Numerical estimation of electrical conductivity in saturated porous media with a 2-D lattice gas

Author:

Küntz Michel1,Mareschal Jean Claude2,Lavallée Paul3

Affiliation:

1. Stevin Laboratory, Faculty of Civil Engineering, Delft Univ. of Technology, 2628 GA Delft, The Netherlands.

2. University of Québec at Montréal, GEOTOP, Centre de Géochimie Isotopique et de Géochronologie, Pavillon Kennedy, C.P. 8888, Succ. Centre Ville, Montréal, Québec H3C 3P8, Canada.

3. University of Québec at Montréal, Department of Physics, Pavillon Kennedy, C.P. 8888, Succ. Centre Ville, Montréal, Québec H3C 3P8, Canada.

Abstract

A 2-D lattice gas is used to calculate the effective electrical conductivity of saturated porous media as a function of porosity and conductivity ratio [Formula: see text] between the pore‐filling fluid and the solid matrix for various microscopic structures of the pore space. The way the solid phase is introduced allows the porosity ϕ to take any value between 0 and 1 and the geometry of the pore structure to be as complex as desired. The results are presented in terms of the formation factor [Formula: see text], with [Formula: see text] the effective conductivity of the saturated rock and [Formula: see text] the conductivity of the fluid. It is shown that the formation factor F as a function of the porosity ϕ follows a power law [Formula: see text], equivalent to the empirical Archie’s law. The exponent m varies with the microgeometry of the pore space and could therefore reflect the microstructure at the macroscopic scale. The prefactor a of the power law, however, is close to 1 regardless of the microstructure. For a given microgeometry of the pore space, the variation of the residual electrical conductivity of the solid matrix induced by a finite conductivity ratio [Formula: see text] does not significantly influence the variation of the effective conductivity of the fluid‐solid binary mixture unless the porosity is low.

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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