Soil moisture variability effect on GPR data

M. R. Ardekani, X. Neyt, D. Benedetto, E. Slob, B. Wesemael, P. Bogaert, C. Craeye, S. Lambot

Research output: Chapter in Book/Report/Conference proceedingConference contributionpeer-review

Abstract

In this paper the effect of local variability of soil moisture within the antenna footprint on GPR data is studied. A combination of GprMax3D with GPR full-wave model of Lambot and André (2013) is used for an errorless set of measurements. The GprMax3D simulations are used as real GPR measurements regarding several physical-based configurations. The Greens functions of the simulated data are extracted using calibrations based on GPR full-wave models. The inversion results of horizontal local soil moisture variability focusing on the surface wavelet reflection are compared with the averaged soil moisture values within different antenna footprints which led to the antenna footprint of -9 dB as the best. Finally, the inversion results of the vertical soil moisture variability shows significant effect of shallow soil moisture layering on the GPR-retrieved soil moisture values, which is highly correlated to the antenna height from the ground surface.

Original languageEnglish
Title of host publicationProceedings of the 15th International Conference on Ground Penetrating Radar, GPR 2014
EditorsLara Pajewski, Christophe Craeye, Antonis Giannopoulos, Frederic Andre, Sebastien Lambot, Evert Slob
PublisherInstitute of Electrical and Electronics Engineers Inc.
Pages214-217
Number of pages4
ISBN (Electronic)9781479967896
DOIs
Publication statusPublished - 1 Dec 2014
Event15th International Conference on Ground Penetrating Radar, GPR 2014 - Brussels, Belgium
Duration: 30 Jun 20144 Jul 2014

Publication series

NameProceedings of the 15th International Conference on Ground Penetrating Radar, GPR 2014

Conference

Conference15th International Conference on Ground Penetrating Radar, GPR 2014
Country/TerritoryBelgium
CityBrussels
Period30/06/144/07/14

Keywords

  • GprMax3D
  • Ground-penetrating radar
  • full-wave inversion
  • spatial soil moisture variability

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