a human intrusion (see
§ 197.26) could occur without
recognition by the drillers.
(b) The DOE must demonstrate that
there is a reasonable expectation that
the reasonably maximally exposed
individual will receive an annual
committed effective dose equivalent, as
a result of the human intrusion, of no
more than:
(1) 150 microsieverts (15 millirems)
for 10,000 years following disposal; and
(2) 1 millisievert (100 millirems) after
10,000 years, but within the period of
geologic stability.
(c) The analysis must include all
potential environmental pathways of
radionuclide transport and exposure.
■ 8. Section 197.35 is removed and
reserved.
§ 197.35
[Removed and Reserved]
9. Section 197.36 is revised to read as
follows:
■
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§ 197.36 Are there limits on what DOE
must consider in the performance
assessments?
(a) Yes, there are limits on what DOE
must consider in the performance
assessments.
(1) The DOE’s performance
assessments conducted to show
compliance with §§ 197.20(a)(1),
197.25(b)(1), and 197.30 shall not
include consideration of very unlikely
features, events, or processes, i.e., those
that are estimated to have less than one
chance in 100,000,000 per year of
occurring. Features, events, and
processes with a higher chance of
occurring shall be considered for use in
performance assessments conducted to
show compliance with §§ 197.20(a)(1),
197.25(b)(1), and 197.30, except as
stipulated in paragraph (b) of this
section. In addition, unless otherwise
specified in these standards or NRC
regulations, DOE’s performance
assessments need not evaluate the
impacts resulting from features, events,
and processes or sequences of events
and processes with a higher chance of
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occurring if the results of the
performance assessments would not be
changed significantly in the initial
10,000-year period after disposal.
(2) The same features, events, and
processes identified in paragraph (a)(1)
of this section shall be used in
performance assessments conducted to
show compliance with §§ 197.20(a)(2)
and 197.25(b)(2), with additional
considerations as stipulated in
paragraph (c) of this section.
(b) For performance assessments
conducted to show compliance with
§§ 197.25(b) and 197.30, DOE’s
performance assessments shall exclude
unlikely features, events, or processes,
or sequences of events and processes.
The DOE should use the specific
probability of the unlikely features,
events, and processes as specified by
NRC.
(c) For performance assessments
conducted to show compliance with
§§ 197.20(a)(2) and 197.25(b)(2), DOE’s
performance assessments shall project
the continued effects of the features,
events, and processes included in
paragraph (a) of this section beyond the
10,000-year post-disposal period
through the period of geologic stability.
The DOE must evaluate all of the
features, events, or processes included
in paragraph (a) of this section, and also:
(1) The DOE must assess the effects of
seismic and igneous scenarios, subject
to the probability limits in paragraph (a)
of this section for very unlikely features,
events, and processes. Performance
assessments conducted to show
compliance with § 197.25(b)(2) are also
subject to the probability limits for
unlikely features, events, and processes
as specified by NRC.
(i) The seismic analysis may be
limited to the effects caused by damage
to the drifts in the repository, failure of
the waste packages, and changes in the
elevation of the water table under Yucca
Mountain. NRC may determine the
magnitude of the water table rise and its
significance on the results of the
performance assessment, or NRC may
require DOE to demonstrate the
magnitude of the water table rise and its
significance in the license application. If
NRC determines that the increased
elevation of the water table does not
significantly affect the results of the
performance assessment, NRC may
choose to not require its consideration
in the performance assessment.
(ii) The igneous analysis may be
limited to the effects of a volcanic event
directly intersecting the repository. The
igneous event may be limited to that
causing damage to the waste packages
directly, causing releases of
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Sfmt 4700
radionuclides to the biosphere,
atmosphere, or ground water.
(2) The DOE must assess the effects of
climate change. The climate change
analysis may be limited to the effects of
increased water flow through the
repository as a result of climate change,
and the resulting transport and release
of radionuclides to the accessible
environment. The nature and degree of
climate change may be represented by
constant climate conditions. The
analysis may commence at 10,000 years
after disposal and shall extend through
the period of geologic stability. The NRC
shall specify in regulation the values to
be used to represent climate change,
such as temperature, precipitation, or
infiltration rate of water.
(3) The DOE must assess the effects of
general corrosion on engineered
barriers. The DOE may use a constant
representative corrosion rate throughout
the period of geologic stability or a
distribution of corrosion rates correlated
to other repository parameters.
10. Appendix A to part 197 is added
to read as follows:
■
Appendix A to Part 197—Calculation of
Annual Committed Effective Dose
Equivalent
Unless otherwise directed by NRC, DOE
shall use the radiation weighting factors and
tissue weighting factors in this Appendix to
calculate the internal component of the
annual committed effective dose equivalent
for compliance with §§ 197.20 and 197.25 of
this part. NRC may allow DOE to use updated
factors issued after the effective date of this
regulation. Any such factors shall have been
issued by consensus scientific organizations
and incorporated by EPA into Federal
radiation guidance in order to be considered
generally accepted and eligible for this use.
Further, they must be compatible with the
effective dose equivalent dose calculation
methodology established in ICRP 26 and 30,
and continued in ICRP 60 and 72, and
incorporated in this appendix.
I. Equivalent Dose
The calculation of the committed effective
dose equivalent (CEDE) begins with the
determination of the equivalent dose, HT, to
a tissue or organ, T, listed in Table A.2 below
by using the equation:
H T = ∑ DT,R ⋅ w R
R
where DT,R is the absorbed dose in rads (one
gray, an SI unit, equals 100 rads) averaged
over the tissue or organ, T, due to radiation
type, R, and wR is the radiation weighting
factor which is given in Table A.1 below. The
unit of equivalent dose is the rem (sievert, in
SI units).
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(1) 150 microsieverts (15 millirems)
for 10,000 years following disposal; and
(2) 1 millisievert (100 millirems) after
10,000 years, but within the period of
geologic stability.
(b) The DOE’s performance
assessment must include all potential
pathways of radionuclide transport and
exposure.
■ 7. Section 197.25 is revised to read as
follows:
Federal Register / Vol. 73, No. 200 / Wednesday, October 15, 2008 / Rules and Regulations
E = ∑ w T ⋅ HT .
TABLE A.1—RADIATION WEIGHTING
FACTORS, WR1
Radiation type and energy
range 2
TABLE A.2—TISSUE WEIGHTING
FACTORS, WT
wR value
Photons, all energies ................
Electrons and muons, all energies ........................................
Neutrons, energy
< 10 keV ............................
10 keV to 100 keV ............
> 100 keV to 2 MeV ..........
>2 MeV to 20 MeV ............
> 20 MeV ...........................
Protons, other than recoil protons, > 2 MeV .......................
Alpha particles, fission fragments, heavy nuclei ..............
1
Tissue or organ
1
Gonads .....................................
Bone marrow (red) ...................
Colon ........................................
Lung ..........................................
Stomach ....................................
Bladder .....................................
Breast .......................................
Liver ..........................................
Esophagus ................................
Thyroid ......................................
Skin ...........................................
Bone surface ............................
Remainder ................................
5
10
20
10
5
5
20
1 All values relate to the radiation incident
on the body or, for internal sources, emitted
from the source.
2 See paragraph A14 in ICRP Publication 60
for the choice of values for other radiation
types and energies not in the table.
0.20
0.12
0.12
0.12
0.12
0.05
0.05
0.05
0.05
0.05
0.01
0.01
a b 0.05
a Remainder is composed of the following
tissues: adrenals, brain, extrathoracic airways,
small intestine, kidneys, muscle, pancreas,
spleen, thymus, and uterus.
b The value 0.05 is applied to the massweighted average dose to the Remainder tissues group, except when the following ‘‘splitting rule’’ applies: If a tissue of Remainder receives a dose in excess of that received by
any of the 12 tissues for which weighting factors are specified, a weighting factor of 0.025
(half of Remainder) is applied to that tissue or
organ and 0.025 to the mass-averaged committed equivalent dose equivalent in the rest of
the Remainder tissues.
t0 + τ
H T (τ) =
∫
H T ( t ) dt
t0
for a single intake of activity at time t0 where
HT(t) is the relevant equivalent-dose rate in
a tissue or organ at time t. For the purposes
of this rule, the previously mentioned single
intake may be considered to be an annual
intake.
IV. Internal Component of the Annual
Committed Effective Dose Equivalent
If the annual committed equivalent doses
to the individual tissues or organs resulting
from an annual intake are multiplied by the
appropriate weighting factors, wT, from table
A.2, and then summed, the result will be the
internal component of the annual committed
effective dose equivalent E(t):
E(τ) = ∑ w T ⋅ H T (τ).
T
[FR Doc. E8–23754 Filed 10–14–08; 8:45 am]
BILLING CODE 6560–50–P
ER15OC08.002 ER15OC08.003
III. Annual Committed Tissue or Organ
Equivalent Dose
For internal irradiation from incorporated
radionuclides, the total absorbed dose will be
spread out in time, being gradually delivered
as the radionuclide decays. The time
distribution of the absorbed dose rate will
vary with the radionuclide, its form, the
mode of intake and the tissue within which
it is incorporated. To take account of this
distribution the quantity committed
equivalent dose, HT(t) where t is the
integration time in years following an intake
over any particular year, is used and is the
integral over time of the equivalent dose rate
in a particular tissue or organ that will be
received by an individual following an intake
of radioactive material into the body:
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II. Effective Dose Equivalent
The next step is the calculation of the
effective dose equivalent, E. The probability
of occurrence of a stochastic effect in a tissue
or organ is assumed to be proportional to the
equivalent dose in the tissue or organ. The
constant of proportionality differs for the
various tissues of the body, but in assessing
health detriment the total risk is required.
This is taken into account using the tissue
weighting factors, wT in Table A.2, which
represent the proportion of the stochastic risk
resulting from irradiation of the tissue or
organ to the total risk when the whole body
is irradiated uniformly and HT is the
equivalent dose in the tissue or organ, T, in
the equation:
wT value
61289
Agencies
[Federal Register Volume 73, Number 200 (Wednesday, October 15, 2008)]
[Rules and Regulations]
[Pages 61256-61289]
From the Federal Register Online via the Government Printing Office [www.gpo.gov]
[FR Doc No: E8-23754]
[[Page 61255]]
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Part III
Environmental Protection Agency
-----------------------------------------------------------------------
40 CFR Part 197
Public Health and Environmental Radiation Protection Standards for
Yucca Mountain, Nevada; Final Rule
Federal Register / Vol. 73, No. 200 / Wednesday, October 15, 2008 /
Rules and Regulations
[[Page 61256]]
-----------------------------------------------------------------------
ENVIRONMENTAL PROTECTION AGENCY
40 CFR Part 197
[EPA-HQ-OAR-2005-0083; FRL-8724-9]
RIN 2060-AN15
Public Health and Environmental Radiation Protection Standards
for Yucca Mountain, Nevada
AGENCY: Environmental Protection Agency (EPA).
ACTION: Final rule.
-----------------------------------------------------------------------
SUMMARY: We, the Environmental Protection Agency (EPA), are
promulgating amendments to our public health and safety standards for
radioactive material stored or disposed of in the potential repository
at Yucca Mountain, Nevada. Congress directed us to develop these
standards and required us to contract with the National Academy of
Sciences (NAS) to conduct a study to provide findings and
recommendations on reasonable standards for protection of the public
health and safety. The health and safety standards promulgated by EPA
are to be ``based upon and consistent with'' the findings and
recommendations of NAS. Originally, these standards were promulgated on
June 13, 2001 (66 FR 32074) (the 2001 standards).
On July 9, 2004, the U.S. Court of Appeals for the District of
Columbia Circuit vacated portions of the 2001 standards concerning the
period of time for which compliance must be demonstrated. The Court
ruled that the compliance period of 10,000 years was not ``based upon
and consistent with'' the findings and recommendations of the NAS and
remanded those portions of the standards to EPA for revision. These
remanded provisions are the subject of this action.
This final rule incorporates compliance criteria applicable at
different times for protection of individuals and in circumstances
involving human intrusion into the repository. Compliance will be
judged against a standard of 150 microsieverts per year ([mu]Sv/yr) (15
millirem per year (mrem/yr)) committed effective dose equivalent (CEDE)
at times up to 10,000 years after disposal and against a standard of 1
millisievert per year (mSv/yr) (100 mrem/yr) CEDE at times after 10,000
years and up to 1 million years after disposal. This final rule also
includes several supporting provisions affecting the projections of
expected disposal system performance prepared by the Department of
Energy (DOE).
DATES: Effective Date: This final rule is effective on November 14,
2008.
ADDRESSES: EPA has established a docket for this action under Docket ID
No. EPA-HQ-OAR-2005-0083. All documents in the docket are listed on the
https://www.regulations.gov Web site. Although listed in the index, some
information is not publicly available, e.g., Confidential Business
Information (CBI) or other information whose disclosure is restricted
by statute. Certain other material, such as copyrighted material, is
not placed on the Internet and will be publicly available only in hard
copy form. Publicly available docket materials are available either
electronically through https://www.regulations.gov, for purchase or
access from sources identified in the docket (Docket Nos. EPA-HQ-OAR-
2005-0083-0086 and EPA-HQ-OAR-2005-0083-0087), or in hard copy at the
Air and Radiation Docket, EPA/DC, EPA Headquarters West Building, Room
3334, 1301 Constitution Ave., NW., Washington, DC. The Public Reading
Room is open from 8:30 a.m. to 4:30 p.m., Monday through Friday,
excluding legal holidays. The telephone number for the Air and
Radiation Docket is (202) 566-1742.
FOR FURTHER INFORMATION CONTACT: Ray Clark, Office of Radiation and
Indoor Air, Radiation Protection Division (6608J), U.S. Environmental
Protection Agency, 1200 Pennsylvania Ave., NW., Washington, DC 20460-
0001; telephone number: 202-343-9360; fax number: 202-343-2305; e-mail
address: clark.ray@epa.gov.
SUPPLEMENTARY INFORMATION:
I. General Information
A. Does This Action Apply to Me?
DOE is the only entity regulated by these standards. Our standards
affect NRC only to the extent that, under Section 801(b) of the EnPA,
42 U.S.C. 10141 n., NRC must modify its licensing requirements, as
necessary, to make them consistent with our final standards. Before it
may construct the repository or accept waste at the Yucca Mountain site
and eventually close the repository, DOE must obtain authorization for
these activities from NRC. DOE will be subject to NRC's modified
regulations, which NRC will implement through its licensing
proceedings.
B. How Can I View Items in the Docket?
1. Information Files. EPA is working with the Lied Library at the
University of Nevada-Las Vegas (https://www.library.unlv.edu/about/
hours.html) and the Amargosa Valley, Nevada public library (https://
www.amargosalibrary.com) to provide information files on this
rulemaking. These files are not legal dockets; however, every effort
will be made to put the same material in them as in the official public
docket in Washington, DC. The Lied Library information file is at the
Research and Information Desk, Government Publications Section (702-
895-2200). Hours vary based upon the academic calendar, so we suggest
that you call ahead to be certain that the library will be open at the
time you wish to visit. The other information file is in the Public
Library at 829 East Farm Road in Amargosa Valley, Nevada (phone 775-
372-5340). As of the date of publication, the hours are Monday and
Thursday (9 a.m.-7 p.m.); Tuesday, Wednesday, and Friday (9 a.m.-5
p.m.); and Saturday (9 a.m.-1 p.m.). The library is closed on Sunday.
These hours can change, so we suggest that you call ahead to be certain
when the library will be open.
2. Electronic Access. An electronic version of the public docket is
available through the Federal Docket Management System at https://
www.regulations.gov. You may use https://www.regulations.gov to view
comments, access the index listing of the contents of the official
public docket, and to access those documents in the public docket that
are available electronically. To access the docket go directly to
https://www.regulations.gov and select ``Advanced Docket Search'' under
``More Search Options.'' In the Docket ID window, type in the docket
identification number EPA-HQ-OAR-2005-0083 and click on ``Submit.''
Please be patient since the search could take several minutes. This
will bring you to the ``Docket Search Results'' page. From there, you
may access the docket contents (e.g., EPA-HQ-OAR-2005-0083-0002) by
clicking on the icon in the ``Views'' column.
C. Can I Access Information by Telephone or Via the Internet?
Yes. You may call our toll-free information line (800-331-9477) 24
hours per day. By calling this number, you may listen to a brief update
describing our rulemaking activities for Yucca Mountain, leave a
message requesting that we add your name and address to the Yucca
Mountain mailing list, or request that an EPA staff person return your
call. In addition, we have established an electronic listserv through
which you can receive electronic updates of activities related to this
rulemaking. To subscribe to the listserv, go to https://lists.epa.gov/
read/
[[Page 61257]]
all--forums. In the alphabetical list, locate ``yucca-updates'' and
select ``subscribe'' at the far right of the screen. You will be asked
to provide your e-mail address and choose a password. You also can find
information and documents relevant to this rulemaking on the World Wide
Web at https://www.epa.gov/radiation/yucca. The proposed rule for
today's final rule appeared in the Federal Register on August 22, 2005
(70 FR 49014). We also recommend that you examine the preamble and
regulatory language for the earlier proposed and final rules, which
appeared in the Federal Register on August 27, 1999 (64 FR 46976) and
June 13, 2001 (66 FR 32074), respectively.
D. What Documents are Referenced in This Final Rule?
We refer to a number of documents that provide supporting
information for our Yucca Mountain standards. All documents relied upon
by EPA in regulatory decision-making may be found in our docket (EPA-
HQ-OAR-2005-0083). Other documents, e.g., statutes, regulations, and
proposed rules, are readily available from public sources. The
documents below are referenced most frequently in today's final rule.
Item No. (EPA-HQ-OAR-2005-0083-xxxx).
0076 Technical Bases for Yucca Mountain Standards (the NAS Report),
National Research Council, National Academy Press, 1995.
0086 DOE Final Environmental Impact Statement, DOE/EIS-0250,
February 2002.
0383 ``Geological Disposal of Radioactive Waste,'' International
Atomic Energy Agency Final Safety Requirements (WS-R-4), 2006.
0417 ``Radiation Protection Recommendations as Applied to the
Disposal of Long-Lived Solid Radioactive Waste,'' International
Commission on Radiological Protection Publication 81, 2000.
0408 ``Regulating the Long-Term Safety of Geological Disposal:
Towards a Common Understanding of the Main Objectives and Bases of
Safety Criteria,'' OECD Nuclear Energy Agency, NEA-6182, 2007.
0421 ``1990 Recommendations of the International Commission on
Radiological Protection,'' ICRP Publication 60.
0423 ``2007 Recommendations of the International Commission on
Radiological Protection,'' ICRP Publication 103.
0431 Response to Comments Document for Final Rule, EPA-402-R-08-
008, June 2007.
Acronyms and Abbreviations
We use many acronyms and abbreviations in this document. These
include:
BID--background information document
CED--committed effective dose
CEDE--committed effective dose equivalent
CFR--Code of Federal Regulations
DOE--U.S. Department of Energy
EIS--Environmental Impact Statement
EnPA--Energy Policy Act of 1992
EPA--U.S. Environmental Protection Agency
FEIS--Final Environmental Impact Statement
FEPs--features, events, and processes
FR--Federal Register
GCD--greater confinement disposal
HLW--high-level radioactive waste
IAEA--International Atomic Energy Agency
ICRP--International Commission on Radiological Protection
NAS--National Academy of Sciences
NEA--Nuclear Energy Agency
NEI--Nuclear Energy Institute
NRC--U.S. Nuclear Regulatory Commission
NRDC--Natural Resources Defense Council
NTS--Nevada Test Site
NTTAA--National Technology Transfer and Advancement Act
NWPA--Nuclear Waste Policy Act of 1982, as amended
NWPAA--Nuclear Waste Policy Amendments Act of 1987
OECD--Organization for Economic Cooperation and Development
OMB--Office of Management and Budget
RMEI--reasonably maximally exposed individual
SSI--Swedish Radiation Protection Authority
SNF--spent nuclear fuel
TRU--transuranic
UK--United Kingdom
UMRA--Unfunded Mandates Reform Act of 1995
U.S.C.--United States Code
WIPP LWA--Waste Isolation Pilot Plant Land Withdrawal Act of 1992
Outline of This Action
I. What Is the History of This Action?
A. Promulgation of 40 CFR Part 197 in 2001
B. Legal Challenges to 40 CFR Part 197
II. Summary of Proposed Amendments to 40 CFR Part 197 and Public
Comments
A. How Did We Propose To Amend Our 2001 Standards?
B. What Factors Did We Consider in Developing Our Proposal?
C. In Making Our Decisions, How Did We Incorporate Public
Comments on the Proposed Rule?
D. What Public Comments Did We Receive?
III. What Final Amendments Are We Issuing With This Action?
A. What Dose Standards Will Apply?
1. What Is the Dose Standard Between 10,000 Years and 1 Million
Years?
2. What Is the Dose Standard for 10,000 Years After Disposal?
3. How Does Our Final Rule Protect Public Health and Safety?
4. How Did We Consider Uncertainty and Reasonable Expectation?
5. How Did We Consider Background Radiation in Developing the
Peak Dose Standard?
6. How Does Our Rule Protect Future Generations?
7. What is Geologic Stability and Why Is it Important?
8. Why Is the Period of Geologic Stability 1 Million Years?
9. How Will NRC Judge Compliance?
10. How Will DOE Calculate the Dose?
B. How Will This Final Rule Affect DOE's Performance
Assessments?
IV. Statutory and Executive Order Reviews
A. Executive Order 12866: Regulatory Planning and Review
B. Paperwork Reduction Act
C. Regulatory Flexibility Act
D. Unfunded Mandates Reform Act
E. Executive Order 13132: Federalism
F. Executive Order 13175: Consultation and Coordination With
Indian Tribal Governments
G. Executive Order 13045: Protection of Children From
Environmental Health & Safety Risks
H. Executive Order 13211: Actions That Significantly Affect
Energy Supply, Distribution, or Use
I. National Technology Transfer and Advancement Act
J. Executive Order 12898: Federal Actions To Address
Environmental Justice in Minority Populations and Low-income
Populations
K. Congressional Review Act
I. What Is the History of This Action?
Radioactive wastes result from the use of nuclear fuel and other
radioactive materials. Today, we are revising certain standards
pertaining to spent nuclear fuel, high-level radioactive waste, and
other radioactive waste (we refer to these items collectively as
``radioactive materials'' or ``waste'') that may be stored or disposed
of in the Yucca Mountain repository. When we discuss storage or
disposal in this document in reference to Yucca Mountain, we note that,
while Public Law 107-200 approved the site at Yucca Mountain for the
development of a repository for the disposal of spent nuclear fuel and
high-level radioactive waste, no licensing decision has been made
regarding the acceptability of the proposed Yucca Mountain facility for
storage or disposal as of the date of this publication. To save space
and to avoid excessive repetition, we will not describe Yucca Mountain
as a ``potential'' repository; however, we intend this meaning to
apply.
Once nuclear reactions have consumed a certain percentage of the
uranium or other fissionable material in nuclear reactor fuel, the fuel
no longer is useful for its intended purpose. It
[[Page 61258]]
then is known as ``spent'' nuclear fuel (SNF). It is possible to
recover specific radionuclides from SNF through ``reprocessing,'' which
is a process that dissolves the SNF, thus separating the radionuclides
from one another. Radionuclides not recovered through reprocessing
become part of the acidic liquid wastes that the Department of Energy
(DOE) plans to convert into various types of solid materials. High-
level radioactive waste (HLW) is the highly radioactive liquid or solid
wastes that result from reprocessing SNF. The SNF that does not undergo
reprocessing prior to disposal remains inside the fuel assembly and
becomes the final waste form for disposal in the repository.
In the United States, SNF and HLW have been produced since the
1940s, mainly as a result of commercial power production and national
defense activities. Since the inception of the nuclear age, the proper
disposal of these wastes has been the responsibility of the Federal
government. The Nuclear Waste Policy Act of 1982, as amended (NWPA, 42
U.S.C. Chapter 108) sets forth the framework for the disposal of SNF
and HLW. In general, DOE is responsible for siting, constructing, and
operating an underground geologic repository for the disposal of SNF
and HLW and the Nuclear Regulatory Commission (NRC) is responsible for
licensing the construction and operation of this repository, including
permanent closure and decommissioning of the surface facilities. In
making this licensing decision for the Yucca Mountain repository, NRC
must utilize radiation protection standards that EPA establishes
pursuant to section 801(a) of the Energy Policy Act of 1992 (EnPA, Pub.
L. 102-486).\1\ Thus, today we are promulgating amendments to our
public health protection standards at 40 CFR part 197 (which, pursuant
to EnPA section 801(a), apply only to releases of radioactive material
stored or disposed of at the Yucca Mountain site, rather than generally
applicable). NRC will amend its regulations to be consistent with these
standards.
---------------------------------------------------------------------------
\1\ EnPA, Public Law No. 102-486, 102 Stat. 2776, 42 U.S.C.
10141 n. (1994).
---------------------------------------------------------------------------
On June 3, 2008, pursuant to the NWPA, as amended, DOE submitted a
license application to NRC seeking a license to construct the
repository. NRC will determine whether DOE has met NRC's requirements,
including those implementing 40 CFR part 197, and whether to grant or
deny authorization to construct the repository and a license to receive
radioactive material at the Yucca Mountain site.
In 1985, we established generic standards for the management,
storage, and disposal of SNF, HLW, and transuranic (TRU) radioactive
waste (see 40 CFR part 191, 50 FR 38066, September 19, 1985), which
were intended to apply to facilities utilized for the storage or
disposal of these wastes, including Yucca Mountain. In 1987, the U.S.
Court of Appeals for the First Circuit remanded the disposal standards
in 40 CFR part 191 (NRDC v. EPA, 824 F.2d 1258 (1st Cir. 1987)). We
later amended and reissued those standards to address issues that the
court raised. Also in 1987, the Nuclear Waste Policy Amendments Act
(NWPAA, Pub. L. 100-203) amended the NWPA by, among other actions,
selecting Yucca Mountain, Nevada, as the only potential site that DOE
should characterize for a geologic repository for SNF and HLW. In
October 1992, Congress enacted the EnPA and the Waste Isolation Pilot
Plant Land Withdrawal Act (WIPP LWA, Pub. L. 102-579). These statutes
changed our obligations concerning radiation standards for the Yucca
Mountain candidate repository. The WIPP LWA:
(1) Reinstated the 40 CFR part 191 disposal standards, except those
portions that were the specific subject of the remand by the First
Circuit;
(2) Required us to issue standards to replace the portion of the
challenged standards remanded by the court; and
(3) Exempted the Yucca Mountain site from the 40 CFR part 191
disposal standards.
We issued the amended 40 CFR part 191 disposal standards, which
addressed the judicial remand, on December 20, 1993 (58 FR 66398).
The EnPA set forth our responsibilities as they relate to Yucca
Mountain and directed us to set public health and safety radiation
standards for Yucca Mountain. Specifically, section 801(a)(1) of the
EnPA directed us to ``promulgate, by rule, public health and safety
standards for the protection of the public from releases from
radioactive materials stored or disposed of in the repository at the
Yucca Mountain site.'' Section 801(a)(2) directed us to contract with
the National Academy of Sciences (NAS) to conduct a study to provide us
with its findings and recommendations on reasonable standards for
protection of public health and safety from releases from the Yucca
Mountain disposal system. Moreover, it provided that our standards
shall be the only such standards applicable to the Yucca Mountain site
and are to be based upon and consistent with NAS's findings and
recommendations. On August 1, 1995, NAS released its report,
``Technical Bases for Yucca Mountain Standards'' (the NAS Report)
(Docket No. EPA-HQ-OAR-2005-0083-0076).
A. Promulgation of 40 CFR Part 197 in 2001
Pursuant to the EnPA, we developed standards specifically
applicable to releases from radioactive material stored or disposed of
in the Yucca Mountain repository. In doing so, we considered the NAS
Report, our generic standards in 40 CFR part 191, and other relevant
information, precedents, and analyses.
We evaluated 40 CFR part 191 because those standards were developed
to apply to sites selected for storage and disposal of SNF and HLW.
Thus, we believed that 40 CFR part 191 already included the major
components of standards needed for any specific site, such as Yucca
Mountain. However, we recognized that all the components would not
necessarily be directly transferable to the situation at Yucca
Mountain, and that some modification might be necessary. We also
considered that some components of the generic standards would not be
carried into site-specific standards, since not all of the conditions
found among all potential sites are present at Yucca Mountain. See 66
FR 32076-32078, June 13, 2001 (Docket No. EPA-HQ-OAR-2005-0083-0042),
for a more detailed discussion of the role of 40 CFR part 191 in
developing 40 CFR part 197.
We also considered the findings and recommendations of the NAS in
developing standards for Yucca Mountain. In some cases, provisions of
40 CFR part 191 were already consistent with NAS's analysis (e.g.,
level of protection for the individual). In other cases, we used the
NAS Report to modify or draw out parts of 40 CFR part 191 to apply more
directly to Yucca Mountain (e.g., the stylized drilling scenario for
human intrusion). See the NAS Report for a complete description of
findings and recommendations (Docket No. EPA-HQ-OAR-2005-0083-0076).
Because our standards are intended to apply specifically to the
Yucca Mountain disposal system, we tailored our approach to consider
the characteristics of the site and the local populations. Yucca
Mountain is in southwestern Nevada approximately 100 miles northwest of
Las Vegas. The eastern part of the site is on the Nevada Test Site
(NTS). The northwestern part of the site is on the Nevada Test and
Training Range (referred to in our proposal as the Nellis Air Force
Range). The southwestern part of the site is on Bureau of Land
Management land. The
[[Page 61259]]
area has a desert climate with topography typical of the Basin and
Range province. Yucca Mountain is made of layers of ashfalls from
volcanic eruptions that happened more than 10 million years ago. There
are two major aquifers beneath Yucca Mountain. Regional ground water in
the vicinity of Yucca Mountain is believed to flow generally in a
south-southeasterly direction. For more detailed descriptions of Yucca
Mountain's geologic and hydrologic characteristics, and the disposal
system, please see Chapter 7 of the 2001 Background Information
Document (BID) (Docket No. EPA-HQ-OAR-2005-0083-0050) and the preamble
to the proposed rule (64 FR 46979-46980, August 27, 1999, Docket No.
EPA-HQ-OAR-2005-0083-0041).
We proposed the original standards for Yucca Mountain on August 27,
1999 (64 FR 46976). In response to our proposal, we received more than
800 public comments and conducted four public hearings. After
evaluating public comments, we issued final standards (66 FR 32074,
June 13, 2001). See the Response to Comments document from that
rulemaking for more discussion of comments (Docket No. EPA-HQ-OAR-2005-
0083-0043).
The final standards issued in 2001 as 40 CFR part 197 included the
following:
A standard to protect the public during management and
storage operations on the Yucca Mountain site;
An individual-protection standard to protect the public
from releases from the undisturbed disposal system;
A human-intrusion standard to protect the public after
disposal from releases caused by a drilling penetration into the
repository;
A set of standards to protect ground water from
radionuclide contamination caused by releases from the disposal system;
The requirement that compliance with the disposal
standards be shown for 10,000 years;
The requirement that DOE continue its projections for the
individual-protection and human-intrusion standards beyond 10,000 years
to the time of peak (maximum) dose, and place those projections in the
Environmental Impact Statement (EIS) for Yucca Mountain;
The concept of the Reasonably Maximally Exposed Individual
(RMEI), defined as a hypothetical person whose lifestyle is
representative of the local population living today in the Town of
Amargosa Valley, as the individual against whom the disposal standards
should be assessed; and
The concept of a ``controlled area,'' defined as an area
immediately surrounding the repository whose geology is considered part
of the natural barrier component of the overall disposal system, and
inside of which radioactive releases are not regulated.
More detail on these aspects of the 2001 final rule may be found at
66 FR 32074-32134, June 13, 2001, and 70 FR 49019-49020, August 22,
2005.
B. Legal Challenges to 40 CFR Part 197
Various aspects of our standards were challenged in lawsuits filed
with the U.S. Court of Appeals for the District of Columbia Circuit in
July 2001. These challenges and the Court's subsequent ruling are
described briefly here, emphasizing the aspects leading to today's
final rule, and in more detail in the preamble to the proposed rule (70
FR 49014, August 22, 2005).
The State of Nevada, the Natural Resources Defense Council (NRDC),
and several other petitioners challenged various aspects of our final
standards on the grounds that they were insufficiently protective and
had not been adequately justified. The focus of this challenge was the
10,000-year compliance period. Nevada and NRDC claimed that EPA's
promulgation of numerical standards that applied for 10,000 years after
disposal violated the EnPA because such standards were not ``based upon
and consistent with'' the findings and recommendations of the NAS. NAS
recommended standards that would apply to the time of maximum risk,
within the limits imposed by the long-term geologic stability of the
site, and stated that there is ``no scientific basis for limiting the
time period of the individual-risk standard to 10,000 years or any
other value.'' (NAS Report p. 55) The Nuclear Energy Institute (NEI)
challenged the ground-water protection standards as unnecessary to
protect public health and safety, contrary to recommendations of the
NAS, and outside our authority under the EnPA.
The DC Circuit Court's July 9, 2004 decision dismissed NEI's
challenge, and all of the challenges by Nevada and NRDC, except one. On
the question of EPA's 10,000-year compliance period, the Court upheld
the challenge, ruling that EPA's action was not ``based upon and
consistent with'' the NAS Report, and that EPA had not sufficiently
justified on policy grounds its decision to apply compliance standards
only to the first 10,000 years after disposal. Nuclear Energy Institute
v. Environmental Protection Agency, 373 F.3d 1251 (D.C. Cir. 2004) (NEI
).
The Court concluded that ``we vacate 40 CFR part 197 to the extent
that it incorporates a 10,000-year compliance period * * *.'' (Id. at
1315) The Court did not address the protectiveness of the 150 [mu]Sv/yr
(15 mrem/yr) dose standard applied over the 10,000-year compliance
period, nor was the protectiveness of the 15 mrem/yr standard
challenged. It ruled only that the compliance period was not consistent
with or based upon the NAS findings and recommendations and, therefore,
was contrary to the plain language of the EnPA.
As the Court noted, NAS stated that it had found ``no scientific
basis for limiting the time period of the individual-risk standard to
10,000 years or any other value,'' and that ``compliance assessment is
feasible * * * on the time scale of the long-term stability of the
fundamental geologic regime--a time scale that is on the order of
106 years at Yucca Mountain.'' As a result, and given that
``at least some potentially important exposures might not occur until
after several hundred thousand years * * * we recommend that compliance
assessment be conducted for the time when the greatest risk occurs.''
(NAS Report pp. 6-7) Today's action addresses this recommendation and
the DC Circuit ruling.
II. Summary of Proposed Amendments to 40 CFR Part 197 and Public
Comments
The primary goal of our proposal issued in 2005 was to gather
public comment on the appropriate response to the Court decision and
NAS recommendation to assess compliance at the time of maximum dose
(risk). Therefore, our proposed amendments centered on extending the
compliance period to capture the peak projected dose from the Yucca
Mountain disposal system ``within the limits imposed by the long-term
stability of the geologic environment.'' (NAS Report p. 2) Of course,
establishing a radiological protection standard to apply at the time of
peak dose is a uniquely challenging task. Only a small number of
countries have established standards of any kind for the geologic
disposal of SNF and HLW. Of these, only Switzerland has established a
quantitative standard applicable for as long as 1 million years,
although we are aware that other regulatory bodies outside the U.S. are
contemplating the need to establish some type of regulation addressing
these extremely long time frames. Comments received in the course of
this rulemaking have been helpful given the extraordinary technical
complexity of this task.
[[Page 61260]]
A. How Did We Propose To Amend Our 2001 Standards?
We considered carefully the language and reasoning of the Court's
decision in revising our 2001 standards. As originally promulgated in
2001, 40 CFR part 197 contained four sets of standards against which
compliance would be assessed. The storage standard applies to exposures
of the general public during the operational period, when waste is
received at the Yucca Mountain site, handled in preparation for
emplacement in the repository, emplaced in the repository, and stored
in the repository until final closure. The three disposal standards
apply to releases of radionuclides from the disposal system after final
closure, and include an individual-protection standard, a human-
intrusion standard, and a set of ground-water protection standards.
The Court's ruling vacated only one aspect of 40 CFR part 197: The
10,000-year compliance period applicable to the disposal standards.
Therefore, the storage standard, which is applicable only for the
period before disposal, is not affected by the ruling. Further, the
Court recognized that the ground-water protection standards were issued
as an expression of EPA's overall ground-water protection policies and
were not among the standards addressed by the NAS, either in form or
purpose (``NAS treated the compliance-period and ground-water issues
quite differently * * * NAS made no `finding' or `recommendation' that
EPA's regulation could fail to be `based upon and consistent with' ''
(NEI, 373 F.3d at 1282)). Therefore, we concluded that the Court's
vacature of the 10,000-year compliance period, which was explicitly
tied to recommendations concerning the individual-protection standard,
does not extend to the ground-water provisions. As a result, we did not
propose to amend the ground-water protection standards. Nothing in
today's final rule affects those standards.
We proposed to revise only the individual-protection and human-
intrusion standards, along with certain supporting provisions related
to the way DOE must consider features, events, and processes (FEPs) in
its compliance analyses (70 FR 49014, August 22, 2005). In addition, we
proposed to adopt updated scientific factors for calculating doses to
show compliance with the storage, individual-protection, and human-
intrusion standards. We requested comments only on those aspects of the
individual-protection and human-intrusion standards which were to be
amended. Specifically, we proposed to:
Extend the compliance period for the individual-protection
and human-intrusion standards to 1 million years after disposal
(closure), consistent with NAS estimates regarding the ``long-term
stability of the geologic environment'';
Retain the dose standard of 150 [mu]Sv/yr (hereafter, 15
mrem/yr) committed effective dose equivalent (CEDE) for the first
10,000 years after disposal, as promulgated in 2001;
Establish a dose standard of 3.5 mSv/yr (hereafter, 350
mrem/yr) CEDE for the period between 10,000 years and 1 million years;
Clarify that the arithmetic mean of the distribution of
projected results will be compared to the dose standard for the initial
10,000 years, and specify use of the median of the distribution of
projected results between 10,000 and 1 million years;
Retain the probability threshold (1 in 10,000 chance of
occurring in 10,000 years, or 1 in 100 million chance of occurring per
year) below which ``very unlikely'' FEPs may be excluded from
consideration;
Allow FEPs with a probability of occurring above the
probability threshold to be excluded if they would not significantly
affect the results of performance assessments in the initial 10,000
years;
Require consideration of seismic and igneous events
causing direct damage to the engineered barrier system during the 1
million-year period;
Require consideration of the effects of increased water
flow through the repository resulting from climate change, which could
be represented by constant conditions between 10,000 and 1 million
years;
Require consideration of the effects of general corrosion
of the engineered barriers between 10,000 and 1 million years; and
Require use of updated scientific factors, based on
Publications 60 and 72 of the International Commission on Radiation
Protection (ICRP), to calculate dose for comparison with the storage,
individual-protection, and human-intrusion standards.
B. What Factors Did We Consider in Developing Our Proposal?
Of great concern in extending the compliance period to 1 million
years is the increasing uncertainty associated with numerical
projections of radionuclide releases from the Yucca Mountain disposal
system and subsequent exposures incurred by the Reasonably Maximally
Exposed Individual (RMEI). This uncertainty affects not only the
projections themselves, but also the interpretation of the results.
There is general agreement in the international community that dose
projections over periods as long as 1 million years cannot be viewed in
the same context or with the same confidence as projections for periods
as ``short'' as 10,000 years. As a result, the nature of regulatory
decision-making fundamentally changes when faced with the prospect of
compliance projections for the next 1 million years. International
guidance from the International Atomic Energy Agency (IAEA) and Nuclear
Energy Agency (NEA), as well as geologic disposal programs in other
countries, recognize this difficulty and accommodate it by viewing
longer-term projections in a more qualitative manner, to be balanced
and supplemented by other considerations that would provide confidence
in the long-term safety of the disposal system. In effect, numerical
dose projections are given less weight in decision-making at longer
times.\2\ Such approaches discourage comparison of projections against
a strict compliance limit.
---------------------------------------------------------------------------
\2\ For example, the ICRP's most recent recommendations note
that ``both the individual doses and the size of the exposed
population become increasingly uncertain as time increases. The
Commission is of the opinion that in the decision-making process,
owing to the increasing uncertainties, giving less weight to very
low doses and to doses received in the distant future could be
considered.'' (Publication 103, 2007, Docket No. EPA-HQ-OAR-2005-
0083-0423, Paragraph 222)
---------------------------------------------------------------------------
This uncertainty was the overriding reason for limiting the
compliance period to 10,000 years in our 2001 rule. We supplemented
that 10,000-year compliance period by requiring DOE to continue
projections through the time of peak dose, consistent with the approach
favored by the international community. However, while we believed this
approach was consistent with the NAS recommendation to assess
compliance at the time of maximum dose (risk) and the committee's
acknowledgment that policy considerations would also play a role in
determining the compliance period, the Court concluded that it was
inconsistent with the NAS recommendation. We concluded that the most
direct way to address the Court's ruling would be to establish a
numeric compliance standard for the time of peak dose, within the
period of geologic stability at Yucca Mountain, which NAS judged to be
``on the order of one million years.'' (NAS Report p. 2)
In establishing our final standards, we have considered that the
level of uncertainty increases as the time period covered by DOE's
performance
[[Page 61261]]
assessment increases.\3\ Therefore, it is reasonable for us to consider
how the compliance standard itself might also need to change.
Specifically, we do not believe that extending the 10,000-year
individual-protection standard of 15 mrem/yr to apply for 1 million
years adequately accounts for the considerations outlined above or
represents a reasonable test of the disposal system (more extensive
discussion of uncertainty in performance assessments is in section
III.A.4 of this document, ``How Did We Consider Uncertainty and
Reasonable Expectation?''); see also 66 FR 32098. We turned back to the
international technical literature for advice regarding appropriate
points of comparison for doses projected over hundreds of thousands of
years. A number of sources suggested that natural sources of
radioactivity would provide an appropriate benchmark for such
comparisons. In exploring this approach further, we found that the
variation in background radiation across the United States covered a
wide range (from roughly 100 mrem/yr to 1 rem/yr), primarily because of
local variation in radon exposures. We chose for our proposal a level
of 350 mrem/yr, which is close to a widely-cited estimate of 300 mrem/
yr for the national average background radiation exposure (NAS Report
Table 2-1), but specifically represented the difference between
estimated background levels in Amargosa Valley and the State of
Colorado. This level was proposed for both the individual-protection
and human-intrusion standards as offering both a reasonable level of
protection and a sound basis for regulatory decision-making when
exposures are projected to occur hundreds of thousands of years into
the future. Selecting such a level would also provide an indication
that exposures incurred by the RMEI in the far future from the
combination of natural background radiation and releases from the Yucca
Mountain disposal system would not exceed exposures incurred by
residents of other parts of the country today from natural sources
alone. Today's final rule adopts a more stringent standard that is not
derived from an analysis of background radiation, as explained in
sections III.A.1 (``What is the Peak Dose Standard Between 10,000 and 1
Million Years After Disposal?'') and III.A.5 (``How Did We Consider
Background Radiation in Developing The Peak Dose Standard?'') of this
document.
---------------------------------------------------------------------------
\3\ ``We recognize that there are significant uncertainties in
the calculations and that these uncertainties increase as the time
at which peak risk occurs increases.'' (NAS Report p. 56)
---------------------------------------------------------------------------
Uncertainty in long-term projections also influenced our proposal.
Given the probabilistic nature of performance assessments, it is
possible that some combinations of parameter values will result in very
high doses, even if such combinations have an extremely low probability
of occurring. Although there may be only a few results that are very
high, extreme results have the potential to exert a strong influence on
the arithmetic mean, which could make the mean less representative of
all performance projections. This possibility may be increased by the
introduction of additional, and possible excessive, conservatisms as a
way to account for uncertainties. We expressed a preference for a
statistical measure that would not be strongly affected by either very
high- or low-end estimates, believing it appropriate to focus on the
``central tendency'' of the distribution, where the bulk of the results
might be expected to be found. We proposed the median of the
distribution as being most representative of central tendency. Because
it is always located at the point where half the distribution is higher
and half lower, the median depends only on the relative nature of the
distribution, rather than the absolute calculated values. Given our
concerns about specifying a peak dose compliance value against which
performance would be judged for a period up to 1 million years, we
believed the median might also provide a reasonable test of long-term
performance. Today's final rule departs from the proposal by adopting
the arithmetic mean as the statistical measure of compliance to be
applied at all times, as explained in section III.A.9 of this document
(``How Will NRC Judge Compliance?'').
Our consideration of FEPs also was affected to some extent by
uncertainty, as well as by conclusions of the NAS committee. In our
proposal, the overall probability threshold for inclusion of FEPs
remained the same as in the 2001 rule, which we believe provides a very
inclusive initial screen that captures both major and minor factors
potentially affecting performance. Uncertainty plays a role in the
sense that very gradual or infrequent processes and events may begin to
influence performance only at times in the hundreds of thousands of
years, when the overall uncertainty of assessments is increasing. The
additional uncertainty introduced by these slow-acting FEPs led us to
propose the exclusion of FEPs if they were not significant to the
assessments in the initial 10,000 years. We believed this would still
provide for robust assessments that would address the factors of most
importance over the entire 1 million-year period. We did consider in
our proposal whether significant FEPs might not be captured using this
approach. In evaluating whether excluded FEPs might become more
probable or more significant after 10,000 years, and therefore should
not be eliminated, we identified general corrosion as a FEP that is
certain to occur and represents a significant failure mechanism at
longer times, even though it is less significant in the initial 10,000
years.
We also consulted the NAS Report for advice on handling long-term
FEPs. NAS identified three ``modifiers'' that it believed could
reasonably be included in assessments: seismic events, igneous events,
and climate change. (NAS Report p. 91) We developed provisions
addressing these FEPs that incorporated the views expressed by the NAS.
For seismic and igneous events, we proposed that DOE focus its
attention on events causing direct damage to the engineered barriers.
We took this approach because failure of the engineered barrier system,
particularly the waste packages, is the predominant factor in
determining the timing and magnitude of the peak dose, and is the
overriding uncertainty in assessing performance of the disposal system.
To address climate change, we required DOE to focus on the effects of
increased water flow through the repository, which is the climatic
effect with the most influence on release and transport of
radionuclides. We determined that such a focus would provide the basis
for a reasonable test of the disposal system, and that climate change
beyond 10,000 years could be represented by constant conditions
reflecting precipitation levels that differ from current conditions,
which eliminates unresolvable speculation regarding the timing,
magnitude, and duration of climatic cycles over this time frame. We
also directed that NRC establish the exact nature of future climate
characteristics to be used in performance assessments. NRC subsequently
issued a proposal to specify a range of values for deep percolation
into the repository, which DOE would use as another parameter in its
probabilistic performance assessments. (70 FR 53313, September 8, 2005)
Finally, we proposed to update the factors used to calculate dose
for the storage, individual-protection, and human-intrusion standards.
Our generic standards in 40 CFR part 191, and by inference our Yucca
Mountain standards in 2001, specified the factors associated with ICRP
Publications 26
[[Page 61262]]
and 30 (Docket Nos. EPA-HQ-OAR-2005-0083-0425 and 0428, respectively).
Since we issued 40 CFR part 191, ICRP has modified the models and
associated organ-weighting factors to more accurately calculate dose.
See ICRP Publications 60 and 72 (Docket Nos. EPA-HQ-OAR-2005-0083-0421
and 0427, respectively). We used this newer method in 1999 to develop
our Federal Guidance Report 13, ``Cancer Risk Coefficients from
Exposure to Radionuclides'' (Docket No. EPA-HQ-OAR-2005-0083-0072).
Where possible, we believe it is appropriate to adopt the latest
scientific methods.\4\
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\4\ ICRP published its most recent recommendations in
Publication 103, issued in 2007 (Docket No. EPA-HQ-OAR-2005-0083-
0423). EPA has not determined the impact of these recommendations on
its current dose and risk estimates, but may decide to adopt them in
the future. Today's final rule will incorporate the ICRP 60
recommendations as consistent with EPA's current federal guidance;
however, we have provided some flexibility for use of newer
dosimetry in the future if deemed appropriate by NRC.
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C. In Making Our Final Decisions, How Did We Incorporate Public
Comments on the Proposed Rule?
Section 801(a)(1) of the EnPA requires us to set public health and
safety radiation protection standards for Yucca Mountain by rulemaking.
Pursuant to Section 4 of the Administrative Procedure Act (APA),
regulatory agencies engaging in informal rulemaking must provide notice
of a proposed rulemaking, an opportunity for the public to comment on
the proposed rule, and a general statement of the basis and purpose of
the final rule.\5\ The notice of proposed rulemaking required by the
APA must ``disclose in detail the thinking that has animated the form
of the proposed rule and the data upon which the rule is based.''
(Portland Cement Association v. Ruckelshaus, 486 F. 2d 375, 392-94 (DC
Cir. 1973)) The public thus is enabled to participate in the process by
making informed comments on the proposal. This provides us with the
benefit of ``an exchange of views, information, and criticism between
interested persons and the agency.'' (Id.)
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\5\ 5 U.S.C. 553.
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There are two primary mechanisms by which we explain the issues
raised in public comments and our reactions to them. First, we discuss
broad or major comments in the succeeding sections of this preamble.
Second, we are publishing a document, accompanying today's action,
entitled ``Response to Comments'' (Docket No. EPA-HQ-OAR-2005-0083-
0431). The Response to Comments document provides more detailed
responses to issues addressed in the preamble. It also addresses all
other significant comments on the proposal. We gave all the comments we
received, whether written or oral, consideration in developing the
final rule.
D. What Public Comments Did We Receive?
The public comment period ended November 21, 2005. We received more
than 300 individual submittals, although any particular submittal could
contain many specific comments. We also received many more submissions
as part of mass comment efforts, in which organizations encourage
commenters to use prepared texts or comment on specific aspects of the
proposal. All, or representative, comments are available electronically
through the Federal Document Management System (FDMS), available at
https://www.regulations.gov. See the ``General Information'' section of
this document for instructions on how to access the electronic docket.
Some submittals may be duplicated in FDMS, as a commenter may have used
several methods to ensure the comments were received, such as fax, e-
mail, U.S. mail, or directly through FDMS.
A significant number of comments addressed the proposed peak dose
standard of 350 mrem/yr, which would apply between 10,000 and 1 million
years. Most commenters opposed our proposal, arguing that it is much
higher than any previous standard, is not protective, is not equitable
to future generations, and is based on inappropriate use of background
radiation data. Many commenters also took issue with our proposal to
use the median of the distribution of results as the statistical
measure between 10,000 and 1 million years, viewing this measure as
inconsistent with NAS recommendations to use the mean. Commenters also
viewed the median as too ``lax'' and likely to discount scenarios that
would result in high exposures. We also received comment on our
proposal concerning the assessment of FEPs beyond 10,000 years, with
some comments expressing the opinion that we had inappropriately
constrained the analyses, leaving out potentially significant FEPs.
Some commenters disagreed with our general premise that uncertainty
increases with assessment time and further disagreed that we should
take uncertainties into account when considering standards applicable
to the far future. These specific comments, and our responses to them,
will be discussed in more detail in section III of this document and in
the Response to Comments document associated with this action (Docket
No. EPA-HQ-OAR-2005-0083-0431).
Some commenters also questioned our conclusion that extending the
compliance period is the appropriate way to respond to the Court
ruling. These commenters point out that the Court's opinion could be
interpreted to permit us to justify the approach taken in our 2001
standards. They cite statements by the Court such as ``[i]t would have
been one thing had EPA taken the Academy's recommendations into account
and then tailored a standard that accommodated the agency's policy
concerns'' and ``[h]ad EPA begun with the Academy's recommendation to
base the compliance period on peak dosage and then made adjustments to
accommodate policy considerations not considered by NAS, this might be
a very different case'' (NEI, 373 F.3d at 1270 and 1273, respectively)
to support the thesis that the Court's judgment was based primarily on
the presentation of our case, rather than the substance. In the
commenters' view, the Court would have been receptive to our arguments
had they been presented differently, and the Court provided a clear
``road map'' to justify keeping our original standards in place. In
addition, these and other commenters viewed extending the compliance
period to 1 million years as not justifiable either scientifically or
as a matter of public policy. We believe that the approach we are
taking is the most appropriate way to address the concerns raised by
the Court's decision, particularly given the weight accorded by the
Court to the NAS technical recommendations concerning the period of
geologic stability. As we stated in our proposal, ``it is not clear how
EPA's earlier explanation of its policy concerns might be reconciled
with NAS's technical recommendation.'' (70 FR 49032) Accordingly,
today's final rule implements the NAS technical recommendation with
regard to the length of time for the compliance period while still
accommodating our policy concerns in the provisions related to the peak
dose standard, and FEPs.
We received some comments that suggested we should have provided
more or better opportunities for public participation in our decision
making process. For example, comments suggested that we should have
rescheduled public hearings, extended the public comment period, and
provided alternatives to the public hearing process. We provided
numerous opportunities and avenues for public participation in the
development of these standards. For example, we held public hearings in
Washington, DC; Las
[[Page 61263]]
Vegas, NV; and Amargosa Valley, NV. We also opened a 60-day public
comment period and met with key stakeholders before and during that
time. In response to requests from stakeholders, we extended the public
comment period by 30 days and held an additional public hearing in Las
Vegas. We conducted targeted outreach to Native American tribal groups
and have fully considered all comments received through December 31,
2005, after the end of the extended public comment period. These
measures are in full compliance with the public participation
requirements of the Administrative Procedure Act.
Several commenters supported our role in setting standards for
Yucca Mountain. Other commenters thought that aspects of our standards
duplicate NRC's implementation role. We believe the provisions of this
rule clearly are within our authority and they are central to the
concept of a public health protection standard. We also believe our
standards leave NRC the necessary flexibility to adapt to changing
conditions at Yucca Mountain or to impose additional requirements in
its implementation efforts, if NRC deems them to be necessary.
We also received many general comments, and others addressing
topics that are outside the scope of our authority under the EnPA. For
example, several commenters simply expressed their support for, or
opposition to, the Yucca Mountain repository. Other comments suggested
our standards should explicitly consider radiation exposures from all
sources because of the site's proximity to the Nevada Test Site (NTS)
and other sources of potential contamination. Also, a number of
commenters suggested that we should explore alternative methods of
waste disposal, such as neutralizing radionuclides. Comments also
expressed concern regarding risks of transporting radioactive materials
to Yucca Mountain. These comments all raise considerations that are
outside the scope of our authority and this rulemaking.
Many comments touched on issues related to our authority and
standards, but outside the limited scope of this rulemaking. In
particular, many comments urged us to extend the ground-water
protection limits to the time of peak dose within the 1 million-year
compliance period. Many of these commenters disagreed with our position
that the ground-water standards were not the subject of the Court's
ruling, and that in fact the Court left us with discretion regarding
the content and application of those standards. Others believed that we
are obligated to accept comments on this topic, since we were proposing
not to change the standards. We stated clearly in our proposal that we
were not soliciting, and would not consider, comments on this issue.
III. What Final Amendments Are We Issuing With This Action?
This section describes the provisions of our final rule, our
rationale, and our response to public comments on various aspects of
our proposal. Today's final rule establishes the dose standards
applicable for a period up to 1 million years after disposal, the
statistical measures used to determine compliance with those standards,
the methods to be used to calculate the dose, and the requirements for
including features, events, and processes (FEPs) in the performance
assessments.
A. What Dose Standards Will Apply?
Today's final rule includes an individual-protection standard
consisting of two parts, which will apply over different time frames.
The post-10,000-year public health protection standard limits the long-
term peak dose to the RMEI from the Yucca Mountain disposal system to 1
mSv/yr (100 mrem/yr) committed effective dose equivalent (CEDE). This
post-10,000-year (also referred to as the ``peak dose'') standard
addresses and responds to the DC Circuit ruling that our 2001
standards, with the compliance period limited to 10,000 years, were
inconsistent with the recommendations of the NAS. The post-10,000-year
standard was the focus of our proposal and will apply after 10,000
years through the period of geologic stability, up to 1 million years
after disposal. The other part of the individual-protection standard,
which will apply over the initial 10,000 years after disposal, consists
of the 150 [mu]Sv/yr (15 mrem/yr) CEDE individual-protection standard
promulgated in 2001 as 40 CFR 197.20. We believe this approach
maintains an appropriate emphasis on the initial condition of the
repository and its critical early evolution, including the period when
thermal stresses will be most significant.\6\ As the disposal system
evolves, today's final rule establishes a peak dose standard for the
period up to 1 million years that is responsive to the Court's ruling,
consistent with the NAS recommendation to establish a compliance
standard for the time of peak risk, and satisfies our statutory mandate
to protect public health and safety. The final rule also provides a
reasonable test of disposal system performance by appropriately
recognizing the relatively more difficult challenge in treating the
uncertainties associated with projecting performance to such distant
times, and the resulting lessened level of confidence that can be
derived from such performance projections.
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\6\ We noted in our 2001 rule: ``Focusing upon a 10,000-year
compliance period forces more emphasis upon those features over
which humans can exert some control, such as repository design and
engineered barriers. Those features, the geologic barriers, and
their interactions define the waste isolation capability of the
disposal system. By focusing upon an analysis of the features that
humans can influence or dictate at the site, it may be possible to
influence the timing and magnitude of the peak dose, even over times
longer than 10,000 years.'' (66 FR 32099)
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As we noted in our proposal, there was no legal challenge to, and
the Court made no ruling on, the protectiveness of our standards up to
10,000 years. Further, the Court ruled that we must address peak dose,
but did not state, and we do not believe intended, that we could not
have additional measures to bolster the overall protectiveness of the
standard. We believe that promulgating the post-10,000-year peak dose
standard to protect public health and safety while retaining a separate
individual-protection standard that focuses attention on the early
evolution of the repository in the pre-10,000-year period enhances the
overall protectiveness of our rule and is consistent with the findings
and recommendations of the NAS committee. As the Court noted, the EnPA
requires that EPA ``establish a set of health and safety standards, at
least one of which must include an EDE-based, individual protection
standard'' (NEI, 373 F.3d at 1281), but does not restrict us from
issuing additional standards. Thus, as long as we address the NAS
recommendation regarding peak dose, as we are doing today by issuing
the post-10,000-year standard, we are not precluded from issuing other,
complementary, standards to apply for a different compliance period.
The Court's concern was whether we had been inconsistent with the NAS
recommendation by not extending the period of compliance to capture the
peak dose ``within the limits imposed by the long-term stability of the
geologic environment.'' (NAS Report p. 2) Today's final rule defines
the period of geologic stability for purposes of compliance as ending
at 1 million years after disposal. We believe our decision to retain a
separate standard applicable for the first 10,000 years after disposal
during this period, along with ``at least one * * * EDE-based,
individual protection standard'' applying to the peak dose during the
period of geologic
[[Page 61264]]
stability between 10,000 years and 1 million years, protects public
health and safety pursuant to the EnPA, complies with the Court's
decision, falls well within our policy discretion and is supported by
scientific considerations concerning the impact of uncertainties in
projecting doses over extremely long time frames, as discussed in
Section III.A.4 of this document (``How Did We Consider Uncertainty and
Reasonable Expectation?'').
The NAS Report recognized the possible outcome of a rulemaking
establishing separate standards that apply over different time periods.
As discussed in more detail in Section III.A.6 (``How Does Our Rule
Protect Future Generations?''), the committee contrasted an approach in
which ``a health-based risk standard could be specified to apply
uniformly across time and generations'' with ``some other expression of
the principle of intergenerational equity'' to be determined by
``social judgment.'' (NAS Report pp. 56-57) The committee also
recognized, as we have just explained, that ``the scientific basis for
analysis changes with time'' in potentially significant ways as the
time to peak dose increases. (NAS Report pp. 30-31) We also find it
useful to consider the testimony of Mr. Robert Fri, chair of the NAS
committee, before the Senate Environment and Public Works Committee on
March 1, 2006, in his personal capacity, wherein he pointed out that
``the specification of the time horizon and the selection of the person
to be protected are intimately connected.'' As a result, he explained
that retaining the RMEI as the receptor (which the NAS committee
recognized as more conservative than, but ``broadly consistent'' with,
its preferred probabilistic critical group \7\) while at the same time
extending the compliance period ``runs the risk of excessive
conservatism,'' potentially putting the rule where the ``committee
specifically did not want to be.'' He noted that the committee had
considered and rejected such an approach. (See NAS Report pp. 100-103)
Mr. Fri viewed our proposal of a higher dose limit between 10,000 and 1
million years as a way ``to avoid becoming overly conservative.''
Therefore, while he (like the NAS committee itself) offered no opinion
on the level of the proposed post-10,000-year standard, he indicated
that, in his opinion, our approach was not in conflict with the
committee's intention, and would be closer to the committee's overall
goal than would applying the 15 mrem/yr standard to the 1 million-year
compliance period. He concluded by stating ``the committee recognized
that EPA properly had considerable discretion in applying policy
considerations outside the scope of our study to the development of the
health standard for Yucca Mountain.'' (See generally NAS Report p. 3)
See the hearing transcript at Docket No. EPA-HQ-OAR-2005-0083-0380 and
Mr. Fri's prepared testimony at Docket No. EPA-HQ-OAR-2005-0083-0402.
We believe the decision to establish two compliance standards falls
well within our policy discretion and in that context the 10,000-year
individual-protection standard is analogous to our ground-water
protection standards, which were also not addressed by NAS
recommendations.
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\7\ In discussing an alternative subsistence-farmer receptor,
the committee noted that ``it makes the most conservative assumption
that wherever and whenever the maximum concen