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

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By contrast, b<strong>and</strong>-parallel effective permeability is not reduced by an order <strong>of</strong> magnitude<br />

until wb/W=90%, a DB volume density far exceeding the approximate upper limit <strong>of</strong> 20%<br />

observed in the Aztec. Thus for parallel DB patterns within the realistic wb/W range, a<br />

permeability anisotropy <strong>of</strong> up to 2 orders <strong>of</strong> magnitude can be expected, with the<br />

maximum permeability oriented in the b<strong>and</strong>-parallel direction (Figure 6.9). Note also that<br />

b<strong>and</strong>-parallel effective permeability for both kb/km=10 -2 <strong>and</strong> 10 -3 are virtually<br />

indistinguishable below wb/W=80%.<br />

6.2. Cross-hatch<br />

Cross-hatch DB sets in the Valley <strong>of</strong> Fire exhibit a consistent acute intersection angle<br />

<strong>of</strong> ~80°. In other locales, intersection angles ranging from ~20° to ~90° have been<br />

reported (Aydin <strong>and</strong> Reches, 1982; Hill, 1989; Jamison <strong>and</strong> Stearns, 1982; Underhill <strong>and</strong><br />

Woodcock, 1987). We begin our analysis <strong>of</strong> the effective permeability <strong>of</strong> cross-hatch<br />

patterns by studying those <strong>of</strong> evenly spaced, orthogonal DB sets as a function <strong>of</strong> kb/km<br />

<strong>and</strong> wb/W. Figure 6.10 compares our numerical modeling results for kb/km=10 -2 to an<br />

analytical approximation presented by Taylor <strong>and</strong> Pollard (2000) <strong>and</strong> b<strong>and</strong>-normal<br />

effective permeability as calculated by harmonic averaging. The numerical <strong>and</strong> harmonic<br />

averaging results match well over the entire wb/W range, but correspond to the analytical<br />

approximation only for wb/W below about 5%. For kb/km=10 -3 the wb/W range <strong>of</strong><br />

correspondence drops to

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