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Water and gas chemistry from HGP-A geothermal well : January 1980 flow test

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dc.contributor.author Thomas, Donald M.
dc.date.accessioned 2020-04-21T00:01:26Z
dc.date.accessioned 2020-04-21T01:11:22Z
dc.date.available 2020-04-21T00:01:26Z
dc.date.available 2020-04-21T01:11:22Z
dc.date.issued 1980-09
dc.identifier.citation Thomas DM. 1980. Water and gas chemistry from HGP-A geothermal well : January 1980 flow test. Geothermal Resources Council.
dc.identifier.uri http://hdl.handle.net/10524/63240
dc.description.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.
dc.description.abstract Geothermal Resources Council, Transactions, vol. 4, September 1980
dc.description.sponsorship Hawaii Institute of Geophysics and Planetology, University of Hawaii at Manoa
dc.format.extent 4 pages
dc.language.iso eng
dc.publisher Geothermal Resources Council
dc.subject HGP-A
dc.subject brine chemistry
dc.subject chemical analysis
dc.subject geothermal chemistry
dc.subject geochemistry
dc.subject Kilauea
dc.subject Puna
dc.subject Big Island
dc.subject Hawaii
dc.subject.lcsh Geothermal resources--Hawaii--Hawaii Island
dc.subject.lcsh Geothermal resources--Hawaiʻi
dc.title Water and gas chemistry from HGP-A geothermal well : January 1980 flow test
dc.type Journal Article
dc.type.dcmi Text
Appears in Collections: The Geothermal Collection


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