TY - JOUR
T1 - A simple mathematical model for determining the equivalent permeability of fractured porous media
AU - Liu, Jianjun
AU - Sano, Yoshihiko
AU - Nakayama, Akira
PY - 2009/3/1
Y1 - 2009/3/1
N2 - A simple mathematical model has been proposed so as to determine the equivalent permeability of fractured porous media. The model consists of square blocks placed in an array with vertical and horizontal fractures between the blocks. An analytical expression valid for all macroscopic flow directions has been derived for the equivalent permeability of the fractured porous media, assuming a horizontal flow through the blocks placed in a porous medium. The analytical expression agrees well with the existing equations and also with the microscopic numerical results carried out using a unit structure with periodic boundary conditions. The foregoing two-dimensional model has been extended to a three dimensional case in which the cubic rocks are arranged in a cubic array. The resulting three-dimensional analytical expression for the equivalent permeability is found to agree very well with both existing formula and microscopic numerical simulation.
AB - A simple mathematical model has been proposed so as to determine the equivalent permeability of fractured porous media. The model consists of square blocks placed in an array with vertical and horizontal fractures between the blocks. An analytical expression valid for all macroscopic flow directions has been derived for the equivalent permeability of the fractured porous media, assuming a horizontal flow through the blocks placed in a porous medium. The analytical expression agrees well with the existing equations and also with the microscopic numerical results carried out using a unit structure with periodic boundary conditions. The foregoing two-dimensional model has been extended to a three dimensional case in which the cubic rocks are arranged in a cubic array. The resulting three-dimensional analytical expression for the equivalent permeability is found to agree very well with both existing formula and microscopic numerical simulation.
KW - Darcy's law
KW - Equivalent permeability
KW - Fractured porous media
KW - Numerical experiment
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U2 - 10.1016/j.icheatmasstransfer.2008.11.010
DO - 10.1016/j.icheatmasstransfer.2008.11.010
M3 - Article
AN - SCOPUS:60449083681
SN - 0735-1933
VL - 36
SP - 220
EP - 224
JO - International Communications in Heat and Mass Transfer
JF - International Communications in Heat and Mass Transfer
IS - 3
ER -