Abstract

Full waveform inversion of ground-penetrating radar data is an emerging technique for the quantitative, high-resolution imaging of the near subsurface. Here, we present a 2-D frequency-domain full waveform inversion for the simultaneous reconstruction of the dielectric permittivity and of the electrical conductivity. The inverse problem is solved with a quasi-Newton optimization scheme, where the influence of the Hessian is approximated by the L-BFGS-B algorithm. This formulation can be considered to be fully multiparameter since it enables to update permittivity and conductivity values within the same descent step, provided we define scales of measurement through a reference permittivity, a reference conductivity, and an additional scaling factor. Numerical experiments on a benchmark from the literature demonstrate that the inversion is very sensitive to the parameter scaling, despite the consideration of the approximated Hessian that should correct for parameter dimensionalities. A proper scaling should respect the natural sensitivity of the misfit function and give priority to the parameter that has the most impact on the data (the permittivity, in our case). We also investigate the behaviour of the inversion with respect to frequency sampling, considering the selected frequencies either simultaneously or sequentially. As the relative imprint of permittivity and conductivity in the data varies with frequency, the simultaneous reconstruction of both parameters takes a significant benefit from broad frequency bandwidth data, so that simultaneous or cumulative strategies should be favoured. We illustrate our scaling approach with a realistic synthetic example for the imaging of a complex subsurface from on-ground multioffset data. Considering data acquired only from the ground surface increases the ill-posedness of the inverse problem and leads to a strong indetermination of the less-constrained conductivity parameters. A Tikhonov regularization can prevent the creation of high-wavenumber artifacts in the conductivity model that compensate for erroneous low-wavenumber structures, thus enabling to select model solutions. We propose a workflow for multiparameter imaging involving both parameter scaling and regularization. Optimal combinations of scaling factors and regularization weights can be identified by seeking regularization levels that exhibit a clear minimum of final data misfit with respect to parameter scaling. We confirm this workflow by inverting noise-contaminated synthetic data. In a surface-to-surface acquisition configuration, we have been able to reconstruct an accurate permittivity structure and a smooth version of the conductivity distribution, based entirely on the analysis of the data misfit with respect to parameter scaling, for different regularization levels.

Highlights

  • Ground-penetrating radar (GPR) is a non-invasive subsurface prospecting technique based on the propagation of electromagnetic waves

  • Efforts have been oriented towards quantitative GPR imaging using multioffset measurements with velocity analysis (e.g. Fischer et al 1992a), amplitude-versus-offset studies (e.g. Deeds & Bradford 2002; Deparis & Garambois 2009), traveltime and amplitude tomography (Cai et al 1996; Holliger et al 2001; Gloaguen et al 2005; Musil et al 2006), and full waveform inversion (FWI)

  • We have presented a FWI algorithm of on-ground GPR data for the simultaneous reconstruction of permittivity and conductivity in 2-D

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Summary

INTRODUCTION

Ground-penetrating radar (GPR) is a non-invasive subsurface prospecting technique based on the propagation of electromagnetic waves. Deeds & Bradford 2002; Deparis & Garambois 2009), traveltime and amplitude tomography (Cai et al 1996; Holliger et al 2001; Gloaguen et al 2005; Musil et al 2006), and full waveform inversion (FWI) The latter is one of the most promising techniques for building quantitative, high-resolution images of the subsurface. Only Lopes (2009) and El Bouajaji et al (2011) tackle the interpretation of surface-based GPR measurements for the quantitative imaging of 2-D sections of the medium These authors restrict themselves to monoparameter inversions, reconstructing only the permittivity distribution. We propose a FWI method for the simultaneous inversion of permittivity and conductivity in 2-D, with a particular interest in data acquired in surface-to-surface multioffset configuration (on-ground GPR). Noise will be introduced in the data in order to investigate the feasibility of such approach for future real data inversion

Forward problem
Inverse problem
M U LT I PA RAMETERIM AG INGOF PERMITTIVITY AND CONDUCTIVITY
Parameter scaling
A REALISTIC SYNTHETIC TEST
Benchmark design
DISCUSSION
CONCLUSION
Full Text
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