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

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WATER QUALITY INTERACTIONS<br />

vary over time. High levels <strong>of</strong> temporal variability were also observed in the contaminant<br />

concentrations within the discharging <strong>ground<strong>water</strong></strong>, perhaps associated with changes in the<br />

source, levels <strong>of</strong> natural attenuation, recharge and <strong>ground<strong>water</strong></strong> flow, and interaction with the<br />

<strong>surface</strong> <strong>water</strong>.<br />

It is difficult to say how representative the riverbed piezometer sampling results are to the<br />

overall level <strong>of</strong> contaminant discharge to the Tame. <strong>The</strong> large heterogeneity <strong>of</strong> the system<br />

means that small variations in the position <strong>of</strong> the piezometer are likely to produce significant<br />

variations in concentration. Sample spacing, both along and across the river channel, needs to<br />

be closer to characterise the system fully. Significant changes in contaminant concentrations<br />

may also occur in the vertical plane including the upper 30 cm <strong>of</strong> the riverbed which is<br />

difficult to sample. It is also very likely that some contaminant plumes were not detected and<br />

that, even within the plumes that were, localised zones <strong>of</strong> high concentration were missed.<br />

Nevertheless, despite these limitations, the riverbed data yield a valuable insight into the<br />

processes and contaminant concentrations occurring across the riverbed and on the larger<br />

scale <strong>of</strong> the study reach.<br />

<strong>The</strong> results <strong>of</strong> the <strong>surface</strong> <strong>water</strong> sampling under dry weather baseflow conditions were<br />

complex and difficult to interpret as the river displays considerable temporal variation in<br />

terms <strong>of</strong> both flow and mass flux. <strong>The</strong>re are several time scales apparent in these variations:<br />

on a seasonal basis with changes in baseflow, and over a daily cycle determined by pipe<br />

discharges primarily from the sewage treatment works. In addition to this temporal variation<br />

there is the spatial variation <strong>of</strong> discharge accretion that occurs progressively downstream. All<br />

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