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

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WATER QUALITY INTERACTIONS<br />

source for the <strong>surface</strong> <strong>water</strong> contamination. No information is available on pipe discharge<br />

concentrations across the aquifer but it is thought that some discharges comprise<br />

contaminated <strong>ground<strong>water</strong></strong> abstracted for use in industrial processes and eventually<br />

discharged to the river.<br />

<strong>The</strong> <strong>surface</strong> <strong>water</strong> concentration pr<strong>of</strong>ile for TCE (Figure 7.21a) is complex and shows<br />

considerable variation between different sampling periods. It is not possible to relate high<br />

levels <strong>of</strong> TCE in the <strong>ground<strong>water</strong></strong> at a particular location directly with local increases in<br />

<strong>surface</strong> <strong>water</strong> concentrations. However, levels <strong>of</strong> TCE are maintained or increased across the<br />

aquifer despite volatilisation and this indicates continuing input from what are believed to be<br />

<strong>ground<strong>water</strong></strong> sources. <strong>The</strong>re is perhaps a general increase for all the sampling periods in the<br />

TCE <strong>surface</strong> <strong>water</strong> concentrations from 4 km onwards which may correspond to the changes<br />

in land use and hydrogeological factors discussed for the inorganic <strong>water</strong> quality. <strong>The</strong>re is<br />

evidence to suggest that some <strong>of</strong> the TCE is being derived from intermittent sources, probably<br />

pipe discharges. An example <strong>of</strong> this was the large peak detected on 11/5/01 at 3 km which<br />

was not detected in any <strong>of</strong> the previous sampling. A similar high degree <strong>of</strong> variability is seen<br />

in both the PCE and TCM <strong>surface</strong> <strong>water</strong> pr<strong>of</strong>iles (Figure 7.21 b and c). Reasons for the<br />

variability between and within sampling periods may be a combination <strong>of</strong> factors:<br />

1. changes in pipe and <strong>ground<strong>water</strong></strong> plume discharge rates and concentrations;<br />

2. variation in river flow;<br />

3. different temperatures and <strong>surface</strong> <strong>water</strong> mixing will alter rates <strong>of</strong> volatilisation;<br />

4. the quantities detected are low and may be subject to large percentage errors in the<br />

analyses; and<br />

5. variation in the type and quantity <strong>of</strong> suspended particulate matter may alter sorption rates.<br />

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