Evaluation of starting model approaches and effective source wavelet variations for high-frequency ground-penetrating radar full-waveform inversion

被引:0
|
作者
Hoven, Dominik [1 ,2 ]
Mester, Achim [3 ]
Vereecken, Harry [1 ,2 ]
Klotzsche, Anja [1 ,2 ]
机构
[1] Forschungszentrum Julich, Institue Bioand Geosci, IBG 3 Agrosphere, Julich, Germany
[2] Geoverbund ABC J, Ctr High Performance Sci Comp Terr Syst TerrSys, Julich, Germany
[3] Forschungszentrum Julich, Cent Inst Engn Elect & Analyt, ZEA 2 Elect Syst, Julich, Germany
关键词
ELECTRICAL-RESISTIVITY TOMOGRAPHY; SOIL-WATER CONTENT; AQUIFER CHARACTERIZATION; GPR DATA; PERMITTIVITY; CONDUCTIVITY; ALGORITHM;
D O I
10.1190/GEO2021-0683.1
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
High-frequency ground-penetrating radar (GPR) full -wave-form inversion (FWI) can enhance the characterization of small-scale structures in the subsurface below the decimeter scale. We have investigated the potential and requirements to use FWI for higher-frequency data. Thereby, we focus on the two most important criteria to achieve reliable FWI results: ad-equate starting models that fulfill the half-wavelength criterion and the accuracy of the effective source wavelet. Therefore, we have defined a realistic reference model, generated synthetic GPR data sets (200, 450, and 700 MHz), and tested different standard ray-based starting model methods and frequency -hop-ping approaches to derive results close to our reference model. Although standard starting models provide good parameter reconstruction for lower-frequency data, a frequency-hopping approach is required for the 700 MHz data. In addition, we have seen that the reconstruction of the conductivity results is more sensitive to the presence of noise (25 dB) than the per-mittivity tomograms. The definition of the effective source wavelets is directly linked to the accuracy of the starting models; therefore, we investigate the effect on the FWI results for high -frequency data by varying the source wavelets in terms of start-ing time and/or amplitude. Considering the multiparameter nature of FWI, we observe that time shifts have a greater influ-ence on the performance of the FWI than amplitude variations. Large time shifts of approximately 0.1 ns for the 700 MHz data may lead to the failure of the inversion, whereas amplitude var-iations (+/- 5% of the maximum amplitude) affect the quantita-tive conductivity results only (no effect on permittivity) with an increased root-mean-square error of the data of up to 20%. Using a stochastically perturbed synthetic model, we de-termine an improved parameter reconstruction for higher frequencies. On the basis of our findings, we develop a work-flow to obtain reliable results for high-frequency GPR FWI for future users.
引用
收藏
页码:KS27 / KS45
页数:19
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