基于本征模的钻孔探地雷达测层状土壤复介电常数方法

R. Showalter-Bucher, J. M. Martinez Lorenzo, C. Rappaport
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引用次数: 0

摘要

钻孔探地雷达系统探测地表以下不同深度,以确定土壤性质并寻找异常情况。目前的检测方法使用飞行时间估计或断层扫描来确定土壤的性质。这些方法使用了一个不准确的假设,即信号在层状土壤介质中从发射器到接收器以直接的路径传播。我们提出了一种新的特征模方法,类似于介质波导分析,以估计土层边界,介电常数和电导率,考虑到波在层状介质中的真实传播。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Eigenmode-based method to determine the complex permittivities of layered soil via a borehole ground penetrating radar
Borehole ground penetrating radar systems probe at varying depths below the surface to determine soil properties and search for anomalies. Current detection approaches use time of flight estimations or tomography to determine the properties of the soil. These methods use the inaccurate assumption that the signal propagates in a straight direct path from transmitter to receiver in layered soil media. We propose a novel eigenmode method, similar to dielectric waveguide analysis, to estimate soil layer boundaries, permittivity, and conductivity, taking into account the true propagation of waves in layered medium.
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