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On the use of dispersive APVO GPR curves for thin-bed properties estimation: Theory and application to fracture characterization

机译:色散APVO GPR曲线在薄层性质评估中的应用:理论及在裂缝表征中的应用

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The presence of a thin layer embedded in any formation cre_ates complex reflection patterns caused by interferences within the thin bed. The generated reflectivity amplitude variations with offset have been increasingly used in seismic interpretation and more recently tested on ground-penetrating radar (GPR) data to characterize nonaqueous-phase liquid contaminants. Phase and frequency sensitivities of the reflected signals are generally not used, although they contain useful information. The present study aims to evaluate the potential of these combined properties to characterize a thin bed using GPR data acquired along a com_mon-midpoint (СМР) survey, carried out to assess velocity vari_ations in the ground. It has been restricted to the simple case of a thin bed embedded within a homogeneous formation, a situation often encountered in fractured media. Dispersive properties of the dielectric permittivity of investigated materials (homoge_neous formation, thin bed) are described using a Jonscher para-meterization, which permitted study of the dependency of amp_litude and phase variation with offset (APVO) curves on frequen_cy and thin-bed properties (filling nature, aperture). In the second part, we discuss and illustrate the validity of the thin-bed approx-imation as well as simplify assumptions and make necessary careful corrections to convert raw СМР data into dispersive APVO curves. Two different strategies are discussed to correct the data from propagation effects: a classical normal-moveout approach and an inverse method. Finally, the proposed method_ology is applied to a СМР GPR data set acquired along a vertical cliff. It allowed us to extract the characteristics of a subvertical fracture with satisfying resolution and confidence. The study mo_tivates interest to use dispersion dependency of the reflection coefficient variations for thin-bed characterization.
机译:嵌入在任何地层中的薄层的存在会造成由薄层内部的干涉引起的复杂反射图案。所产生的具有偏移的反射率振幅变化已越来越多地用于地震解释中,并且最近在探地雷达(GPR)数据上进行了测试,以表征非水相液体污染物。尽管反射信号包含有用的信息,但通常不使用它们的相位和频率灵敏度。本研究旨在使用通过评估地面速度变化进行的共同中点(СМР)测量获得的GPR数据,评估这些组合特性表征薄层的潜力。仅限于在均匀地层中埋置薄层的简单情况,这种情况经常在裂隙介质中遇到。使用Jonscher参数化描述了所研究材料(均质层,薄层)的介电常数的色散特性,该特性允许研究幅值和相位变化与频偏(APVO)曲线对频率和薄层特性的依赖性(填充性质,孔径)。在第二部分中,我们讨论并说明了薄床近似法的有效性,并简化了假设并进行了必要的仔细修正,以将原始СМР数据转换为分散的APVO曲线。讨论了两种不同的策略来校正来自传播效应的数据:经典的法线偏移方法和逆方法。最后,将所提出的method_ology应用于沿垂直悬崖获取的СМРGPR数据集。它使我们能够以令人满意的分辨率和置信度提取亚垂直裂缝的特征。这项研究引起了人们的兴趣,即使用反射系数变化的色散依赖性来进行薄层表征。

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