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Cold Water Invasion in Producing Liquid Dominated Geothermal Reservoirs

P.F. Bixley

Location
Wairakei, New Zealand; Kawerau, New Zealand; Broadlands, New Zealand; Taupo Volcanic Zone
Conference
Stanford Geothermal Workshop
Year
1990
Session
Field Results
Language
English

Full text

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Abstract

Pressure reduction at depth as a result of fluid withdrawal has rtsulted in cold water invasion in several liquid dominated geothermal reservoks. Cooi waters enter the hot rtservoir by the same paths via which surface springs w a t fed before exploitation, and cooling is first observed in wells near such features. In and area. Understanding the coofig processes can about the nscrvoir s a w and performance. Such ' cold water invasion appears now to be expectcd in most liauid dominated TtsQyoiTs, although this nsponse may some nservok the affected 81tas ale rtstricted in depth providethenservoirmgineerwithwrminformatiion be-difficult to separate from rtinjech effecis.

Copyright 1990, Stanford Geothermal Program. Readers who download papers from this site should honour the copyright of the original authors, and may not copy or distribute the work further without the permission of the original publisher.

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