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

Abstract

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.

Authors:
Publication Date:
Research Org.:
Hawaii Inst. of Geophysics, Honolulu
OSTI Identifier:
6297641
Report Number(s):
CONF-800920-
Journal ID: CODEN: TGRCD
Resource Type:
Conference
Journal Name:
Trans. - Geotherm. Resour. Counc.; (United States)
Additional Journal Information:
Journal Volume: 4; Conference: Geothermal Resource Council annual meeting, Salt Lake City, UT, USA, 9 Sep 1980
Country of Publication:
United States
Language:
English
Subject:
15 GEOTHERMAL ENERGY; GEOTHERMAL WELLS; GEOCHEMICAL SURVEYS; HAWAII; BRINES; CHEMICAL COMPOSITION; GASES; ISOTOPE RATIO; KILAUEA VOLCANO; RIFT ZONES; SALINITY; SEAWATER; TESTING; THERMAL WATERS; WATER CHEMISTRY; WELL PRESSURE; CHEMISTRY; FLUIDS; GEOLOGIC STRUCTURES; HYDROGEN COMPOUNDS; NORTH AMERICA; OXYGEN COMPOUNDS; RESERVOIR PRESSURE; SURVEYS; USA; VOLCANOES; WATER; WELLS; WESTERN REGION; 150302* - Geothermal Exploration & Exploration Technology- Geochemical Techniques & Surveys

Citation Formats

Thomas, D M. Water and gas chemistry from HGP-A geothermal well: January 1980 flow test. United States: N. p., 1980. Web.
Thomas, D M. Water and gas chemistry from HGP-A geothermal well: January 1980 flow test. United States.
Thomas, D M. 1980. "Water and gas chemistry from HGP-A geothermal well: January 1980 flow test". United States.
@article{osti_6297641,
title = {Water and gas chemistry from HGP-A geothermal well: January 1980 flow test},
author = {Thomas, D M},
abstractNote = {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.},
doi = {},
url = {https://www.osti.gov/biblio/6297641}, journal = {Trans. - Geotherm. Resour. Counc.; (United States)},
number = ,
volume = 4,
place = {United States},
year = {Mon Sep 01 00:00:00 EDT 1980},
month = {Mon Sep 01 00:00:00 EDT 1980}
}

Conference:
Other availability
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