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

Conference · Mon Sep 01 00:00:00 EDT 1980 · Trans. - Geotherm. Resour. Counc.; (United States)

OSTI ID:6297641

Thomas, D M

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.

• Research Organization: Hawaii Inst. of Geophysics, Honolulu
• OSTI ID: 6297641
• Report Number(s): CONF-800920-
• Journal Information: Trans. - Geotherm. Resour. Counc.; (United States), Vol. 4; Conference: Geothermal Resource Council annual meeting, Salt Lake City, UT, USA, 9 Sep 1980
• Country of Publication: United States
• Language: English

Related Subjects

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