Thermal recovery processes such as cyclic steam stimulation and steam assis
ted gravity drainage induce significant shear dilation in oil sand formatio
ns. Shear dilation deformation results in an increase in pore volume, there
by enhancing permeability. In previous studies, it was assumed that the cha
nge in absolute permeability is a function of porosity or volumetic strain,
which is. in turn, a function of mean or minimum effective stress. In such
conventional semi-empirical correlations (e.g., the Kozeny-Carman equation
), the changes in permeability are equal in all directions even though the
changes in strains are different in each direction. This paper proposes a n
ew deformation-dependent permeability model for the shear dilation of oil s
ands. This model is based on a granular interaction approach. The fundament
al approach accounts for how pore throat areas along flow channels and grai
n contacts change with shear dilation. This allows one to quantify the evol
ution of changes in permeability in one direction under continuous shearing
. The model explicitly states that the permeability changes are highly anis
otropic, dependent on the induced principal strains. Comparison with experi
mental data is presented to show the validity of the proposed model. In add
ition, the proposed model is extended and formulated in a generalized 3D te
nsor notation so that it can be implemented into existing reservoir or coup
led geomechanics-reservoir simulators.