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

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STUDY SETTING<br />

dry cleaning industry. Sorption experiments indicate the low organic carbon contents, from<br />

core analyses, are not a dominant factor in the transport <strong>of</strong> organic contaminants within the<br />

aquifer (Shepherd., 2002).<br />

3.7 Summary<br />

<strong>The</strong> Birmingham and West Midlands region has a long industrial history dating back to the<br />

beginnings <strong>of</strong> the industrial revolution in 1800, and this, together with <strong>urban</strong> development,<br />

has led to widespread contamination <strong>of</strong> the <strong>ground<strong>water</strong></strong>. Previous work has identified<br />

inorganic contaminants within the Birmingham Aquifer, including heavy metals and organic<br />

contaminants, primarily chlorinated solvents. This industrial footprint on the <strong>urban</strong><br />

<strong>ground<strong>water</strong></strong> in the Birmingham area, and its implications for future river basin management<br />

and protection policy, warrants further investigation, hence the rationale for my research.<br />

<strong>The</strong> River Tame was selected for study because it runs from east to west through the heart <strong>of</strong><br />

the <strong>urban</strong>/industrial area, and because some <strong>of</strong> the contaminated <strong>ground<strong>water</strong></strong> within the Tame<br />

Valley discharges to the river. A 23.8 km stretch <strong>of</strong> the Tame was chosen for the study as it is<br />

known to receive an increased (20%) inflow <strong>of</strong> <strong>ground<strong>water</strong></strong>, in particular, along a 7.4 km<br />

section that flows over the Birmingham Aquifer. This section was targeted for a detailed study<br />

<strong>of</strong> the contaminant flux via <strong>ground<strong>water</strong></strong> to the river. In addition to the bedrock aquifer, there<br />

is <strong>ground<strong>water</strong></strong> flow to the river through the alluvial gravels deposited on the flood plain.<br />

Site selection was also based on the fact that the 23.8 km reach <strong>of</strong> the Tame is conveniently<br />

delimited by two gauging stations, Bescot at the upstream limit and Water Orton downstream.<br />

55

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