Measurement of Aperture Distribution, Capillary Pressure, Relative Permeability and Saturation in a Rock Fracture Using CT Scanning

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Abstract/Contents

Abstract
We developed an experimental technique that uses CT scanning to provide high resolution measurements of aperture distribution and in-situ saturation along with capillary pressure and relative permeability for the same rough-walled fracture. We applied this technique to an induced fracture in a cylindrical basalt core under going air/water drainage. The sum of the liquid and gas relative permeabilities was much less than 1 at intermediate saturations and krw showed a sharp change over a narrow range of average water saturations. In-situ saturation maps showed channeling of air and significant retention of the wetting phase (water). Capillary pressures exhibited non-monotonic variation with water saturation. Examination of the saturation maps indicated that decreases in the capillary pressure with increasing air saturation are due to the local rearrangement of fluid under the influence of both capillary and viscous forces. This suggests that a macroscopic capillary pressure, based theoretically on considerations of capillary equilibrium, may be inadequate for describing fracture flow.

Description

Type of resource text
Date created June 1999

Creators/Contributors

Author Bertels, Stephanie Petra
Primary advisor Blunt, Martin
Degree granting institution Stanford University, Department of Petroleum Engineering

Subjects

Subject School of Earth Energy & Environmental Sciences
Genre Thesis

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Preferred Citation
Bertels, Stephanie Petra. (1999). Measurement of Aperture Distribution, Capillary Pressure, Relative Permeability and Saturation in a Rock Fracture Using CT Scanning. Stanford Digital Repository. Available at: https://purl.stanford.edu/jq221dh9354

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Master's Theses, Doerr School of Sustainability

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