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

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GROUNDWATER FLOW TO THE RIVER TAME<br />

channel (61 Mld -1 , 20% <strong>of</strong> flow), after the mean values <strong>of</strong> known discharges have been<br />

subtracted. On the catchment scale if tributary flow is considered as <strong>ground<strong>water</strong></strong> derived,<br />

then flow at Water Orton comprises between 40 and 67% <strong>ground<strong>water</strong></strong>. Clearly, the influence<br />

<strong>of</strong> <strong>ground<strong>water</strong></strong> contaminants on the dry weather <strong>surface</strong> <strong>water</strong> concentrations will vary<br />

considerably and will be dependent on the baseflow conditions and changing levels <strong>of</strong><br />

industrial (STW) discharge. <strong>The</strong> mean values <strong>of</strong> baseflow derived using the filter technique<br />

were compared with values based on the analyses (Section 4.9.1, Appendix 17) <strong>of</strong> seven<br />

periods (54 days total) <strong>of</strong> baseflow recession during 1999. <strong>The</strong> results (Table 5.2) show a<br />

reasonable correlation with the recession estimates generally 14 to 18 % lower than the filter<br />

estimates.<br />

Gauging Station<br />

Average Baseflow – Recession<br />

Method (Mld -1 )<br />

Average Baseflow – Filter<br />

Method<br />

(Mld -1 )<br />

Bescot 113 131<br />

Calthorpe 31 38<br />

Water Orton 260 308<br />

Table 5.2 Comparison <strong>of</strong> mean baseflow obtained using filter and recession analyses methods.<br />

<strong>The</strong> effect <strong>of</strong> industrial discharges was subtracted from the mean baseflow to provide an<br />

estimate <strong>of</strong> diffuse baseflow discharge per unit <strong>of</strong> catchment area (Table 5.3). <strong>The</strong> values for<br />

Water Orton and Calthorpe are higher than Bescot and may reflect high levels <strong>of</strong> <strong>ground<strong>water</strong></strong><br />

discharge from the sandstone and drift, though differences in recharge rates and land use will<br />

also be significant. A difference between catchments is also evident from the variation<br />

118

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