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Regional trends in transmissivity and hydraulic conductivity, lower cretaceous sands, north-central Texas

Technical Report ·
DOI:https://doi.org/10.2172/6610552· OSTI ID:6610552
Depositional and structural history control the regional trends in transmissivity and hydraulic conductivity in Lower Cretaceous-age sands along the Balcones Ouachita trend in North-Central Texas. Because of scarcity of pumping tests, delineation of trends was only possible by incorporating transmissivities estimated from specific capacities. Statistical comparison of estimated and pumping-test transmissivities confirmed the validity of this approach. The resulting contour maps should be useful in the evaluation of these aquifers for potential as low-temperature-geothermal resources; the method can be applied to other aquifers to facilitate ground-water-management programs.
Research Organization:
Texas Univ., Austin (USA). Bureau of Economic Geology
DOE Contract Number:
AS07-79ID12057
OSTI ID:
6610552
Report Number(s):
DOE/ID/12057-T1; ON: DE83005475
Country of Publication:
United States
Language:
English