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Title: Geothermal applications on the Madison (Pahasapa) aquifer system in South Dakota. Final report, October 1, 1976--September 30, 1977

Technical Report ·
DOI:https://doi.org/10.2172/6807926· OSTI ID:6807926

Pertinent geologic, hydrologic, and chemical data for the Madison Formation underlying western South Dakota are presented in text and in graphic form. A temperature anomaly in west central South Dakota makes 130 to 160/sup 0/F water available at depths of less than 3500 ft. A central geothermal space heating system designed for Midland, South Dakota indicates that by 1980 geothermal heat will be competitive with existing energy sources. Preliminary tests indicate the superiority of 304 or 316 stainless steel for fabrication of equipment to utilize the warm, corrosive Madison water. South Dakota has no statutes governing geothermal resources; under existing water law, geothermal water would be classified as a top priority domestic use. Suggestions are made for state legislation pertaining to the development of geothermal energy.

Research Organization:
South Dakota School of Mines and Technology, Rapid City (USA)
DOE Contract Number:
EY-76-C-07-1570
OSTI ID:
6807926
Report Number(s):
IDO-1625-2
Country of Publication:
United States
Language:
English

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