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