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首页> 外文期刊>IEEE Transactions on Geoscience and Remote Sensing. >Full-Wave Electromagnetic Scattering From Rough Surfaces With Buried Inhomogeneities
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Full-Wave Electromagnetic Scattering From Rough Surfaces With Buried Inhomogeneities

机译:具有埋藏不均匀性的粗糙表面的全波电磁散射

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We develop a methodology for modeling coherent electromagnetic scattering from rough surfaces with buried inhomogeneities in three dimensions. The inhomogeneities considered in this paper include random spherical media, random cylindrical media, and root-like cylindrical clusters. They are used to simulate rocks, ice particles, and vegetation roots buried beneath the ground surface that can be seen by the low-frequency radars in Earth remote sensing applications. The approach we develop first calculates volumetric scattering from the media using coherent approaches, including both the conventional recursive transition matrix (T-matrix) method as well as a new generalized iterative extended boundary condition method we developed for tilted finite cylinders, and then transforms the T-matrix to the scattering matrix, which is then used to form the full scattered field of layered structures with rough surface and subsurfaces. We validate the methodology by comparing with other numerical solutions for special cases, and show sensitivity results for scattering from rough surface with buried random spherical media and random cylindrical media of different densities. We also construct a basic root model and calculate the scattering cross sections from single and multiple root clusters with or without a subsurface interface underneath. With the approach developed in this paper, we are able to study the sensitivity of radar signals to subsurface scatterers. For example, our simulations show that, depending on their density and water content, buried roots could enhance the backscatter from a single rough surface by as much as 5 dB in co-pol components, and substantially more in cross-pol components. The results of this model are expected to enable more accurate geophysical retrievals of soil moisture as well as soil organic content.
机译:我们开发了一种方法,用于对来自粗糙表面的相干电磁散射进行建模,这些粗糙表面具有三个维度的埋藏不均匀性。本文考虑的不均匀性包括随机球形介质,随机圆柱介质和根状圆柱簇。它们用于模拟掩埋在地面下的岩石,冰粒和植被根,在地球遥感应用中的低频雷达可以看到这些根。我们开发的方法首先使用相干方法来计算介质的体积散射,包括常规的递归转换矩阵(T-matrix)方法以及为倾斜有限圆柱体开发的新的广义迭代扩展边界条件方法,然后将其转化T矩阵到散射矩阵,然后用于形成具有粗糙表面和次表面的分层结构的完整散射场。通过与特殊情况下的其他数值解进行比较,我们验证了该方法的有效性,并显示了使用不同密度的随机球形埋入介质和圆柱形随机埋入介质从粗糙表面散射的灵敏度结果。我们还构建了基本的根模型,并计算了单个或多个根簇的散射截面,这些簇在下面或不下面都有地下界面。利用本文开发的方法,我们能够研究雷达信号对地下散射体的敏感性。例如,我们的模拟表明,根据根源的密度和含水量,埋根可以使单个粗糙表面的反向散射在共极化分量中增强多达5 dB,而在交叉极化分量中增强得多。该模型的结果有望实现对土壤水分以及土壤有机物的更精确的地球物理检索。

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