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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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 />
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