Show simple item record



Item Description

dc.contributor.author Zheng, Ping en_US
dc.contributor.author Lau, Kah Hie en_US
dc.date.accessioned 2012-04-10T17:43:00Z en_US
dc.date.accessioned 2012-04-10T18:58:43Z en_US
dc.date.available 2012-04-10T17:43:00Z en_US
dc.date.available 2012-04-10T18:58:43Z en_US
dc.date.issued 1978-09 en_US
dc.identifier.citation Cheng P, Lau KH. 1978. Modelling of a Volcanic Island Geothermal Reservoir. Honolulu (HI): Hawaii Geothermal Project, University of Hawaii at Manoa. en_US
dc.identifier.uri http://hdl.handle.net/10125/22344 en_US
dc.description Bibliography: p. 38-39. At head of title: Hawaii Geothermal Project. en_US
dc.description.abstract Prior to the drilling of the HGP-A well at the Kapoho geothermal field in December 1975, it had generally been assumed that geothermal reservoirs on the Island of Hawaii were low-temperature liquid-dominated reservoirs which were constantly recharged from the ocean. Two numerical studies based on this conceptual model were carried out to investigate heat transfer and fluid flow characteristics in such a reservoir. It was found that (1) even under the most unfavorable conditions, i.e., in the absence of caprock for the prevention of heat loss and with constant recharge from cold seawater, it is possible to have a large amount of hot water at shallow depth, (2) the upwelling of the water table resulting from geothermal heating is small, and (3) the rate of contraction of isotherms resulting from the withdrawal of fluid from a production well depends not only on the withdrawal rate, but also on the size of the heat source as well as the relative location of the production well and the heat source. After the drilling of the HGP-A well had been completed in April 1976, it was found from the core samples that the permeability of the formation varies with depth, and that the low salinity of the water samples taken from the well indicates that there is a barrier between the well and the ocean, preventing the free flow of seawater. Thus, a third numerical model taking into consideration the layered structure of the formation, with recharge and discharge through an upper permeable boundary, was carried out to simulate the free convection processes at the Kapoho geothermal field. In addition, analytical studies on convective heat transfer from dikes and sills in an aquifer with high permeability have been performed, and analytical expressions for heat transfer rates and the size of the hot water zone from hot intrusives have been obtained. The results of this investigation have given considerable insight on heat and mass transfer processes in a liquid-dominated volcanic geothermal reservoir. en_US
dc.description.sponsorship Department of Energy, Contract EY-76-C-03-1093 Energy Research and Development Administration, Contract E(04-3)-1093 National Science Foundation, Grant GI 38319 State of Hawaii, Grants RCUH 5774, 5784, 5942 County of Hawaii, Grant RCUH 5773 Hawaiian Electric Company, Grants RCUH 5809, 5828 en_US
dc.format.extent 48 pages en_US
dc.language.iso en-US en_US
dc.publisher Hawaii Geothermal Project, University of Hawaii at Manoa en_US
dc.subject reservoir modeling en_US
dc.subject theoretical en_US
dc.subject engineering en_US
dc.subject.lcsh Geothermal resources--Mathematical models en_US
dc.subject.lcsh Geothermal engineering--Mathematical models en_US
dc.subject.lcsh Geothermal resources--Mathematical models en_US
dc.subject.lcsh Geothermal engineering--Mathematical models en_US
dc.subject.lcsh Hawaii Geothermal Project en_US
dc.title Modelling of a volcanic island geothermal reservoir en_US
dc.type Report en_US
dc.type.dcmi Text en_US
local.identifier.callnumber TJ280.7 .C45 en_US

Item File(s)

Files Size Format View
1978-HIGP-ModellingOfAVolcanicIsland.PDF 15.63Mb PDF View/Open

This item appears in the following Collection(s)

Show simple item record

Search


Advanced Search

Browse

My Account

Statistics

About