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

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5.3.1. Results<br />

With the regional gradient directed roughly parallel to the dominant b<strong>and</strong> trend, the<br />

resulting contaminant plume is narrower <strong>and</strong> longer than would be the case in the absence<br />

<strong>of</strong> the CB array (Figure 7.12a) <strong>and</strong> extends some 60 m up-gradient from the leak location.<br />

The long axis <strong>of</strong> the two plumes (with <strong>and</strong> without CBs) remains coincident, however,<br />

<strong>and</strong> parallel to the b<strong>and</strong> trend. Looking in detail, the plume has clearly channeled along<br />

the b<strong>and</strong> array <strong>and</strong> been constrained from spreading laterally (Figure 7.12b).<br />

With the regional gradient directed obliquely to the dominant b<strong>and</strong> trend, the shape<br />

<strong>and</strong> orientation <strong>of</strong> the resulting plume departs substantially from that <strong>of</strong> the CB-free<br />

control case, remaining constrained by <strong>and</strong> aligned with the b<strong>and</strong> array (Figure 7.13a).<br />

The plume is, however, wider <strong>and</strong> shorter than in the parallel scenario, extends 80 m<br />

obliquely up-gradient from the leak (along the b<strong>and</strong> trend), <strong>and</strong>, where gaps in the CB<br />

pattern allow, turns into the regional down-gradient direction (Figure 7.13b).<br />

With the regional gradient directed normal to the dominant b<strong>and</strong> trend, the resulting<br />

plume bears scant resemblance to the CB-free control case, remaining distinctly elongated<br />

along the b<strong>and</strong> array (Figure 7.14a). The plume is shorter <strong>and</strong> broader again than in the<br />

oblique scenario, <strong>and</strong> turns strongly into the regional down-gradient direction at a major<br />

gap in the b<strong>and</strong> pattern (Figure 7.14b, upper left). Finally, the trailing edge <strong>of</strong> the plume is<br />

essentially straight, having pushed uniformly almost 20 m in the regional up-gradient<br />

direction.<br />

5.3.2. Discussion<br />

As with the reservoir-production simulations above, the plume evolution results<br />

reveal a dominating influence on fluid transport by the CB pattern, regardless <strong>of</strong> the<br />

regional gradient direction. Limited sensitivity testing also indicated that realistic<br />

variations in the magnitudes <strong>of</strong> the regional gradient <strong>and</strong>/or contaminant leak rate do not<br />

substantially affect the results. For the hydrogeologist designing a pump-<strong>and</strong>-treat<br />

remediation system therefore, recognizing <strong>and</strong> accounting for the effects <strong>of</strong> the CBs<br />

would prove crucial, particularly with 100% contaminant capture as the goal.<br />

For example, the st<strong>and</strong>ard cleanup approach for a leaking underground storage tank is<br />

to install the minimum number <strong>of</strong> wells that can be spaced immediately down gradient<br />

from the plume front to provide complete capture, assuming radial drawdown at an<br />

192

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