Thursday, October 30, 2008

Ambrosia Lake (Phillips Petroleum) Mill Site

This article and the 2 below it all relate to the same place. This one, from the Dept of Energy, was last modified in October, 2005. The other 2 were written in 2008, the first in March, 2008 and the 2nd in October, 2008. A photo of the tailings mound is above.


Location: The Phillips mill site is located in the Ambrosia Lake Valley about 25 miles north of Grants, New Mexico. It is one of two uranium mills that were operated in the valley. A total of five mills were built between December 1956 and December 1959 in the Ambrosia Lake district of the uranium mining area known as the Grants mineral belt, which extends from near Albuquerque, New Mexico, westward for about 100 miles across the southern margin of the San Juan Basin.

Background: Phillips Petroleum Company began construction of the mill in 1957, and it entered operation in mid 1958. The company had signed a contract with the U.S. Atomic Energy Commission (AEC) in September 1957 for a mill at Grants, New Mexico. The original mill site covered about 200 acres. Over time, about 570 additional acres were impacted by the spreading of radioactively contaminated debris from the mill tailings pile by wind and rainwater erosion. A conventional alkaline leach process was used at the mill from June 1958 to April 1963. During its operating years, the mill processed about 1,800 tons of ore per day that averaged 0.23 percent U3O8, and generated some 3 million tons of tailings. Ore for the mill came mainly from underground mines in the Ambrosia Lake district. United Nuclear Fuels Corporation (UNC) purchased the Phillips mill and uranium mine properties in February 1963, and the AEC uranium procurement contract with Phillips was transferred to UNC. In March 1963, ore processing at the Phillips mill was ended and the mill was closed by mid year. In June 1995, UNC arranged for toll milling of its ore at the nearby Homestake-Sapin mill in which UNC was a limited partner. About 400,000 tons of tailings materials from the Phillips mill site were eventually used by UNC for backfilling mines, and in early 1981 about 2.6 million tons of tailings-pile materials remained at the mill site. The tailings lie on unconsolidated valley fill material. A thick, impervious shale formation separates the tailings from the confined groundwater aquifers. Contamination of the aquifers by the tailings material is highly unlikely. The Phillips mill did not operate after March 1963, though it was maintained on a stand-by basis. From the mid 1970s until the Phillips mill site was permanently closed in 1982, a resin ion exchange (IX) plant to recover uranium from waste mine water was operated in the main mill building. This operation did not increase the size of the tailings pile stored at the mill site. The IX product was treated at the nearby United Nuclear-Homestake uranium mill at Grants, New Mexico.


UMTRA Surface Remediation: Phase I remedial activities comprised the construction of decontamination facilities, removal of asbestos materials, demolition of mill buildings, and other site preparation activities. This work was completed between July 1987 and April 1989. In Phase II, contaminated materials, including structural debris from the dismantled mill, soil, and other radioactive materials from the site, were placed in the existing tailings pile. Cleaned up areas were backfilled with clean soil, re-contoured for good drainage, and re-vegetated. The north portion of the tailings pile was “folded” onto the top of the south portion of the original pile, burying the contaminated material added to the pile. Cleanup of windblown material began in 1994. During the project, 5 vicinity properties associated with this mill site were cleaned up.


Disposal Area: The final tailings pile, consisting of mill tailings with the added contaminated materials, was stabilized in place and became the site disposal cell. A multilayered soil-and-rock cap varying from 3.5 to 4.0 feet in thickness covers the cell to assure cell longevity, control radon emanation, and protect against erosion: a 2.5 foot thick compacted sandy-clay layer serves as the radon barrier and minimizes rain water infiltration and potential leaching of contaminated material; a 6-inch thick, a granular bedding layer of crushed-stone protects the radon barrier; and an erosion-protection layer of up to 12 inches of riprap material tops the cell. The disposal cell was closed in July 1995. It was licensed by the Nuclear Regulatory Commission (NRC) in September 1998. The Phillips mill site came under a general license for custody and long-term care in 1998, when NRC agreed that the site met the cleanup standards and accepted the proposed long-term surveillance plan.


Responsibility for Remediation: U.S. Government, 90 percent ; State of New Mexico, 10 percent.


Stewardship: The Phillips Ambrosia Lake disposal cell site is being managed under the U.S. Department of Energy’s Long-Term Surveillance and Monitoring Program in accordance with the approved site specific plan.


Groundwater Program:
No groundwater remediation was performed under the UMTRA program at the Phillips mill site, and none is planned. Groundwater monitoring is not required, as the supplemental standards (Title 10, CFR, Part 192.22) have been applied for this site. The uppermost aquifer at the site is considered a “limited use” aquifer and is not suitable for drinking water nor a source of irrigation water because of low yield.

http://www.eia.doe.gov/cneaf/nuclear/page/umtra/ambrosia_title1.html

No comments: