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

Geohydrology of the proposed waste-isolation pilot-plant site in southeastern New Mexico

Conference ·
OSTI ID:6495409

The drilling and testing of 30 hydrologic test holes have identified three flow zones above the Salado Formation that could potentially transport wastes to the biosphere if the proposed storage facility were breached. These zones include the contact between the Salado and Rustler formations and the Culebra and Magenta Dolomite Members of the Permian Rustler formation. Potentiometric-surface maps (as equivalent freshwater heads) show flow to the west toward Nash Draw within the Rustler-Salado contact and the Magenta Dolomite Member, and flow to the south within the Culebra Dolomite Member. Determinations of hydraulic gradients, directions of flow, and hydraulic properties have been hindered because of the low permeability of the water-bearing zones. Special techniques in drilling completion and hydraulic testing have been developed to adapt conventional methods to low permeable rock. Calculations from pump, slug, and pressure-pulse tests indicate that transmissivity varies laterally within as well as between the beds. Because groundwater may flow predominantly along fractures, a two-well recirculating test was performed to evaluate the effective porosity and coefficients of dispersivity.

Research Organization:
Geological Survey, Albuquerque, NM (USA); Sandia National Labs., Albuquerque, NM (USA)
DOE Contract Number:
AC04-76DP00789
OSTI ID:
6495409
Report Number(s):
SAND-81-0197C; CONF-810457-1
Country of Publication:
United States
Language:
English