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VAPORISING LIQUID CURRENTS DRlVEN BY GRAVITY THROUGH GEOTHERMAL RESERVOIRS

Andrew W. Woods

Conference
Stanford Geothermal Workshop
Year
1997
Language
English

Full text

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Abstract

We present a series of solutions describing the propagation of injected water through a geothermal reservoir accounting for both the effects of gravity and also boiling at the advancing front. These new similarity solutions provide new insight into the complex coupled flow driven by gravity and can be readily extended to account for the effects of surface tension which may cause some residual liquid to remain in the pores once the main front has descended.

Copyright 1997, 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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