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

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2.3.1 UK Legislation<br />

REVIEW<br />

<strong>The</strong> new Water Framework Directive (Council <strong>of</strong> Europe, 2000, Environment Agency, 2002)<br />

has been introduced to ensure an integrated approach to the management <strong>of</strong> catchment <strong>surface</strong><br />

and <strong>ground<strong>water</strong></strong> quality and flow. Consultations are under way in the UK on the<br />

implementation <strong>of</strong> this directive (DEFRA, 2002). It will be implemented in conjunction with<br />

other legislation such as Part IIa <strong>of</strong> the Environmental Protection Act 1990 designed to<br />

maintain and improve the quality <strong>of</strong> <strong>surface</strong> and <strong>ground<strong>water</strong></strong>. Under the legislation, the<br />

<strong>impact</strong> <strong>of</strong> land causing pollution <strong>of</strong> controlled <strong>water</strong>s must be assessed by comparison to the<br />

background <strong>water</strong> quality and suitable standards such as drinking <strong>water</strong> and environmental<br />

quality standards (EQS) for <strong>surface</strong> <strong>water</strong>s (Smith, 2002). Contaminated land and<br />

contaminated <strong>ground<strong>water</strong></strong>s arising, where found to cause significant <strong>impact</strong>s on the <strong>surface</strong><br />

<strong>water</strong> are likely to require remedial action (Rivett et al., 2002).<br />

2.4 Monitoring methods<br />

Comprehensive reviews <strong>of</strong> the existing analytical, numerical, field and chemical investigative<br />

techniques for <strong>ground<strong>water</strong></strong>/<strong>surface</strong> <strong>water</strong> interactions have been carried out by HRU (2001)<br />

and Winter (1995). On the catchment scale, the most widely-used approach is river<br />

hydrograph separation and baseflow recession analyses to derive the <strong>ground<strong>water</strong></strong> component<br />

<strong>of</strong> river flow (Meyboom, 1961, Mau et al., 1997, Gustard et al., 1992). Several workers<br />

(Pinder et al., 1969, O’Conner 1976, Birtles 1978) have used differences in <strong>ground<strong>water</strong></strong> and<br />

<strong>surface</strong> <strong>water</strong> chemistry and total dissolved solids to resolve further the <strong>ground<strong>water</strong></strong><br />

component <strong>of</strong> the river hydrographs. At the smaller scale <strong>of</strong> the river reach, stream tracers<br />

22

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