GPR Full-waveform Inversion of Horizontal ZOP Borehole Data Using GprMax

被引:0
作者
Klotzsche, A. [1 ]
van der Kruk, J. [1 ]
He, G. [1 ]
Vercecken, H. [1 ]
机构
[1] Forschungszentrum Julich, Inst Bio & Geosci, Agrosphere, HPSC TerrSys,ABC J Geoverbund, Julich, Germany
来源
PROCEEDINGS OF 2016 16TH INTERNATIONAL CONFERENCE ON GROUND PENETRATING RADAR (GPR) | 2016年
关键词
Full-waveform inversion; Hydrogeophysics; source wavelet estimation; shuffle complex evolution; GROUND-PENETRATING RADAR;
D O I
暂无
中图分类号
TM [电工技术]; TN [电子技术、通信技术];
学科分类号
0808 ; 0809 ;
摘要
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 in and 0.2 in 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.
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页数:5
相关论文
共 11 条
[1]  
Busch S, 2012, GEOPHYSICS, V77, pH79, DOI [10.1190/geo2012-0045.1, 10.1190/GEO2012-0045.1]
[2]   EFFECTIVE AND EFFICIENT GLOBAL OPTIMIZATION FOR CONCEPTUAL RAINFALL-RUNOFF MODELS [J].
DUAN, QY ;
SOROOSHIAN, S ;
GUPTA, V .
WATER RESOURCES RESEARCH, 1992, 28 (04) :1015-1031
[3]   Application of a new 2D time-domain full-waveform inversion scheme to crosshole radar data [J].
Ernst, Jacques R. ;
Green, Alan G. ;
Maurer, Hansruedi ;
Holliger, Klaus .
GEOPHYSICS, 2007, 72 (05) :J53-J64
[4]   Modelling ground penetrating radar by GprMax [J].
Giannopoulos, A .
CONSTRUCTION AND BUILDING MATERIALS, 2005, 19 (10) :755-762
[5]   Imaging and characterization of facies heterogeneity in an alluvial aquifer using GPR full-waveform inversion and cone penetration tests [J].
Gueting, Nils ;
Klotzsche, Anja ;
van der Kruk, Jan ;
Vanderborght, Jan ;
Vereecken, Harry ;
Englert, Andreas .
JOURNAL OF HYDROLOGY, 2015, 524 :680-695
[6]   Chlorides and moisture assessment in concrete by GPR full waveform inversion [J].
Kalogeropoulos, A. ;
van der Kruk, J. ;
Hugenschmidt, J. ;
Busch, S. ;
Merz, K. .
NEAR SURFACE GEOPHYSICS, 2011, 9 (03) :277-285
[7]  
Keskinen J., APPL GEOPHYS UNPUB
[8]   3-D characterization of high-permeability zones in a gravel aquifer using 2-D crosshole GPR full-waveform inversion and waveguide detection [J].
Klotzsche, Anja ;
van der Kruk, Jan ;
Linde, Niklas ;
Doetsch, Joseph ;
Vereecken, Harry .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2013, 195 (02) :932-944
[9]   Full-waveform inversion of cross-hole ground-penetrating radar data to characterize a gravel aquifer close to the Thur River, Switzerland [J].
Klotzsche, Anja ;
van der Kruk, Jan ;
Meles, Giovanni Angelo ;
Doetsch, Joseph ;
Maurer, Hansruedi ;
Linde, Niklas .
NEAR SURFACE GEOPHYSICS, 2010, 8 (06) :635-649
[10]   A New Vector Waveform Inversion Algorithm for Simultaneous Updating of Conductivity and Permittivity Parameters From Combination Crosshole/Borehole-to-Surface GPR Data [J].
Meles, Giovanni Angelo ;
Van der Kruk, Jan ;
Greenhalgh, Stewart A. ;
Ernst, Jacques R. ;
Maurer, Hansruedi ;
Green, Alan G. .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2010, 48 (09) :3391-3407