Snake River Plain Aquifer
at Risk [1]
June 2003
I. Summary
The preponderance of
data currently available to the Environmental Defense Institute at the time of
this writing clearly indicate that there is a major public health and safety
hazard looming related to the migration of Department of Energy (DOE) Idaho
National Engineering and Environmental Laboratory (INEEL) waste
discharges. This pollution is currently
contaminating the Snake River Plain Aquifer that eventually will (if not
already) threaten all downstream users of this sole source aquifer, as well as
communities along the Snake River due to huge aquifer contribution to the river
volume. Immediate action is needed by federal and state regulators, in addition
to public pressure, to ensure that all tank waste, buried radioactive
and hazardous chemical wastes are exhumed (into safe interim storage), and that
continued dumping of INEEL liquid process waste into unlined percolation ponds
is terminated because it facilitates the flushing of pollution into the
aquifer. Time is of the essence, since every day that goes by, more of this
deadly pollution migrates beyond any means of mitigation. The hazard of INEEL
contaminates extends to most of Idaho via the Snake River. Arguably, since the
Snake River is a primary tributary to the Columbia River, the INEEL contaminate
impact zone extends to northern Oregon and southern Washington states.
II. Snake River Plain Aquifer
In 1991 the
Environmental Protection Agency (EPA) ruled that the Snake River Plain Aquifer
is a “sole source aquifer.” Under the Safe Drinking Water Act, EPA can
determine that an area has an aquifer that is the sole or principal drinking
water source for the area and if contamination would create a significant
hazard to public health. The Snake River Aquifer is the sole water source for
nearly one fourth of Idahoans (<200,000 residents), second only in
size/volume to the Ogallala Aquifer in northern Texas and southern
Oklahoma. The Snake River Aquifer flows
to the south and southwest (starting near Island Park Reservoir on the east and
Bliss on the west) and covers an area of 9,611 square miles. Water storage in the aquifer is estimated at
two billion acre-feet, and a drainage area of 35,000 square miles. [2]
On a total per capita
water usage basis, Idaho ranks first in the nation with 22,000
gallons/person/day - with second place going to Wyoming at 13,052
gal/person/day. [3]University of Idaho, publication #877, herein after called UIWR.. So much water is being drawn from the aquifer
that the water table has dropped three feet in the late 1980's. [AP(a),1/1/89] Municipal water for 41 communities also
adds to the drain on this aquifer. [UI WR # 887] Three years of drought have exacerbated
these conditions requiring even greater demands on the aquifer. [AP(a),1/1/89]
Drought conditions continue with June 1992 Snake River average flow of 3.7
billion gallons per day. The previous low was in 1977 at 5.2 billion gallons
per day. [Times-News(d)] USGS studies show Snake River Plain Aquifer draw_down
in excess of recharge is 410,000 acre feet/yr. [Times News (f) 7/19/92] Recharge
from the 1996-1997 winter show pack run off halted this trend but it is unclear
whether previous loses were completely made up.
![]()
The Snake River Aquifer via spring discharges
(ranging from Bliss, Idaho on the west to American Falls Reservoir near
Pocatello, Idaho on the east) provides in the summer months the entire flow
(due to upstream irrigation) of the Snake River. See attached USGS maps. Thus the aquifer supplies (in the summer
months) all the communities downstream that rely on the river as their primary
water source. The US Geological
Survey has identified 19 major springs,
in an area called Thousand Springs, that discharge to the Snake River starting
with Devils Washbowl (near Kimberly, about 10 miles east of Twin Falls) on the
east and ending with Birch Creek (about 3 miles west of Hagerman) on the west. [4] There are also significant aquifer
discharges to the Snake River further east in the vicinity of American Falls
Reservoir west of Pocatello. DOE estimates that the aquifer discharges 7.1
million acre feet (8,754 trillion cubic meters) of groundwater into the Snake
River every year. [5]
The hazard of INEEL
contaminates extends to most of Idaho via the Snake River. Arguably, since the
Snake River is a tributary to the Columbia River, the INEEL contaminate impact
zone extends to northern Oregon and southern Washington states. A State of
Oregon report found that after the DOE Hanford nuclear reactors in Washington
State were shut down and ended direct discharges to the Columbia River, the
highest radioactive pollutant contributor to the Columbia was the Snake River. [6]
III. Pollution Threats to the Aquifer
The State of Idaho now finally, but quietly in Federal Court briefs, acknowledges that: “Over the years approximately twenty (20) thousand gallons of high-level radioactive waste have leaked into soil and groundwater at INEEL. [7] DOE’s own earlier internal reports note:
"Radioactive, inorganic, and organic wastes releases from active
and inactive waste sites have resulted in contamination of the Snake River
Aquifer. Some of the injection wells, such as at Test Reactor Area, Power Burst
Facility, Test Area North, and ICPP, disposed of the wastes directly into the
Snake River Aquifer. Significant
spills and leaks have frequently occurred over INEEL's history. Most spills have been the result of line and
tank failures, leaking valves, and equipment and tank overfilling. [Spill and/or leak] volumes range up to
45,000 gal. It should be noted that
rather large quantities of chemicals were routinely disposed of via the ICPP
disposal well." [8]
These waste
discharges are the most deadly material in the world. Direct contact for only a
few minutes of this high-level waste would result in death from the radiation
exposure. To offer a perspective, EPA
knows this material is so deadly that its emission regulations are in units of
pico curies or one trillionth of one curie.
Over 10 million gallons containing more than 50 million curies of
high-level waste have already been “processed” in unpermitted unregulated INEEL
waste operations. [9] Due to DOE’s non-compliant waste processing
plants, in operation today, much of the radioactive pollution is simply
exhausted out the stack unimpeded by state and federal regulators. [10]
Because of
flooding of the INEEL dump, another eleven billion gallons previously injected
directly into the aquifer, along with an additional current discharge of ~2
million gallons every day to unlined percolation ponds, these liquid
radioactive waste disposal sites pose a significant hazard due to contaminates
being flushed through the soil column to the aquifer. US Geological Survey (USGS) reports show the hydro-geologic
vulnerability of the INEEL buried waste sites. Flooding incidents have already
occurred in 1952,1962, 1969, and 1982, and these sites are within the Big Lost
River 100-year flood plain. This is
where DOE plans to permanently leave buried waste and dispose of high-level and
transuranic non-liquid waste currently in tank sediments.
![]()
The Natural
Resources Defense Council (NRDC), together with two northwest Native American
Tribes, filed a lawsuit challenging this DOE high-level waste disposal policy. [11]
The INEEL radioactive
waste dump is located in a regional depression about 40 feet lower than
the Big Lost River that flows immediately north of the dump. Buried or
otherwise dumped radioactive high-level and transuranic waste is currently
contaminating the Snake River Plain Aquifer. The State of Idaho reported
plutonium in the aquifer under the INEEL dump at 66 pCi/L or 4.4 times above
the drinking water standard of 15 pCi/L. [12] Depending on
the species of plutonium, its toxic half-life can be as long as 24,000 years.[13]
US Geologic
Survey (USGS) conducted a study of the INEEL RWMC burial ground
plutonium propensity to migrate and found that
plutonium: “is soluble in the water from the perched aquifer, and in time could
be leached from the waste. Once
dissolved, it could persist in solution and ultimately reach the Snake River
Plain aquifer. Nevertheless, to conclude that the plutonium in the waste would
not leach into the ground water over a period of time is not warranted.
In addition, americium, although relatively insoluble and not subject to
oxidation-state changes, could ultimately be leached from the waste to a small
but radiologically significant extent.” [14] [emphasis
added]
More recent
USGS reports show plutonium-239/239/240, americium-241, and cesium-137 in aquifer
wells some twenty miles southwest of the INEEL boundary.[15] Although
these off-site plutonium concentrations (0.013 pCi/L) are well below the EPA
safe drinking water standard, independent scientists argue the standard is not
protective of human health. Arjun Makhijani, Ph.D., a nationally recognized
independent analyst of DOE’s operations, discusses risks to the Snake River
Aquifer from INEEL waste in a recently released book, Poison in the Vadose
Zone where he states:
“It should be noted, however, the Safe Drinking Water
standard of 15 picocuries per liter for alpha emitting transuranics like
plutonium-238, plutonium-239, or americium-241 allows doses on the order of a
hundred times higher than the 4 millirem annual limit specified for most beta
emitters. A concentration of plutonium of only about 0.08 picocuries per liter
in drinking water is required to produce a dose of 4 millirem per year to the
bone surface (the crucial organ for plutonium).” “The Safe Drinking Water
standard specifies dose limits, concentrations limits, and calculation
procedures for doses that are not consistent and are more stringent in some
cases (such as nickel-63, cesium-137, and tritium) and less stringent in
others, notably transuranic radionuclides and strontium-90. Since the latter are among those presenting
the most serious threats in Idaho, a more conservative approach that would
limit groundwater contamination from transuranics is warranted. None of these limits take into account the
potentially more serious problems arising from fetal [unborn baby] exposure.” [16]
Idaho has recently discontinued monitoring
for plutonium and americium at off-site wells for no reported reason. [17] Also the State acknowledges that chromium (a
known carcinogen) “exceeded the drinking water [standard] MCL of 100 ug/l” by
161%. [18]
Federal
drinking water maximum contaminate level (MCL) standards recognize that
radioactive pollutants are cumulative. For instance, in a given water sample,
individual contaminates may be below the individual MCL, however collectively
the sum of the individual contaminates can exceed the standard. [19] The collective contamination is estimated
by adding the sum of the ratios of the actual level of each radionuclide to the
MCL for that radionuclide. If the sum of the ratios for all radionuclides is
less than one, (or less than 100%) the sample complies with the standard.
Although the
federal standards provide for cumulative radionuclide contaminates, they do not
accommodate the cumulative hazard posed by both radioactive and toxic
chemical contamination, which is the case with the Snake River Aquifer. IEER’s Poison in the Vados Zones
report took a scientifically defensible approach to conservatively evaluate the
cumulative ground water hazard.
“While
each single pollutant as well as the sum of the radionuclide pollution
percentages are currently less than allowable drinking water limits [at some
INEEL sample wells], the commutative burden is greater than the allowable
drinking water limits in the [INEEL] RWMC well [by 146%], if TCE and carbon
tetrachloride are added. This is a
standard procedure for radionuclides.
However, it is not mandated for hazardous chemicals, even though it provides
a reasonable estimate of the quality of the water. It is not the most conservative way to estimate the impact of the
pollutants in the water, since simple addition ignores synergistic effects
between various hazardous chemicals and between hazardous chemicals and
radionuclides.” [20]
USGS samples
taken in 1991 at INTEC found radioactive Iodine-129 near INTEC 3.82 times above
the drinking water standard. [21] A 1993 USGS report found Iodine-129 from
INEEL INTEC’s 3.4 square mile ground water plume, in two wells eight miles
south of the INEEL boundary near Big Southern Butte. [22] Earlier USGS
studies show aquifer Iodine-129 concentrations at 41 pCi/L. [23] Iodine-129, a byproduct of the fission or
uranium is of concern because of its 15.7 million-year half-life, and its known
ability (like iodine-131) to lodge in the thyroid causing cancer. Because of this it is considered by EPA to
be a permanent environmental pollutant and the drinking water standard for
I-129 is set by EPA at one (1) pCi/l.
Radioactive
tritium from INEEL dumping reported by DOE in 1992 at 3,940,000 pCi/L [24]
has migrated the 50 miles via the aquifer to the Snake River. USGS 1994-99 spring discharges to the Snake
River sampling data show significant tritium concentrations of 65 pCi/L in the
Twin Falls and Hagerman areas. The highest tritium concentrations were found in
the eastern aquifer discharges to the Snake River at Devils Washbowl near
Kimberly, Idaho. [25]
USGS reports
also show groundwater flow, or “conductivity” in the Snake River Plain Aquifer
can reach 32,000 feet per day, or 6.06 miles per day. [26] Contaminates
discharged at INEEL have the potential to move rapidly through the aquifer to
public water sources and to the Snake River. This rapid flow is attributed to
the basalt lava flows underlying INEEL that have gaps called “lava tubes” that
can “conduct” large amounts of water. [27]
A 2001 USGS
report analyzed the relative “age” of different water strata within the Snake
River Aquifer using sophisticated analytic tools that measure dissolved
elements to determine how recently the water was on the surface. The study found that 20-50% of the aquifer
water is between 14 and 21 years “old” (length of time since it was last on the
surface before becoming subsurface aquifer recharge). The study also found
chlorofluorocarbon gases generated from INEEL chemical waste discharges about
20 kilometers south of the INEEL boundary. [28] This USGS
“age” study of the aquifer indicates a relatively rapid “turnover” of
groundwater in the aquifer. The
ramification being that radioactive and chemical contaminates in the aquifer
are also likely moving as rapidly with the water through the aquifer. These findings are consistent with
previously discussed sampling of aquifer spring discharges into the Snake River
containing radioactive tritium that has a half-life of about seven years. These
USGS research findings moreover contrast dramatically with DOE’s public claims
that contaminates discharged at INEEL will take hundreds or thousands of years
to reach the Snake River via the aquifer.
INEEL, over
its operating history, has received significant quantities of spent reactor
fuel from dozens of sources and recent minimal (non-compliant) cleanup costs
run between as 21 and 44.3 billion
dollars. [29] Basically, this far exceeds the cumulative
costs of all public works (including dams) in the history of the State of
Idaho. And who will pay? Not the DOE
contractors who, thanks to DOE, mostly have loopholes so they pay no taxes. The American taxpayer is left with the bill.
Even regulatory violation penalties on INEEL operators are passed on by DOE
contractors as expenses for doing business at INEEL and are thus paid by the
taxpayer!
A high
percentage of this INEEL irradiated reactor fuel was “reprocessed” using an
aqueous process which dissolves the fuel rods in acid/solvent solution that
then makes it possible to extract highly enriched uranium and other nuclear
isotopes for various United States military programs. The mixed hazardous and high-level radioactive liquid waste and
transuranic waste left over from this extraction process was then interned
primarily but not exclusively in underground storage tanks. These fifty-year-old tanks were never
intended to be the permanent repository for this waste because of the known
toxicity of the waste, the limited service life of the tanks themselves, and
the fact that at the time (and arguably currently) it was illegal under federal
statute. The concrete vaults that encase the eleven high-level 300,000-gallon
tanks at the Idaho Nuclear Technology and Environmental Center (INTEC),
formerly the Idaho Chemical Processing Plant, are known to leak. A 1994 State of Idaho investigation showed
that over a twenty-three month period (11/92 - 9/94) about 123,500 gallons of
contaminated water was pumped from the tank vault sumps. The investigation concluded that the source
of the water was precipitation, irrigation, and leaking high-level tank waste
system lines.[30]
DOE’s
reliance on these failed high-level tank containment systems for permanent
disposal of high-level waste under a new DOE Order 435.1 is misguided and puts
the general public and future generations at significant risk. As previously
noted, the Natural Resources Defense Council, together with numerous Native
American Tribes, is currently challenging this DOE Order in US Federal Court. [31]
Because the INEEL sits directly atop the Snake River Plain Aquifer, designated
by US Environmental Protection Agency (EPA) as a regional sole source aquifer,
protection of this aquifer is a main component of the 1995 Settlement Agreement
between the State of Idaho and DOE. [32]
Past and
current high-level and transuranic waste mismanagement practices have resulted
in massive contamination of the groundwater under the INEEL operations. This
recognized groundwater contaminate pathway represents a significant hazard to
the general public solely with current contaminate levels. Migration of buried
waste contaminates into underlying soil and perched ground-water zones is
extensively studied by US Geologic Survey and their report notes: “These zones are an integral part of the
pathway for contaminates to move to the Snake River Plain Aquifer. Water moves rapidly through surficial [sic]
sediments ...” [33] Plutonium-239-240 have been detected under
INEEL at 66 pCi/L, or 4.4 times the drinking water standard. [34]
IV. DOE Current Actions Pose an Imminent Threat
The INEEL
over its fifty-year operating history has generated on-site, or received via
off-site shipments, significant quantities of high-level radioactive nuclear
fuel waste (i.e. Nuclear Navy and Hanford reactor fuel), and transuranic waste
(i.e. DOE’s Colorado Rocky Flats Site) from fabrication of plutonium nuclear
bomb components.
INEEL uses
many sites (in addition to dumps) for permanent disposal of transuranic waste
including injection wells into the aquifer and unlined percolation ponds. [35] The largest and most significant INEEL
disposal sites are the Radioactive Waste Management Complex (RWMC) dump, and
the Argonne National Laboratory-West, Radioactive Scrap and Waste Facility,
located on the INEEL site. [36] Internal DOE documents, gained by the
Environmental Defense Institute (EDI) through Freedom of Information Act
requests and other state and federal agency records, show more than ninety (90)
metric tons of high-level irradiated reactor fuel was dumped at the RWMC. EDI’s Amicus brief shows the itemized
listing of this irradiated reactor fuel interned at the dump. [37] Generally, in the first several decades of
INEEL operation, the only reactor fuel put into storage was fuel the DOE
intended to reprocess. The rest,
apparently was simply dumped in the burial ground.
DOE’s Rocky
Flats Plant in Colorado shipped substantial quantities of plutonium waste to
INEEL. EDI’s investigations into these
Rocky Flats shipments show that considerably more plutonium was shipped to
INEEL and dumped than is disclosed by Idaho or DOE. EDI’s documentation
contends and further shows that the concentrations of plutonium and
highly enriched uranium waste dumped in the INEEL dump poses a significant
criticality hazard. [38]
Prior
to 1973, all waste shipped to INEEL for burial was simply dumped from the truck
into an open pit or trench. Normally only one pit or trench was open at any
given time, no sorting or assessment of what was in the barrels or boxes was
made. Nuclear waste shippers like the Rocky Flats Plant in Colorado knew there
would be no assessment of what was listed on the shipping manifest so there was
no incentive to do thorough characterization prior to shipment. Although DOE is not publicly acknowledging
the fact, its internal reports show the buried waste contains 11,000,000 curies
[39]
of radioactivity including 1,455 kilograms of plutonium from Rocky Flats alone.
[40] According to DOE, the total buried
plutonium (2,160 kg) from both Rocky Flats and other sources contains
700,400 curies of radioactivity. [41]
The
above DOE totals are now known to be grossly understated due to 1996
revelations about Rocky Flats plutonium waste shipments to INEEL. The
radioactivity in the INEEL buried waste cited above is still significantly
understated because it relies on original Rocky Flats shipping manifest records
that are completely unreliable. There were no checks at the INEEL dump to
confirm the accuracy of the manifests because these were shipments between DOE
facilities.
These
discrepancies were revealed only in the last few years when DOE was forced to
disclose (stipulated in international nuclear non-proliferation treaty
agreements) where all its nuclear bomb material is located and give precise
inventories. Rocky Flats Plant (largest
plutonium waste shipper to INEEL) conducted a physical inventory of plutonium,
compared it to the book inventory, and determined that 1,191.8 kg of plutonium
was unaccounted for and 953 kg of that total was shipped as waste to INEEL, and
not previously acknowledged in shipping manifests. [42]
So how much
plutonium is dumped in Idaho? If the
unreported Rocky Flats plutonium shortfall shipped to INEEL (953 kg) is added
to what DOE previously thought was in the INEEL dump (2,160 kg) from Rocky
Flats and other sources, it adds up to 3,113 kg in the dump from all sources.
This is an enormous amount of plutonium (enough for about 1,000 bombs) given
that it takes only about three to four kg of plutonium to make a nuclear bomb.[43] As previously discussed, this plutonium is
migrating from the dump site into the aquifer and, therefore, continues to pose
a public health threat.
A July, 2000
article in the Twin Falls, Idaho Times News discussed how much trouble
INEEL is having shipping stored waste to the DOE’s New Mexico transuranic waste
dump (WIPP), due mainly to serious underestimates of the total plutonium in
each drum. [44]
Forty-seven barrels of plutonium-contaminated waste couldn’t be shipped because
they contained too much plutonium.
V. INEEL Waste Tank Hazard
At INEEL,
the primary facility for reprocessing irradiated nuclear reactor fuel, is the
INTEC formerly known as the Idaho Chemical Processing Plant (ICPP). The INTEC underground high-level Tank Farm,
consisting of eleven 300,000-gallon tanks with a current volume of about 1.4
million gallons, [45] is only part of a large complex of an additional
127 high-level waste tanks that are part of the INTEC high-level waste
operations. EDI has listed these 127 tanks, their location
and what process they are attached too, however the waste volume of their
sediment contents is uncertain. [46] Some of these tanks are a significant
criticality hazard due to the high concentration of fissile (uranium and
plutonium) material content of the tanks. [47]
If DOE’s new
attempt to obfuscate the legal requirements and allow permanent disposal
in these already leaking waste tank units is not stopped, more pollution will
migrate to the aquifer, further putting the general public at risk. [48] DOE’s own reports show radioactive
groundwater contamination under INTEC greater than 60,000 times, and at Test
Reactor Area 176,000 times, the EPA-regulated maximum radionuclide
concentration level for drinking water. [49]
The hazard
is intensified by the fact that the U.S. Geological Survey report shows that
the top ground level of the INTEC high-level Tank Farm is within the Big Lost
River 100-year flood plain, which means the bottom of the tanks are some 50
feet below the flood levels. [50] Flooding of these tanks and the related
high-level waste processing buildings will flush pollutants into the aquifer
and endanger the general public, since these radionuclides are toxic for tens
of thousands of years.
1995
ICPP Well Sample Data
[51]Plan (final) Volume 1, August 1995, Lockheed
Idaho Technologies Co.
|
ICPP Well |
Gross Alpha (pCi/l) |
Gross Beta
(pCi/l) |
Strontium-90 (pCi/l) |
|
CPP-55-06 |
7,290 |
191,000 |
65,600 |
|
MW-2 |
4,700 |
925,000 |
516,000 |
|
MW-5 |
520 |
211,000 |
110,000 |
[INEEL-95/0056@2-162] [INEEL-95/0056 @ 5-25]
2002 INTEC Perched Ground
Water Sample Data [52]
|
Contaminate |
Concentration pCi/L |
Regulatory Std. pCi/L [53] |
Number Times Over Standard |
|
Gross Alpha |
1,100 |
15 |
73.3 |
|
Gross Beta |
590,000 |
4 millirem/yr |
-*- |
|
Tritium |
40,400 |
20,000 |
2.02 |
|
Strontium-90 |
136,000 |
8 |
17,000 |
|
Plutonium-238 |
0.0501 |
7.02 |
< 1 |
|
Americium-241 |
0.0374 |
6.34 |
< 1 |
|
Iodine-129 |
3.0 |
1 |
3 |
|
Technetium-99 |
457 |
900 |
< 1 |
|
Uranium-233/234 |
15.3 |
13.8 |
1.02 |
|
Uranium-235/236 |
0.142 |
14.5 |
< 1 |
|
Uranium-238 |
6.94 |
14.6 |
< 1 |
* Beta particle/photon radioactivity shall not produce
annual dose equivalent to the total body or internal organ greater than 4
millirem per year.
VI. Tank Closure Begins
The process of closure of these high-level
waste tanks at INEEL has begun. At
issue here is not the need to close the tanks, but what federal statutes and
the Settlement Agreement stipulations on buried high-level and transuranic
waste will be appropriately implemented and enforced to assure proper closure
in order to protect the public and environment. The Idaho Department of Environmental Quality (IDEQ) issued a
high-level waste tank Closure Plan for two INTEC tanks. [54]
The IDEQ
Tank Closure Plan violates environmental regulation that states in pertinent
part, “A detailed description of the steps needed to remove or decontaminate all
hazardous waste residues and contaminated containment system components,
equipment, structures, and soils during partial and final closure including,
but not limited to, procedures for cleaning equipment and removing contaminated
soils, methods for sampling and testing surrounding soils, and criteria for
determining the extent of decontamination necessary to satisfy the closure
performance standard.” (Emphasis added). [55] Closure and post-closure care regulation
also states “ At closure of a tank system, the owner or operator must remove
or decontaminate all waste residues, contaminated containment system
components (liners, etc.), contaminated soils, and structures and equipment
contaminated with waste, and manage them as hazardous waste.” [Emphasis added] [56] “As such, these liquids contain radioactive
fission products in sufficient concentrations to warrant permanent isolation in
a geologic repository.” [57]
DOE’s
attempt to delist the high-level tank wastes defies its own internal contractor
documents that show the history of these tanks. DOE estimates that about 20,000 gallons of tank sediment heels are in each of the
eleven Tank Farm units which would leave a total of 220,000 gallons permanently interned. [58]
The bottom
line is Idahoans and all communities downstream from INEEL can ill afford to
compromise the region’s most valuable
water resource for this and future generations. The state has already demonstrated its lack of enforcement
“due-diligence” by approving a tank closure plan that will permanently leave
thousands of gallons of high-level and transuranic waste in place over the
aquifer. This is as much an issue of
“homeland security” as fighting terrorists and the Bush Administration must
commit the requisite resources to cleaning up the INEEL nuclear legacy of the
cold war. It’s unconscionable that the
State of Idaho is actively blocking crucial information offered by EDI, and
needed by the federal court and the general public to make informed decisions about
the disposition of the INEEL massive waste problem. One can only assume that
both the state and DOE want to keep both the court and the public in the dark
about the extent of the INEEL problems.
VII. Percolation Pond Dumping Hazard
The Test
Reactor Area extensive use of unlined percolation ponds to dump radioactive and
chemical liquid wastes is cited here only as an example of the INEEL site-wide
use of this misguided practice. This
deadly pollution will eventually migrate to the Snake River Aquifer.
"Contaminates may also form or absorb onto
colloidal particles, which allows them to move with, or faster than the average
groundwater flow. Flow can result from
an apparently unrelated force, such as the flow of water and contaminates due
to a thermal or electrical gradient instead of the expected hydraulic
gradient. Chemical reactions and
biotransformation may occur, possibly changing the toxicity or mobility of
contaminates. Some contaminates dissolve and move with the water; some are in
the gas phase; others are nonaqueous phase liquids; some are more dense than
water and may move in a direction different from groundwater; others may be
less dense than water and float on top of it." [59] [OTA(a) @ 38]
Liquid
Waste Volumes Disposed at TRA [60]
|
Disposal Site |
Period Used |
Total Discharge (gal) |
|
Warm Waste Pond |
1952 - 1996 |
5.35 x 109 |
|
Cold Waste Pond |
1982- 1996 |
2.13 x 109 |
|
Chemical Waste Pond |
1962 - 1996 |
726 x 108 |
|
Sanitary Waste Pond |
1952- present |
310 x 106 |
|
Injection Well -05 |
1964-1982 |
3.89 x 109 |
|
Injection Well - USGS-53 |
1960-1964 |
2.2 x 108 |
|
Totals |
|
8.45 x 1010 or 84.5 billion gallons |
[TRA Record of Decision(a) @ 5]
Test
Reactor Area Perched Ground Water Sample Data
|
Nuclide |
Concentration pCi/L |
EPA Standard pCi/L |
Times over Standard |
|
Cobalt-60 |
12,200,000 |
100.00 |
122,000.0 |
|
Zinc-65 |
105,000 |
300.00 |
350.0 |
|
Cesium-134 |
62,400 |
8.13* |
7,675.0 |
|
Cesium-137 |
21,000,000 |
119.0* |
176,470.0 |
|
Europium-152 |
108,000 |
60.00 |
1,800.0 |
|
Europium-154 |
130,000 |
200.00 |
650.0 |
|
Europium-155 |
20,400 |
600.00 |
34.0 |
|
Americium-241 |
16,700 |
6.34 |
2,634.0 |
|
Chromium-51 |
2,540,000 |
6,000.00 |
423.0 |
|
Scandium-46 |
4,140 |
863.0* |
4.7 |
|
Iron-59 |
2,600 |
200.00 |
13.0 |
|
Zirconium-95 |
11,500 |
200.00 |
57.0 |
|
Niobium-95 |
12,000 |
300.00 |
40.0 |
|
Ruthenium-103 |
3,970 |
200.00 |
19.8 |
|
Rhodium-106 |
4,980 |
30.00 |
166.0 |
|
Silver-108 |
14,400 |
90.00 |
160.0 |
|
Antimony-124 |
150 |
60.00 |
2.5 |
|
Cerium-141 |
6,140 |
300.00 |
20.4 |
|
Ytterbium-175 |
3,500 |
300.00 |
11.6 |
|
Hafnium-181 |
136,000 |
200.00 |
680.0 |
|
Tantalum-182 |
3,180 |
100.00 |
31.8 |
|
Lead-203 |
1,680 |
1,000.00 |
1.6 |
|
Plutonium-239 |
12 |
15.00 |
0 |
|
Uranium-234 |
520 |
13.9* |
37.0 |
|
Strontium-90 |
18,000 |
8.00 |
2,250.0 |
|
Tritium |
3,940,000 |
20,000.00 |
197.0 |
The above
tables and other tables in this report citing EPA Maximum Contaminate Levels
(MCL) utilize both the current standards (40 CFR 141.66) that specify a 15
pCi/L gross alpha and a cumulative dose: “If two or more radionuclides are
present the sum of their annual dose equivalent to the total dose or to any
organ shall not exceed 4 millirem/yr.”
The 4 millirem/year (mrem/yr) dose limit and the EPA 1976 published
determination, and listing, for individual radionuclide MCL’s that are based on
the 4 mrem/yr limit are used in this report.
EPA attempted unsuccessfully in the late 1970's and again in 1991 to
propose changes to these standards.
General public outrage that the standards are not protective of public
health resulted in EPA falling back on the original 4 mrem/yr standard. Thus currently EPA regulations do not show
individual radionuclide MCL’s but the
earlier EPA individual 4 mrem/yr radionuclide doses are apparently not in
contention. [61]
VIII. Injection Wells Continue Contaminate Migration
INEEL
Radioactive and Chemical Waste Injection Wells
|
Injection Well |
History |
Contamination |
Status |
|
Test Area North (TSF-05) |
Drilled 1953 305 feet |
Radioactive and Volatile Organic |
Now used for groundwater
remediation |
|
Test Area North Initial Engine Test (IET-06) |
Drilled 1953, 329 feet Nuclear Engine coolant and fuel |
Radionuclides and chemicals |
Converted to a monitoring well 1982 |
|
Test Area North WRRTF well (WRRTF-05) |
Drilled 1957 313 feet |
50 mCi Cobalt-60 212 liter (56 gal) Turbine oil |
Abandoned 1984 |
|
Test Reactor Area (TRA-05) |
Drilled 1964 |
Chromium and radionuclides |
Converted to monitoring well 1982 |
|
Test Reactor Area (USGS-53) |
Drilled 1960 |
Chromium and radionuclides |
Converted to monitoring well 1964 |
|
ICPP (CPP-23) |
Drilled 1952 580 feet |
21,302 Curies of rad. and chemicals |
Pressure grouted closed 1989 |
|
ICPP (USGS-50) |
Used Sept.1970 to present |
Chemicals and radionuclides |
Currently used for emergency disposal & as a monitoring well |
|
Axillary Reactor Area Power Burst Facility (PBF-15) |
Used 1972 to 1978 for reactor coolant discharge and
corrosive waste |
Sulfuric acid Sodium Hydroxide Chromium |
Capped in 1979 |
|
Axillary Reactor Area Power Burst Facility (PBF-05) |
Used 1973 to 1984 discharge rad. waste and reactor coolant |
Radionuclides |
Capped in 1984 |
[ICPP RI/FS] [USGS Report
00-4222, DOE/ID-22168]
The Test Area North (TAN) at INEEL is yet another area were
significant radioactive and chemical waste was dumped via injection wells
directly into the Snake River Plain Aquifer.
Maximum
contaminant in TAN TSF-05 injection well sludge
[OU 1-07B TAN groundwater RI/FS
workplan, Appendix B and G]
|
Substance |
Concentration EPA
Standard |
|
1,1 dichloroethylene |
24 ug/gm 7
ug/L |
|
methylene chloride |
290 ug/l ? |
|
trans-1,2-dichloroethylene |
410 ug/gm 5
ug/gm |
|
trichloroethylene |
30,000
ug/gm 5 ug/gm |
|
tetrachloroethylene |
2,800 ug/gm 5
ug/gm |
|
2-butanone(methyl ethylketone) |
180 ug/gm ? |
|
barium |
326 ug/gm 1,000
ug/gm |
|
lead |
180 ug/gm 50 ug/gm |
|
chromium |
91 ug/gm 50 ug/gm |
|
mercury |
101 ug/gm 2 ug/gm |
|
|
|
|
Gross Beta |
4,900,000 pCi/l 8
pCi/l |
|
Gross Alpha |
6,000
pCi/l 15 pCi/l |
|
cobalt-60 |
812 pCi/gm
|
|
cesium-137 |
2,340 pCi/gm
|
|
emporium-154 |
6.62 pCi/gm |
|
americium-241 |
23.6 pCi/l 6.34
pCi/l |
|
tritium |
1,000,000 pCi/l
20,000 pCi/l |
|
plutonium-241 |
123.6 pCi/l 62.6 pCi/l |
|
plutonium-239 |
12.2 pCi/gm |
[TAN Sludge] [TAN ROD
@18][EGG-ER-10643][INEEL-95/0056@5-25]
The above
TAN aquifer sampling data is derived from DOE documents. [62]1992, Idaho National Engineering Laboratory This
information on TAN is cited here only as an example to the extensive problem
throughout INEEL from the use of direct injection of wastes into the aquifer.
IX. Off INEEL Site Snake River Aquifer Water Sampling
INEEL’s southern boundary is about 53 miles from the Rupert area
and about 110 miles from the Hagerman area (see map below). INEEL over the past
five decades has dumped vast quantities of radioactive waste into shallow pits,
trenches, and unlined percolation ponds.
Billions of gallons of radioactive waste water was also injected
directly into the aquifer until the early 1980's when then Governor Cecil
Andrus forced the federal government to end the practice. A 1995 U.S.
Geological Survey report notes:
“In the past, wastewater
containing chemical and radio chemical wastes generated at the INEL was
discharged mostly to ponds and wells.
Since 1983, most aqueous wastes have been discharged to infiltration
ponds. Many of the constituents in the
wastewater enter the aquifer indirectly following percolation through the
unsaturated zone.”
[DOE/ID-22130,p.3]
The following tables show U. S. Geologic Survey (USGS) 1989-2001
water sample data from 33 of the 55 monitoring wells in the Snake River Aquifer
south of INEEL between Rupert on the east and Bliss/Hagerman on the west. These monitoring wells are in the Magic
Valley group of wells checked by USGS in multi-year sampling campaigns. The sample data show gross beta and alpha
radioactivity over the period and is used as a screening method to determine if
additional testing is needed.
The comparative water sample data is a means of identifying
trends in the migration of radioactive contaminates. The USGS emphasizes that the Magic Valley monitoring wells remain
below the Environmental Protection Agency maximum concentration level (MCL)
standard for drinking water. Generally, this is correct except for Well MV-45
located between Bliss and Hagerman, Idaho about 65 miles southwest of INEEL
that registered 18.70 + 2.4 for gross alpha.[63] The drinking water MCL standard for alpha is
15 pCi/l. If increasing trends are
confirmed, then additional isotope specific tests may be needed to identify the
source of the contamination. As
discussed previously, independent experts believe that this “Safe Drinking Water standard of 15 picocuries per
liter for alpha emitting transuranics like plutonium-238, plutonium-239, or
americium-241 allows doses on the order of a hundred times higher than the 4
millirem annual limit specified for most beta emitters. A concentration of
plutonium of only about 0.08 picocuries per liter in drinking water is required
to produce a dose of 4 millirem per year to the bone surface (the crucial organ
for plutonium).” [64]
The following tables compare
gross beta and gross alpha particle radioactivity, which is a measure of
the total radioactivity given off as beta or alpha particles during the radioactive
decay process. USGS instruments were calibrated for dissolved cesium-137 (gross
beta) and dissolved thorium-230 (gross alpha).
The concentrations of gross beta/alpha particle activity is for
reference only and does not imply that the radioactivity is attributed to these
specific isotopes. The numbers in the
tables are the mean or middle number between an analytic plus or minus (+ ) uncertainty range published in USGS reports.
Snake River Aquifer Water
Sample Data
Gross Beta (as dissolved Cesium-137)(pCi/L)
|
Well # |
1989 |
1990-92 |
1994-95 |
1996-98 |
1999-01 |
|
MV-01 |
7.8 +1.21 |
7.3 +1.65 |
|
6.86 +1.76 |
10.7+2.4 |
|
MV-02 |
10.65 +1.65 |
7.57 +2.01 |
7.64 +1.58 |
11.1+4.3 |
8.09 +2.68 |
|
MV-03 |
4.88 +0.77 |
4.33 +1.28 |
4.58 +2.91 |
5.84 +1.36 |
6.5+1.7 |
|
MV-04 |
6.54 +1.2 |
7.38 +1.67 |
|
5.83 +3.11 |
7.43+ 2.6 |
|
MV-05 |
7.36
+ 1.29 |
6.69
+ 1.51 |
12.0
+ 5.38 |
6.99 + 1.89 |
9.28+2.55 |
|
MV-06 |
6.12 +
1.02 |
8.01
+ 1.63 |
7.93.. + 4.86 |
6.12 + 1.61 |
8.52+2.18 |
|
MV-07 |
4.62
+ 0.77 |
4.00
+ 1.26 |
6.49
+ 4.24 |
7.1 + 4.2 |
3.2+2.16 |
|
MV-09 |
10.6 +2.0 |
8.96 +2.31 |
|
10.2+4.2 |
17.34 +5.36 |
|
MV-10 |
10.60
+ 1.7 |
9.67 +
2.23 |
9.93
+ 1.96 |
|
8.31 +3.43 |
|
MV-11 |
11.50 +
1.90 |
13.40 +
2.85 |
8.20 + 3.5 |
8.2 + 3.5 |
9.67 +5.18 |
|
MV-12 |
7.26 +1.25 |
7.34 +1.78 |
|
7.22 +1.89 |
3.72 +4.68 |
|
MV-13 |
9.31 +
1.5 |
7.50 +
1.54 |
10.1 +
5.9 |
8.24 + 1.72 |
9.0+2.17 |
|
MV-14 |
5.36 +1.17 |
3.56 +1.12 |
|
5.78 +1.89 |
5.79 +2.6 |
|
MV-15 |
8.25 +
1.39 |
10.60
+ 2.22 |
8.12 + 2.07 |
8.12+2.07 |
4.65 +4.85 |
|
MV-16 |
4.39 + 0.73 |
3.99 +
1.26 |
4.66 +
1.15 |
7.6 + 4.1 |
5.06 +2.46 |
|
MV-17 |
4.64 + 0.79 |
4.15 +
1.24 |
7.01 +
4.14 |
5.10 + 2.84 |
5.91+1.23 |
|
MV-18 |
7.73 +1.38 |
7.51 +1.86 |
|
6.24+2.6 |
8.5 +4.93 |
|
MV-19 |
6.8 +1.07 |
4.7 +1.4 |
6.5 +1.44 |
3.2+3.9 |
4.61 +2.42 |
|
MV-20 |
6.17 +
1.01 |
4.51 +
1.14 |
5.48 +
1.27 |
7.4 + 4.1 |
5.36 +2.05 |
|
MV-21 |
4.98 +0.8 |
4.6 +1.29 |
|
4.43+1.13 |
5.01 +1.39 |
|
MV-23 |
9.37 +
1.53 |
8.41 +
1.89 |
4.39 + 1.04 |
8.83+3.45 |
7.69 +2.65 |
|
MV-24 |
|
|
11.0 +2.39 |
|
|
|
MV-24-A |
|
|
|
8.38+3.62 |
11.4 +3.65 |
|
MV-25 |
22.21 +2.85 |
9.13 +2.08 |
10.5 +2.2 |
11.5+ 4.4 |
8.66+2.97 |
|
MV-26 |
5.99 + 0.92 |
5.40 +
1.26 |
9.02 +
4.63 |
4.44 + 1.47 |
7.81 +2.63 |
|
MV-27 |
6.81 +
1.04 |
6.73 +
1.51 |
9.57 +
5.18 |
6.06 + 1.54 |
7.61+2.51 |
|
MV-29 |
5.43 +0.9 |
3.96 +1.2 |
4.68 +1.36 |
4.11+1.12 |
1.13 +4.3 |
|
MV-30 |
7.16 +1.22 |
6.25 +1.62 |
|
6.59+3.19 |
7.93 +4.93 |
|
MV-31 |
6.80 +
1.22 |
7.32 +
1.55 |
13.1 + 4.37 |
9.53 + 1.64 |
8.02 +3.39 |
|
MV-32 |
8.38 +
1.38 |
8.15 +
1.91 |
9.45 +
1.9 |
7.5 + 4.2 |
8.28+2.63 |
|
MV-33 |
4.82 +
0.78 |
3.27 +
1.06 |
4.39 + 1.04 |
4.39 +1.04 |
5.74 +1.79 |
|
MV-36 |
5.44 +
0.91 |
4.80 + 1.18 |
7.03 + 4.22 |
4.2 + 1.05 |
4.98+1.59 |
|
MV-37 |
6.83 +1.07 |
4.75 +1.45 |
|
3.75+1.21 |
2.93 +4.36 |
|
MV-38 |
3.65 + 0.69 |
3.87 +
1.21 |
4.71 +
3.85 |
3.93 + 1.06 |
5.27+1.26 |
|
MV-39 |
8.56 +1.52 |
7.81 +1.88 |
|
5.26 +3.08 |
7.34 +2.73 |
|
MV-40 |
5.93 +0.9 |
4.11 +1.19 |
4.13 +1.18 |
5.4+4.0 |
4.67 +4.44 |
|
MV-41 |
6.39 + 1.04 |
7.33 +
1.89 |
7.24
+ 1.81 |
7.0 +
4.2 |
6.89+2.41 |
|
MV-42 |
6.00 +
0.94 |
0.71 +
0.58 |
8.65 +
4.36 |
6.03 + 1.18 |
6.97+1.49 |
|
MV-43 |
10.1 +1.71 |
9.17 +2.13 |
|
6.68 +3.32 |
8.91+5.06 |
|
MV-45 |
4.69 + 0.78 |
4.45 +
1.30 |
6.10 +
4.19 |
4.0 + 3.9 |
|
|
MV-46 |
4.49 +0.73 |
4.17 +1.25 |
4.21 +1.24 |
4.08 + 1.03 |
3.49 +1.67 |
|
MV-47 |
4.82 + 0.76 |
4.07 +
1.06 |
|
3.6 + 3.9 |
5.06 +1.8 |
|
MV-49 |
3.62 + 0.7 |
2.52 +
0.87 |
3.15 +
0.95 |
4.2 + 3.9 |
4.79 +2.43 |
|
MV-50 |
7.51 +
1.25 |
8.75 +
1.77 |
9.43 +
1.87 |
4.95 +3.1 |
8.96 +3.39 |
|
MV-51 |
8.06 +
1.53 |
7.22 + 1.83 |
|
11.2 + 4.4 |
3.96+4.7 |
|
MV-52 |
9.56
+
1.44 |
8.93 +
1.88 |
8.44 +
1.68 |
8.4 + 4.2 |
8.81 +3.42 |
|
MV-53 |
9.43 +
1.58 |
9.94 +
2.06 |
9.57 +
5.4 |
10.7 + 2.23 |
|
|
MV-54 |
8.82 + 1.52 |
9.19 +
2.12 |
9.40 +
2.05 |
8.4 + 4.3 |
10.37 +4.88 |
|
MV-55 |
4.80 + 0.92 |
3.55 +
1.10 |
8.46 +
4.25 |
6.04 + 1.37 |
2.78+2.34 |
|
MV-56 |
4.89 +
0.86 |
4.73 +
1.32 |
5.21 +
1.24 |
3.8 + 3.9 |
0.48+4.33 |
|
MV-57 |
4.11 +
0.67 |
2.81 +
0.85 |
3.48 +
1.06 |
3.25 + 1.03 |
2.47+1.02 |
|
MV-59 |
5.35 +
0.83 |
4.37 + 1.24 |
6.13 + 2.37 |
8.44 +2.75 |
2.78+4.53 |
|
MV-60 |
|
|
|
|
11.0+2.98 |
|
MV-61 |
4.65 +0.85 |
4.70 +1.35 |
|
6.13 +2.37 |
-.55+4.28 |
Gross Alpha (as dissolved thorium-230) (pCi/L)
|
Well # |
1989 |
1990-92 |
1994-96 |
1997-1998 |
1999-2001 |
|
MV-03 |
2.62 +0.65 |
2.0 +0.76 |
0.218 +1.2 |
4.48 + 2.89 |
1.61+2.07 |
|
MV-05 |
4.65 +
0.85 |
2.22 +0.8 |
3.56 +
2.96 |
5.26 + 3.39 |
4.9+2.3 |
|
MV-06 |
1.88 +
0.5 |
1.67
+ 0.65 |
4.22 +
3.11 |
6.23 + 3.36 |
2.8+2.39 |
|
MV-07 |
2.46
+ 0.62 |
1.51 +0.63 |
3.36
+ 2.71 |
2.17 + 2.48 |
1.1+1.4 |
|
MV-10 |
2.87
+ 0.65 |
3.35 +
0.97 |
3.22 +
2.14 |
2.3 + 2.7 |
0.62 +0.85 |
|
MV-11 |
3.05
+ 0.65 |
3.91 +
1.04 |
5.79 + 3.79 |
|
1.88 +2.59 |
|
MV-12 |
2.7 +0.66 |
2.28 +0.79 |
2.56 +1.98 |
|
6.08 +3.62 |
|
MV-13 |
5.12 +
0.97 |
2.15 + 0.72 |
4.20 +
3.09 |
4.55 + 3.07 |
3.7+1.8 |
|
MV-15 |
2.30 +
0.54 |
2.58 + 0.82 |
4.84 + 2.86 |
|
3.39 +3.24 |
|
MV-16 |
2.32 +
0.66 |
1.95 +
0.73 |
1.42 +
0.95 |
1.1 + 2.1 |
1.33 +1.47 |
|
MV-17 |
1.07 +
0.59 |
1.31 + 0.06 |
0.103 +
1.82 |
5.1 +2.84 |
0.69+1.56 |
|
MV-20 |
1.08 +
0.52 |
1.92 +
0.074 |
3.02 +
1.62 |
5.5 + 3.0 |
1.19 +0.78 |
|
MV-23 |
1.85 +
0.48 |
2.39 +
0.79 |
3.54 + 2.77 |
|
-.21 +2.43 |
|
MV-26 |
2.32 +
0.62 |
1.59 +
0.65 |
2.22 +
2.36 |
0.96 +2.35 |
0.81 +1.26 |
|
MV-27 |
4.09 +
0.8 |
2.62 +
0.82 |
2.56 +
2.73 |
4.83 +3.12 |
5.12+3.37 |
|
MV-31 |
3.04 +
0.72 |
2.31
+ 0.77 |
10.9 +
4.65 |
9.22 +3.8 |
1.42 +1.73 |
|
MV-32 |
6.00 +
1.04 |
3.75 +
1.05 |
2.85 +
2.06 |
3.9 + 3.1 |
3.34+3.13 |
|
MV-33 |
0.68 +
0.46 |
2.29 +
0.81 |
1.19 + 1.3 |
|
0.72 +0.52 |
|
MV-36 |
5.12 +
1.0 |
2.10 +
0.70 |
4.54 +
3.08 |
2.64 +2.34 |
2.3+1.7 |
|
MV-37 |
4.75 +0.99 |
4.15 +1.06 |
1.94 +1.61 |
|
4.05 +3.37 |
|
MV-38 |
1.86 +
0.51 |
1.19 +
0.58 |
1.62 +
2.26 |
4.58 +2.73 |
2.05+1.85 |
|
MV-41 |
4.76 +
0.98 |
5.24 +
1.15 |
7.21 +
3.16 |
4.3 + 3.2 |
3.13 +3.2 |
|
MV-42 |
2.08 +
0.55 |
3.18 +
0.93 |
3.21 +
2.72 |
2.76 +2.46 |
2.24+2.8 |
|
MV-43 |
5.01 +0.92 |
4.58 +1.13 |
4.49 +3.01 |
|
4.64 +3.25 |
|
MV-46 |
1.82 +0.53 |
1.10 +0.54 |
0.73 +0.79 |
4.4 + 2.62 |
1.23 +0.66 |
|
MV-45 |
18.70 +
2.4 |
1.27 +
0.54 |
3.96 +
2.85 |
2.1 + 2.2 |
|
|
MV-47 |
1.66 +
0.51 |
2.02 +
0.73 |
0.8 +1.9 |
|
0.3 +0.54 |
|
MV-49 |
0.00 +
0.7 |
1.56 +
0.63 |
3.04 +
1.49 |
2.8 + 2.4 |
1.36 +1.51 |
|
MV-50 |
7.74 +
1.33 |
3.09 +
0.87 |
2.12 +
2.09 |
|
1.95 +1.35 |
|
MV-51 |
2.92 +
0.67 |
3.15 +
0.93 |
3.2 +3.0 |
3.2 + 3.0 |
5.15 +3.45 |
|
MV-52 |
3.80 +
0.73 |
4.00 +
1.02 |
4.15 +
2.2 |
2.8 + 2.8 |
2.16 +1.92 |
|
MV-53 |
3.25 +
0.69 |
2.89 +
0.87 |
1.55 +
1.27 |
8.95 + 4.2 |
5.2+3.86 |
|
MV-54 |
3.87 +
0.75 |
2.38 +
0.84 |
4.51 +
2.6 |
4.4 + 3.5 |
2.18 +2.97 |
|
MV-55 |
2.38 +
0.65 |
1.57
+
0.63 |
0.80 +
1.44 |
3.33 + 2.79 |
1.4+1.5 |
|
MV-56 |
1.97 + 0.59 |
1.48 +
0.66 |
1.11 +
1.01 |
2.1 + 2.3 |
2.05 +2.83 |
|
MV-57 |
0.03 +0.29 |
1.34 +
0.058 |
1.71 +
0.93 |
-.12 +1.78 |
2.2+1.13 |
|
MV-58 |
2.08 +0.54 |
1.02 +0.5 |
0.58 +1.03 |
-.12 + 1.83 |
1.1+1.2 |
|
MV-59 |
0.31 + 0.26 |
1.76
+ .67 |
2.19 + 2.0 |
|
2.56 +2.91 |
|
MV-60 |
|
|
|
|
4.16+3.78 |
|
MV-61 |
11.2 +1.6 |
2.97 +0.95 |
3.68 +2.43 |
|
|
Sources for above tables are
drawn from USGS:
DOE/ID-22124, DOE/ID-22130, DOE/ID-22133, DOE/ID-22141;
DOE-IDO-22161; DOE/ID-22152; DOE/ID-22169;
DOE-ID-22176; DOE/ID-22185.
The above table units abbreviation - pCi/L - stands for pico
curies per liter or one trillionth of one curie per liter. The maximum
contaminate levels (MCL) for selected radioactivity and selected radionuclides
in drinking water is established by the Environmental Protection Agency. For comparison, the MCL for the beta emitter
strontium-90 is 8 pCi/L, and the MCL for cesium-137 it is 120 pCi/L based on an average concentration assumed to
produce a total body or organ dose of 4 millirem per year. The MCL for gross alpha particulate
radioactivity is 15 pCi/L.
As with all water sampling techniques, there is a range of
uncertainty from instrument and sampling procedure variation. So the sample
concentration is stated as the mean or middle of the uncertainty range which in
turn is stated as plus or minus(+). A slight increase or decrease in
different samples from the same well may be a result of this analytic
uncertainty or variation. A major
component of uncertainty is the standard deviation which varies with each
sample. USGS uses a factor of two times
the sample’s standard deviation to identify the uncertainty range which is
noted as a plus or minus number after the mean concentration number. The USGS uncertainty range appears to vary
widely between sampling periods. For
instance the average uncertainty in 1989 and 1990-92 sample campaigns was about
21 percent where as the average uncertainty in 1994-95 was nearly 60 percent. More detailed testing of a broad range of
isotopes may be needed to identify the sources of this well contamination. The
State INEEL Oversight Program, Idaho State University, and the Environmental
Research Foundation are also doing testing, however their instruments are
according to USGS, a thousand times less sensitive than the USGS’s
National Water Quality Laboratory. The usefulness of the above tables is to
demonstrate trends in contaminate levels in the Snake River Aquifer south of
the INEEL and factor this information into waste management decisions.
X. Clean Water Act Violations
David McCoy
did a legal analysis that, among other issues, identified major Clean Water Act
violations at INEEL.[65]
McCoy notes that the INTEC (located at INEEL) lies within the 100 year
floodplain of the Big Lost River. The
INTEC facilities service wastewater system and the Percolation Ponds are also
located within the 100 year floodplain of the Big Lost River.
DOE Order
5400.1 requires DOE to comply with the mandatory requirements of Executive
Order 11988 for Floodplain Management and Executive Order 11990 for Protection
of Wetlands. (See 10 CFR 1022 et seq.).
DOE Order
5400.1 requires DOE to comply with the requirements of the Clean Water Act, 33
U.S.C. § 1251 et seq. DOE violates DOE
Order 5400.1 and the Clean Water Act by its failure to obtain a National
Pollution Discharge Elimination System (NPDES) permit for the INTEC facilities.
The INTEC
facilities are considered point sources under the CWA. 33 U.S.C. § 1362(14).
Section 301
of the CWA, 33 U.S.C. § 1311(a) prohibits the discharge of any pollutant from a
point source into the waters of the United States unless such discharge is
permitted in a National Pollution Discharge Elimination System (NPDES)
permit. As shown below, DOE has
discharged pollutants including hazardous wastes and radionuclides to the
waters of the United states without a NPDES permit, in violation of § 301(a) of
the CWA, 33 U.S.C. §1311(a).
The INTEC
facilities do not have a NPDES permit.
The unlined
Percolation Ponds at INTEC, which receive the point source wastes from the HLLWE and the other INTEC facilities, are
surface impoundments located in the floodplain above the Snake River Plain
Aquifer which is hydrologically connected to and part of the Snake River. The
Snake River and its aquifer are waters of the United States. Waters of the United States include waters
that are tributary to navigable waters.
Congress intended to regulate the discharge of any pollutants that could
affect surface waters of the United States, whether it reaches the surface
water directly or through groundwater.
The INTEC Percolation Ponds discharge water into
the waters of the United States, but DOE has failed to obtain a NPDES permit
for the ponds. Also see US District Court for Idaho ruling in Idaho Rural
Council v. Bosma, No. CV-99-0581-S-BLW. where Judge Winmill ruled in favor of the citizen suit
alleging noncompliance with NPDES
permit. The court ruling acknowledges that if toxic waste ends up in
surface waters, then it is covered under the Clean Water Act.
The USGS scientific studies show INEEL discharged waste eventually flows to the Snake River Plain Aquifer that then discharges to the Snake River, and federal court rulings document that the Clean Water Act regulations apply to INEEL toxic waste discharges. Court rulings state:
“Congress intended to regulate
‘discharges of pollutants that could affect surface waters for the United
States,’ the rationale supporting this conclusion is simple and persuasive:
‘since the goal of the CWA is to protect the quality of surface waters, any
pollutant which enters such waters, whether directly or through groundwater, is
subject to regulation by NPDES permit. Stated even more simply, whether
pollution is introduced by a visible, above-ground conduit or enters the
surface water through the aquifer matters little to the fish, waterfowl, and
recreational users which are affected by the degradation of our nation’s rivers
and streams.” [66]
XI. Conclusion
This report is not, and cannot claim to offer all the relevant
information related to the INEEL impact on the Snake River Plain Aquifer.
Nonetheless, we feel compelled to offer this “snapshot” in the interest of
expanding the information base upon which the residents of the northwest can
make informed decisions on the disposition of INEEL’s radioactive and chemical
wastes. Much is at stake, and DOE’s gross past waste mismanagement may well
continue into the future if fundamental changes are not implemented.
Fundamentally, given the long half-life of radioactive
contaminates, and the fact that toxic chemicals have NO half-life, it makes no
difference when various water samples were collected because this pollution
will eventually reach somebody’s water tap since it is already in the water
system. The limited data currently available to the Environmental Defense
Institute at the time of this writing, clearly indicate that there is a major
public health and safety hazard looming related to the migration of the INEEL
waste discharges and plans to permanently leave huge quantities of waste, in
effect, create a “nuclear sacrifice zone.”
This pollution is currently, and will continue for millennia,
contaminating the Snake River Aquifer Plain Aquifer that eventually will (if
not currently do) threaten all downstream (including Oregon and Washington)
users of this regional water source. Immediate action is needed by federal and
state regulators, in addition to public pressure, to ensure that tank waste,
buried radioactive and hazardous chemical wastes are exhumed, and that
continued dumping of INEEL process waste into unlined percolation ponds is
terminated. Time is of the essence, since every day that goes by, more of this
deadly pollution migrates beyond any means of mitigation.
XII. Attachments:
USGS maps that show locations
of off-site INEEL Snake River Plain Aquifer Sample Wells and Snake River Plain
Aquifer discharge springs into the Snake River noted in this report. These
attachments however are not available in the electronic version of this report,
but are available upon request.
XIII. References:
Citizens
Guide to the Idaho National Engineering Laboratory, Environmental Defense
Institute, Chuck Broscious, Revised
2002.
Comprehensive Remedial Investigation / Feasibility Study for
Argonne National Laboratory-West Operable Unit 9-04 at the Idaho National
Engineering Laboratory, U.S. Department of Energy
DOE/ID-12111; Summaries of the INEL Radioecology
and Ecology Program, O. Markham, June
1987
DOE/ID/12119; INEL Historical Dose Evaluation,
USDOE ID Operations Office, Aug 1991
DOE/ID-22071;
Capacity of the Diversion Channel Below the Flood Control Dam on the Big Lost
River at the Idaho National Engineering Laboratory, US Geological Survey,
Investigations Report 86-4204, C. Bennett, October 1986
DOE/ID-22109;
Statistical Summaries of Streamflow Data for Selected Gauging Stations on and
near the
Idaho National Engineering Laboratory through 1990, US Geological Survey
Investigations
Report 92-4196,
M. Stone, L. Mann, L.Kjelstrom, 1993
DOE/ID-22124;
Radionuclides, Stable Isotopes, Inorganic Constituents, and Organic Compounds
in Water from Selected Wells and Springs from the Southern Boundary of the
Idaho National Engineering Laboratory to the Hagerman Area, Idaho 1994, U.S.
Geological Survey Open File Report 95-718, October 1995, R. Bartholomay, L.
Williams
DOE/ID-22125;
Chemical Constituents in Water from Wells in the Vicinity of the Naval Reactors
Facility, Idaho National Engineering Laboratory, Idaho 1994-95, US Geological
Survey, Open-File Report 95-725
DOE/ID-22130;
Radionuclides, Stable Isotopes, Inorganic Constituents, and Organic Compounds
in Water from Selected Wells and Springs from the Southern Boundary of the
Idaho National Engineering Laboratory to the Hagerman Area, Idaho 1991-93, U.S.
Geological Survey Open File Report 95-725, November 1995, B. Tucker, L.Knobel,
R. Bartholomay
DOE/ID-22133;
Evaluation of Radionuclide, Inorganic Constituent, and Organic Compound Data
from Selected Wells and Springs from the Southern Boundary of the Idaho National
Engineering Laboratory to the Hagerman Area, Idaho 1989 through 1992, U.S.
Geological Survey Water Resources Investigations Report 97-4007, January 1997,
R. Bartholomay, L. Williams
DOE/ID-22139; Preliminary Delineation of Natural
Geochemical reactions, Snake River Plain Aquifer System,
Idaho
National Engineering Laboratory, US Geological Survey, Water Resources
Investigations Report 97-4093, May 1997
DOE/ID-22141;
Radiochemical and Chemical Constituents in Water from Selected Wells and
Springs from the Southern Boundary of the Idaho National Engineering Laboratory
to the Hagerman Area, Idaho 1996, US Geological Survey, Open-File Report 97-360
DOE/ID-22143;
Chemical and Radiochemical Constituents in Water from Wells in the Vicinity of
the Naval Reactors Facility, Idaho National Engineering Laboratory, Idaho
1994-95, US Geological Survey, Open-File Report 97-806
DOE/ID-22152;
Radiochemical and Chemical Constituents in Water from Selected Wells and
Springs from the Southern Boundary of the Idaho National Engineering Laboratory
to the Hagerman Area, Idaho 1997, US Geological Survey, Open-File Report 98-646
DOE/ID-22155;
Geologic Controls of Hydraulic Conductivity in the Snake River Plain Aquifer at
and Near the INEEL, Idaho, US Geological Survey, Report 99-4033, February 1999.
DOE/ID-22161;
Radiochemical and Chemical Constituents in Water from Selected Wells and
Springs from the Southern Boundary of the Idaho National Engineering Laboratory
to the Hagerman Area, Idaho 1998, US Geological Survey, Open-File Report 99-473
DOE/ID-22169;
Radiochemical and Chemical Constituents in Water from Selected Wells and
Springs from the Southern Boundary of the Idaho National Engineering Laboratory
to the Hagerman Area, Idaho 1999, US Geological Survey, Open-File Report 00-399
DOE/ID-22175; Radiochemical and Chemical
Constituents in Water from Selected Wells South of INEEL, Open
File
Report 01-138, May 2001.
DOE/ID-22176;
Radiochemical and Chemical Constituents in Water from Selected Wells and
Springs from the Southern Boundary of the Idaho National Engineering Laboratory
to the Hagerman Area, Idaho 2000, US Geological Survey, Open-File Report 01-358
DOE/ID-22180;
Tritium in Flow from Selected Springs that Discharge to the Snake River, Twin
Falls - Hagerman Area, Idaho, 1994-99, Open File Report 02-185, May 2002
DOE/ID-22181; Estimating the Magnitude of the
100-Year Peak Flow in the Big Lost River at the INEEL, Idaho, USGS Water
Resources Investigations Report 02-4299,
http://idaho.usgs.gov/public/reports.html
DOE/ID-22185; Radiochemical and Chemical
Constituents in the Water From Selected Wells and Springs from the Southern
Boundary of the INEEL To the Hagherman Area, Idaho, 2001, US Geological Survey
Open File Report 03-168, April 2003.
For More Information Contact
Environmental Defense Institute
P.O. Box 220, Troy, Idaho 83871
208-835-6162
email: edinst@tds.net website: http://personalpages.tds.net/~edinst
[1] This report is a publication of the
Environmental Defense Institute, written by Chuck Broscious and edited by
Patricia Diaz, Ph.D. First released in April and revised June 2003.
[2] Idaho High-Level Waste and Facilities
Disposition, Final Environmental Impact Statement, September 2002,
DOE/EIS-0287, page 4-47. Herein after called DOE/EIS-0287.
[3] University
of Idaho; Snake River Plain Aquifer , Idaho Water Resources Research Institute,
[4] Tritium in Flow from Selected Springs that
Discharge to the Snake River, Twin Falls-Hagerman Area, Idaho, US Geological
Survey, Open Report 02-185, DOE/ID-22180, page 6.
[5] EGG-ER-10643; Remedial Investigation Final
Report with Addenda for the Test Area North Groundwater Operable Unit 1-07B at
INEEL, J. Kaminsky, EG&G Idaho, January 1994.
[6] Environmental Radiological Surveillance Report
on Oregon Surface Waters, 1961- 1983, Oregon Department of Human Services,
Radiation Control Section.
[7] Joint Amicus Brief of Idaho, Washington,
Oregon and South Carolina, NRDC vs. DOE, US Federal Court District of Idaho,
Case No. CV-01-413-S-BLW, March 24, 2003, page 4.
[8] Environment, Safety, and Health Needs of the
US Department of Energy, September
1988, pages 3-166, 3-115, and 3-116. DOE/EH/OEV-22-P.
[9] Notice of Intent to Sue DOE, EPA, and IDEQ,
June 14, 2001 Environmental Defense Institute
and David McCoy.
[10] Notice of Intent to Sue DOE, EPA, and IDEQ,
July 9, 2002 by Environmental Defense Institute, Keep Yellowstone Nuclear Free,
and David McCoy.
[11] NRDC
vs. DOE, U.S. District Court for State of Idaho, Case No. CV-01-413-S-BLW
[12] INEEL Oversight Program,
Environmental Surveillance Program, Quarterly Data Report, October – December,
2000, page 25, State of Idaho. Hereinafter called INEEL OP December 2000. Well
M1S located at the Radioactive Waste Management Complex, Subsurface Disposal
Area detected plutonium 241 at 66 pCi/L (dated 7/99), and plutonium-239/240 at
24 pCi/L (dated 10/00). It is very important
to note that these two separate samples were taken nearly a year apart
which adds significant credibility to this not being a sampling anomaly.
[13] The toxic half-life of Plutonium-238 is
87.74 years, Pu-239 is 24,110 years, Pu-240 is 6,537 years, Pu-241 is 14.4
years, and americium-241 is 432.2 years. The full term toxic life of
radionuclides is generally considered to be ten times the half-life. Crucial to this is the fact that
radionuclides decay to other radionuclides called the “decay chain” or
“daughter” that are substantially
longer than the original nuclear parent isotope. In essence, these radioisotopes
are a permanent contaminate in Idaho in perpetuity.
[14] Speciation of Plutonium and Americium in
Ground Waters from the Radioactive Waste Management Complex, Idaho National
Engineering Laboratory, Idaho, U.S. Geological Survey, Water Resources Investigations
Report 93-4035,1993, page 1, 4, and 9.
[15]
Radiochemical and Chemical Constituents in Water from Selected Wells South of
the INEEL, Idaho, May 2001, US Geological Survey, Report 01-138, DOE/ID-22175.
The wells sampled were Grazing Well #2, Grazing Service CC #3, Haughland Well,
Crossroads Well, and Fingers Butte Well, page 16. Plutonium concentrations ranged from 0.01 to 0.013 pCi/L in
Grazing Service well CCC # 3.
[16] Poison in
the Vadose Zone, An examination of the threats to the Snake River Plain Aquifer
from the INEEL, Institute for Energy and Environmental Research, Arjun
Makhijani, Ph.D., Michele Boyd, October 2001, page 54. Herein after called
IEER.
[17] INEEL Oversight Program, Environmental
Surveillance Program, Quarterly Data Report, January - March 2002
[18] INEEL Oversight Program, Quarterly Report,
April - June 2002, State of Idaho, page 17 and 29.
[19] 40 CFR 141.15
and 141.16. “If two or more radionuclides are present, the sum of their annual
dose equivalent to the total body or to any organ shall not exceed 4
millirem/yr.”
[20]
IEER (2001) page 63 and 66.
[21] Iodine-129 in the Snake River Plain Aquifer
at and Near the INEEL, 1990-91, Report 94-4257, US Geological Survey, April
1994.
[22] Environmental Science Foundation, July 1997.
Well number 11 located 4 miles south of INEEL
and 3.5 miles west of Big Southern Butte contained concentrations of I-129 of 1
x 10-5. Well number 14
located 8 miles south of INEEL and 6 miles southeast of Big South Butte has
I-129 concentrations of 3 x 10-5. Also phone conversation with
INEEL Oversight Program 2/18/93
[23] Iodine-129 in the Snake River Plain Aquifer at
the Idaho National Engineering Laboratory, Idaho, U.S. Geological Survey Water
Resources Investigations Report 88-4146, September 1988, page 1, DOE/ID-22076
[24] INEEL Test Reactor Area, Perched Water
Systems, Record of Decision, December 1992, Waste Area Group OU-2-12, pages 14
through 16, DOE Idaho Operations Office.
[25] Tritium in Flow from Selected Springs that
Discharge to the Snake River – Hagerman Area, Idaho, 1994-99, US Geological
Survey, Report 02-185, May 2002, DOE/ID-22180, page 7. The drinking water standard for tritium is
20,000 pCi/L which independent experts believe is not protective of human
health.
[26] Geologic Controls of Hydraulic Conductivity
in the Snake River Plain Aquifer at and Near the Idaho National Engineering
Laboratory, US Geological Survey, Report 99-4033, February 1999, DOE/ID-22155,
page 1 and 16.
[27] Aley, Thomas, INEL[sic] Ground Water Study
sponsored by DOE contractor EG&G, a six man group led by Wigus Creath,
written by Thomas Aley, 1980, was canceled after its preliminary results showed
that contamination “could move from INEL to the Magic Valley within months.”
[28] Estimated Age and Source of the Young Fraction
of Ground Water at the Idaho National Engineering and Environmental Laboratory,
US Geological Survey, Water Resources Investigations Report 01-4265,
DOE/ID-22177, page 1.
[29] C. Stephen
Allred, Director of Idaho Department of Environmental Quality, affidavit
to US Federal Court in (USA v.
Kempthorne, 91-0035) 2/8/02.
[30] Investigative Evaluate Report, State of Idaho
INEEL Oversight Program 1994 Progress Report, page 10.
[31] Natural Resources Defense Council et al. vs.
Department of Energy, US District Court for the District of Idaho, Civil No
91-0035. Co-plaintiffs, as of this writing, include Confederated Tribes and
Bands of the Yakima Nation, Shoshone-Bannock Tribes, and Snake River
Alliance.
[32] Public Service Co. v. Batt, No. CV91-0035 S-
EJL, US Federal Court for the State of Idaho, 1995 Settlement Agreement, page
8.
[33] A Transient Numerical Simulation of Perched
Ground-Water Flow at the Test Reactor Area, Idaho National Engineering and
Environmental Laboratory, Idaho, 1952-94, US Geologic Survey, Report 99-4277,
DOE/ID-22162.
[34] Idaho INEEL Oversight Program Report,
December 2000, page 25.
[35] Hydrologic Conditions and Distribution of
Selected Constituents in Water, INEEL, Idaho, 1996 through 1998, Report
00-4192, US Geological Survey, September 2000, DOE/ID-22167.
[36] Kathleen Trever, Declaration, US Federal
Court for the District of Idaho, 2/18/02, in USA vs. Kempthorne.
[37] The
90 metric ton (MT) numbers, are drawn from DOE's Radioactive Waste Management
Information System Database (P61SH090, and P61SH070, Run Date 10/24/89) and
represent about 57 shipments specifically identified as "irradiated
fuel". Not included in the
this 90 MT listing are even more numerous shipments called "unirradiated
fuel", "fuel rods", "control rods", and other reactor
fuel not identified specifically as "irradiated". The curie content of these non-included
waste in this summary are shipments identified as "fuel rods" (>7,000 curies each) suggests that they
are also irradiated reactor fuel. The
listing also does not include 7 shipments of "irradiated fuel" during
the same period to the RWMC Transuranic Storage Area amounting to 621.549
kilograms, and which also were not included in DOE’s Spent Nuclear Fuel
Environmental Impact Statement. Equally
significant are nuclear reactor fuel related waste shipments to the RWMC burial
grounds. This waste includes reactor
fuel parts cut off the fuel elements prior to storage and fuel storage
"canal trash" that represents over 9,866,112 curies. The INEEL burial grounds are a shallow
disposal area that would not meet municipal garbage landfill regulations.
[38] Criticality occurs when sufficient
quantities of fissionable material spontaneously (or under controlled
conditions in a nuclear reactor) produce a self sustained nuclear reaction. An uncontrolled criticality event in buried
waste represents an extreme hazard due to radioactive releases to the
environment. Three spontaneous and apparent criticality fires occurred at the
RWMC in September 1996 and June 1970. (PR-W-79-038 page 30. For a more complete
discussion see EDI’s INEEL News December 2000 issue.
[39]
A Comprehensive Inventory of
Radiological and Non-radiological Contaminates in the Waste Buried in the
Subsurface Disposal Area of the INEL RWMC During the Years 1952-1983, Volume 1,
Idaho National Engineering Laboratory, EG&G Idaho, Inc., June 1994, page
6-25, herein after referred to as EGG-WM-10903.
[40]
DOE/ID Contractor Report,
EGG-WM-10903, page 2-76 and C-5 Table C-1.
[41] DOE/ID
Contractor Report, EGG-WM-10903, page xxix, Table S-2.
[42]
Openness Press Conference Fact
Sheets, February 6, 1996, U.S. Department of Energy, page 65. In 1996, then DOE
Secretary O'Leary revealed that 1,191.8 kg of Plutonium could not be accounted for at Rocky Flats.
An August 1994 internal Rocky Flats report called "A Discussion of
Inventory Difference, Its Origin and Effect," by N. J. Roberts says 200 to
300 kg of the unaccounted Plutonium (Pu) may be in holdup (in piping,
duct-work, equipment and the like). Roberts thought Pu contained in waste sent to
INEEL may have been understated by 600 to 800 kg. On Feb 21, 1996, then Rocky Flats DOE manager Mark Silverman said
that up to 80% of the total unaccounted for Rocky Flats Pu -- that is, up to
953 kg-- went to INEEL.
[43] Plutonium-239 is a nuclear weapons grade
isotope, however other species of plutonium are also fissionable.
[44]
Data Raises Concerns About Accidental Nuclear Reaction, Twin Falls Times News,
11/11/00 Quoting Wayne Pierre of EPA.
Also see, Subsurface
Treatability Study Report, July 2000, INEEL/EXT-2000-0040-3.
[45] Idaho High-Level Waste and Facilities
Disposition Draft Environmental Impact Statement, December 1999, DOE/EIS-0287D,
page C.9-10, herein after called HLW/EIS.
[46]
Environmental Defense Institute Amicus Curiae Brief filed in federal court
8/2/02, Natural Resources Defense Council et al. vs. Department of Energy, Case
No. 01-CV-413 (BLW).
[47] HLW/EIS, page 5-206.
[48] IEER, October 2001, page 54, citing Environmental Science Foundation, July 1997.
[49] INEEL Test Reactor Area Record of Decision, Perched Water Systems, December 1992, OU-2-12,
page 14 - 16.
[50]
Preliminary Water-Surface Elevations and Boundary of the 100 Year Peak Flow in
the Big Lost River at the Idaho National Engineering and Environmental
Laboratory, Idaho, US Geological Survey, Water-Resources Investigations Report
98-4065, DOE/ID-22148
[51] INEL-95/0056;
Waste Area Group 3 Comprehensive Remedial Investigation/Feasibility Study Work
[52] DOE/EIS-0287, page 4-52 and 4-57
[53] 40 CFR 140 and 141
[54] See Idaho Department of Environmental
Quality, RCRA/HWMA Permit Docket No. 10HW-0204.
[55]
40 CFR 265.112(b)(4)
[56] 40
CFR Sec. 265.197(a) Subpart J--Tank Systems
[57] IHLW/EIS, page F-3.
[58] IHLW/EIS, page 1-17
[59] OTA(a);
Complex Cleanup, The Environmental Legacy of Nuclear Weapons Production,
US Congress Office of Technology Assessment, Feb.1991
[60] TRA ROD(a); Record of Decision, Test Reactor
Area Perched Water System, Operable Unit 2-12, Idaho National Engineering
Laboratory, December 1992, US Department of Energy. Also Administrative Record, TRA
Summary Tables of Chemical and Radiological Analysis, Appendix G-484 and 485, Analytica-ID-12782-1 @ D-615 to
D-632] [EPA-570/9-76-003] *[FR-7/18/91].
[61] National Primary Drinking Water Standards, Current
EPA Maximum Concentration Levels for Radionuclides in Drinking Water, Tables
IV-2A and IV-2B, EPA-570/9-76-003
[62] TAN ROD;
Record of Decision, Technical Support Facility Injection Well (TSF-05) and
Surrounding Groundwater Contamination (TSF-23), Operable Unit 1-07A, Waste Area
Group 1, Idaho National Engineering Laboratory, September 1992 ; TAN Sludge; Summary of RCRA Facility
Investigations Activities at Test Area North, Table 1, Tan Sludge Sample
TSF-050, Collection Date 071090 to 071090 page B-5; TAN-5171; Test Area North Leach Pond Sediments, Operable Unit
TSF-07, D. B. Harelson, 9/1/92, Number 5171;
TAN ROD; Record of Decision, Technical Support Facility Injection
Well (TSF-05) and Surrounding
Groundwater Contamination (TST-23), Operable Unit 1-07A, Waste Area
Group 1, September
[63] Evaluation of Radionuclide, Inorganic
Constituent, and Organic Compound Data from Selected Wells and Springs from the
Southern Boundary of the Idaho National Engineering Laboratory to the Hagerman
Area, Idaho 1989 through 1992, U.S. Geological Survey Water Resources
Investigations Report 97-4007, January 1997, R. Bartholomay, L. Williams,
DOE/ID-22133, page 23.
[64] IEER, 2001
[65] David B. McCoy is an attorney living in Idaho Falls,
ID who has written extensively about INEEL’s violations of environmental law. mccoydb@msn.com
[66] Washington Wilderness Coalition, 870 F.Supp.
at 990; cited in Idaho Rural Council v. Bosma, No CV-99-0581-S-BLW. Also see
State of New York v. PVS Chemicals, No 97-CV-596-A.