1887
25th International Conference and Exhibition – Interpreting the Past, Discovering the Future
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

GPR in clay rich environments is often assumed to yield poor results due to signal attenuation, however it can still be possible to penetrate deep enough to reflect off targets of interest. Finding the bedrock level in an old quarry filled with clay and building rubble was successful using GPR reflection image profiling primarily due to the fact the fill material had previously been dewatered. Distinctive layers were observed in the fill material which when drilled corresponded to specific dominant material types. It appears the compaction level of the clay and the moisture content of the fill were important factors in the success of the GPR profile.

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/content/journals/10.1071/ASEG2016ab193
2016-12-01
2026-01-14
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References

  1. Conyers, L.B. 2004, Moisture and soil differences as related to the spatial accuracy of GPR amplitude maps at two archaeological test sites: 10th International conference on Ground Penetrating Radar, Delft, The Netherlands
  2. Jol, H. M and Bristow, C.S. 2003, GPR in sediments: advice on data collection, basic processing and inpretation, a good practice guide. In: Bristow, C.S, and Jol, H.M (eds) Ground Penetrating Radar in Sedimetns, Geological Society, London Special Publication, 211, 9-27.
  3. Renolds, J.M 1997, An introduction to Applied and Enviromental Geophsyics: John Wiley and Sons.
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  • Article Type: Research Article
Keyword(s): bedrock depth; clay; fill; GPR imaging
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