Water and gas chemistry from HGP-A geothermal well : January 1980 flow test
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1980-09
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Geothermal Resources Council
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Abstract
During January 1980, a two-week production test was conducted on the geothermal well HGP-A. Brine chemistry indicates that approximately six percent of the well fluids are presently derived from seawater and that this fraction will probably increase during continued production. Reservoir production is indicated to be from two chemically distinct aquifers: one having relatively high salinity and low production and the other having lower salinity and producing the bulk of the discharge.
Geothermal Resources Council, Transactions, vol. 4, September 1980
Geothermal Resources Council, Transactions, vol. 4, September 1980
Description
Keywords
HGP-A, brine chemistry, chemical analysis, geothermal chemistry, geochemistry, Kilauea, Puna, Big Island, Hawaii, Geothermal resources--Hawaii--Hawaii Island, Geothermal resources--Hawaiʻi
Citation
Thomas DM. 1980. Water and gas chemistry from HGP-A geothermal well : January 1980 flow test. Geothermal Resources Council.
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4 pages
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