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Finite-difference time-domain simulation of ground penetrating radar on dispersive, inhomogeneous, and conductive soils

机译:离散,非均质和导电土壤上探地雷达的时域有限差分模拟

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摘要

A three-dimensional (3D) time-domain numerical scheme for simulation of ground penetrating radar (GPR) on dispersive and inhomogeneous soils with conductive loss is described. The finite-difference time-domain (FDTD) method is used to discretize the partial differential equations for time stepping of the electromagnetic fields. The soil dispersion is modeled by multiterm Lorentz and/or Debye models and incorporated into the FDTD scheme by using the piecewise-linear recursive convolution (PLRC) technique. The dispersive soil parameters are obtained by fitting the model to reported experimental data. The perfectly matched layer (PML) is extended to match dispersive media and used as an absorbing boundary condition to simulate an open space. Examples are given to verify the numerical solution and demonstrate its applications. The 3D PML-PLRC-FDTD formulation facilitates the parallelization of the code. A version of the code is written for a 32-processor system, and an almost linear speedup is observed.
机译:描述了一种三维(3D)时域数值方案,用于模拟具有导电损耗的分散性和非均质土壤上的探地雷达(GPR)。时域有限差分法(FDTD)用于离散化偏微分方程,用于电磁场的时间步进。通过多年期Lorentz和/或Debye模型对土壤扩散进行建模,并使用分段线性递归卷积(PLRC)技术将其纳入FDTD方案。通过将模型拟合到所报告的实验数据,可以获得分散的土壤参数。完美匹配层(PML)进行了扩展以匹配分散介质,并用作吸收边界条件来模拟开放空间。给出了一些例子来验证数值解并演示其应用。 3D PML-PLRC-FDTD公式有助于代码的并行化。该代码的版本是为32处理器系统编写的,并且观察到几乎线性的加速。

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