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Hot-water aquifer storage: A field testThe basic water injection cycle used in a large-scale field study of heat storage in a confined aquifer near Mobile, Alabama is described. Water was pumped from an upper semi-confined aquifer, passed through a boiler where it was heated to a temperature of about 55 C, and injected into a medium sand confined aquifer. The injection well has a 6-inch (15-cm) partially-penetrating steel screen. The top of the storage formation is about 40 meters below the surface and the formation thickness is about 21 meters. In the first cycle, after a storage period of 51 days, the injection well was pumped until the temperature of the recovered water dropped to 33 c. At that point 55,300 cubic meters of water had been withdrawn and 66 percent of the injected energy had been recovered. The recovery period for the second cycle continued until the water temperature was 27.5 C and 100,100 cubic meters of water was recovered. At the end of the cycle about 90 percent of the energy injected during the cycle had been recovered.
Document ID
19800014340
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Parr, A. D.
(Auburn Univ. AL, United States)
Molz, F. J.
(Auburn Univ. AL, United States)
Andersen, P. F.
(Auburn Univ. AL, United States)
Date Acquired
August 10, 2013
Publication Date
March 1, 1980
Publication Information
Publication: NASA. Lewis Res. Center Thermal Energy Storage
Subject Category
Energy Production And Conversion
Accession Number
80N22828
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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