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An Improved and Novel Approach for Frequency Domain Forward Modeling of GPR Data Using the Finite Difference Staggered Grid Technique

机译:使用有限差异交错网格技术的GPR数据频域正向建模的改进和新方法

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Forward modeling of ground penetrating radar (GPR) data is important for understanding relationships between dielectric layers. For the inversion of GPR data, an effective and advanced forward modeling scheme is always desirable. Here, staggered grid formulations for the finite difference frequency domain (FDFD) method have been developed and modified for the forward modeling of GPR data. The forward problem is first solved using a nine-point regular staggered grid that basically approximates and discretizes the Laplacian operator. In the case of transverse electric mode FDFD method, the implementation of a perfectly matched layer (PML) has been shown to be effective. Among the several PML techniques, the complex frequency shifted perfectly matched layer method has proven to be most useful for absorbing evanescent waves. In this paper, a new and improved nine-point mixed staggered grid formulation is proposed by considering the combination of a five-point Cartesian and nine-point rotated staggered grid. The derived stencils are compared after estimating the reflection errors from the computed simulated wavefields (E-y) of the homogeneous subsurface model. This newly developed technique exhibits less error than the regular and unstaggered mixed stencils. Lastly, this better and less-time consuming grid is used to extract GPR data from realistic sedimentary models with a surface acquisition setup.
机译:探地雷达(GPR)数据的正演模拟对于理解电介质层之间的关系非常重要。对于探地雷达数据的反演,一种有效的、先进的正演模拟方法一直是需要的。在这里,有限差分频域(FDFD)方法的交错网格公式已被开发和修改,用于探地雷达数据的正演模拟。正问题首先使用九点规则交错网格来解决,该网格基本上近似并离散拉普拉斯算子。在横电模FDFD方法的情况下,完美匹配层(PML)的实现已被证明是有效的。在几种PML技术中,复频移完全匹配层法被证明是吸收倏逝波最有用的方法。本文将五点笛卡尔网格和九点旋转交错网格相结合,提出了一种新的九点混合交错网格格式。在根据均匀地下模型的计算模拟波场(E-y)估计反射误差后,对导出的模板进行比较。这种新开发的技术比常规和无标记的混合模板显示的误差更小。最后,使用这种更好、更省时的网格从具有表面采集装置的真实沉积模型中提取探地雷达数据。

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