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Inversion of dispersive APVO GPR curves: a thin-layer approach for fracture characterization on a vertical cliff

机译:色散APVO GPR曲线的反演:用于垂直悬崖裂缝表征的薄层方法

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Reliability of stability assessment of prone to fall rock masses suffers from the lack of information about the geometry and the properties of the fracture networks. GPR profiles associated to Common Mid-Point (CMP) data, all recorded on the cliff wall, recently proved their efficiency to image correctly the extension of fractures with a satisfying resolution. However, besides velocity, CMP data also contain information generally not used, i.e. Amplitude and Phase variations of the reflectivity for a given reflector as function of Offset (APVO) and frequency. In this study, we analyzed the potential of these curves in the context of thin layers, where multiple reflections generate interferences and complex patterns. We notably present an inversion of real APVO curves derived from a CMP profile acquired directly on a limestone cliff wall. The reflected wave was primary deconvoluated in order to correct wave propagation effects and to evaluate radiation patterns. In a second step, APVO curves were inverted considering a neighborhood algorithm. This procedure permitted to obtain the Jonscher parameters describing the complex permittivity of the thin-layer and of the limestone formation, as well as the aperture and depth of the studied fracture.
机译:易于下落的岩体进行稳定性评估的可靠性因缺乏有关裂缝网络的几何形状和性质的信息而受到困扰。与通用中点(CMP)数据相关的GPR剖面(全部记录在悬崖壁上)最近证明了其以令人满意的分辨率正确成像裂缝扩展的效率。但是,除了速度之外,CMP数据还包含通常不使用的信息,即,给定反射器的反射率的振幅和相位变化是偏移(APVO)和频率的函数。在这项研究中,我们分析了在薄层情况下这些曲线的潜力,在薄层情况下,多次反射会产生干扰和复杂的图案。我们特别提出了直接从石灰石悬崖墙上获取的CMP剖面推导的实际APVO曲线的反演。为了校正波的传播效果并评估辐射方向图,对反射波进行了初级反卷积处理。第二步,考虑邻域算法,反转APVO曲线。该程序允许获得描述薄层和石灰岩地层的复介电常数以及所研究裂缝的孔径和深度的Jonscher参数。

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