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Impact of soil structure on microwave volume scattering evaluated by a two-dimensional numerical model

机译:用二维数值模型评价土壤结构对微波体积散射的影响

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摘要

Soil volumetric structure is an important parameter for tillage operation. The aim of this paper is to assess whether volume characteristics can be inferred from radar measurements. A 2-D numerical model (the 2DSCAT model) was developed based on a numerical solver using a time-domain finite-element method to solve Maxwell's equations. Perfectly matched layers were implemented as well as a near- to far-field transformation. A focused incident beam was generated by adapting the boundary conditions. To represent the soil structure, a simulator was developed describing the soil as biphasic media (fine earth and clods). Clods were represented by randomly deformed ellipses, with randomly determined dimensions, locations, and orientations. The model performed successfully, as evaluated against exact analytical solutions available for an infinite perfectly conducting cylinder and the reflection of flat semi-infinite media. The model was then evaluated against measurements made by an X-band FM continuous-wave radar on a box filled with dry clods of different sizes. The effect of the clod size on the backscattering power was very well reproduced, showing the potential of using a 2-D numerical model to understand microwave-backscattering patterns from cloddy soils. Analysis of the volume scattering shows that this phenomenon can be mostly hidden in the scatter diagram by surface scattering when the latter occurred. However, the volume scattering gives a stronger residual signal in time because of propagation through the medium. Thus, time studies of the scattering signal provide further information about volume heterogeneities
机译:土壤体积结构是耕作操作的重要参数。本文的目的是评估是否可以从雷达测量中推断出体积特征。基于数值求解器,使用时域有限元方法开发了二维数值模型(2DSCAT模型)以求解麦克斯韦方程组。实现了完美匹配的图层以及近场到远场的转换。通过调整边界条件产生聚焦的入射光束。为了表示土壤结构,开发了一个将土壤描述为双相介质(细土和土块)的模拟器。土块由随机变形的椭圆形代表,具有随机确定的尺寸,位置和方向。该模型成功执行,并针对可用于无限完美导电圆柱体和平坦半无限介质的反射的精确解析解进行了评估。然后根据X波段FM连续波雷达在装有不同大小干土块的盒子上进行的测量评估模型。土块大小对反向散射能力的影响得到了很好的再现,显示了使用二维数值模型理解土质土壤微波反向散射模式的潜力。对体积散射的分析表明,当表面散射发生时,该现象可以通过散点图大部分隐藏在散点图中。但是,由于通过介质传播,体积散射在时间上会提供更强的残留信号。因此,散射信号的时间研究可提供有关体积异质性的更多信息

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