Frequency-Dependent Streaming Potentials: A Review

The interpretation of seismoelectric observations involves the dynamic electrokinetic coupling, which is related to the streaming potential coefficient. We describe the different models of the frequency-dependent streaming potential, mainly Packard's and Pride's model. We compare the trans...

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Main Authors: L. Jouniaux, C. Bordes
Format: Article
Language:English
Published: Wiley 2012-01-01
Series:International Journal of Geophysics
Online Access:http://dx.doi.org/10.1155/2012/648781
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author L. Jouniaux
C. Bordes
author_facet L. Jouniaux
C. Bordes
author_sort L. Jouniaux
collection DOAJ
description The interpretation of seismoelectric observations involves the dynamic electrokinetic coupling, which is related to the streaming potential coefficient. We describe the different models of the frequency-dependent streaming potential, mainly Packard's and Pride's model. We compare the transition frequency separating low-frequency viscous flow and high-frequency inertial flow, for dynamic permeability and dynamic streaming potential. We show that the transition frequency, on a various collection of samples for which both formation factor and permeability are measured, is predicted to depend on the permeability as inversely proportional to the permeability. We review the experimental setups built to be able to perform dynamic measurements. And we present some measurements and calculations of the dynamic streaming potential.
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institution Kabale University
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spelling doaj-art-fcefe257c62f4431b5c6108fa407fb782025-02-03T01:10:12ZengWileyInternational Journal of Geophysics1687-885X1687-88682012-01-01201210.1155/2012/648781648781Frequency-Dependent Streaming Potentials: A ReviewL. Jouniaux0C. Bordes1Institut de Physique du Globe de Strasbourg, UdS-CNRS UMR 7516, Université de Strasbourg, 5 rue René Descartes, 67084 Strasbourg, FranceLaboratoire des Fuides Complexes et leurs Réservoirs, UPPA-CNRS UMR5150, Université de Pau et des Pays de l'Adour, 64013 Pau, FranceThe interpretation of seismoelectric observations involves the dynamic electrokinetic coupling, which is related to the streaming potential coefficient. We describe the different models of the frequency-dependent streaming potential, mainly Packard's and Pride's model. We compare the transition frequency separating low-frequency viscous flow and high-frequency inertial flow, for dynamic permeability and dynamic streaming potential. We show that the transition frequency, on a various collection of samples for which both formation factor and permeability are measured, is predicted to depend on the permeability as inversely proportional to the permeability. We review the experimental setups built to be able to perform dynamic measurements. And we present some measurements and calculations of the dynamic streaming potential.http://dx.doi.org/10.1155/2012/648781
spellingShingle L. Jouniaux
C. Bordes
Frequency-Dependent Streaming Potentials: A Review
International Journal of Geophysics
title Frequency-Dependent Streaming Potentials: A Review
title_full Frequency-Dependent Streaming Potentials: A Review
title_fullStr Frequency-Dependent Streaming Potentials: A Review
title_full_unstemmed Frequency-Dependent Streaming Potentials: A Review
title_short Frequency-Dependent Streaming Potentials: A Review
title_sort frequency dependent streaming potentials a review
url http://dx.doi.org/10.1155/2012/648781
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