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A MEASUREMENT OF STEAM-WATER RELATIVE PERMEABILITY

Cengiz Satik

Key words
relative permeability
Conference
Stanford Geothermal Workshop
Year
1998
Session
MODELING
Language
English

Full text

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Abstract

This paper reports experimlmtal efforts towards measuring accurate steam-water relative permeability functions under steady-state and non-adiabatic conditions. A steady-state experiment was conducted
and a set of relative permeability curves for simultaneous flow of steam and water in porous media has been obtained. These relations show that
the relative permeabilities for both steam and water phases in porous media vary with saturation in a curvilinear fashion. The saturations in this experiment were measured by using a high resolution X-ray
computer tomography (CT) scanner. In addition the pressure gradients were obtained from accurate measurements of liquid-phase pressure over regions with flat saturation profiles. These two aspects constitute a major improvement in the experimental method compared to those used in the past.

Copyright 1998, 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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