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Vapor Generation in Hot Permeable Rock Through Injection of Water

S. D. Fitzgerald and A.W. Woods

Conference
Stanford Geothermal Workshop
Year
1992
Session
Injection
Language
English

Full text

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Abstract

We present a non-linear model to describe vapour generation in a hot, permeable rock through injection of water. We develop similarity solutions describing the steady injection of fluid from a line source. A systematic parameter study has shown that, with other parameters fixed, as (i) the reservoir pressure increases, the mass fraction vaporised decreases; (ii) the reservoir temperature increases, the mass fraction vaporised increases; (iii) as the mass injection rate increases, the mass fraction vaporised decreases; and (iv) as the porosity increases, the mass fraction vaporised decreases. We then present similarity solutions which describe injection from (i) a point source, with the mass flux injected proportional to t l / ' ; and (ii) a planar source, with the mass flux injected proportional to t-'/', where t is the time of injection. These results suggest that for steady injection, the vapour production gradually increases for injection from a point source, and gradually decreases for planar injection. We confirm this prediction with numerical calculations describing the vapour production resulting from steady injection from line, point and planar sources.

Copyright 1992, 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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