Geology and hydrology in the vicinity of the inactive uranium mill tailings pile, Ambrosia Lake, New Mexico
- Author
- Purtymun, W. D.
- Published
- United States : [publisher not identified], 1977
[Oak Ridge, Tennessee] : [U.S. Atomic Energy Commission], 1977 - Physical Description
- microfiche : negative ; 11 x 15 cm
- Additional Creators
- Dreesen, D. R. and Wienke, C. L.
- Summary
- A study was made of the geology and hydrology of the immediate area around a uranium mill at Ambrosia Lake, New Mexico. The mill was in operation from June 1958 through April 1963 and produced 2.7 x 10/sup 9/ kg of tailings. The possible environmental consequences of this inactive tailings pile must first be delineated so that stabilization needs and future stabilization success can be properly assessed. The Ambrosia Lake area is underlain by over 1000 m of alternating shales, siltstones, and sandstones that dip gently to the northeast into the San Juan Basin. Water-bearing sandstones make up less than 25 percent of this sedimentary section. Water quality in the sandstones is fair to poor, with total dissolved solids ranging from 500 to 2000 mg/l. The present total volume of tailings is estimated at 1.5 x 10/sup 6/ m/sup 3/ and ranges in thickness from about 1 to 10 m. The tailings pile is underlain by the Mancos shale which dips to the northeast. The shale is about 120 m thick with three interbedded silty sandstones that are about 9 m in thickness. One of these sandstones outcrops beneath the western part of the pile; the eastern part of the pile is underlain by shale. Ground water in the shales and sandstones beneath the pile is recharged by runoff north of the pile and from three ponds located north, northeast, and east of the pile. The movement of water in shale and sandstones is to the southwest. Secondary recharge to the water in the shales and sandstone is from the basin within the tailings pile. Water in the southeast part of the tailings basin is forming a ground water mound above the underlying sediments. The major transport mechanisms of tailings and possible contaminants from the pile include wind erosion, surface water runoff, movement of ground water beneath the pile, and gaseous diffusion from the pile (radon).
- Report Numbers
- LA-6839-MS
- Other Subject(s)
- 050400 - nuclear fuels- feed processing
- 053000 - nuclear fuels- environmental aspects
- 11 nuclear fuel cycle and fuel materials
- Environmental transport
- Geology
- Hydrology
- Machining
- Management
- Mass transfer
- Metamorphic rocks
- Mill tailings
- Milling
- New mexico
- North america
- Ore processing
- Ores
- Processing
- Radioactive waste disposal
- Radionuclide migration
- Rocks
- Sandstones
- Sedimentary rocks
- Shales
- Solid wastes
- Southwest region
- Uranium ores
- Usa
- Waste disposal
- Waste management
- Wastes
- Collection
- U.S. Atomic Energy Commission depository collection.
- Note
- DOE contract number: W-7405-ENG-36
OSTI Identifier 7220367
Research organization: Los Alamos National Lab. (LANL), Los Alamos, NM (United States).
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