Testing Gassmann fluid substitution in carbonates: sonic log versus ultrasonic core measurements

The technique of fluid substitution is widely used to model elastic properties of rocks saturated with different fluids The applicability of this technique to in-situ seismic and sonic measurements is a matter of frequent debate. Most of the analysis is based on laboratory measurements, with little...

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Main Authors: De Paula, Osni, Pervukhina, M., Gurevich, Boris
Other Authors: Society of Exploration Geophysics
Format: Conference Paper
Published: SEG 2010
Online Access:http://hdl.handle.net/20.500.11937/21097
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author De Paula, Osni
Pervukhina, M.
Gurevich, Boris
author2 Society of Exploration Geophysics
author_facet Society of Exploration Geophysics
De Paula, Osni
Pervukhina, M.
Gurevich, Boris
author_sort De Paula, Osni
building Curtin Institutional Repository
collection Online Access
description The technique of fluid substitution is widely used to model elastic properties of rocks saturated with different fluids The applicability of this technique to in-situ seismic and sonic measurements is a matter of frequent debate. Most of the analysis is based on laboratory measurements, with little or no constraints from field environments. In addition, until recently, most of the data were from sand reservoirs. Applicability of Gassmann fluid substitution to carbonates is even more uncertain. To analyze this problem, we compare elastic moduli obtained using fluid substitution against the moduli obtained from sonic and density logs The dry moduli for fluid substitution are obtained from ultrasonic measurements on 50 core samples from a cretaceous reservoir buried at 5000 meters depth in Santos Basin, offshore Brazil. The good agreement between the saturated moduli obtained from cores and logs is obtained. This shows that the Gassmann equations can be applied not only in siliciclastic reservoirs, but also deep and complex carbonates reservoirs.
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spelling curtin-20.500.11937-210972017-09-13T16:00:43Z Testing Gassmann fluid substitution in carbonates: sonic log versus ultrasonic core measurements De Paula, Osni Pervukhina, M. Gurevich, Boris Society of Exploration Geophysics The technique of fluid substitution is widely used to model elastic properties of rocks saturated with different fluids The applicability of this technique to in-situ seismic and sonic measurements is a matter of frequent debate. Most of the analysis is based on laboratory measurements, with little or no constraints from field environments. In addition, until recently, most of the data were from sand reservoirs. Applicability of Gassmann fluid substitution to carbonates is even more uncertain. To analyze this problem, we compare elastic moduli obtained using fluid substitution against the moduli obtained from sonic and density logs The dry moduli for fluid substitution are obtained from ultrasonic measurements on 50 core samples from a cretaceous reservoir buried at 5000 meters depth in Santos Basin, offshore Brazil. The good agreement between the saturated moduli obtained from cores and logs is obtained. This shows that the Gassmann equations can be applied not only in siliciclastic reservoirs, but also deep and complex carbonates reservoirs. 2010 Conference Paper http://hdl.handle.net/20.500.11937/21097 10.1190/1.3513396 SEG fulltext
spellingShingle De Paula, Osni
Pervukhina, M.
Gurevich, Boris
Testing Gassmann fluid substitution in carbonates: sonic log versus ultrasonic core measurements
title Testing Gassmann fluid substitution in carbonates: sonic log versus ultrasonic core measurements
title_full Testing Gassmann fluid substitution in carbonates: sonic log versus ultrasonic core measurements
title_fullStr Testing Gassmann fluid substitution in carbonates: sonic log versus ultrasonic core measurements
title_full_unstemmed Testing Gassmann fluid substitution in carbonates: sonic log versus ultrasonic core measurements
title_short Testing Gassmann fluid substitution in carbonates: sonic log versus ultrasonic core measurements
title_sort testing gassmann fluid substitution in carbonates: sonic log versus ultrasonic core measurements
url http://hdl.handle.net/20.500.11937/21097