Cold Water Invasion in Producing Liquid Dominated Geothermal Reservoirs
- Location
- Wairakei, New Zealand; Kawerau, New Zealand; Broadlands, New Zealand; Taupo Volcanic Zone
- Conference
- Stanford Geothermal Workshop
- Year
- 1990
- Session
- Field Results
- Language
- English
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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.
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