TY - GEN
T1 - GPR full-waveform inversion of horizontal ZOP borehole data using GprMax
AU - Klotzsche, A.
AU - Van Der Kruk, J.
AU - He, G.
AU - Vereecken, H.
N1 - Publisher Copyright:
© 2016 IEEE.
Copyright:
Copyright 2017 Elsevier B.V., All rights reserved.
PY - 2016/9/20
Y1 - 2016/9/20
N2 - Full-waveform inversion of GPR data has shown a high potential in many applications to obtain accurate and quantitative high resolution images of the subsurface. We implemented a new full-waveform inversion that combines an accurate 3D forward modeling approach with a shuffled complex evolution method that incorporates the complicated wave interactions and interferences that cannot be resolved by standard processes. This new approach is applied to zero-offset profile GPR data that were acquired in horizontal boreholes to monitor soil water content and water uptake by roots under different soil and treatment conditions. Using standard ray-based processing methods, the determined permittivity values close to the surface were not reliable due to interferences from the critically refracted air wave and the direct wave through the subsurface. Synthetic studies showed that traces at depths 0.1 m and 0.2 m are affected by these interferences and hence no reliable permittivity values and soil water content values can be obtain by standard ray-based approaches. The new full-waveform inversion was used to obtain reliable permittivity and soil water content results for three different treatment plots and six different depth positions between 0.06-1.16m of the horizontal boreholes. The inverted results show a good fit with the observed data and quantitative permittivity results were obtained for all depths.
AB - Full-waveform inversion of GPR data has shown a high potential in many applications to obtain accurate and quantitative high resolution images of the subsurface. We implemented a new full-waveform inversion that combines an accurate 3D forward modeling approach with a shuffled complex evolution method that incorporates the complicated wave interactions and interferences that cannot be resolved by standard processes. This new approach is applied to zero-offset profile GPR data that were acquired in horizontal boreholes to monitor soil water content and water uptake by roots under different soil and treatment conditions. Using standard ray-based processing methods, the determined permittivity values close to the surface were not reliable due to interferences from the critically refracted air wave and the direct wave through the subsurface. Synthetic studies showed that traces at depths 0.1 m and 0.2 m are affected by these interferences and hence no reliable permittivity values and soil water content values can be obtain by standard ray-based approaches. The new full-waveform inversion was used to obtain reliable permittivity and soil water content results for three different treatment plots and six different depth positions between 0.06-1.16m of the horizontal boreholes. The inverted results show a good fit with the observed data and quantitative permittivity results were obtained for all depths.
KW - Full-waveform inversion
KW - Hydrogeophysics
KW - Shuffle complex evolution
KW - Source wavelet estimation
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U2 - 10.1109/ICGPR.2016.7572695
DO - 10.1109/ICGPR.2016.7572695
M3 - Conference contribution
AN - SCOPUS:84992109361
T3 - Proceedings of 2016 16th International Conference of Ground Penetrating Radar, GPR 2016
BT - Proceedings of 2016 16th International Conference of Ground Penetrating Radar, GPR 2016
PB - Institute of Electrical and Electronics Engineers Inc.
T2 - 16th International Conference of Ground Penetrating Radar, GPR 2016
Y2 - 13 June 2016 through 16 June 2016
ER -