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Some Natural Transients in Geothermal Fields Part 1: Two-Phase Flow in Fissures

A. McNabb and R.W. Henley

Conference
New Zealand Geothermal Workshop
Year
1998
Language
English

Full text

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Abstract

Equations governing two phase slug flow in large scale fracture permeability are derived. Estimates for fissure permeability, fluid capacity in the two-phase zone and the fluid flux rates entering these large scale fractures show it is possible to excite slug flows with periods and liquid volume fluxes that are characteristic of geyser activity.

Copyright 1998, University of Auckland. 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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