GPR and ERT combined analysis on the basis of advanced wavelet methodology: The Montagnole testing area

L. Alperovich, L. Eppelbaum, J. Dumoulin, V. Zheludev, F. Soldovieri, M. Proto, M. Bavusi, A. Loperte
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Abstract

Ground Penetrating Radar (GPR) and Electric Resistivity Tomography (ERT) are well assessed and accurate geophysical methods for the investigation of subsurface geological sections. In this paper, we present the joint exploitation of these methods al the Montagnole (French Alps) experimental site with the final aim to study and monitor effects of possible catastrophic rockslides in transport infrastructures. It is known that factors as the ambiguity of geophysical field examination, the complexity of geological scenarios, and the low signal-to-noise ratio affect the possibility to build reliable physical-geological models of the investigated subsurface structure. Here, we applied for the GPR and ERT methods at Montagnole site, the recent advances in the wavelet theory and data mining. Wavelet approach was specifically used to achieve enhanced (e.g., coherence portraits) images resulting from the integration of the different geophysical fields. This methodology based on the matching pursuit combined with wavelet packet dictionaries permitted us to extract desired signals in different physical-geological conditions, even in presence of strongly noised data. Such tools as complex wavelets were employed to the coherence portraits, combined GPR-ERT coherency orientation angle, to name a few, enable performing non-conventional operations of integration and correlation in subsurface geophysics. The estimation of the above mentioned parameters proved useful not only for location of buried inhomogeneties but also for a rough estimation of their electromagnetic and related properties. Therefore, the combination of the above approaches has allowed to set-up a novel methodology, which may enhance reliability and confidence of each separate geophysical method and their integration.
基于先进的小波方法进行 GPR 和 ERT 综合分析:蒙塔格诺尔试验区
探地雷达(GPR)和电阻率层析成像(ERT)是测量地下地质剖面的有效、准确的地球物理方法。在本文中,我们介绍了这些方法在蒙塔格诺尔(法国阿尔卑斯山)试验场的联合开发,最终目的是研究和监测可能发生的灾难性滑坡对交通基础设施的影响。众所周知,地球物理野外考察的模糊性、地质场景的复杂性和低信噪比等因素影响了所调查地下构造建立可靠的物理地质模型的可能性。本文将GPR和ERT方法应用于Montagnole遗址,介绍了小波理论和数据挖掘的最新进展。小波方法被专门用于实现由不同地球物理场的整合而产生的增强(例如相干肖像)图像。这种基于匹配追踪与小波包字典相结合的方法使我们能够在不同的物理地质条件下提取所需的信号,即使存在强噪声数据。将复杂小波等工具用于相干性肖像,结合GPR-ERT相干定向角,仅举几例,可以在地下地球物理中进行非常规的积分和相关操作。上述参数的估计不仅对埋藏非均匀性的定位有用,而且对其电磁性质和相关性质的粗略估计也很有用。因此,上述方法的组合可以建立一种新的方法,可以提高每种单独的地球物理方法及其集成的可靠性和可信度。
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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