Estimation of mixed soil water content by impedance inversion of GPR data

Jing Li, Z. Zeng, Lingna Chen, Fengshan Liu
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引用次数: 5

Abstract

In the vadose zone, soil has become an object of research due to its importance for environmental issues. Description and estimation of the mixed soil water content or dielectric parameter is the essential condition and the key to improving soil investigation with GPR detection. In this paper, first of all, a way to describe 3D random media which the preferred orientation of the multi-scale inhomogeneity is proposed and the importance of reducing the numerical errors with tapering function is stated. Then, we apply the FDTD method to simulate the GPR signal response of random model and use S-transform to test the simulation accuracy. For the complex random soil media, conventional method likes transmission wave method provide model parameter estimation of limited resolution only. Here, we apply a novel reflection amplitude inversion workflow for GPR data which is capable of resolving the subsurface dielectric permittivity and related water content distribution with markedly improved resolution. The synthetic results demonstrate that this method has extensive applicability in complex mixed random soil media detection and physics parameters estimation.
利用探地雷达数据阻抗反演估算混合土壤含水量
在渗透带中,土壤因其对环境问题的重要性而成为研究的对象。混合土壤含水量或介电参数的描述和估计是提高探地雷达探测土壤质量的必要条件和关键。本文首先提出了一种描述三维随机介质的方法,即多尺度非均匀性的优选方向,并指出了用锥形函数减小数值误差的重要性。然后,利用时域有限差分法对随机模型的探地雷达信号响应进行仿真,并利用s变换对仿真精度进行检验。对于复杂随机土体介质,传统的透射波法等方法只能提供有限分辨率的模型参数估计。本文采用了一种新的GPR数据反射振幅反演工作流程,该流程能够以显着提高的分辨率求解地下介电常数和相关含水量分布。综合结果表明,该方法在复杂混合随机土介质检测和物理参数估计中具有广泛的适用性。
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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