Measuring the soil water content profile of a sandy soil with an off-ground monostatic ground penetrating radar

article
We explore the possibility of measuring a continuously variable soil moisture profile by inversion of a ground penetrating radar (GPR) signal. Synthetic experiments were conducted to demonstrate the well- posedness of the inverse problem for the specific case of identifying a soil moisture profile in hydrostatic equilibrium with a water table. In this case, the profile agrees with the water retention curve of the soil. The analysis subsequently extends to an actual case study in con- trolled outdoor conditions on a large tank filled with sand. Due to the presence of a discontinuity in the actual dielectric profile, inversion of the continuous model (Model 1) led to poor results. Only the surface soil moisture was well estimated. Including the observed dis- continuity in the model (Model 2) led to a good estimation of the water content profile. Finally, we observed that the surface water con- tent can be accurately estimated using a simplified three-layer model (Model 3). Generally, the observed confidence intervals on the esti- mated parameters are large, which denotes a lack of model sensitivity to the soil parameters. We attributed the low sensitivity to the high operating frequency range. Lower frequencies would have been re- quired to obtain more information from the larger depths. Never- theless, high frequencies allowed for an accurate estimation of the surface soil moisture, which offers particularly promising perspec- tives in humanitarian demining and agricultural applications. © Soil Science Society of America.
TNO Identifier
953736
ISSN
15391663
Source
Vadose Zone Journal, 3(4), pp. 1063-1071.
Pages
1063-1071
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