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

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dc.contributor.authorThomas, Donald M.
dc.date.accessioned2020-04-21T00:01:26Z
dc.date.available2020-04-21T00:01:26Z
dc.date.issued1980-09
dc.description.abstractDuring 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.abstractGeothermal Resources Council, Transactions, vol. 4, September 1980
dc.description.sponsorshipHawaii Institute of Geophysics and Planetology, University of Hawaii at Manoa
dc.format.extent4 pages
dc.identifier.citationThomas DM. 1980. Water and gas chemistry from HGP-A geothermal well : January 1980 flow test. Geothermal Resources Council.
dc.identifier.urihttp://hdl.handle.net/10524/63240
dc.language.isoeng
dc.publisherGeothermal Resources Council
dc.subjectHGP-A
dc.subjectbrine chemistry
dc.subjectchemical analysis
dc.subjectgeothermal chemistry
dc.subjectgeochemistry
dc.subjectKilauea
dc.subjectPuna
dc.subjectBig Island
dc.subjectHawaii
dc.subject.lcshGeothermal resources--Hawaii--Hawaii Island
dc.subject.lcshGeothermal resources--Hawaiʻi
dc.titleWater and gas chemistry from HGP-A geothermal well : January 1980 flow test
dc.typeJournal Article
dc.type.dcmiText

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