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

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River Discharge (m 3 s -1 )<br />

Depth <strong>of</strong> Piezometer Tip below River Bed (m)<br />

4.7<br />

4.2<br />

3.7<br />

3.2<br />

2.7<br />

2.2<br />

1.7<br />

Carboniferous<br />

Coal Measures<br />

23/05/00<br />

02/06/00<br />

22/05/01<br />

23/05/01<br />

07/07/1999*1<br />

20/07/1999*1<br />

27/07/1999*1<br />

06/07/2000*2<br />

11/07/2000*2<br />

10/08/2000*2<br />

*1 Clay 1999<br />

*2 Knowles 2000<br />

Triassic<br />

Sandstone<br />

23/05/00<br />

y = 0.0001x + 1.4887<br />

y = 6E-05x + 1.3261<br />

y = 3E-05x + 1.1252<br />

1.2<br />

0 5000 10000 15000 20000 25000<br />

Distance Downstream from Bescot Gauging Station (m)<br />

23/05/01<br />

27/07/99<br />

Figure 5.8 Dry weather discharge accretion along the River Tame.<br />

Mercia<br />

Mudstone<br />

Head <strong>of</strong> Piezometer above River Stage (m)<br />

-0.04 -0.02 0 0.02 0.04 0.06 0.08 0.1 0.12 0.14 0.16<br />

0<br />

0.2<br />

0.4<br />

0.6<br />

0.8<br />

1<br />

1.2<br />

1.4<br />

<strong>The</strong> multilevel data<br />

refers to 3 distinct<br />

lateral positions across<br />

the channel at pr<strong>of</strong>ile 8<br />

All data<br />

Eastern Multilevel<br />

Central Multilevel<br />

Western<br />

Figure 5.9 Variation in the difference in head between the river and the riverbedpiezometers<br />

with depth.

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