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OCR for page 11
2
Hanford Site Background
The region around the present-day Hanford Site was occupied by
Native Americans for more than 10,000 years before the arrival of the first
European American explorers, the Meriwether Lewis and William Clark
party, in 1805. Euro-American settlement of the area was promoted by
several events: the relinquishment of Indian lands to the government at
the Treaty Council of 1855 and military action against Indian resistance in
1858, and the development of irrigation canals and construction of the
railroad in the 1880s and 1890s the latter of which led to the founding of
the towns of Kennewick and Pasco. By the early 1 940s, the region had a
population of about 19,000, supported mostly by farming and ranching.
In December 1942, an officer assigned to the Army Corps of
Engineers Manhattan Engineering District and two DuPont engineers
began a tour of the western United States to locate a site for a highly
classified "atomic" project associated with the war effort. They were
seeking a large tract of land with abundant cold water and electricity
supplies that was also isolated from highways, railroads, and population
centers. After visiting a region along the Columbia River near its
confluence with the Yakima River (Figure 2.1), they reported to General
Leslie R. Groves, head of the Manhattan Engineering District, that the site
"was far more favorable in virtually all respects than any other' (Gerber,
1992~. By March 1943, Groves had acquired about 500,000 acres (almost
800 square molest of land at a cost of a little more than $5 million, and
ground was broken for the world's first production facility to make
plutonium for atomic weapons (Rhodes, 1986~. The site was first
designated as Site W and later as the Hanford Engineering Works.
The site design (Figure 2.1 ) called for three graphite-moderated
"atomic piles," or reactors, to be built at 6-mile (about 1 O-kilometer)
intervals along the Columbia River. These areas are referred to
collectively as the "100 Areas" and individually by the reactor designation,
for example, the "1 OO-B" Area for the B-Reactor. These reactors would
irradiate fuel slugs made from natural uranium' to create plutonium-239,
which had been made in minute quantities for the first time at the
Radiation Laboratory (now the E.O. Lawrence Berkeley National
Laboratory) in 1941. The river water was needed to cool the piles, which
operated at about 200°C. Some 10 to 15 miles (16 to 24 kilometers)
The graphite piles were effective neutron moderators and absorbed few
neutrons, making it possible to use natural uranium to fuel the reactors. Later,
slightly enriched uranium was used to fuel the reactors to increase plutonium
production rates.
11
OCR for page 12
12
Science and Technology for Environmental Cleanup
Priest ~ . Vernita Bridge
Rapids
Dam
_
-
-
Rattlesnal
Mountain
.....
r
Kennew~-- _
=== = _
=
=
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. _
-
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_~ Arid Lands
Ecolotgy
Reserve
~BC White Bluffs
tt~hl" R''tt^_~ _
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-
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200-West
Gable Mt.
-
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IBM
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~ = = =
1
\
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;,OO-F
r Old Hanford,
| TO sin'
0 5
l
Scale: Miles
Seattle Spokane
V WASHINGTON
Hanford
~Tri-Cities
·Portland OREGON
Figure 2.1 Plan view of the present-day Hanford Site showing locations of
major plutonium production areas. SOURCE: BHI, 1999, Figure
1-1; DOE, 1998a.
south, on a plateau near the center of the site behind two elevated ridges
called Gable Mountain and Gable Butte, two other industrial sites were
established, referred to as the 200 East Area and 200 West Area, each
containing two massively shielded chemical processing plants to dissolve
the irradiated uranium slugs to recover plutonium. The recovered
Dlutonium would then be shipped off-site2 for orocessino to make
-
2Plutonium was recovered as a nitrate paste, which was shipped to Los
Alamos, New Mexico, for conversion to metallic plutonium. A facility to make
metallic plutonium at the Hanford Site the Plutonium Finishing Plant was
constructed in 1949.
OCR for page 13
Hanford Site Background
plutonium metal that would form the cores of atomic bombs. Sixty-four
underground storage tanks were initially constructed near these plants to
store the highly radioactive liquid waste from processing operations
(Figure 2.2~. Additional facilities were constructed downstream of the
reactors to manufacture the uranium slugs, in the 300 Area. Given the
Figure 2.2 Construction of single-shell tanks in the BX Tank Farm, 1947.
The partially constructed tank in the front-right portion of the
photo is filled with liquid, presumably for leak testing. After
construction of the steel shells, the tanks were encased in
concrete shells and domes, as shown at the left-center and left-
rear of the photo. The tanks were constructed below grade (note
land surface at the rear of the photo) to provide radiation
shielding. SOURCE: David Briggs, Pacific Northwest National
Laboratory, Negative 1313.
13
OCR for page 14
14
Science and Technology for Environmental Cleanup
large potential hazards involved with the operation of these first-of-a-kind
facilities, the site design called for these reactors and processing plants to
be separated by large distances to minimize potential impacts from
routine radionuclide releases as well as catastrophic accidents.
By May 1945, barely two years after groundbreaking, Hanford
had produced enough plutonium for the first test of a plutonium bomb,
which was carried out at the Trinity Site in New Mexico on July 16. After
this successful test, another bomb made from Hanford plutonium
(code-named "Fat Man") was dropped on Nagasaki, Japan, on August 9,
1945, thereby forcing an end to the war in the Pacific.3 By the end of the
second world war, the Hanford Site contained more than 500 buildings,
almost 400 miles of roadway, and about 160 miles of railroad. A nearby
town (Richland) was expanded to house more than 17,000 workers and
their families. The total cost of construction was about $230 million
(Gerber, 1992~.
The Hanford Site was expanded several times after the war to
meet national security needs (Table 2.1; see DOE, 1998f, for details).
After President Harry Truman's declaration of the Cold War with the
Soviet Union in March 1947, Hanford embarked on a $350 million
expansion that added two new reactors, a plant to produce metallic
plutonium, and new underground high-level waste storage tanks.
Following the Soviet Union's detonation of its first atomic bomb in August
1949, a second expansion was undertaken that added yet another
reactor, the REDOX chemical processing plant, additional underground
waste storage tanks, and two waste evaporators to reduce the large
volumes of tank waste being produced from chemical processing
operations.4 The third and final expansion of the Hanford Site occurred
during the peak of Cold War tensions during the Eisenhower, Kennedy,
and Johnson administrations: three more reactors were built along the
Columbia River, another chemical processing plant (PUREX) went into
operation, and additional underground waste storage tanks were
constructed.
3An atomic bomb was dropped on Hiroshima, Japan, on August 6, 1945. This
bomb, code-named "Little Boy," used uranium-235 as the nuclear explosive. The
uranium was produced at the Oak Ridge Site in Tennessee, which was also
established during the Manhattan Project.
4During this expansion period, many other sites were also established to aid
the Cold War effort, most notably the Nevada Test Site, the Idaho Reactor Testing
Station (now the Idaho National Engineering and Environmental Laboratory), the
Savannah River Site in South Carolina, the Rocky Flats Site in Colorado, the
Pantex Plant in Texas, the Fernald Site in Ohio, and the Paducah Plant in
Kentucky.
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Hanford Site Background
TABLE 2.1 Chronology of Major Production Facilities at the Hanford Site
. . .
Facility Operation Start Operation End
Date Date
Production Reactors
B-Reactor 1944 1968
D-Reactor 1944 1967
F-Reactor 1945 1965
H-Reactor 1949 1965
DR-Reactor 1950 1964
C-Reactor 1952 1969
KW-Reactor 1954 1970
KE-Reactor 1955 1971
N-Reactor 1963 1987
Fuel Processing Facilities
T-Plant 1944 1956
B-Plant 1945 1952
REDOX 1952 1967
U-Plant 1952 1958
PUREX 1956 1990
Materials Processing
Plutonium Finishing Plant 1949 1989
Hiah-Level Waste Tanks
B-Tank Farm 1945 Inactive
T-Tank Farm 1945 Inactive
C-Tank Farm 1946 Inactive
U-Tank Farm 1946 Inactive
BX-Tank Farm 1948 Inactive
TX-Tank Farm 1949 Inactive
BY-Tank Farm 1950 Inactive
S-Tank Farm 1951 Inactive
TY-Tank Farm 1953 Inactive
SX-Tank Farm 1954 Inactive
A-Tank Farm 1956 Inactive
A)(-Tank Farm 1965 Inactive
AY-Tank Farm (D) 1976 Still in service
AZ-Tank Farm (D) 1976 Still in service
SY-Tank Farm (D) 1977 Still in service
AW-Tank Farm (D) 1980 Still in service
AN-Tank Farm (D) 1981 Still in service
AP-Tank Farm (D) 1986 Still in service
15
.
Note: The ~inactive" tanks contain mostly saltcake, sludge, and some drainable
liquids, but they are no longer being used for storage of liquid waste. (D) denotes
double containment tank.
SOURCES: DOE, 1998f, Table 2.3.6; tank data from Brevick, 1994, 1995a, 1995b,
1995c.
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16
Science and Technology for Environmental Cleanup
Production at the Hanford Site began to decline after 1965 in
response to decreased national needs for plutonium and other nuclear
materials. By 1972, all but one plutonium production reactor was shut
down. The last reactor operated until 1987, mainly to produce electricity
for the regional power grid.5
Twenty-eight additional underground waste storage tanks, each
having a storage capacity of between 1.0 million and 1.1 million gallons,
were constructed and began receiving waste between 1976 and 1986.
These tanks have a double-shell design and are used to hold newly
generated waste, as well as waste pumped out of older
single-containment tanks, some of which had started leaking in the late
1 950s.
At present, all plutonium production reactors and reprocessing
plants are permanently shut down. Most facilities have been deactivated,
and some are now being torn down. As noted later in this chapter, the
Department of Energy (DOE) has also started to remediate contaminated
soil and groundwater at the site and to ship transuranic solid waste to the
Waste Isolation Pilot Plant (WIPP) in New Mexico.
During its roughly 40 years of operation, Hanford produced about
67 metric tons of plutonium—approximately two-thirds of the nation's
plutonium stockpile (DOE, 1 99Bg). In the process, large areas of the site
around the production facilities, from the surface to the groundwater, were
contaminated with radioactivity and hazardous chemicals. The United
States is now spending more than $1 billion per year at Hanford alone to
manage residual waste and nuclear materials at the site and to clean up
contaminated soil and grounclwater, reactors, tanks, chemical processing
plants, and ancillary facilities.
WASTE PRODUCTION AND MANAGEMENT
The production of plutonium and other nuclear materials at
Hanford consumed more than 95,000 metric tons of uranium fuel and
created large volumes of liquid and solid wastes. In the press of the effort
to win the Second World War and then to accelerate production during
the ensuing Cold War, production of plutonium and other nuclear
materials at the site took priority over environmental protection. Most of
the high-activity waste produced contains actinides and fission products
and is stored in the 200 Area tank farms. In addition, large amounts of
radioactive and chemical contaminants were also released into the
5Eight of the nine reactors at the Hanford site were designed only to produce
plutonium. The ninth reactor, designated UN-Reactor," was built with an isolated
cooling loop and could produce both plutonium and electricity.
OCR for page 17
Hanford Site Background
17
atmosphere, the Columbia River, and the subsurface during the site's 40-
year operational history. Until the 1970s, relatively poor records were kept
for many of these releases. Some waste continues to be released to the
environment today from waste management and cleanup operations at
the site. These controlled environmental releases are now regulated by
the Environmental Protection Agency and Washington State.
Although plutonium production took priority at the site, there was
a concern about potential environmental impacts even from the earliest
days of site operations. Programs were established to monitor and limit
worker exposures and make environmental measurements of the
Columbia River and its aquatic life, site vegetation, wildlife, and
groundwater. Extensive studies of the Columbia River ecosystem
concentrated on both radionuclide and thermal (heat) releases (e.g.,
Vaughan and Hebling, 1975; Becker, 1990~. After the war, additional
studies were made of site sediments to determine their capacity to retard
the migration of radionuclides, which were being released into the
subsurface along with large volumes of water. As noted elsewhere in this
section, some operational practices were modified to reduce waste
releases based on these monitoring programs.
Because of incomplete record keeping, an exact mass balance of
historical releases of radioactivity and chemicals to the environment at the
site does not exist. The Integration Project has established a program to
obtain such an estimate, as described in Chapter 5 of this report. The
following sections summarize what is currently known about contaminant
releases at the site, organized by environmental medium as illustrated in
Figure 2.3. More detailed discussions of waste releases can be found on
the Hanford web site; see especially the History of the Plutonium
Production Facilities at the Hanford Site Historic District (DOE, 1 997a;
http:llwww. hanford.gov/docs/rl-97-1 047/index.htm) and many of the
references cited therein.
Releases to the Atmosphere
The operation of production reactors resulted in the release of
about 12 million curies of volatile fission products to the atmosphere
(Heeb, 1994~. Volatile radioisotopes were also released during chemical
processing of the fuel to recover plutonium,6 especially during the war
years (Napier, 1992~. Emissions from the chemical processing plants
were reduced after the war through the use of scrubbers and filters and
6The chemical processing plants had 200-foot-high vent stacks to disperse
these releases.
OCR for page 18
~8
Since and ~chno~ far e~nmen~/ Bang
~~'~;!'~'~~!~.~!~'
.
,_
. ~
! .. ~
Fag
~ ...- -~.._- ~..~.
~"~_~$~.~<'?~1'S#~,~^ ~ ,_~.-~ 3,,,,, ,. .; ?~/,:`~.~-~- ,
gu[e2.3 Boor contain and subsurface release pathways in the
(A) 100 and 300 Areas and (B) 200 Area at the Hanford Site.
SOURCE: DOE, 19988, Figures 1-5 and 1-6.
OCR for page 19
Hanford Site Background
by allowing more time for the fuel to "cool" after irradiation to allow short-
lived radionuclides to decay.
19
Once released into the atmosphere, radionuclides were dispersed
by atmospheric mixing. The impacts of atmospheric releases of
radionuclides at Hanford on human health have been assessed in the
Hanford Environmental Dose Reconstruction Project and the Hanford
Thyroid Disease Study (National Research Council, 1994a, 1995, 2000b).
These studies have shown that iodine-131 (half-life-8 days) contributed
most of the radiation dose received by members of the public from
atmospheric releases at Hanford.
Releases to the Ground
The release of radionuclides and hazardous chemicals to the
ground at the Hanford Site occurred at all of the major production areas.
These contaminants are among the most significant potential
environmental hazards that exist at the site today in addition to the
spent nuclear fuel, high-level waste, and other nuclear materials under
active management at Hanford. These releases can, for convenience, be
grouped into the following three categories: (1 ) solid waste disposal, (2)
liquid waste disposal, and (3) accidental releases and discharges.
Solid Waste Disposal
Radioactive and chemically contaminated solid waste has been
disposed of in shallow land burial grounds around all of Hanford's
production facilities. Almost 70 burial sites containing more than 650,000
cubic meters of waste are known to exist (DOE, 1 997d, 2000h). Solid
waste was placed in unlined trenches, lined excavations, and
underground vaults and consisted of a wide variety of materials, including
failed hardware, construction and demolition waste, soil contaminated by
spills and leaks, contaminated clothing, and various kinds of process
waste.
During the first two decades of site operation, burial grounds were
built in close proximity to production facilities, and both chemical and
radioactive wastes were disposed with little or no segregation. Moreover,
no detailed records were kept of the kinds or amounts of waste disposed.
By the 1960s, the burial grounds were centralized, mostly in the 200 Area,
and waste segregation and better record-keeping practices were
implemented. By the 1970s, all radioactive solid waste was being
disposed of in the 200 Area, and transuranic waste was being segregated
OCR for page 20
20
Science and Technology for Environmental Cleanup
and stored.7 Additionally, computerized databases began to be used to
track inventories of waste disposed of in the burial grounds. In 1995, the
Environmental Restoration Disposal Facility (ERDF)9 was established
between the 200 East Area and the 200 West Area (see Figure 2.1~. It
now receives most of the solid radioactive and mixed wasted generated
by cleanup and waste management activities at the site.
The burial grounds in the 200 Area also hold waste generated off-
site by other DOE sites and laboratories, universities, the military, and
private companies. Most notable, perhaps, is the burial ground in the 200
East Area that holds more than 80 reactor compartments from
decommissioned U.S. nuclear submarines. A private-sector organization
(U.S. Ecology) also operates a commercial low-level waste disposal
facility on land owned by Washington State.
Liquid Waste Disposal
Liquid radioactive and chemical wastes were discharged to the
ground at all operating facilities on the Hanford Site. In terms of volume
and toxicity, the most significant releases occurred in the 200 Area from
chemical processing operations. After irradiation, the fuel was brought to
the 200 Area by train, where it was dissolved and chemically processed to
recover plutonium, uranium, and sometimes neptunium. These
processing operations produced 26 distinct waste streams containing
actinides and fission products and a wide range of chemicals, including
nitric acid, bismuth phosphate, potassium permanganate, methyl isobutyl
ketone, aluminum nitrate, tributyl phosphate, kerosene, ammonium
fluoride, and sodium hydroxide.
7A 1970 Atomic Energy Commission directive required the segregation of
transuranic waste and also required that it be placed in retrievable storage. That
stored waste is now being shipped to the WIPP in New Mexico for disposal.
8The database is now referred to as the Solid Waste Tracking System (see
Chapter 5~.
The ERDF is a Resource Conservation and Recovery Act- and
Comprehensive Environmental Response, Compensation, and Liability Act-
compliant land disposal facility for disposal of waste from Hanford cleanup
operations. It comprises a series of disposal cells, each measuring about 500 feet
on a side and 70 feet deep, with a combined capacity of almost 12 million cubic
yards.
'°Mixed waste contains both radionuclides and hazardous chemicals.
Neptunium was used to make plutonium-238 for radioisotope thermoelectric
generators (also known as RTGs) for space applications.
OCR for page 21
Hanford Site Background
21
Table 2.2 provides an inventory of the high-level waste produced
by chemical processing operations between 1944 and 1988.42 The
numbers given in Table 2.2 are rough estimates only43 and are based on
process knowledge supplemented with records where available. Detailed
records of soil discharges were not kept, and even the current high-level
waste inventory of specific radionuclides and chemicals in the tanks is not
well known.44 As noted previously, an effort is under way at the site to
obtain better estimates of historical releases to aid the long-term cleanup
effort.
The following discussion is based on the inventory estimates
given in Table 2.2. Chemical processing operations generated more than
500 million gallons of high-level waste with a radionuclide content of
about 800 million curies.~5 This waste was transferred to the waste
storage tanks by underground transfer lines. Once in the tanks, the waste
was subjected to additional treatment to reduce its volume by more than
90 percent, to the 54 million gallons that exist in the tanks today (Table
2.2~. This was done using the following processes:
1. Beginning in about 1948, when tank space was in short
supply,. gravity separation of the solid and liquid fractions of the high-level
waste was accomplished using multiple tanks connected in series. Waste
was introduced into the upstream tank, and as it cascaded through
successive tanks, the solid fraction, which contained most of the actinide
elements and strontium, would settle out, leaving a liquid supernate that
contained cesium and other soluble fission products such as technetium.
At the end of the cascacle, the supernate was discharged to soil.
2. After cascading was discontinued in the 1 950s, the supernate
in some tanks was treated with potassium ferrocyanide to precipitate
cesium. Once the cesium was removed, the remaining liquid was
discharged to soil.
42The committee is indebted to Roy Gephart, Pacific Northwest National
Laboratory (PNNL), who provided some of the background material used in this
section and in Table 2.2 and who reviewed a draft of this chapter.
43The committee cannot evaluate the accuracy of the estimates given in
Table 2.2 but believes that they are likely to be highly uncertain. The numerical
ranges shown for some entries in the table represent differences in estimating
procedures and do not necessarily represent the uncertainty ranges of the
estimates themselves, which have not been determined, in part because the
quality of the estimates is unknown.
~ The waste tanks are highly heterogeneous, and not all of the tanks have
been sampled.
45This estimate is based on a rough calculation and was provided by Roy
Gephart (PNNL).
OCR for page 29
Hanford Site Background
(B) r
r
r
r
-
~_ 100 H
#_ Area I
r Ares
r 10~8~ i)
J
_ _
_
}< ' Area ~ ~F; HI TEDF ~Oid
RiversJ~s
salt Above Water Table
~ Chromium {MCL 100 ug/L)
~ Nitrate (20 mg/L)
~ Nitrate (MCL 45 mg/L)
~ Carbon Tetrachlondo (MCL 5 uo/O
29
Canto \
Landfill
\ Supp y
\ 6t8-10
Crowds
400 Ares
that Flux Ted Facility)
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Dashed Where Inferred
` - Area i 2 0 1
2406~ n ~
p~as024f~yt9,'~1~~ .
E98~082.215
OCR for page 30
30 Science and Technology for Environmental Cleanup
; SIDEBAR,:(j1
~ ~~ ~~ ~~ Th
Range and
lacustrIr~e
:Group, or
-.~-n~.~}ie Columbia .P
t ~O Rome MUDS
- basa.lts ~ And. ~~.~ ~ Panic
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OCR for page 31
Hanford Site Background
West (A)
400 - Yalcima
j Ridge
300-
;>
v:
::
ct
c;
;>
a:
O-
c'
100 -
-100 -
\ 200-E stArea
HOa f0ardon[~: = ~ ~ — ~ ~~ a
Ringold
Formation
~ _ ~ ~ ~ it
\_ Kilt
Interbed ~
Basalt
G99030045.93
Figure 2.9 Generalized east-west section through the Hanford Site
showing the principal geologic formations. SOURCE: PNNL,
1999, Figure 6.1.3.
31
leaks of high-level waste from tanks and waste transfer lines. Leakage of
high-level waste to the subsurface is suspected to have occurred in at
least 67 of the 149 single-containment underground waste tanks in the
200 Area (Gephart and Lundgren,1998~. The word "suspected" is used to
describe these leaks because the single-containment tanks were not
designed with systems to detect leaks. Rather, leakage has been inferred
by monitoring liquid levels in the tanks and by radiation monitoring in
about 800 dry wells48 drilled in many of the tank farms (Figure 2.10~.
The single-containment tanks were constructed beginning in 1945
and had a 20-year design life. The first tank leak, estimated to be around
10,000 gallons, is believed to have occurred in the U Tank Farm in 1956,
about 10 years after it was constructed (Table 2.1~. The largest leak,
estimated to be more than 100,000 gallons, is believed to have occurred
in the T-Tank Farm in 1973 (DOE, 1 997a). The total amount of leakage
from all 67 tanks is estimated to have been between 750,000 and 1.5
million gallons of high-level waste with an activity between about 450,000
swells completed in the vadose zone above the water table.
OCR for page 32
32
Science and Technology for Environmental Cleanup
and 1.8 million curies (Table 2.2~. Most of the liquids contained in these
leaking tanks have been pumped into double-containment tanks (Gephart
and Lundgren, 1998~. In some cases the remaining liquids were absorbed
by adding diatomaceous earth.
The subsurface in the 200 Area was also been contaminated with
uranium from operation of the U-Plant from 1952 to 1958. An estimated
N ~
Cs-137 Concentration {pCilg)
i ) ~
i. i , .
~ I,,, ~ ,-!jj4A ,,, ~Jr,
Figure 2.10 Calculated cesium-137 distributions in soil beneath the SX
Tank Farm. Vertical lines represent dry wells in which gamma-ray
measurements were made to determine cesium concentrations.
Tanks labeled in red font are known leakers. SOURCE: DOE,
1 998a.
OCR for page 33
Hanford Site Background
4,000 kilograms of uranium was disposed in two cribs during operation of
this plant. Some of the uranium was later remobilized and transported to
groundwater beneath the 200 Area when acid waste was inadvertently
disposed to these cribs and additional disposal cribs were put into
operation nearby. The acid remobilized the uranium in the crib and
underlying sediment, and the liquids from a nearby crib transported this
remobilized uranium to groundwater. This groundwater contamination is
being contained through pump-ancl-treat operations (DOE, 2000e).
Releases to the Columbia River
33
There were many releases of radioactive and chemical
contaminants to the Columbia River during operation of the production
facilities at the Hanford Site, and some releases from contaminated
groundwater continue to the present. By far the largest releases occurred
from the eight "single-pass" production reactors in the 100 Area, which
released about 1 10 million curies to the river (Heeb and Bates, 1994~.'9
Up to 200,000 gallons per minute of treated river water was used to cool
these eight reactors, and as the treated water passed through the reactor
cores, naturally occurring elements in the water became activated by
capturing neutrons. Additionally, a small percentage of the radionuclides
released to the water were fission products from damaged fuel elements.
The principal contaminants in the reactor effluents are shown in Table
2.3.
Reactor operations also resulted in discharge of liquids into the
subsurface around reactor sites, which later migrated through the
grounclwater and into the river. As noted previously, cooling water
contaminated with radionuclides from damaged fuel elements was
sometimes diverted into trenches, as was contaminated water from the
primary cooling loop on the N-Reactor. Process waste and water
treatment chemicals (e.g., sodium dichromate) leaked or were disposed
of at the reactor sites. Some of these contaminants continue to leak into
the river. Pump-and-treat facilities and other treatment approaches20 are
being implemented to reduce the inflow of these contaminants to the river.
49As noted elsewhere in this chapter, all of the production reactors except for
the N-Reactor were cooled by pumping treated river water directly through the
cores. On exiting the cores, the water was held in a retention basin for a few
hours before being pumped back into the river. The N-Reactor had a closed
primary loop to cool the core. Cooling water from the river was provided in a
secondary loop that was isolated from the reactor core.
20For example, the oxidation state of chromium is being manipulated in
groundwater near the D-Reactor to immobilize it in place and limit its migration
into the river.
OCR for page 34
34
Science and Technology for Environmental Cleanup
TABLE 2.3 Selected Radionuclide Releases to the Columbia River from
Single-Pass Hanford Reactors, 1944-1971
Radionuclidea Half-Life Total Curies (millions]
Sodium-24 15 hours 12.6
Phosphorus-32 14.3 days 0.23
Zinc-65 245 days 0.49
Arsenic-76 26.3 hours 2.5
Neptunium-239 2.4 days 6.3
aAccording to the Hanford Dose Reconstruction Project (Ferris et al., 1994), these
five radionuclides contributed more than 94 percent of the total dose to
representative individuals who used Columbia River resources.
SOURCE: Heeb and Bates, 1994.
Production activities in the 200 East Area have created large
groundwater contaminant plumes that are discharging nitrate and tritium
into the Columbia River downstream of the 100 Area (Figure 2.8~. About
3,000 curies, on average, of tritium is discharged into the river each year
from the site, based on sampling data (e.g., PNNL, 1999, 2000a) from the
river near the upstream and downstream boundaries of the site. The
Hanford Site contribution increases the radionuclide load in the Columbia
River by about one-third. The remaining radioactivity in the river is from
natural or man-made24 sources upstream of the Hanford Site.
CLEANUP OF THE HANFORD SITE
Hanford Site's defense mission waned in the late 1 980s,
prompted by the shutdown of the N-Reactor in response to the Chernobyl
accident and a thaw in the Cold War, and the focus of site activities
shifted from plutonium production to environmental restoration. In 1989,
DOE, the State of Washington Department of Ecology, and the U.S.
Environmental Protection Agency entered into the Hanford Federal
Facility Agreement and Consent Order, also known as the "Tri-Party
Agreement," for achieving compliance with CERCLA (the Comprehensive
Environmental Response, Compensation, and Liability Act) and RCRA
(the Resource Conservation and Recovery Act) provisions of federal
24 Primarily from fallout left over from atmospheric tests of nuclear weapons.
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Hanford Site Background
statutes, as well as state environmental protection laws.22 The Tri-Party
Agreement defines and ranks cleanup and waste management
commitments, establishes cleanup responsibilities, and provides
enforceable milestones for achieving these commitments. Cleanup work
at the Hanford Site has proceeded under this agreement since it was
signed, although DOE has had to renegotiate many of the agreed-to
milestones.
In 1999, DOE released the Final Hanford Comprehensive Land-
Use Plan Environmental Impact Statement (DOE, 1 999a),23 which lays
out its preferred future land use at the Hanford Site after the cleanup
program is completed. DOE's preferred alternative (Figure 2.11 ) includes
the following provisions:
35
· The land surrounding the core of the Hanford Site (the
Wahluke Slope north of the Columbia River and Arid Lands Ecology
Reserve southwest of the Central Plateau) and Rattlesnake Mountain and
Gable Butte will be preserved from impacts from intensive land-disturbing
activities (e.g., mining or extraction of nonrenewable resources).
.
The Columbia River corridor will have a variety of land uses.
The river islands and a quarter-mile buffer zone on each side of the river
channel will be preserved to protect cultural and ecological resources.
However, the "cocooned" reactors will not be moved for at least 50 years,
and remediation will continue as necessary along the river. Additionally,
B-Reactor will become a museum. Several sites along the river will be
designated for recreational use.
· Most of the Hanford Site will be designated as conservation
zones to protect cultural, ecological, and natural resources. However,
excavation will be permitted to obtain materials needed for DOE
missions—for example, to construct barriers and caps to retard future
contaminant movement at waste disposal sites.
· The Central Plateau will be designated as industrial-exclusive
use, which would allow current waste management activities to continue
and new compatible facilities to be developed.
· The portion of the site north of Richland will be designated as
industrial, which would support future DOE missions or commercial
industrial development.
.
An area in the southeastern portion of the site will be
designated for research and development to support DOE's continuing
22CERCLA provisions govern the cleanup of contaminated sites, whereas
RCRA provisions govern the treatment, storage, and disposal of waste generated
at the site.
23Available on the Hanford Website at http://www.hanford.gov/eis/hraeis/
hraeis.htm.
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36
Science and Technology for Environmental Cleanup
energy research mission. This area now contains the Laser Interferometer
Gravitational Observatory.
DOE recognizes that cleanup is likely to be incomplete, even in
the areas designated for recreation and preservation, and that deed
restrictions and continuing (in some cases, perpetual) institutional
management will be required over much of the site to protect public and
environmental health.
Within the Central Plateau, the 200 Area will serve the site's
continuing waste management mission. The major waste management
Recreation
(High Intensit!
, . . .
me, ~ (Mining)
/~ Research and
~~ Development
Recreation ~
(High Ir~ten~ty)
Figure 2.11 Future land use at the Hanford Site. SOURCE: DOE, 1 999a,
Figure 3.3.
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Hanford Site Background
and cleanup activities planned in this area are approximately the
following:24
37
· Spent nuclear fuel, special nuclear materials, and cesium and
strontium capsules will be shipped off-site to a geologic repository for
disposition.
· All retrievable transuranic solid waste will be shipped to the
Waste Isolation Pilot Plant in New Mexico.
· High-level waste in the 200 Area tanks will be retrieved,
immobilized in glass, and eventually shipped to a geologic repository. The
low-activity radioactive waste streams created by processing this high-
level waste will be immobilized and disposed of on site.
· Soil and groundwater contamination from past tank leaks and
leaks during the waste retrieval process, as well as any waste remaining
in the tanks after retrieval, the tanks themselves, and ancillary equipment
(e.g., piping and diversion boxes) will remain in place. It is likely that
surface caps and barriers will be placed over tank farms.
· Solid waste burial sites (including the ERDF) containing
transuranic and low-level radioactive waste will remain in place and will
be covered with surface caps and barriers.
Vadose zone contamination from liquid discharges will mostly
remain in place and be covered with surface caps and barriers.
· Facilities, with the exception of chemical processing facilities
("canyons"), will be torn down, and some may be covered with surface
caps or barriers.
· Canyons with significant amounts of fixed contamination will
be left in place and covered with a surface cap or barrier.
Currently, "there is no single collection of DOE documents that
constitute (or identify fully) the approved post closure end state" for the
Hanford Site (DOE, 1 999g, p. 2.3~.25 To date, some end states for
individual areas within the site have been established and are detailed in
various environmental impact statements, environmental assessments,
24This information was provided in writing to the committee by the Integration
Project after the committee's second meeting.
25The term end state is used to denote the condition of the site after DOE
cleanup is completed. The end state can be characterized in terms of acceptable
levels of residual contaminants or permissible site uses. The term is used in both
its singular and its plural forms—for example, to refer to the overall end state for
the Hanford Site or to the end states for specific regions or facilities within the site.
See also An End State Methodology for Identifying Technology Needs for
Environmental Management, with an Example from the Hanford Site Tanks (NRC,
1 999a).
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38
Science and Technology for Environmental Cleanup
strategic plans, and recorcis of decision (e.g., DOE, 1998b, 1998e, 1999a,
2000f; see also the Hanford Strategic Plan at http://www.hanford.gov/
hsp/~. However, several end states are not fully agreed upon, particularly
in the 200 Area. For example, end states for groundwater remediation,
high-level waste tank closure, and other facility closures (e.g., closure of
the chemical processing facilities) have not yet been established. Also,
final cleanup levels have not been determined for much of the waste to be
permanently disposed of in the 200 Area.
The Columbia River comprehensive impact assessment (Kincaid
et al., 2000, p. 3-3) coined the phrase "Hanford Site Disposition Baseline"
(HSDB) to describe the suite of disposal and remedial actions that will
occur as the Hanford Site moves towards closure. Accelerating Cleanup:
Paths to Closure (DOE, 1 998b, p. ES-3) states that "where decisions
have not yet been made, sites make assumptions (e.g., site planning end
states) about how those cleanup actions might be carried out so that sites
can define work and develop schedule and cost estimates."
An initial statement of the Hanford Site Disposition Baseline
(HSDB-2000) is available, and it consists of three tables covering the 100
Area; the 300, 400, and 600 Areas; and the 200 Area (Kincaid et al.,
2000~. The tables list the material type requiring remediation, the
corresponding HSDB assumptions, and data needs. A similar set of
tables is available for the same three areas, which are titled "Identification
of Differences and Issues for Material Type and Areas at Hanford."26 This
has the advantage of referring to the Hanford Strategic Plan and to the
environmental impact statements, environmental assessments, and
records of decision to distinguish between disposition agreements,
requirements, and assumptions. It also includes a summary of key
differences among available documents and key issues.
DISCUSSION
The committee recognized early on in its information-gathering
meetings that the absence of a clearly articulated end-state vision for the
Hanford Site made it difficult to obtain a clear understanding of the exact
nature and timing of future cleanup decisions. The lack of clearly defined
decision points and options also makes it difficult for the Integration
Project to develop an S&T program that is focused on filling well-defined
knowledge gaps required to support well-defined site decisions, as
detailed later in this report.
26These tables were provided to the committee by the Integration Project after
its second meeting.
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Hanford Site Background
Nevertheless, the Hanford Site Disposition Baseline and
associated documents are, in the committee's view, very important to the
S&T program because they indicate the general direction of work at the
site and the kinds of knowledge gaps that may be important. In turn, this
suggests the generic types of S&T that may be useful.
39
· These documents raise key issues for the S&T program for
example, How clean is clean enough? especially as applied to the need to
retrieve 99 percent of the waste from the high-level waste tanks as
currently stipulated in the Tri-Party Agreement. S&T could help formulate
logical scientific and technical approaches for resolving these sorts of
issues.
They allow gaps in site remediation programs to be identified
so that S&T efforts can be focused. For example, there is no mention of
long-term stewardship (see Chapter 1 ) in the baseline, and in other
documents, stewardship is restricted to 50 to 75 years. Stewardship in the
context of these documents does not deal with long-term degradation of
facilities and barriers, particularly in the 200 Area, which could require
S&T to develop a robust monitoring and maintenance capability to ensure
the long-term stability of the site.
· They indicate that the number of material dispositions not
currently agreed upon is rather large. Agreements are being reached one
at a time. A system that generically addresses the concerns of site
stakeholders using logical, scientifically based information could help
accelerate these decisions. If properly focused and timed, S&T could play
a key role in resolving these issues by providing a technical basis for
decision making by participating regulators and stakeholders.
These documents are also valuable because they provide useful
guidance to the Hanford S&T programs in progress. They highlight key
issues that require resolution (e.g., decisions concerning material
dispositions and end states not yet agreed upon) and potential knowledge
gaps to be addressed by S&T. Planning end points and planning end
states will no doubt continue to evolve with time as S&T results become
available and remediation progresses, which in turn will influence the
future course of S&T. This interplay between the cleanup program and
S&T is discussed in more detail in Chapter 10.
Representative terms from entire chapter:
columbia river