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U.S. Department of Energy
Office of Scientific and Technical Information

Potential of coal strip-mine spoils as aquifers in the Powder River Basin

Book ·
OSTI ID:6019086
The Tongue River Formation contains most of the strippable coal deposits in the Powder River Basin. Flat lying low sulfur coal beds up to 200 ft. thick are typically overlain by semiconsolidated shale and sandstone. Typical overburden to coal thickness ratios in working mines are 2:1. The overburden is generally dragline or scraper-dumped into the excavated pit. Pump tests were conducted to determine the aquifer characteristics of the mine spoils of two coal strip mines in western Sheridan County, Wyoming. Six other coal strip mines were studied using field infiltration and laboratory permeability apparatus to determine hydrologic characteristics. Data from 44 sites indicate that the permeability is primarily related to density, which in turn is due to method of emplacement and composition. Spoils emplaced by dragline show higher laboratory permeability than those emplaced by scraper or truck. This is presumably due to greater compaction caused by machinery moving over the surface of the spoils. Local stratigraphy, however, has a great influence on the hydrologic characteristics of the spoils. Chemical analyses of 32 water samples show a significant difference of the quality of ground water in spoils compared to natural ground water from wells in the Tongue River Formation. The possibility of utilizing the abandoned spoils as ground water storage areas is feasible due to the moderately high permeability. However, the poor quality of the ground water that would be pumped out of the spoils would appear to limit its usefulness.
OSTI ID:
6019086
Report Number(s):
NP-23777
Country of Publication:
United States
Language:
English