GPR profiling and electrical resistivity tomography for buried cavity detection: A test site at the abbaye de l'Ouye (France)

N. Boubaki, A. Saintenoy, P. Tucholka
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引用次数: 11

Abstract

The abbaye de l'Ouye (France) presents an underground room situated under a flat graveled path perfect for testing the complementarity of two geophysical methods, ground-penetrating radar (GPR) and electrical resistivity tomography (ERT), for buried cavity detection. One GPR mono-offset profile was acquired along with a 2D ERT profile on the surface above the cavity of known dimensions. We use our field site to test 2D ERT data acquisition and inversion parameters and how to complete GPR data information with ERT and vice-versa. As expected the mono-offset GPR profile contains strong reflections on the ceiling and the floor of the room. Arrival times of those reflections are translated to depth using classical GPR data processing techniques. The measured electrical apparent resistivities were inverted using the Loke (2001) software with three different options: i) no a priori information, ii) a priori information included as high resistivity value in an area determined from the GPR reflections, iii) a priori information included as boundary positions derived from the GPR reflections.
地下空腔探测用GPR剖面和电阻率层析成像:abbaye de l'Ouye的一个试验场(法国)
修道院de l'Ouye(法国)展示了一个位于平坦砾石路径下的地下房间,非常适合测试两种地球物理方法的互补性,即探地雷达(GPR)和电阻率断层扫描(ERT),用于地下空洞探测。在已知尺寸的空腔上方的表面上获得了一个GPR单偏移剖面和一个二维ERT剖面。我们利用我们的现场测试了二维ERT数据采集和反演参数,以及如何用ERT完成GPR数据信息,反之亦然。正如预期的那样,单偏移GPR剖面在房间的天花板和地板上包含强烈的反射。利用传统的探地雷达数据处理技术将这些反射的到达时间转换为深度。使用Loke(2001)软件对测量的视电阻率进行了反演,有三种不同的选择:i)没有先验信息,ii)由探地雷达反射确定的区域内作为高电阻率值的先验信息,iii)由探地雷达反射导出的边界位置的先验信息。
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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