We next present a sample calculation of the relative
permeability for the 22% porosity Fontainebleau sandstone.
In this case, the pore space is filled with two fluids.
One fluid preferentially wets the solid surface and the second
fluid is non-wetting. The degree of saturation,
w is Vw
/ Vp, where the Vw is the
volume of the wetting phase in the pore space and Vp is
the volume of the pore space. Although there is debate as to the correct
formulation of the macroscopic two phase flow equations
[14], we use the
following empirical relation to describe the response of a multiphase fluid
system to an external driving force:
Here the Kij are the components of a permeability tensor
and the applied pressure gradient on each fluid component
is from a simple body force,
, where g is an acceleration constant.
The average velocity of each fluid component is given by
and
.
The forcing can be applied to each phase separately allowing
determination of the off-diagonal terms in the permeability tensor.
The viscosity µ i is the same for both fluids.
Relative permeability data is usually presented in
terms of constant capillary number,
, where
is the
interfacial surface tension. For our body force driven fluids, we can define an
effective capillary number,
, by replacing v with the
Darcy velocity so that
.
Figure 5
shows the relative permeability of the
= 22% rock
for the cases of
= 7.5 x 10-4 and
7.5 x 10-5.

Figure 5:
Relative permeabilities of 22% porosity Fontainebleau sandstone
versus wetting fluid saturation,
W.
The solid and dashed lines correspond to
= 7.5 x 10-4 and
= 7.5 x 10-5 respectively.
The lower curves correspond to the off-diagonal elements of the permeability
tensor with the * denoting the case where the nonwetting fluid is driven.