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Feasabiliy of the use of coherent dielectric interfaces as a GPR analysis methodology in the context of coastal masonry: An experimental approach

机译:在沿海砌体环境中使用相干介电界面作为GPR分析方法的可行性:一种实验方法

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The durability of coastal masonry structures is the controlling factor in determining the risks of defects propagation in piers, jetties, harbors, seawalls, etc... This work proposes a methodology in adequacy with the problems met on these structures on the field, for the processing and for the interpretation of the data. The methodology proposed aims to be easily implemented by the user in order to obtain results from a GPR investigation on coastal man-made masonry structures. The process uses an initial visualization and selection of coherent dielectric reflectors showing lateral phase continuity which defines their time-space positions and amplitudes. The selection of each reflector from a profile to another is based on a sufficient gridding of the area investigated and on its shape (geometry, intensity and depth). The consistency of the reflectors selected will be demonstrated by their interpolation and mapping. Their amplitudes will be mapped and will enable the user to interpret the relative variability of the reflectors in terms of depth and energy backscattered. The amplitude added to the reflectors 3D positions will provide the key information at this scale of interest. The proposed methodology has been validated and its accuracy discussed, as well as its limitations considering its application. The mapping successfully ensured consistency compared to other ground investigation methods. Thus, this method could be jointly used with other geophysical or geotechnical methods as part of a larger ground investigation. More particularly, the resulting mapping may be used to constrain geotechnical models, image-guided ERT inversion or any other geophysical investigation.
机译:沿海砌体结构的耐用性是确定缺陷在码头,码头,港口,海堤等中传播的风险的控制因素。这项工作提出了一种方法,可以充分解决这些结构在现场所遇到的问题。处理和解释数据。所提出的方法旨在易于用户实施,以便从GPR对沿海人造砖石结构的调查中获得结果。该过程使用初始可视化和相干介电反射器的选择,以显示横向相位连续性,从而定义其时空位置和幅度。每个反射器从一个轮廓到另一个轮廓的选择均基于所研究区域的充分网格划分及其形状(几何形状,强度和深度)。所选反射器的一致性将通过其插值和映射来证明。它们的振幅将被映射,并使用户能够根据深度和反向散射的能量来解释反射器的相对变化性。添加到反射器3D位置的幅度将在此感兴趣的范围内提供关键信息。所提出的方法已经过验证,并讨论了其准确性,并考虑了其应用方面的局限性。与其他地面调查方法相比,该地图成功地确保了一致性。因此,该方法可以与其他地球物理或岩土方法联合使用,作为较大的地面调查的一部分。更具体地,所得的映射可以用于约束岩土模型,图像引导的ERT反演或任何其他地球物理研究。

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