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

Evaluation and targeting of geothermal energy resources in the southeastern United States. Progress report, May 1, 1976--June 30, 1976

Technical Report ·
OSTI ID:7154278

The optimum sites for geothermal development in the tectonically stable eastern United States will probably be associated with crustal igneous rocks containing relatively high concentrations of radiogenic heat-producing elements. In order to locate such sites, a methodology employing geological, geochemical, and geophysical techniques is being developed and applied. One geologic environment suitable for the storage of commercially exploitable geothermal heat at accessible depths is a radiogenic source buried beneath an insulating blanket of sediments of low thermal conductivity, such as the sedimentary rocks of the Coastal Plain of South Carolina, North Carolina, and Virginia. Preliminary determinations of geothermal gradients in Coastal Plain sediments of South Carolina indicate gradients that range from about 20/sup 0/C/km to at least 45/sup 0/C/km. Representative average gradients determined from bottom-hole temperatures are about 30/sup 0/C/km. The observed gradients are consistent with those to be expected for an efficient sedimentary insulator with a low thermal conductivity.

Research Organization:
Virginia Polytechnic Inst. and State Univ., Blacksburg (USA)
OSTI ID:
7154278
Report Number(s):
VPI-SU-5103-1
Country of Publication:
United States
Language:
English