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The impact of urban groundwater upon surface water - eTheses ...

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Elevation <strong>of</strong> cell centre m.a.o.d<br />

100<br />

90<br />

80<br />

70<br />

60<br />

50<br />

40<br />

30<br />

20<br />

10<br />

0<br />

Specific discharge across the left (East) and right (West) hand boundaries <strong>of</strong> the<br />

model under steady state conditions<br />

Underflow to the flood plain<br />

Flow through the deep<br />

sandstone aquifer<br />

Velocity ~0.05 md -1<br />

Flow through the Drift<br />

deposits<br />

Velocity ~0.18 md -1<br />

-0.01 0.01 0.03 0.05 0.07 0.09<br />

Gravel<br />

Sandstone<br />

Specific discharge across boundary cell md -1<br />

Figure 6.9a Specific discharge across the FAT3D model boundaries when gravel<br />

Kx = 5 md -1<br />

Weathered<br />

sandstone<br />

Conductivities Kx (md -1 )<br />

Gravel 5<br />

Weathered Sandstone 3<br />

Sandstone 2<br />

Eastern Boundary, R23<br />

Western Boundary, R23

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