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

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REVIEW<br />

investigated the transport and fate <strong>of</strong> Fe, Mn, Cu, Zn, Cd, Pb and SO4 in a <strong>ground<strong>water</strong></strong> plume<br />

and in the downstream <strong>surface</strong> <strong>water</strong>s in the Coeur d’Alene Mining District in the US. He<br />

found that <strong>upon</strong> mixing with higher pH <strong>surface</strong> <strong>water</strong> the metals were lost from solution in the<br />

following order: Fe>Al>Pb>Cu>Mn>Zn> Cd. Less than 10% <strong>of</strong> the dissolved Zn and Cd<br />

were lost, despite a 5 km journey through both the <strong>ground<strong>water</strong></strong> and <strong>surface</strong> <strong>water</strong> regimes.<br />

Paulson and Balistrieri (1999) used model simulations and laboratory experiments to examine<br />

the removal <strong>of</strong> Cd, Cu, Pb and Zn in acidic <strong>ground<strong>water</strong></strong> during neutralisation by ambient<br />

<strong>surface</strong> <strong>water</strong>s. <strong>The</strong>y concluded that hydrous Fe oxides and particulate organic carbon are<br />

more important than hydrous Al oxides in removing metals from the <strong>ground<strong>water</strong></strong>. Tessier et<br />

al. (1996) found that trace metals present in <strong>water</strong> influent to two lakes in Canada sorbed<br />

directly to the OH functional groups <strong>of</strong> iron and manganese oxyhroxides and organic matter<br />

found in the lake sediments. Kuwabara et al. (1999) found that <strong>water</strong> flowing through the bed<br />

<strong>of</strong> lake Coeur d’Alene caused a significant flux <strong>of</strong> metal from the lake sediments to the <strong>water</strong><br />

column.<br />

2.2.2 Flow Studies<br />

<strong>The</strong> <strong>ground<strong>water</strong></strong> support <strong>of</strong> river baseflow and its relationship to the underlying geology has<br />

has long been recognised and studied (Meyboom, 1961, Mau et al., 1993, Pinder et al., 1969,<br />

O’Conner 1976,). Several studies have investigated the relationship between reduced <strong>surface</strong><br />

<strong>water</strong> flows and increased levels <strong>of</strong> <strong>ground<strong>water</strong></strong> abstraction (Sophocleous 2000). A<br />

comprehensive study on the interaction <strong>of</strong> the Equus Beds alluvial aquifer and the Arkansas<br />

River, USA, found that abstraction for irrigation significantly reduced river baseflow levels<br />

and induced <strong>surface</strong> <strong>water</strong> seepage into the aquifer (Ziegler et al., 2001). <strong>The</strong> response <strong>of</strong><br />

<strong>ground<strong>water</strong></strong> to transient <strong>surface</strong> <strong>water</strong> levels has been used to derive estimates <strong>of</strong> the aquifer<br />

property S/T (Reynolds, 1987, Workman et al., 1997, Erskine 1991). Devito et al. (1996)<br />

18

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