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structural geology, propagation mechanics and - Stanford School of ...

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the discontinuous nature <strong>of</strong> the pattern <strong>and</strong> the availability <strong>of</strong> preferred flow paths<br />

crossing a minimum number <strong>of</strong> DBs. Nonetheless, the anastomosing parallel pattern<br />

studied still could induce a significant effective permeability anisotropy between the<br />

maximum (b<strong>and</strong>-parallel) <strong>and</strong> minimum (b<strong>and</strong>-normal) directions. For kb/km=10 -2 about a<br />

0.5 order-<strong>of</strong>-magnitude anisotropy results, for kb/km=10 -3 the anisotropy increases to<br />

about 1.3 orders <strong>of</strong> magnitude.<br />

7. Summary<br />

We have presented a numerical method for calculating the effective permeability<br />

induced by any given pattern <strong>of</strong> deformation b<strong>and</strong>s (DBs), <strong>and</strong> then used it to assess the<br />

2-D effective permeability for volumes <strong>of</strong> porous s<strong>and</strong>stone containing each <strong>of</strong> three<br />

characteristic DB patterns present in the Aztec s<strong>and</strong>stone <strong>of</strong> the Valley <strong>of</strong> Fire State Park,<br />

Nevada—parallel, cross-hatch <strong>and</strong> the dominant anastomosing.<br />

For substantially parallel patterns, we found that b<strong>and</strong>-parallel effective permeability<br />

remains relatively unaffected for realistic DB volume fractions up to 20%. Likewise,<br />

b<strong>and</strong>-parallel effective permeability is only slightly affected by changes in the<br />

permeability contrast between the DBs <strong>and</strong> the host rock. By contrast, b<strong>and</strong>-normal<br />

effective permeability drops even for low volume fractions <strong>of</strong> DBs <strong>and</strong> is extremely<br />

sensitive to varying internal DB permeability. Parallel b<strong>and</strong> patterns such as those<br />

observed in the Aztec can induce permeability anisotropy <strong>of</strong> up to 2 orders <strong>of</strong> magnitude,<br />

with the maximum principal permeability aligned in the b<strong>and</strong>-parallel direction. For<br />

idealized parallel patterns, our modeling results exactly match those computed<br />

analytically.<br />

Cross-hatch b<strong>and</strong> patterns can be analyzed numerically, or in a somewhat simplified<br />

way using a combination <strong>of</strong> numerical <strong>and</strong> analytical methods. They yield highly<br />

anisotropic effective permeability reductions for acute intersection angles close to 0°, <strong>and</strong><br />

isotropic effective permeability for angles close to 90°. For relatively regular, evenly<br />

spaced patterns, the direction <strong>of</strong> maximum permeability bisects the acute angle <strong>of</strong><br />

intersection. For DB volume fractions <strong>of</strong> ~10% <strong>and</strong> acute intersection angles <strong>of</strong> ~80 o ,<br />

such as found in the Aztec, the cross-hatch pattern can produce up to a 1.5-order-<strong>of</strong>-<br />

magnitude reduction in bulk permeability <strong>and</strong> more than an order-<strong>of</strong>-magnitude<br />

permeability anisotropy.<br />

165

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