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Transient Steam Flow in Porous Media - Theory and Experiment

W.N. Herkelrath, A.F. Moench

Conference
Stanford Geothermal Workshop
Year
1980
Session
Reservoir Physics
Language
English

Full text

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Abstract

A previous workshop summary (Herkelrath and Moench, 1978) described laboratory studies of transient steam flow in a porous medium. The results indicated that the time required for steampressure transients to propagate through the medium was as much as 30 times greater than predicted by standard noncondensable gas-flow theory. breakthrough was caused by adsorption of steam in the porous sample. This "adsorption lag effect " has been incorporated in to the following revised model of steam flow in a porous medium.

Copyright 1980, 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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