Role of compliant porosity in stress dependency of ultrasonic velocities in carbonates and sandstones

A study of complex dual-nature porosity of reservoir rocks is necessary for quantitative understanding of seismic wave propagation in reservoirs. We analyze here the ratios of stiff and compliant porosities in 6 samples of carbonates and 6 samples of sandstones, and effect of compliant porosity on u...

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Main Authors: De Paula, Osni, Pervukhina, M., Gurevich, Boris
Other Authors: Brazilian Geophysical Society
Format: Conference Paper
Published: SBGf 2008
Online Access:http://hdl.handle.net/20.500.11937/44617
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author De Paula, Osni
Pervukhina, M.
Gurevich, Boris
author2 Brazilian Geophysical Society
author_facet Brazilian Geophysical Society
De Paula, Osni
Pervukhina, M.
Gurevich, Boris
author_sort De Paula, Osni
building Curtin Institutional Repository
collection Online Access
description A study of complex dual-nature porosity of reservoir rocks is necessary for quantitative understanding of seismic wave propagation in reservoirs. We analyze here the ratios of stiff and compliant porosities in 6 samples of carbonates and 6 samples of sandstones, and effect of compliant porosity on ultrasonic shear and compressional wave velocities measured at effective stresses from 0 to 60 MPa. The compliant porosity is estimated from stress dependency of dry rock compressibility using isotropic Shapiro theory (2003). In the case of sandstones, we have direct measurements of porosity variations with pressure whichvalidate the estimated compliant porosities. Finally, we use Gassmann equations to estimate the stress dependence of shear and compressional wave velocitiesin saturated rocks. Two examples discussed here show that a better estimation is obtained using the high frequency unrelaxed frame shear and bulk modulus(Mavko&Jizzba,1991) to “saturate” the samples.
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institution Curtin University Malaysia
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last_indexed 2025-11-14T09:21:57Z
publishDate 2008
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spelling curtin-20.500.11937-446172017-01-30T15:15:10Z Role of compliant porosity in stress dependency of ultrasonic velocities in carbonates and sandstones De Paula, Osni Pervukhina, M. Gurevich, Boris Brazilian Geophysical Society A study of complex dual-nature porosity of reservoir rocks is necessary for quantitative understanding of seismic wave propagation in reservoirs. We analyze here the ratios of stiff and compliant porosities in 6 samples of carbonates and 6 samples of sandstones, and effect of compliant porosity on ultrasonic shear and compressional wave velocities measured at effective stresses from 0 to 60 MPa. The compliant porosity is estimated from stress dependency of dry rock compressibility using isotropic Shapiro theory (2003). In the case of sandstones, we have direct measurements of porosity variations with pressure whichvalidate the estimated compliant porosities. Finally, we use Gassmann equations to estimate the stress dependence of shear and compressional wave velocitiesin saturated rocks. Two examples discussed here show that a better estimation is obtained using the high frequency unrelaxed frame shear and bulk modulus(Mavko&Jizzba,1991) to “saturate” the samples. 2008 Conference Paper http://hdl.handle.net/20.500.11937/44617 SBGf restricted
spellingShingle De Paula, Osni
Pervukhina, M.
Gurevich, Boris
Role of compliant porosity in stress dependency of ultrasonic velocities in carbonates and sandstones
title Role of compliant porosity in stress dependency of ultrasonic velocities in carbonates and sandstones
title_full Role of compliant porosity in stress dependency of ultrasonic velocities in carbonates and sandstones
title_fullStr Role of compliant porosity in stress dependency of ultrasonic velocities in carbonates and sandstones
title_full_unstemmed Role of compliant porosity in stress dependency of ultrasonic velocities in carbonates and sandstones
title_short Role of compliant porosity in stress dependency of ultrasonic velocities in carbonates and sandstones
title_sort role of compliant porosity in stress dependency of ultrasonic velocities in carbonates and sandstones
url http://hdl.handle.net/20.500.11937/44617