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

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WATER QUALITY INTERACTIONS<br />

attenuation will decrease contaminant concentrations but this is partially dependent on travel<br />

times, and the least amount <strong>of</strong> attenuation will occur for contaminants with sources close to<br />

the river. <strong>The</strong> high concentration plumes detected in this study may have sources within 100<br />

m <strong>of</strong> the river where the protection afforded by the unsaturated zone is least.<br />

Mixing <strong>of</strong> <strong>ground<strong>water</strong></strong> from different origins may occur in the focussed discharge zone<br />

around the river, and this would cause dilution <strong>of</strong> contaminant concentrations. In some<br />

instances, a substantial variation was observed in the composition <strong>of</strong> <strong>water</strong>s discharging from<br />

opposite banks, and this together with further variations in concentrations observed across the<br />

riverbed may reflect the culmination <strong>of</strong> other <strong>water</strong> types from a variety <strong>of</strong> flow paths. <strong>The</strong><br />

vertical extent <strong>of</strong> the active <strong>ground<strong>water</strong></strong> system is unknown but modelling indicates that the<br />

deeper <strong>ground<strong>water</strong></strong> does not discharge to the river. <strong>The</strong> older <strong>ground<strong>water</strong></strong> from depth would<br />

be expected to discharge through the middle <strong>of</strong> the channel and younger, shallower<br />

<strong>ground<strong>water</strong></strong>, through the riverbanks, but the chemical data set is insufficient to confirm this.<br />

<strong>The</strong> similarities in <strong>water</strong> quality between the shallow and the riverbed piezometers are greater<br />

than between the abstraction wells and the riverbed piezometers, implying that the majority <strong>of</strong><br />

<strong>ground<strong>water</strong></strong> discharging to the river is <strong>of</strong> relatively shallow origin.<br />

Interaction between <strong>ground<strong>water</strong></strong> and <strong>surface</strong> <strong>water</strong>s was observed in multilevel piezometers<br />

using the concentration gradient between high levels <strong>of</strong> chloride in the <strong>surface</strong> <strong>water</strong> and<br />

usually lower levels in the <strong>ground<strong>water</strong></strong>. <strong>The</strong> maximum observed depth <strong>of</strong> <strong>surface</strong> <strong>water</strong><br />

penetration into the riverbed was

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