2019
DOI: 10.1016/j.jappgeo.2019.103823
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GPR full-waveform inversion of a variably saturated soil-aquifer system

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Cited by 15 publications
(4 citation statements)
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“…Ground penetrating radar is highly effective and accurate for interpreting the results, but its detection depth is limited under the technical limitations of the method itself, for example, the transmitting power is relatively small compared to the MT method. As a result, one cannot address the goaf with the depth of >100 m by using GPR (Cheng et al, 2010;Klotzsche et al, 2019;Ozkaya et al, 2021). Compared with other methods, transient electromagnetic method (TEM) is notably advantageous for detecting water-bearing coal goaf.…”
Section: Introductionmentioning
confidence: 99%
“…Ground penetrating radar is highly effective and accurate for interpreting the results, but its detection depth is limited under the technical limitations of the method itself, for example, the transmitting power is relatively small compared to the MT method. As a result, one cannot address the goaf with the depth of >100 m by using GPR (Cheng et al, 2010;Klotzsche et al, 2019;Ozkaya et al, 2021). Compared with other methods, transient electromagnetic method (TEM) is notably advantageous for detecting water-bearing coal goaf.…”
Section: Introductionmentioning
confidence: 99%
“…In 2019, Klotzsche, Anja et al, using crosshole GPR full-waveform inversion to visualize a soil aquifer system with variable saturation in critical regions, estimated four effective source wavelets with different source wavelets during inversion depending on the transmitter and receiver present in the saturated and/or unsaturated regions. Experiments have shown that this method can be used for imaging over the entire depth range starting from critical regions and can be applied to a wide range of applications [30]. Full waveform inversion is often used to estimate the geophysical parameters of recorded waveforms (observations) and is often expressed as a least squares optimization problem, but least squares FWI has a cycle jump problem.…”
Section: Introductionmentioning
confidence: 99%
“…It is at present not standard procedure to model antennae explicitly and it is therefore necessary to estimate a source wavelet, which is typically assumed constant for a given survey. Furthermore, the FWI results depend heavily on the choice of starting model (e.g., Klotzsche, Vereecken, & van der Kruk, 2019; Z. Zhou et al., 2021), as the method requires a starting model that fulfills that its forward response lies within half a period of the observed waveform data to enable global convergence of the algorithm (G. Meles et al., 2011). The estimated structures in the dielectrical permittivity tomograms are considered more reliable than the conductivity tomograms, as investigated in Oberröhrmann et al.…”
Section: Introductionmentioning
confidence: 99%