Wenyu,
To clarify, your question is whether n = 2/3 is appropriate for
f = ((\phi - \phi_c)/(\phi_0 - \phi_c))^n
with porosity \phi, initial porosity \phi_0 and critical porosity \phi_c, and where f is a scaling factor for the intrinsic permeability, correct?
There is discussion below these equations, in the paragraph beginning with “The two-thirds power arises from the assumption that…”, that explains the assumption of spherical mineral grains. If your porosity will approach 100%, I agree that the assumption is
likely not applicable to your conceptual model.
Peter,
Do you want to comment on this?
Glenn
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