GPR clutter modeling taking into account soil heterogeneity

Kazunori Takahashi, J. Igel, H. Preetz
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Abstract

In small-scale measurements, a ground-penetrating radar (GPR) is often used with a higher frequency to detect a small object or changes in the ground. GPR becomes more sensitive to the heterogeneity of soil when a higher frequency is used. Soil heterogeneity scatters electromagnetic waves and the scattered waves are observed as unwanted reflections that are often referred to as clutter. Data containing high amplitude clutter are difficult to analyze and interpret because clutter disturbs reflections from objects to be detected. Therefore, modeling GPR clutter is useful to assess the effectiveness of GPR measurements. The authors have developed and demonstrated such a technique with data acquired during an infiltration experiment. In this study, the technique was applied to GPR and time domain reflectometry (TDR) data repeatedly acquired on an outdoor test site for a few months. The modeling results using the TDR data are similar to the clutter power directly extracted from the GPR data. Therefore, the technique works although it requires some modifications for more accurate modeling.
考虑土壤非均质性的探地雷达杂波建模
在小规模测量中,探地雷达(GPR)通常使用较高的频率来探测地面的小物体或变化。当使用较高的频率时,探地雷达对土壤的非均质性更加敏感。土壤的非均质性使电磁波散射,而这些散射波被观测为不需要的反射,通常被称为杂波。含有高振幅杂波的数据很难分析和解释,因为杂波会干扰被探测物体的反射。因此,建立探地雷达杂波模型有助于评估探地雷达测量的有效性。作者已经开发并演示了这种技术与在渗透实验中获得的数据。在本研究中,该技术应用于在室外试验点重复获取的探地雷达和时域反射(TDR)数据,持续数月。利用TDR数据的建模结果与直接从探地雷达数据中提取的杂波功率相似。因此,该技术是有效的,尽管它需要一些修改以获得更准确的建模。
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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