Theoretical derivation of a Brie-like fluid mixing law
Theoretical derivation of a Brie-like fluid mixing law
Prediction of the velocity of acoustic waves in partially saturated rocks is very important in geophysical applications. The need to accurately predict acoustic velocities has resulted in a widespread popularity of Brie's effective fluid mixing law. This empirical model together with Gassmann's formula are used routinely in fluid substitution problems in petroleum geophysics and seismic monitoring of carbon capture and storage. Most attempts to justify Brie's model have been focused on interpretation in terms of patchy saturation models and attaching meaning to the Brie parameter in terms of the patch size. In this paper, using a microstructural description of the rock and a parameter relating to capillary pressure, we calculate an effective fluid modulus that is very similar to Brie's law. The fluid mixing law we propose is independent of frequency and has a solid theoretical foundation. This proposed law produces analytically harmonic and arithmetic averaging at the endpoints. Our results indicate that Brie-like behaviour may not necessarily be related to frequency- and patch-size- dependent phenomena.
1048-1053
Papageorgiou, Giorgos
8181cca9-12a0-4fa6-93a3-d5711132bc87
Amalokwu, Kelvin
a88bc1e5-5577-49a6-a503-fcd9ea12d8fe
Chapman, Mark
6f13eb72-ad0e-4c7a-b60c-92387a707cf4
July 2016
Papageorgiou, Giorgos
8181cca9-12a0-4fa6-93a3-d5711132bc87
Amalokwu, Kelvin
a88bc1e5-5577-49a6-a503-fcd9ea12d8fe
Chapman, Mark
6f13eb72-ad0e-4c7a-b60c-92387a707cf4
Papageorgiou, Giorgos, Amalokwu, Kelvin and Chapman, Mark
(2016)
Theoretical derivation of a Brie-like fluid mixing law.
Geophysical Prospecting, 64 (4), .
(doi:10.1111/1365-2478.12380).
Abstract
Prediction of the velocity of acoustic waves in partially saturated rocks is very important in geophysical applications. The need to accurately predict acoustic velocities has resulted in a widespread popularity of Brie's effective fluid mixing law. This empirical model together with Gassmann's formula are used routinely in fluid substitution problems in petroleum geophysics and seismic monitoring of carbon capture and storage. Most attempts to justify Brie's model have been focused on interpretation in terms of patchy saturation models and attaching meaning to the Brie parameter in terms of the patch size. In this paper, using a microstructural description of the rock and a parameter relating to capillary pressure, we calculate an effective fluid modulus that is very similar to Brie's law. The fluid mixing law we propose is independent of frequency and has a solid theoretical foundation. This proposed law produces analytically harmonic and arithmetic averaging at the endpoints. Our results indicate that Brie-like behaviour may not necessarily be related to frequency- and patch-size- dependent phenomena.
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Accepted/In Press date: 1 February 2016
e-pub ahead of print date: 13 May 2016
Published date: July 2016
Organisations:
Geology & Geophysics
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Local EPrints ID: 394503
URI: http://eprints.soton.ac.uk/id/eprint/394503
ISSN: 0016-8025
PURE UUID: 532bf4f6-adb2-4156-a87e-a7ada54e9953
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Date deposited: 16 May 2016 10:34
Last modified: 15 Mar 2024 00:24
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Author:
Giorgos Papageorgiou
Author:
Kelvin Amalokwu
Author:
Mark Chapman
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