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Numerical simulation for ground penetrating radar in dispersive medium

机译:色散介质中探地雷达的数值模拟

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The earth material probed by Ground Penetrating Radar (GPR) is often dispersive. To investigate the detecting capability of GPR in dispersive medium, we introduced a Finite Difference Time Domain (FDTD) method to solve Maxwell's equations. We give an iterative method for electrical displacement and magnetic field in Debye medium, and a method to compute electric field from electrical displacement. The physical parameters are used only in calculating electric field. A new absorbing boundary algorithm is introduced by adding fictitious dielectric constant and magnetic permeability therefore the wave can be attenuated without reflection in absorbing layer. This method overcomes the troublesome caused by field split in Berenger's Perfectly Matched Layer (PML), so that the computing efficiency is increased. Examples demonstrate that the electromagnetic wave in dispersive medium attenuates very fast and the measured signals are very weak.
机译:探地雷达(GPR)探测到的土壤材料通常是分散的。为了研究分散介质中GPR的检测能力,我们引入了时域有限差分(FDTD)方法来求解麦克斯韦方程组。我们给出了德拜介质中电位移和磁场的迭代方法,以及从电位移计算电场的方法。物理参数仅用于计算电场。通过添加虚拟的介电常数和磁导率,引入了一种新的吸收边界算法,因此可以在吸收层中将波衰减而无需反射。该方法克服了贝伦格完全匹配层(PML)中字段拆分带来的麻烦,从而提高了计算效率。实例表明,分散介质中的电磁波衰减非常快,并且测得的信号非常弱。

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