Cross well radar and vertical radar profiling methods for time lapse monitoring of rainfall infiltration

The relationship between electromagnetic velocities derived from in-hole radar surveying and soil saturation can be exploited to map changes in recharge from rainfall infiltration in the vadose zone against time. We have completed time-lapse cross-well radar and vertical radar Profiling (VRP) experi...

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Published inASEG Extended Abstracts Vol. 2012; no. 1; pp. 1 - 4
Main Authors Strobach, Elmar, Harris, Brett D., Christian Dupuis, J., Kepic, Anton W., Martin, Michael W.
Format Journal Article
LanguageEnglish
Published Taylor & Francis 01.12.2012
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Abstract The relationship between electromagnetic velocities derived from in-hole radar surveying and soil saturation can be exploited to map changes in recharge from rainfall infiltration in the vadose zone against time. We have completed time-lapse cross-well radar and vertical radar Profiling (VRP) experiments with the objective of monitoring rainfall infiltration during the winter season at two sites on the Gnangara Mound in the Perth Basin, Western Australia. Depth-velocity profiles have been derived from the direct transmission measurements. Results obtained from Vertical Radar Profiling and Zero vertical offset cross well profiling are evaluated and the influence of different geometries and test-site conditions are discussed. We find that zero vertical offset cross well radar experiments were highly repeatable. Further changes in ground conditions such as an increase in moisture content can be observed with great confidence. The interpretation of vertical radar profiles was more challenging. However both techniques successfully reveal the time-lapse response of water migrating through the unsaturated soil profile for the two trial sites.
AbstractList The relationship between electromagnetic velocities derived from in-hole radar surveying and soil saturation can be exploited to map changes in recharge from rainfall infiltration in the vadose zone against time. We have completed time-lapse cross-well radar and vertical radar Profiling (VRP) experiments with the objective of monitoring rainfall infiltration during the winter season at two sites on the Gnangara Mound in the Perth Basin, Western Australia. Depth-velocity profiles have been derived from the direct transmission measurements. Results obtained from Vertical Radar Profiling and Zero vertical offset cross well profiling are evaluated and the influence of different geometries and test-site conditions are discussed. We find that zero vertical offset cross well radar experiments were highly repeatable. Further changes in ground conditions such as an increase in moisture content can be observed with great confidence. The interpretation of vertical radar profiles was more challenging. However both techniques successfully reveal the time-lapse response of water migrating through the unsaturated soil profile for the two trial sites.
Author Strobach, Elmar
Martin, Michael W.
Christian Dupuis, J.
Kepic, Anton W.
Harris, Brett D.
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  givenname: Elmar
  surname: Strobach
  fullname: Strobach, Elmar
  email: elmar.strobach@postgrad.curtin.edu.au
  organization: Dept. of Exploration Geophysics, Curtin University
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  givenname: Brett D.
  surname: Harris
  fullname: Harris, Brett D.
  organization: Dept. of Exploration Geophysics, Curtin University
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  givenname: J.
  surname: Christian Dupuis
  fullname: Christian Dupuis, J.
  organization: Dept. of Exploration Geophysics, Curtin University
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  givenname: Anton W.
  surname: Kepic
  fullname: Kepic, Anton W.
  organization: Dept. of Exploration Geophysics, Curtin University
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  givenname: Michael W.
  surname: Martin
  fullname: Martin, Michael W.
  organization: Water Corporation Ltd
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SubjectTerms Vertical Radar Profiling
water infiltration
Zero vertical offset crosswell Profiling
Title Cross well radar and vertical radar profiling methods for time lapse monitoring of rainfall infiltration
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