M. Kuntz et al., Numerical estimation of electrical conductivity in saturated porous media with a 2-D lattice gas, GEOPHYSICS, 65(3), 2000, pp. 766-772
A 2-D lattice gas is used to calculate the effective electrical conductivit
y of saturated porous media as a function of porosity and conductivity rati
o R-c between the pore-filling fluid and the solid matrix for various micro
scopic structures of the pore space. The way the solid phase is introduced
allows the porosity phi to take any value between 0 and 1 and the geometry
of the pore structure to be as complex as desired. The results an presented
in terms of the formation factor F = sigma(w)/sigma(r), with a, the effect
ive conductivity of the saturated rock and a,. the conductivity of the flui
d. It is shown that the formation factor F as a function of the porosity ph
i follows a power law F = a phi(-m), equivalent to the empirical Archie's l
aw The exponent in varies with the microgeometry of the pore space and coul
d therefore reflect the microstructure at the macroscopic scale. The prefac
tor a of the power law however, is close to 1 regardless of the microstruct
ure. For a given microgeometry of the Fore space, the variation of the resi
dual electrical conductivity of the solid matrix induced by a finite conduc
tivity ratio R-c does not significantly influence the variation of the effe
ctive conductivity of the fluid-solid binary mixture unless the porosity is
low.