Abstract
We examine the permeability of a medium with thin tapered cracks to a single‐phase fluid flow in the presence of immobile matter which is accumulated in the tips of cracks. The original Kozeny‐Carman relation shows an increase in permeability of such a material relative to the case when tips are free of accumulated matter. To resolve this paradox we introduce a corrected version of the Kozeny‐Carman relation for the case when the shape of a crack cross‐section can be described by a power law. This class of crack shapes includes the important cases of triangular cracks and space between two contacting circular grains. The revised relation includes the original porosity Φ and specific surface area S of the material without accumulated matter as well as the degree of filling a crack space by accumulated matter Z. The permeability is proportional to Φ3 and S−2, and decreases with increasing Z.
Original language | English |
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Pages (from-to) | 877-880 |
Number of pages | 4 |
Journal | Geophysical Research Letters |
Volume | 18 |
Issue number | 5 |
DOIs | |
State | Published - May 1991 |
Externally published | Yes |