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- W4128353 abstract "The low to moderate geothermal resource base of the Snake River plain is extensive. Estimates of mean reservoir energy of over 455 x 10/sup 18/ J have been made by Mabey in 1983, and energy offset of over 26 MW thermal were made by Bloomquist et al in 1985. These low-temperature (< 150/sup 0/C, hydrothermal resources are presently being used for commercial and domestic space heating and aquaculture. The thermal waters are generally high in F and NaHCO/sub 3/ constituents, but have low concentrations of dissolved solids. Consequently, most developers use the resource directly, without pretreatment. In general, the resource is associated with the Tertiary Idavada Volcanics, a series of rhyolites and ash flow tuffs. Circulation of the thermal waters is controlled by faults, joints, and fractures. Temperatures range from 30/sup 0/ to 70/sup 0/C, and well depths range from 800 to 3000 ft. Most flowing wells have high yields (2000 gpm) and shut-in pressures (250 psi)." @default.
- W4128353 created "2016-06-24" @default.
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- W4128353 date "1987-08-01" @default.
- W4128353 modified "2023-09-24" @default.
- W4128353 title "Geothermal resource base, Snake River plain" @default.
- W4128353 hasPublicationYear "1987" @default.
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