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The use of electrical resistivity tomography in deriving local-scale models of recharge through superficial deposits

M.O. Cuthbert, R. Mackay, J.H. Tellam and R.D. Barker
Quarterly Journal of Engineering Geology and Hydrogeology, 42, 199-209, 2 June 2009, https://doi.org/10.1144/1470-9236/08-023
M.O. Cuthbert
Hydrogeology Research Group, School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham B15 2TT, UK
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R. Mackay
Hydrogeology Research Group, School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham B15 2TT, UK
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J.H. Tellam
Hydrogeology Research Group, School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham B15 2TT, UK
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R.D. Barker
Hydrogeology Research Group, School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham B15 2TT, UK
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Abstract

Abstract The way in which superficial deposits affect groundwater recharge is often a significant source of uncertainty in groundwater resources and vulnerability assessments. A study of a small catchment in Shropshire, UK, shows how electrical resistivity tomography (ERT), with a degree of borehole control, can be an effective tool for defining the geometry of superficial deposits for purposes of inferring the hydraulic processes controlling groundwater recharge. Major lithological units were mapped to within c. 0.5 m vertically and 5 m horizontally using ERT surveys with a minimum electrode spacing of 2 m. Interpretation was aided by the strong contrast in resistivity between till and glaciolacustrine deposits (20–40 Ω m) and glaciofluvial deposits (generally >100 Ω m) that overlie the Permo-Triassic sandstone aquifer (saturated resistivity 60–145 Ω m) in the study area. A range of local-scale (tens to hundreds of metres) recharge models are presented, based on the findings of the field surveys, and it is shown how existing mapping misses key features of the superficial geology that may be very significant in enhancing or restricting aquifer recharge.

  • © 2009 Geological Society of London
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Quarterly Journal of Engineering Geology and Hydrogeology: 42 (2)
Quarterly Journal of Engineering Geology and Hydrogeology
Volume 42, Issue 2
May 2009
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The use of electrical resistivity tomography in deriving local-scale models of recharge through superficial deposits

M.O. Cuthbert, R. Mackay, J.H. Tellam and R.D. Barker
Quarterly Journal of Engineering Geology and Hydrogeology, 42, 199-209, 2 June 2009, https://doi.org/10.1144/1470-9236/08-023
M.O. Cuthbert
Hydrogeology Research Group, School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham B15 2TT, UK
  • Find this author on Google Scholar
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  • For correspondence: m.cuthbert@bham.ac.uk
R. Mackay
Hydrogeology Research Group, School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham B15 2TT, UK
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J.H. Tellam
Hydrogeology Research Group, School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham B15 2TT, UK
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R.D. Barker
Hydrogeology Research Group, School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham B15 2TT, UK
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The use of electrical resistivity tomography in deriving local-scale models of recharge through superficial deposits

M.O. Cuthbert, R. Mackay, J.H. Tellam and R.D. Barker
Quarterly Journal of Engineering Geology and Hydrogeology, 42, 199-209, 2 June 2009, https://doi.org/10.1144/1470-9236/08-023
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