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The Effect of Radially Varying Transmissivity on the Transient Pressure Phenomenon

L. D. Mlodinow and C. F. Tsang

Conference
Stanford Geothermal Workshop
Year
1977
Session
Modeling
Language
English

Full text

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Abstract

During reinjection of cooled geothermal fluid into a reservoir, chemical precipitation and other processes may occur changing the permeability of the aquifer. In general, the permeability becomes a function both of time and space. This will, of course, affect the injection well. Some attempts have been made to analytically predict the pressure response. The present paper describes our calculations which yield analytic expressions, in terms of a single integral, for a wide class of physically reasonable permeability functions. Results are presented for a few typical examples.

Copyright 1977, 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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