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DEPARTMENT OE HEALTH & HUMAN SERVICES
Public Health Service
' ' ~.-~.: K 1 1/ _ `} Agency for Toxic Substances
R~ and Disease Registry
' ,'' I 7 ~l 1 11. 1. Li Atlanta GA 30333
Septe ber 16, 2008
_ '~t ~ -
Ms. Co ' -
ryHarden _-~ d (1' ., i~ ;--t, •;:., ,~~
Sierra Club - Moku Loa Group '
Post Office Box L 137
Hilo, Hawaii 96721-1137
Dear Ms. Harden:
Thank you for your June 13, 2008, letter addressed to the Agency for Toxic Substances and Disease
Registry (ATSDR), the Centers for Disease Control and Prevention, the U.S. Environmental
Protection Agency; and the U.S. Nuclear Regulatory Commission, requesting a review of the Army
studies and decisions on depleted uranium spotting rounds in Hawaii. Several of the issues -such as
why 'certain decisions were made or your concerns about statements made by the Army or by other
agencies -can best be addressed by the agencies directly involved in those actions. ATSDR is,
however, authorized by the Comprehensive Environmental Response, Compensation, and Liability
Act to evaluate the human health effects of exposure to hazardous substances. The goal of the agency
is to help prevent or reduce harmful human health effects from exposure to hazardous substances.
I am enclosing a health consultation entitled "Depleted Uranium at Hawaiian Military Sites
(Schofield Barracks Impact Area, Makua Military Reservation, and Pohakuloa Training Area on 'the
Islands of Oahu and Hawaii." which ATSDR recently prepared (August 25, 2008). This consultation
is relevant to your concern about the use of M101 spotting rounds containing depleted uranium at
Army firing ranges on the Hawaiian Islands. To assess the impact on public health from depleted
uranium at the three Hawaii ranges and impact areas, ATSDR reviewed documents and information
obtained from the Department of Defense. In its evaluations, ATSDR considers such factors as the
levels of the contaminants in the environment; how people may contact the contaminants and how
frequently the contact occurs. If you have questions about evaluation methods, our conclusions, or
other radiation related issues please do not hesitate to contact Ms. Carol Connell, an ATSDR health
physicist, at (770) 488-0772 or ccc8~cdc.gov.
Sincerely,
`~~'~- `
Howard Frumkin, M.D., Dr.P.H.
Director, National Center for Environmental Health/
Agency for Toxic Substances and Disease Registry
Enclosure
cc: (with enclosures)
Susan Muza, ATSDR, Region IX
con,. -~. / 2 ~ o. 3
Ref. to: ~~.
Ref. Date L `2QU~
Page 2-Ms. Cory Harden
(cc's cont.)
Dr. Julie Gerberding, CDC
Dr. Henry Falk, CDC, CCEHIP
Rob Terry, EPA
Eliot Brenner, USNRC
COL Howard Killian, US Army -Pacific
Russell Takata, HI DOH
Governor Linda Lingle
Senator Daniel Akaka
Senator Daniel Inouye
Senator Lorraine Inouye
Senator Russell Kokubun
Representative Neil Abercrombie
Representative Cindy Evans
Representative Jerry Chang
Representative Josh Green
Representative Faye Hanohano
Representative Bob Herkes
Representative Mazie Hirono
Representative Dwight Takamine
Representative Clift Tsuji
Mayor Hany Kim, HI County
Brenda Ford, HI Council
Pete Hoffmann, HI Council
Stacy Higa, HI Council
Donald Ikeda, HI Council
K. Angel Pilago, HI Council
Bob Jacobson, HI Council
Emily Naeole, HI Council
Dominic Yagong, HI Council
J. Yoshimoto, HI Council
Health Consultation
DEPLETED URANIUM AT HAWAIIAN MILITARY SITES
SCHOFIELD BARRACKS IMPACT AREA
MAKUA MILITARY RESERVATION
POHAKULOA TRAINING AREA
ON
ISLANDS OF OAHU AND HAWAII
AUGUST 25, 2008
U.S. DEPARTMENT OF HEALTH AND HUMAN SERVICES
Public Health Service
Agency for Toxic Substances and Disease Registry
Division of Health Assessment and Consultation
Atlanta, Georgia 30333
Health Consultation: A Note of Explanation
An ATSDR health consultation is a verbal or written response from ATSDR
request for inforniation about health risks related to a specific site, a chemica
the presence of hazardous material. In order to prevent or mitigate e
consultation may lead to specific actions, such as restricting use of or repl
supplies; intensifying environmental sampling; restricting site access; or re
contaminated material.
In addition, consultations may recommend additional public health act:
conducting health surveillance activities to evaluate exposure or trends in a
outcomes; conducting biological indicators of exposure studies to assess ~
providing health education for health care providers and community m
concludes the health consultation process for this site, unless additional i
obtained by ATSDR which, in the Agency's opinion, indicates a need to rep
the conclusions previously issued.
You May Contact ATSDR Toll Free at
~ 1-800-CDC-INFO
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Visit our Home Page at: http://www.atsdr.cdc.gov
HEALTH CONSULTATION
DEPLETED URANIUM AT HAWAIIAN MILITARY SITES
SCHOFIELD BARRACKS IMPACT AREA
MAKUA MILITARY RESERVATION
POHAKULOA TRAINING AREA
ON
ISLANDS OF OAHU AND HAWAII
Prepared By:
The U.S. Department of Health and Human Services
Agency for Toxic Substances and Disease Registry
Depleted Uranium at Hawaiian Military Sites
Summary and Statement of Issues
Final
The Agency for Toxic Substances and Disease Registry (ATSDR) prepared this health
consultation in response to a request by the United States Army to assess the public
health risks from the presence of M101 spotting rounds containing depleted uranium at
Army firing ranges in the Hawaiian Islands and to review related documents. This
depleted uranium, a Cold War legacy, was used in spotting rounds for the Davy Crockett
recoilless guns that were produced from 1956 until 1963 and were used in soldier training
exercises in Hawaii from 1962 through 1968. The Davy Crockett launched a large
projectile from either a 120-millimeter or 155-millimeter recoilless rifle with maximum
ranges of 1.24 miles or 2.49 miles, respectively. Before firing the large projectile from
the 120-millimeter recoilless rifle, a smaller 20-millimeter spotting M101 cartridge was
fired mirroring the trajectory of the larger projectile to identify where the weapon system
was aimed and to identify the need for adjustments to obtain correct positioning of the
rifle. The cartridge consisted of several components which included a nosecone, a body,
and a tailfm. The body of this spotting round was made of a depleted uranium alloy. (For
more detail, refer to the Brief History and Description of Weapon System section of this
report.) After the cartridge was fired and upon impact of the spotting round, a small
cloud of smoke identified the impact point. The use of these spotting cartridges is
significantly different from the use of depleted uranium armor penetrating rounds in the
Persian Gulf where depleted uranium partially aerosolized when the penetrator hit a
hardened target such as steel or concrete.
ATSDR staff consulted, reviewed, and discussed with Army representatives and-their
consultants environmental sampling and analysis procedures and identified data gaps in
environmental sampling, analyses, and methodologies for three sites (Schofield Barracks,
Makua Military Reservation, and Pohakuloa Training Area). ATSDR staff also reviewed
and provided comments on reports and documents prepared by or for the Army on the
presence of depleted uranium at Schofield Barracks on the Island of Oahu, which
included the Schofield Barracks Impact Range Baseline Human Health Risk Assessment
for Residual Depleted Uranium, dated Apri12008.
ATSDR staff also reviewed the following documents prepared by Cabrera Services for
the Department of the Army: Characterization Report Schofield Barracks Davy Crockett
Impact Area, Schofield Barracks Firing Range Monitoring of Air Quality During Burning
of Vegetation, and Technical Memorandum Depleted Uranium Scoping Investigations:
Makua Military Reservation, Pohakuloa Training Area, Schofteld Barracks Impact Area
Islands of Oahu and Hawaii. Other reviewed documents included Depleted Uranium,
Natural Uranium and Other Naturally Occurring Radioactive Elements in Hawaiian
Environments and Natural and Depleted Uranium in Hawaii Fact Sheet, both prepared
by Kenneth H. Rubin, Ph.D. from the University of Hawaii.
As requested by the Army, ATSDR focused on depleted uranium rather than addressing
other potential contaminants at these sites. The ATSDR health consultation and public
health assessment (sometimes referred to as an exposure assessment) differ significantly
from the classical risk assessment in purpose and methodology. ATSDR staff evaluate if
exposures to one or more toxicants are or have occurred at a site, at what level of
1
Depleted Uranium at Hawaiian Military Sites
Final
exposure, and if potential adverse health effects have occurred or could occur
of these exposures. As a public health agency, and not an environmental regal
clean up authority, ATSDR staff act as advisors to citizens, groups, and agenc
regarding the body of scientific knowledge of human exposures to chemicals
radioactive materials in the environment and whether such exposures would li
in adverse health effects. ATSDR makes recommendations to stop, reduce, or
exposures and for additional public health actions, if needed.
Findings
Public Health Impact
ATSDR representatives reviewed several reports and visited three sites to deter.
public health implications of the presence of depleted uranium spotting rounds ;
ranges at Schofield Barracks, Pohakuloa Training Area, and potentially Makua
Reservation. ATSDR also reviewed and advised the US Army on environrnenta
monitoring programs for the Hawaiian Islands firing ranges. While in Hawaii, f
representatives attended technical discussion meetings with Army and contract<
representatives and the press conference at Fort Shaffer in Honolulu on Apri12:
for the release of the Schofield Barracks Impact Range Baseline Human Health
Assessment for Residual Depleted Uranium.
- Although ATSDR provided detailed comments and recommendations fo
report, ATSDR agrees with the conclusion, based on the information rev
and current knowledge about the site and past use of M101 spotting roar
containing depleted uranium at Schofield Barracks, that no adverse hum.
effects would be expected as a result of potential exposure to the deplete
uranium in its current location.
- Based on information about the condition of the spotting rounds, the site
environment, the limited environmental sampling results; the distance to
populated areas, and restricted access at Pohakuloa Training Area's imps
ATSDR also concludes that no adverse human health effects would be e:
as a result of potential exposure to depleted uranium at Pohakuloa Traini
if the depleted uranium rounds were left at their current locations.
- The Makua Military Reservation has easier accessibility, has cultural sig
and has a different history and use of the impact areas than the other site
use of the depleted uranium spotting rounds at the Makua Military Reier
has not been determined and insufficient environmental survey data are <
at this time, ATSDR did not make a determination for this site.
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Additional information that led to ATSDR conclusions for each site is included in this
report.
Depleted Uranium at Hawaiian Military Sites Final
Background and History
Brief History and Description of Weapon System
The Davy Crockett (M28 and M29 series) recoilless guns that used spotting rounds
containing depleted uranium were produced from 1956 until 1963 and were used in
soldier training exercises in Hawaii from 1962 through 1968 (Brookings 2008; USACE
2007). Records indicate that 714 rounds of the Spotting M101 Cartridges were shipped to
Oahu in 1962 (USACE 2007). These rounds were used at the Schofield Barracks and the
Pohakuloa firing ranges and possibly at the Makua Military Reservation.
- -The Davy Crockett Iaunched a large projectile from either a 120-millimeter (-mm) or
155-mm recoilless rifle with maximum ranges of 1.24 miles or 2.49 miles, respectively.
The 155-mm recoilless rifle fired a 37 mm spotting round that did not contain depleted
uranium. Before firing the 120-mm projectile, a 20-mm cartridge (Spotting M101
Cartridge) was feed to identify the impact point and to identify the need for adjustments
to obtain correct positioning of the rifle (USACE 2007). The 20-mm cartridge (similar to
a large bullet) consisted of several components: a projectile, a primer (small detonator), a
propellant (an explosive charge to propel the projectile), and a casing. The projectile
consisted of a nosecone, a body, and a tailfin. The nosecone fuze was screwed onto a
hollow body made of depleted uranium alloy (92% depleted uranium and 8%
molybdenum) into which a red phosphorus charge was placed. An aluminum tailfm was
epoxied into the rear of the body for in-flight stability. When used, the cartridge was
chambered into a large bore rifle attached below the larger recoilless rifle. When the
cartridge was.fired and the projectile impacted its target, the fuze ignited the red
phosphorus charge. The pressure ruptured the sidewall of the projectile's body releasing a
cloud of smoke approximately two to three meters in diameter, two to five meters in
height, and visible for several seconds. This is similar to setting off a firecracker in a
metal can where the side is ruptured ejecting large metal fragments but leaving a large
part of the can intact. The use of the Spotting M 101 Cartridges containing depleted
uranium is significantly different from the use of depleted uranium armor penetrating
rounds in the Persian Gulf where the depleted uranium partially aerosolized when the
penetrator hit a hardened target such as steel or concrete (USAEPI 1994).
Site Descriptions
The Hawaiian sites where spotting rounds containing depleted uranium were used or
potentially used include firing ranges and impact areas at three locations: Schofield
Barracks, Makua Military Reservation, and Pohakuloa Training Area, Schofield Barracks
and Makua Military Reservation are located on the Island of Oahu (Figure 1). Pohakuloa
Training Area is located on the Island of Hawaii (Figure 2). ATSDR representatives
visited these sites on Apri123 and 24, 2008.
~.,
• •
Depleted Uranium at Hawaiian Military Sites
Final
• •
Depleted Uranium at Hawaiian Military Sites Final
Schofield Barracks
Schofield Barracks is the largest Army post in the State of Hawaii, located on 17,725
acres (72 km'`) on the north central plateau of the Island of Oahu approximately 22 miles
northwest of the city of Honolulu. The post is divided into two sections: the East Range
and the Main Post (also referred to as Schofield Barracks Military Reservation). The
Main Post, which has controlled access, includes an active training area and a cantonment
area. The cantonment area is east-southeast of the training area (Figure 3). The training
area is in a large valley facing east with ridgelines to the north, west and southwest. The
training area can be reached by several roads through the cantonment area or by the
Kolikole Pass Road that crosses over the Waianae ridgeline to the west (globalsecurity
2008a).
The training area has maneuver training areas, firing ranges and impact areas. The impact
area is on the eastern slope of the Waianae Mountain Range and extends eastwazd toward
Highway 801 (Figure 3). The steep slopes to the west and southwest are tmsuitable for
maneuvers but provide a safety zone for the impact area. The firing ranges aze primarily
along the eastern and southern boundary of the impact area (globalsecurity 2008a).
Figure 3. Schofield Barracks, Center of the Island of Oahu
• •
Depleted Uranium at Hawaiian Military Sites Final
Vegetation varies from heavily wooded on the steeper slopes to open grassland in the
impact and firing range area. Several thickly wooded gullies cut through the impact area.
The impact areas have a high fire hazard rating due to the tall grasses and dry conditions
from April through October (US Army 2008a). To reduce the risk of uncontrolled fires,
the Army performs regular controlled burns in the impact areas. Since these clearing
operations of the training area began in 2005, unexploded ordnance has been discovered.
Several legacy (from WWI and WWII) chemical munitions recovered during range
cleazance activities were detonated in place or in a specially designed detonation chamber
(Honolulu Advertiser 2008).
The prevailing winds are northeasterly trade winds from 4 to 12 mph in the warmer
summer months and lighter southeasterly winds in the winter months (US Army 2008a).
The soils on the training site are silty clay originally created from basalt flow and alluvial
sediments from the Wai'anae Volcano to the west and the Koolau Volcano to the east
(US Army 2008b, 2008c). Soils that appear grey or black are rich in magnesium oxide.
Soils that appear reddish are richer in iron oxide (Figures 4 and 5).
Schofield Barracks Impact Area toward the
Wai'anae Mountain Range (west)
--`
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Depleted Uranium at Hawaiian Military Sites Final
Wheeler Army Airfield (formerly Wheeler Air Force Base) is between and south of
Schofield Barracks' Main Post and East Range. It is approximately four miles from the
training area (globalsecurity 2008a). As of the 2000 census, this base had a total
population of 2,829 military personnel and family members (Census 2000b).
The closest municipality is Wahiawa. It is adjacent to and immediately north of the East
Range but is separated from most of Schofield Barracks by Lake Wilson (also known as
Wahiawa Reservoir). It is approximately four miles from the training area (globalsecurity
2008a). As of the 2000 census, the population of Wahiawa was 16,151 (Census 2000c).
The Schofield Forest Reserve (a conservation district) and the Oahu Agricultural District
are north and Northwest of the Schofield Barracks training area (globalsecurity 2008a).
Makua Military Reservation
Makua Military Reservation is on the west coast of the Island of Oahu, 38 miles
northwest of Honolulu and approximately three miles north of Makaha (population of
7,753) (Census 2000d). Highway 93` (Farrington Highway) runs through the site along the
shoreline terminating at the northern boundary of the site (globalsecurity 2008b). South
of the reservation numerous beach dwellers live in temporary housing and tents between
Currently, the 25`h Light Infantry Division and the 45`h Support Group are headquartered
at Schofield Barracks. As of the 2000 census, the base population in the cantonment area
was 14~ 428 military personnel and family members (Census 2000a).
• •
Depleted Uranium at Hawaiian Military Sites Final
5. Schofield Barracks Impact Area down the valley toward the east-northeast
Wheeler Army Airfield (formerly Wheeler Air Force Base) is between and south of
Schofield Barracks' Main Post and East Range. It is approximately four miles from the
training area (globalsecurity 2008a). As of the 2000 census, this base had a total
population of 2,829 military personnel and family members (Census 2000b).
The closest municipality is Wahiawa. It is adjacent to and immediately north of the East
Range but is separated from most of Schofield Barracks by Lake Wilson (also known as
Wahiawa Reservoir). It is approximately four miles from the training area (globalsecurity
2008a). As of the 2000 census, the population of Wahiawa was 16,151 (Census 2000c).
The Schofield Forest Reserve (a conservation district) and the Oahu Agricultural District
are north and northwest of the Schofield Barracks training area (globalsecurity 2008a).
Makua Military Reservatio~t
Makua Military Reservation is on the west coast of the Island of Oahu, 38 miles
northwest of Honolulu and approximately three miles north of Makaha (population of
7,753) (Census 2000d). Highway 93 (Farrington Highway) runs through the site along the
shoreline terminating at the northern boundary of the site (globalsecurity 2008b). South
of the reservation numerous beach dwellers live in temporary housing and tents between
Currently, the 25`h Light Infantry Division and the 45`h Support Group are headquartered
at Schofield Barracks. As of the 2000 census, the base population in the cantonment area
was 14,428 military personnel and family members (Census 2000a).
Depleted Uranium at Hawaiian Military Sites
Final ~
Highway 93 and the shoreline. It is not clear whether these people are permaneit or
transient residents.
Figure 6. Makua Military Reservation, Northeast Corner of the Island of Oahu
The reservation covers 4,856 acres (globalsecurity 2008b). It has a beautiful shoreline
and two valleys, the Makua and the Kahanahaiki that drain to the Wai'anae Coast
(Lucking 2001). The Makua Valley has been used by the Army and other United States
military forces as a training area since before World War II. Steep cliffs partially
surround the impact area from the southwest to the north. The cliffs are too steep to be
used for maneuvers. Several thickly wooded gullies cut through the impact arealand the
cliffs (Figure 7).The soils in this valley are similaz to those found at Schofield Barracks.
A forest reserve is to the north and to the south with the Waianae Mountain Range to the
east (globalsecurity 2008b).
Temperatures range across the site with the warmest temperatures near the coast and the
coolest temperatures at the ridge line. The wind directions and speed can change quickly
and dramatically from easterly to westerly (Onyx 2001). A dramatic wind change caused
a planned "controlled" burn of 900 acres to turn into an "uncontrolled" burn scotching
2,500 acres in July 2003 (Honolulu Advertiser 2003).
8
Depleted Uranium at Hawaiian Military Sites ~ Final
The Army has been responsible for the site since 1943; however, the training area has
also been used by the Marine Corps, Coast Guard, Air Force, the Army Reserve, and the
Hawaii Army National Guard (Onyx 2001). Currently, for legal reasons, this site is not
being used as an active training area. In the past, the Makua Valley has been subjected to
air bombing, ship to shore firing, amphibious operations and live firing of infantry and
artillery weapons leaving the reservation dotted with unexploded ordnance. Since 1950,
there have been several clearing operations that included controlled burning of
undergrowth and detonating unexploded ordnance, but the site is still known to have a
variety of unexploded ordnance. In August 1998, five World War II-era bombs were
discovered while surveying and mapping the site. These bombs were safely detonated.
Later, 81 smaller pieces of unexploded ordnance were located and detonated (Lucking
2001). Although the use of the M101 spotting rounds has not been confirmed at Makua, i
is possible that training on the Davy Crockett recoilless guns could have taken place at
this site due to the size of the fuing range.
No personnel or families reside at this reservation. Portions of these lands have been
designated as cultural places or sacred sites important to native Hawaiian populations as
traditional religious, hunting, gathering, and fishing areas (Lucking 2001); however,
native Hawaiians are not currently being allowed to enter the site (AP 2007). (Note: This
may have recently changed. If escorted, cultural monitors may now be allowed to access
portions of this site.)
Depleted Uranium at Hawaiian Military Sites
Pohakuloa Training Area
Final
The Pohakuloa Training Area (PTA) located near the center of the Island of Hai
central saddle area between Mauna Loa, Mauna Kea and the Hualalai Volcanic
Mountains covers 108,863 acres (Figure 8). The mountains and the central sadd
are designated as a conservation district. Hilo on the east coast and Kailua-Kon:
Kawaihae Hazbor on the west coast aze approximately 40 miles from the trainin
way of Saddle Road which crosses the center of the island (globalsecurity 20081
Figure 8. Map of the Island of Hawaii
Legend
- Pohekuba Training Area
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The terrain is mostly level or gently sloping and mostly uninhabited with few to
gullies. Even so, ten plants and nine animals listed on the endangered species lis
within the site borders (more than on any other Army installation). Approximate
acres can be used for lazge maneuver exercises; however, few lazge exercises ar
conducted since troops, vehicles and equipment have to be transported by ship f
Oahu. Most of the 108,863 acres are unusable for maneuvers (globalsecurity 20~
large percentage of the surface area is covered with two types of lava flow: pahi
`a'a. Pahoehoe is a Hawaiian term for basaltic lava that has smooth undulating
and can be traversed on foot for short distances. Aa (or `a'a) is a Hawaiian term
basaltic lava.that has a surface covered with thick, jumbled piles of loose, sharp
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10
Depleted Uranium at Hawaiian Military Sites Final
(SDSU 2008). The rough `a'a are jagged, slag-like piles of very sharp material which are
very difficult to traverse on foot (Figure 9).
The eastern portion of the training area is sparsely vegetated. The northern and western
portions have the deepest soils and slightly more vegetation (Beavers 2000). Pohakuloa's
51,000-acre impact area located in the eastern portion is over ten times the size of the
impact area at Schofield Barracks. It is surrounded on the north by several ranges and
designated firing points for artillery (globalsecurity 2008c). Cinder cone hills (or puu's)
dot the landscape and can be used for artillery practice (Figures 10 & 11).
Trade winds blow through the saddle from the east in the mornings and from the west in
the early afternoon. During this transition, wind speeds and direcfions are unpredictable.
At Bradshaw Army Aitreld (adjacent to Pohakuloa), the average annual wind speed in
the late 1990s was 10.7 mph with little variation. Precipitation supplemented by fog drip
is sparse. Temperatures show little variation throughout the year. The average annual
temperature for the late 1990s was 17.7 C (63.8 F) (Beavers 2000).
The Kilohana Girl Scout Camp is within five miles to the west of the training area. The
Army has agreed to install an air monitoring system at this location. The State of Hawaii
Department of Health (DOH) did some preliminary air monitoring downwind from
Pohakuloa Training Area in the summer or late spring of 2007 and reported that all
results were "normal" (Honolulu Advertiser 2007). The Army has purchased four
additional air monitoring systems which will be placed at locations agreed upon by the
Army and the State of Hawaii Department of Health.
11
Depleted Uranium at Hawaiian Military Sites
Final ~
10. Artillery range at Pohakuloa Training Area (puu and mountains to the 1
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12
Depleted Uranium at Hawaiian Military Sites
Chronology of Current Events
Final
In August 2005, during range clearance activities to allow the installation of new range
targets at Schofield Barracks Impact Area, 15 projectile bodies and tailfms from Davy
Crockett Spotting M101 Cartridges containing depleted uranium were found at the
Schofield Barracks munitions impact range (Cabrera 2007). After a controlled grass burn
in the summer of 2006, Schofield personnel surveyed the eastern edge of the impact
range and discovered several additional depleted uranium fragments (Cabrera 2008a).
Between November 27 and 30, 2006, a scoping survey of accessible portions of the
Schofield impact range was performed to determine whether additional depleted uranium
was present and to gather information for the follow-up characterization survey. (Cabrera
2007).
On November 1, 2006, the U.S. Army Joint Munitions Command notified the U.S.
Nuclear Regulatory Commission of the situation and of their plans to perform a scoping
survey and historical archive search for relevant information by the U.S. Anny Corps of
Engineers, St. Louis District (US Anny 2008b). On May 15, 2007, the U.S. Army Corps
of Engineers released their report, Archives Search Report (ASR) On the Use of
Cartridge, 20mm Spotting M101 For Davy Crockett Light Weapon M28, Schofield
Barracks and Associated Training Areas, Islands of Oahu and Hawaii. According to the.
researched records, 714 spotting rounds were shipped to Hawaii in the 1960s, but the
records did not indicate how many rounds were fired and where they were used (USAGE
2007).
Five surface water samples were collected during March of 2007 from outfalls that drain
the impact area at Schofield Barracks. Although only two samples had detectable activity
ofnaturally-occurring uranium well below EPA's drinking water standards, the Army has
agreed to continue the water sampling program (Cabrera 2008a). Precipitation at
Schofield Barracks is low, and the sampling of surface water runoff is feasible only when
significant rainfall occurs.
During the summer of 2007, the Army found more depleted uranium fragments in the
northern and eastern portions of the firing range at Schofield Barracks, confirmed that
depleted uranium was also used at Pohakuloa Training Area (PTA) on the Island of
Hawaii, and said that spotting rounds also may have been fired in Makua Valley (Cabrera
2008b, US Army 2007b). Between July 30 and August 2, 2007, prescribed burns
(reference area, test, and range burns) were performed at the Schofield Barracks firing
range. Downwind and upwind air monitoring samples were collected to measure
concentrations of uranium isotopes in air during the bums. Soil, vegetation, and ash
samples were also collected and analyzed. (Cabrera 2008c, 2008a).
On July 1, 2007, the State of Hawaii Legislature enacted House Bill Number 1452 that
requires the State of Hawaii Department of Health to take soil samples at least every
three months within SOO meters of Schofield Barracks but not beyond ten meters from the
impact sites. The Department of Health was directed to develop a sampling plan and to
submit summaries of their findings to the legislature no later than twenty days prior to
13
Depleted Uranium at Hawaiian Military Sites Final
each regular session beginning in 2008. The bill also provided for depleted uranium
urinalysis screening of personnel (civilian or Hawaii National Guard) reporting
symptoms compatible with Gulf War Syndrome, or those exposed to military ranges or
other suspected depleted uranium sites (Hawaii 2007). However, it appears that fiindin€
for these projects was never approved.
In August 2007, field scoping survey investigations were conducted at all three sites to
assess the presence of depleted uranium fragments (Cabrera 2008a). The investigations
included review of the archived records search, site reconnaissance, and additional
surface soil sampling. The site reconnaissance included aerial surveillance of the Miring
ranges and ground investigations of accessible areas. Sampling results are discus ~ed in
the next section, Review of Environmental Data.
- The document search did not reveal any documentation that the Davy Crockett
weapon system had been used at the Makua Military Reservation. Due to dense
vegetation, the aerial survey was limited to ravines and dry stream beds. No
depleted uranium fragments were located. Physical entry to the impact areas was
not allowed due to safety concerns. Soil samples were collected where sediment
had accumulated from past runoff/erosion events.
- The document search and map analyses identified twelve possible locations at
Pohakuloa Training Area where the spotting rounds could have been used. After
further review, it was narrowed down to four potential ranges. An aerial survey
confirmed that the Davy Crockett weapon system had been used at the foixr
ranges. It was estimated that approximately 30 to 100 spotting rounds could have
been used at each location. Rough terrain limited accessibility to the ranges. One
spotting round resting on top of lava rock was recovered intact. Soil samples
could not be taken in this area so soil samples were collected around the perimeter
of the impact areas and sediment samples were collected from areas of past
runoff/erosion.
- During the site reconnaissance at Schofield Barracks, an area with bright yellow
soil, small yellow fragments, and elevated gross gamma activity was observed in
the northeast portion of the training area. This yellow color is consistent with
highly oxidized uranium or uranium octaoxide (U3Os). Only a single soil sample
was collected during this investigation. It was positive for depleted urami .New
boundaries for the site characterization survey were established.
From August to October 2007, additional soil samples were collected from the Schofie]
Barracks impact area and a reference area (Cabrera 2008b). There were 1,226 soil
samples collected from 646 sample locations in the accessible portions of the impact
areas (biased and systematic sampling), reference area (random sampling), and in the
deep gullies of the impact area (biased sampling). Soil samples were collected at 0 to 6
inches below ground surface (surface soils) or 6 to 12 inches below ground surface
(shallow subsurface).
During the week of Apri120, 2008, ATSDR representatives participated in site visits of
these three locations and attended a media briefing for the final release of the document,
14
Depleted Uranium at Hawaiian Military Sites Final
Schofield Barracks Impact Range Baseline Human Health Risk Assessment for Residual
Depleted Uranium, dated Apri12008. The media briefimg on April 22, 2008, conducted
by Colonel Howard Killian, the Army's Deputy Director for IMCOM-Pacific, was
attended by six media outlets. Questions from the media representatives were addressed
by Colonel Killian, Greg Komp (U.S. Army Radiation Safety Officer), and Russell
Takata (State of Hawaii Department of Health). Various branches of the Army hosted or
participated in the site visits and the media briefing. Other participants included
representatives from the Department of Defense, the U.S. Nuclear Regulatory
Commission (both headquarters and Region IV), the State of Hawaii's Department of
Health, Cabrera Services (contractor) and Mississippi State University (contractor).
Review of Environmental Data
ATSDR reviewed drafts and final copies of five environmental investigation documents
covering the three military sites in Hawaii where depleted uranium was either used or
potentially used in the past. These documents were prepared by Cabrera Services for the
U.S. Department of the Army. The final copies were all dated Apri12008. Below are
discussions of information from each report relevant to our review:
Technical Memorandum -Schofield Barracks Firing Range Phase I Depleted
Uranium Investigation, Wahiawa, Hawaii (Cabrera 2007) -This scoping survey
of the western portion of Schofield Barracks impact area was conducted on
November 27 and 30, 2006. Visual inspections of the area along with low energy
gamma scans were conducted. Soil samples were collected if spotting rounds,
yellow fragments, or elevated readings were encountered. One background and
five other soil samples were collected. Three metallic fragments were retrieved.
One soil sample contained depleted uranium (238U concentration of 209 f 36
pCi/g ). Two samples were consistent with naturally-occurring uranium. The
metallic fragments were identified as depleted uranium. This survey indicated that
more spotting round fragments could possibly be located on this training area.
- Final Technical Memorandum -Depleted Uranium Scoping Investigations -
Makua Military Reservation, Pohakuloa Training Area, Schofield Barracks
Impact Area, Islands of Oahu and Hawaii (Cabrera 2008a) -This document
covers scoping surveys performed at all three sites in August 2007.
o For Makua Military Reservation, aerial surveillance and ground
investigations were limited due to thick vegetation and areas where
unexploded ordhance prevented safe access. No surface water samples
were collected; however; ten soil/sediment samples were collected from
outfalls for suspected impact areas. The samples contained low levels of
naturally occurring uranium (less than 1 pCi/g). None of the samples
revealed any evidence of the presence of depleted uranium, and no
depleted uranium spotting round fragments have been found at this site.
o The Pohakuloa Training Area aerial surveys confirmed that the Davy
Crockett weapon systems had been used on at least four ranges. There was
15
Depleted Uranium at Hawaiian Military Sites
Final
limited access to the suspected impact areas due to the rough tem
spotting round was recovered intact resting on top of the lava roc;
samples were collected at this location. Nine soil samples were cc
from around the perimeter of the suspected impact areas where se
had accumulated from past runoff or erosion. All nine samples ha
levels of naturally occurring uranium (less than 1 pCi/g) but no it
of depleted uranium.
o The focus for the scoping survey at Schofield Barracks included ~
mostly flat northern and eastern portions of the impact area. Visu
reconnaissance identified the additional eastern area training rant
was confirmed with a field survey and surface soil sample. The s~
sam le contained depleted uranium (2,180 pCi/g 238U and 360 pC
z33iz~aU). No surface water samples were collected during this
investigation; however,~the Army monitors surface water runoff i
Schofield Barracks under another program. Five of the surface w.
samples collected in March of 2007 were analyzed for isotopic w
Three of the samples had no detectable uranium activity. Two of
samples had detectable activity for naturally occurring uranium ('
than 1 pCi/L 238U and less than 1 pCi/L 2331 3aU), well below EPA
drinking water standard of 30 pCi/L. There was no evidence of d~
uranium in the runoff.
Final Technical Memorandum -Schofield Barracks Firing Range Moni
Quality During Burning of Vegetation, Wahiawa, Hawaii (Cabrera 200
document evaluated the potential release of depleted uranium during pre
burns at Schofield Barracks in July and August 2007. A reference area b
area known not to contain depleted uranium) and a test burn (in a small
where depleted uranium was known to be present) were performed prior
burning the full firing range. Soil and vegetation samples were collected
the burns to confirm the presence or non-presence of depleted uranium i
Air samples were collected to demonstrate whether particles of uranium
airborne during the bums. Concentrations of uranium in these air filters
samples collected after the burn indicated that uranium did not get airbo
the burn.
The reference bran was performed on one acre of land in an area
depleted uranium. Two air samplers were placed upwind and six
samplers were placed about 200 feet apart downwind. Of sixteen
sam les collected during the reference burn, only one sample res
z33i2s~aU was slightly above the minimum detectable air concentra
well below an action level set in the sampling plan. This sample
downwind from the burn but had no detectable 238U concentratio
vegetation samples were collected prior to the burn and five vegc
samples were collected after the burn. The ash samples after the
a higher concentration of uranium than the vegetation samples p~
burn; however, the ash samples were not collected from the same
r. One
No soil
low
which
Both less
's
pleted
gyring Air
d) -This
cribed
crn (in an
rea
to
prior to
~ the area.
were
nd ash
ne during
with no
air
air
rlt for
ion but
i. Five
ration ash
Burn had
or to the
location
16
Depleted Uranium at Hawaiian Military Sites
Final
as the vegetation samples. The vegetation and ash samples contained very
low concentrations of naturally occurring uranium.
Visual identification and field surveys confirmed the presence of depleted
uranium in the test burn area. Prior to the burn two soil samples and three
vegetation samples were analyzed to confum the presence of depleted
uranium. Two air samplers were placed upwind and six samplers were
placed downwind. Sixteen air samples were collected during the test burn;
however, one of the samplers had shut down during the bum. No airborne
depleted uranium particulates were observed in the air monitoring results.
Five ash samples were collected after the test burn, but their location did
not correspond with the location of the vegetation and soil samples prior to
the burn. Although depleted uranium was present in at least one of the
vegetation samples (180 pCUg 238U) and one soil sample (470 pCi/g 238U)
prior to the burn, none of the ash samples contained significant ,
concentrations of depleted uranium after the burn.
For the range burn, two air samplers were placed upwind and six air
samplers were placed downwind. The range burn continued for several
days, but since the burn was less intense and outside the area of known
depleted uranium after the second day, air monitoring did not continue. On
the second day the downwind monitors had to be moved due to a different
area of the range being burned. The wind direction (from the east-
northeast) did not change. Twenty-four air samples were collected with
only three considered to be above the minimum detectable activity. All
three samples appeared to be naturally occurring uranium and not depleted
uranium. The maximum concentrations were below the action levels
designated in the sampling plan.
In this study, no evidence of depleted uranium was found in the airborne
particulates generated by the controlled burns at the Schofield Barracks training
range. If the range and conditions remain unchanged from the current situation, no
additional air monitoring is suggested.
Final Characterization Report, Schofield Barracks Davy Crockett Impact Area
(Cabrera 2008b) -This document covers the results of a more comprehensive
survey of the 428-acre Schofield Barracks Impact Area. The survey included a
gamma walkover survey, exposure rate measurements, and the collection of 1,225
soil and sediment samples.
o The gamma walkover survey covered approximately 25% of the
accessible land area, defined the boundaries of the areas of concern, and
revealed areas of elevated gamma activity. Soil samples were collected in
these areas with elevated gamma activity.
o Exposure rate measurements were made in 5821ocations on the Schofield
Barracks Impact Area and 12 reference area locations in order to evaluate
potential external radiation exposures to individuals who may enter or may
have entered the site. The readings were taken at three feet from the
ground surface (midline of the body). The maximum exposure rate on the
17
Depleted Uranium at Hawaiian Military Sites
Final
impact area was 0.07 milliroetgen per hour (mR/hr), and the mean
exposure rate was 0.01 mR/hr. Both the maximum and mean exposure
rates are the same or slightly above the exposure rate at the reference
location (0.01 mR/hr). The median exposure rates for both azeas are the
same (0.01 mR/hr); therefore, most of the exposure rates for the impact
area are consistent with natural background. An individual would have to
be at the maximum exposure location for eight hours per day for over 200
days per year to exceed ATSDR's Minimal Risk Level (MRL) for chronic
exposure of 100 mrem/year above background levels. Even if an
individual were exposed to the mean exposure rate 24 hours per day, they
would not exceed the MRL based on external exposure. Therefore, on-site
external exposure to the depleted uranium would not cause any a i verse
health effects.
Surface (0" to 6" below ground surface) and shallow subsurface (;6" to 12"
below ground surface) soil samples were collected at 416 locations
(approximately one location per acre) for a total of 832 samples. These
samples were mainly collected from the flatter areas including the areas
between the ravines (fingers). Also, 318 soil samples were collected at 166
locations where elevated gamma activity was indicated during the gamma
walkover survey, 52 sediment samples were collected from ravines where
depleted uranium may have washed down and collected during ram
storms, and 12 surface and 11 shallow subsurface soil samples were
collected from a reference area at Wheeler Army Airfield.
^ For the reference surface soil samples, the maximum; average, and
minimum 238U concentrations were 1.9 pCi/g, 1.48 pCi/g, and 1.11
pCi/g, respectively. For the reference shallow subsurface soil
samples, the maximum, average; and minimum'38U concentrations
were 2.92 pCi/g, 1.82 pCi/g, and 1.22 pCi/g, respectively
^ Only two out of 52 ravine samples had concentrations above
background (148 pCi/g 238U with 22.6 pCi/g'34U; and 5.69 pCi/g
238U with 1.2 pCi/g ZsaU). Both of these samples obviously
contained depleted uranium and were located near Fingerl5 in the
far west central portion of the impact area. Although samples were
collected from various portions of the impact area, sampling was
limited to sediments where the depleted uranium may ha ~e washed.
down during rain storms and did not include ravines in the entire
impact area. The only conclusion that could be reached ati this time
is that depleted uranium is present iri at least one of the ravines and
runoff should be monitored for a sufficient period of timei to
understand migration potential.
^ Of the 1,150 systematic and biased soil samples, 29 samples (16
surface and 13 shallow subsurface) contained depleted uranium
with 238U concentrations ranging from 5.48 pCi/g to 7,030 pCUg.
Not all locations that had surface soil contamination had shallow
subsurface contamination. Generally, for locations that did have
some shallow subsurface contamination, the 238U concentration
18
Depleted Uranium at Hawaiian Military Sites
Final
was significantly lower than the concentration of 238U at the
surface. Only one sample had higher shallow subsurface
contamination than the surface which could have been caused by
the impact of the spotting round. Since the survey of 166 locations
indicated elevated gamma activity, the corresponding 318 soil
samples were biased. Still, approximately 2.5% of the results
indicated elevated levels of uranium assumed to be depleted
uranium; thus, the contamination is not uniformly spread across the
impact area nor does it appear to be spreading significantly from
the original impact locations.
Final Schofield Barracks Impact Range Baseline Human Health Risk Assessment
for Residual Depleted Uranium (Cabrera 2008e) -This document evaluates the
potential for adverse human health effects from exposure to depleted uranium
present at Schofield Barracks Impact Area. Results from investigations discussed
in the previously listed documents were used to identify the nature and extent of
depleted uranium contamination, identify contaminated media, and identify
potential pathways to human exposure. Pathways considered were external
radiation exposure, dermal (skin) exposure, incidental ingestion of soil, inhalation
of airborne particulates, and ingestion of food crops grown in contaminated soil.
Health risks were estimated based on both the radiological properties and the
chemical toxicity of uranium. For this risk assessment, four on-site exposure
scenarios were evaluated: current and future maintenance workers, future
construction/remediation workers, future adult cultural monitors/trespassers/
visitors, and future site workers. One off-site exposure scenario (a subsistence
farmer living 1500 meters from the impact area) was also evaluated. The potential
exposures and the related risk were estimated using computer codes: The Argonne
National Laboratory's RESidual RADioactivity (RESRAD) code, Version 6.3
(ANL 2005) for effects from radiological exposures and the U.S. Environmental
Protection Agency's Risk Assessment Guidance for Superfund, Volume 1,
Human Health Evaluation Manual for effects from chemical exposures. This
document concludes that no adverse health effects are expected from either the
radiological or chemical exposures on-site or off-site.
19
Depleted Uranium at Hawaiian Military Sites Final
Conclusions and Recommendations
ATSDR agrees with the conclusions of the Final Schofield Barracks Impact Rarige
Baseline Human Health Risk Assessment for Residual Depleted Uranium based on the
following additional factors that would indicate any significant changes to the cinent
situation:
The Army has agreed to continue sampling surface water outfalls for urahium at
Schofield Barracks Impact Area. (Depleted uranium is present in the impact area
including at least one of the ravines; therefore, runoff should be monitored for a
sufficient period of time to understand migration potential.)
Air sampling indicated that depleted uranium does not appear to become airborne
under either normal conditions or during range burns, and would not pose any
adverse health impact to persons offsite.
Due to the nature of the soil sample results, it appears that the depleted uranium is
not uniformly distributed on the site and has not significantly spread from the
point of original impact; therefore, it does not appear that other weapons fired on
this range, range burns, or weather conditions have spread the contamination.
ATSDR recommends that anyone (military or civilian) entering the Schofield Barracks
impact area should have apre-briefing so they can identify depleted uranium from the
spotting rounds and, if located, to take appropriate action (not to touch it, but mark and
report the location).
ATSDR has not reviewed a characterization report for Pohakuloa Training Area
however, ATSDR can make some conclusions for this site. Currently, based on the
condition of the intact spotting round located at the site, the results from perimetier
monitoring, the terrain, the current use of the site, and distance to populated areas,
ATSDR does not anticipate any completed pathways of exposure for the general
population. Military personnel and contractors should be instructed as mentioned above.
ATSDR has not seen any evidence that depleted uranium was used at Makua
Reservation. Although there has been limited monitoring and sampling, none
indicate that depleted uranium is present at this site. However, due to the una
the use of the Davy Crockett weapon system of this location, the close proxin
communities, drainage of the site to the ocean, and cultural interest in this prc
further investigations appear to be warranted. Until additional information is
:ATSDR fmds the potential health concerns for this site to be indeterminate.
data
of
to
20
Depleted Uranium at Hawaiian Military Sites Final
Public Health Action Plan
The following action items are planned for these sites:
When surface water runoff is present, the Army will continue to sample and
analyze surface water for depleted uranium at the outfalls for the Schofield
Barracks Impact Area.
The Army will continue to investigate the Pohakuloa Training Area and the
Makua Military Resevation for the presence of depleted uranium.
The Army has agreed to work with the State of Hawaii Department of Health to
monitor for potential airborne particulates of depleted uranium at locations
adjacent to the Pohakuloa Training Area, such as the Kilohana Girl Scout Camp
on the Island of Hawaii.
21
Depleted Uranium at Hawaiian Military Sites
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22
Depleted Uranium at Hawaiian Military Sites Final
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24