Abstract
ABSTRACTTo investigate transient dynamics of soil water redistribution during infiltration, we conducted horizontal borehole and surface ground penetrating radar measurements during a 4‐day infiltration experiment at the rhizontron facility in Selhausen, Germany. Zero‐offset ground penetrating radar profiling in horizontal boreholes was used to obtain soil water content information at specific depths (0.2, 0.4, 0.6, 0.8 and 1.2 m). However, horizontal borehole ground penetrating radar measurements do not provide accurate soil water content estimates of the top soil (0–0.1 m depth) because of interference between direct and critically refracted waves. Therefore, surface ground penetrating radar data were additionally acquired to estimate soil water content of the top soil. Due to the generation of electromagnetic waveguides in the top soil caused by infiltration, a strong dispersion in the ground penetrating radar data was observed in 500 MHz surface ground penetrating radar data. A dispersion inversion was thus performed with these surface ground penetrating radar data to obtain soil water content information for the top 0.1 m of the soil. By combining the complementary borehole and surface ground penetrating radar data, vertical soil water content profiles were obtained, which were used to investigate vertical soil water redistribution. Reasonable consistency was found between the ground penetrating radar results and independent soil water content data derived from time domain reflectometry measurements. Because of the improved spatial representativeness of the ground penetrating radar measurements, the soil water content profiles obtained by ground penetrating radar better matched the known water storage changes during the infiltration experiment. It was concluded that the combined use of borehole and surface ground penetrating radar data convincingly revealed spatiotemporal soil water content variation during infiltration. In addition, this setup allowed a better quantification of water storage, which is a prerequisite for future applications, where, for example, the soil hydraulic properties will be estimated from ground penetrating radar data.
Highlights
Characterizing soil water content (SWC) dynamics in unsaturated soil is important for a range of applications, including monitoring of pollutant transport (e.g. Binley et al, 2001),C 2020 The Authors
Near Surface Geophysics published by John Wiley & Sons Ltd on behalf of European Association of Geoscientists and Engineers., Near Surface Geophysics, 18, 275–294
The use of horizontal borehole ground penetrating radar (GPR) data alone failed to provide information on SWC changes of the top soil since the interpretation of borehole GPR measurements at 0.1 m depth was hindered by the interference of direct and critically refracted waves
Summary
Characterizing soil water content (SWC) dynamics in unsaturated soil is important for a range of applications, including monitoring of pollutant transport (e.g. Binley et al, 2001),C 2020 The Authors. Ground penetrating radar (GPR) is a popular hydrogeophysical method to investigate SWC dynamics because of its potentially high spatial resolution (Huisman et al, 2003a; Slob, Sato and Olhoeft, 2010; Binley et al, 2015) and the direct relationship between SWC and dielectric permittivity, which in turn determines the propagation of electromagnetic waves between GPR antennae. Due to the unclear penetration depth of the ground wave (Galagedara, Parkin and Redman, 2005b; Grote et al, 2010), it is, not possible to determine vertical SWC profiles from this type of GPR measurements.
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