Incorporating near-surface layering in GPR data inversion for improved surface water content estimates

K. Kooper, S. Lambot, E. Slob
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Abstract

We analyze the retrieval of soil surface dielectric permittivity in presence of shallow dielectric contrasts using full-wave inversion of off-ground monostatic ground-penetrating radar (GPR) data. Shallow soil layers affect the surface reflection and lead to constructive or destructive interferences which result, respectively, in overestimated and underestimated surface dielectric permittivity values. Synthetic GPR Green's functions were generated for a series of model configurations with different contrasts and different layer thicknesses. Green's function inversions were then performed to retrieve the initial parameters and analyze the sensitivity of the different parameters in the inverse problem. Two global optimization algorithms were used and compared, namely, a genetic algorithm and the multilevel coordinate search. The results showed that, depending on the contrast and layer thickness, it is not always possible to identify the original soil model. This depends in particular on the width of the frequency range. Both algorithms led to comparable results and did not converge properly in all cases, given their standard parameterization. Yet, the proposed method appears to be promising to improve real-time mapping of surface water content using off-ground GPR and full-wave inversion.
在探地雷达数据反演中结合近地表分层以改进地表水含量估算
利用地面单站探地雷达全波反演方法,分析了浅层介质对比条件下土壤表面介电常数的反演。浅层土层影响表面反射,并导致建设性或破坏性干扰,分别导致高估和低估表面介电常数值。生成了一系列不同对比度和不同层厚的模型构型的合成GPR格林函数。然后进行格林函数反演,检索初始参数,并分析不同参数在反问题中的敏感性。采用了遗传算法和多级坐标搜索两种全局优化算法,并进行了比较。结果表明,根据对比和层厚的不同,并不总是能够识别出原始的土壤模型。这尤其取决于频率范围的宽度。这两种算法的结果比较,并不是在所有情况下正确收敛,给定他们的标准参数化。然而,该方法似乎有望利用离地探地雷达和全波反演提高地表水含量的实时制图。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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