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Quantification of groundwater recharge in the city of Nottingham, UK
Authors:Y Yang  D N Lerner  M H Barrett  J H Tellam
Institution:(1) Environmental Engineering Research Centre, Dept of Civil Engineering, Queen's University of Belfast, David Keir Building, Belfast BT7 1NN, UK, GB;(2) Groundwater Protection and Restoration Group, Dept. of Civil & Structural Engineering, University of Sheffield, Mappin Street, Sheffield S1 3JD, UK e-mail: d.n.lerner@sheffield.ac.uk, GB;(3) Robens Institute, University of Surrey, Guildford, Surrey, GU2 5XH, UK, GB;(4) School of Earth Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, UK, GB
Abstract: Groundwater is an important and valuable resource for water supply to cities. In order to make full and wise use of the asset value, a clear understanding of the quantities and sources of urban groundwater recharge is needed. The water supply and disposal network is often an important source of recharge to urban groundwater through leakage from water mains and sewers. An approach to establishing the spatial and temporal amounts of the three urban recharge sources (precipitation, mains and sewers) is developed and illustrated using the Nottingham (UK) urban aquifer. A calibrated groundwater flow model is supplemented by calibrated solute balances for three conservative species (Cl, SO4 and total N), thus providing four lines of evidence to use in the recharge estimation. Nottingham is located on a Triassic sandstone aquifer with average precipitation of 700 mm/year. Using the models, current urban recharge is estimated to be 211 mm/year, of which 138 mm/year (±40%) is from mains leakage and 10 mm/year (±100%) is from sewer leakage. The wide confidence intervals result from the scarcity of historical field data and the long turnover time in this high volume aquifer, and should be significantly lower for many other aquifer systems. Received: 1 December 1997 · Accepted: 14 September 1998
Keywords:  Solute balance  Urbanisation  Sewer and water supply leakage  Groundwater modelling  Triassic sandstone
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