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SIMULATION OF GROUND-PENETRATING RADAR WAVES IN A 2-D SOIL MODEL

机译:二维土壤模型中的探地雷达波模拟

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We have developed a pseudospectral forward modeling algorithm for ground-penetrating radar (GPR) based on an explicit solution of the 2-D lossy electromagnetic wave equation. Complex soil structures can be accommodated with heterogeneous spatial distributions of both wave velocity and electrical conductivity. This algorithm uses a Gaussian line source with uniform directivity, and there are conductive buffer regions surrounding the soil model to approximate absorbing boundary conditions. Three soil models are used to illustrate different aspects of radar wave propagation. The first model is lossless with homogeneous layers imbedded in a homogeneous background medium, the second model has the same lossless layers in a lossy background medium, and the third model is lossless and uses a nonsaturated water flow simulation to create a complex spatial velocity distribution. Two separate simulations with different source frequencies are presented for each soil model. Results indicate that higher frequency GPR will produce a sharper wavelet and can map soil layering structures with high resolution. In a conductive soil, however, higher frequencies attenuate more rapidly and the radar may not detect deeper layers. [References: 30]
机译:我们基于二维有损电磁波方程的显式解决方案,开发了一种用于探地雷达(GPR)的伪谱正向建模算法。复杂的土壤结构可以容纳波速和电导率的异质空间分布。该算法使用具有均匀方向性的高斯线源,并且在土壤模型周围存在导电缓冲区,以近似吸收边界条件。使用三种土壤模型来说明雷达波传播的不同方面。第一个模型是无损的,均质层嵌入均匀的背景介质中,第二个模型在有损的背景介质中具有相同的无损层,第三个模型是无损的,并使用非饱和水流模拟来创建复杂的空间速度分布。针对每种土壤模型,提出了两种具有不同源频率的独立模拟。结果表明,较高频率的GPR将产生更清晰的小波,并且可以绘制高分辨率的土壤分层结构图。但是,在导电土壤中,较高的频率会更快衰减,并且雷达可能无法检测到更深的层。 [参考:30]

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