Effect of fluid on wave propagation in weakly anisotropic porous media

Predicting seismic velocities in isotropic fluid-saturated rocks is commonly done using the isotropic Biot-Gassmann theory. For anisotropic media, the Biot-Gassmann solution is expressed in terms of stiffness or compliance, which does not provide an intuitive understanding on the impact of fluid on...

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Main Authors: Collet, O., Gurevich, Boris
Other Authors: American Society of Civil Engineers
Format: Conference Paper
Published: American Society of Civil Engineers 2013
Online Access:http://hdl.handle.net/20.500.11937/36755
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author Collet, O.
Gurevich, Boris
author2 American Society of Civil Engineers
author_facet American Society of Civil Engineers
Collet, O.
Gurevich, Boris
author_sort Collet, O.
building Curtin Institutional Repository
collection Online Access
description Predicting seismic velocities in isotropic fluid-saturated rocks is commonly done using the isotropic Biot-Gassmann theory. For anisotropic media, the Biot-Gassmann solution is expressed in terms of stiffness or compliance, which does not provide an intuitive understanding on the impact of fluid on anisotropy. To analyse how the pore fluid affects wave propagation in weakly anisotropic media, we rederived these expressions in terms of dimensionless anisotropy parameters. Besides, we study the effect of fluid on two anisotropy patterns, the one caused by aligned fractures embedded in an isotropic porous background and the stress-induced anisotropy pattern. By deriving an approximation of the anellipticity parameter η, we show that if the dry medium is elliptical, the saturated medium is also elliptical but only if the porosity is not too small. This result can provide a way of differentiating between stress- and fracture-induced anisotropy.
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spelling curtin-20.500.11937-367552017-09-13T15:21:23Z Effect of fluid on wave propagation in weakly anisotropic porous media Collet, O. Gurevich, Boris American Society of Civil Engineers Predicting seismic velocities in isotropic fluid-saturated rocks is commonly done using the isotropic Biot-Gassmann theory. For anisotropic media, the Biot-Gassmann solution is expressed in terms of stiffness or compliance, which does not provide an intuitive understanding on the impact of fluid on anisotropy. To analyse how the pore fluid affects wave propagation in weakly anisotropic media, we rederived these expressions in terms of dimensionless anisotropy parameters. Besides, we study the effect of fluid on two anisotropy patterns, the one caused by aligned fractures embedded in an isotropic porous background and the stress-induced anisotropy pattern. By deriving an approximation of the anellipticity parameter η, we show that if the dry medium is elliptical, the saturated medium is also elliptical but only if the porosity is not too small. This result can provide a way of differentiating between stress- and fracture-induced anisotropy. 2013 Conference Paper http://hdl.handle.net/20.500.11937/36755 10.1061/9780784412992.026 American Society of Civil Engineers restricted
spellingShingle Collet, O.
Gurevich, Boris
Effect of fluid on wave propagation in weakly anisotropic porous media
title Effect of fluid on wave propagation in weakly anisotropic porous media
title_full Effect of fluid on wave propagation in weakly anisotropic porous media
title_fullStr Effect of fluid on wave propagation in weakly anisotropic porous media
title_full_unstemmed Effect of fluid on wave propagation in weakly anisotropic porous media
title_short Effect of fluid on wave propagation in weakly anisotropic porous media
title_sort effect of fluid on wave propagation in weakly anisotropic porous media
url http://hdl.handle.net/20.500.11937/36755