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

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Head in P10 (m.a.o.d)<br />

91.1<br />

91.05<br />

91<br />

90.95<br />

90.9<br />

90.85<br />

90.8<br />

A comparison <strong>of</strong> modelled (Erfc) and recorded head variations in piezometer P10<br />

(13.27m from the bank) during a river flood event .<br />

90.75<br />

90.2<br />

06/03/01 00:00 07/03/01 00:00 08/03/01 00:00 09/03/01 00:00 10/03/01 00:00 11/03/01 00:00<br />

Time<br />

Figure 6.16a Results <strong>of</strong> the transient analytical modelling <strong>of</strong> the hydrograph <strong>of</strong> Piezometer<br />

P10 (6/3/01)<br />

Head in P11 (m.a.o.d)<br />

91<br />

90.95<br />

90.9<br />

90.85<br />

90.8<br />

90.75<br />

P10 Actual<br />

P10 Model<br />

Model river input<br />

Model best fit with<br />

S/T = 0.000399<br />

A comparison <strong>of</strong> modelled (Erfc) and recorded head variations in piezometer P11 (8.9<br />

m from the bank) during a river flood event .<br />

Actual P11<br />

Model P11<br />

Model river input<br />

Best fit for model with<br />

S/T = 0.001934<br />

90.7<br />

90.2<br />

06/03/01 00:00 07/03/01 00:00 08/03/01 00:00 09/03/01 00:00 10/03/01 00:00 11/03/01 00:00<br />

Time<br />

Figure 6.16b Results <strong>of</strong> the transient analytical modelling <strong>of</strong> the hydrograph <strong>of</strong> Piezometer<br />

P11 (6/3/01)<br />

90.8<br />

90.7<br />

90.6<br />

90.5<br />

90.4<br />

90.3<br />

90.8<br />

90.7<br />

90.6<br />

90.5<br />

90.4<br />

90.3<br />

Model river input (m.a.o.d.)<br />

Model river input (m.a.o.d.)

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