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As , one can represent the local fields as
asymptotic series in the small parameter
| |
(60) |
| (61) |
and equivalently for .
The zeroth-order response corresponds to uniform
fluid pressure in the pores and is therfore given by and
| |
(62) |
where the patchy-saturation aij have been employed.
The fact that the quasi-static Skempton's coefficient in the patchy-saturation
model is exactly the harmonic average of the constituents Bi is equivalent to
saying that at low frequencies, the fluid bulk modulus is given by
1/Kf = v1 /Kf1 + v2 /Kf2. The quasi-static response is
thus completely independent of the spatial geometry of the fluid patches; it depends
only on the volume fractions occupied by the patches.
The leading order correction to uniform fluid pressure is then controlled by
the boundary-value problem
| |
(63) |
| (64) |
| (65) |
| (66) |
| (67) |
It is now assumed that for patchy-saturation
cases of interest (air/water or water/oil), the ratio can be considered small.
To leading order in , equations (63), (66), and (67)
require that (a spatial constant).
The fluid pressure in phase 1 is now rewritten as
| |
(68) |
where, from equations (64), (65) and (67) and
to leading order in , the potential is the solution of
the same elliptic boundary-value problem (25)-(27)
given earlier.
Upon averaging (68) over all of , the
leading order in difference in the average fluid pressures can be written
| |
(69) |
where L1 is again the length defined by equation (24).
To connect this fluid-pressure difference to the increment we use
the divergence theorem and the no-flow boundary condition on
to write equation (53) as
| |
(70) |
Replacing with using equation (69)
then gives the desired law
with
| |
(71) |
being the low-frequency limit of interest.
Next: High-frequency limit of
Up: Patchy-Saturation Transport
Previous: Mesoscopic flow equations
Stanford Exploration Project
10/14/2003