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Electromagnetic scattering calculated from pair distribution functions retrieved from planar snow sections

机译:根据从平面积雪部分获取的成对分布函数计算出的电磁散射

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Electromagnetic wave scattering in dense media, such as snow, depends on the three-dimensional (3D) pair distribution function of particle positions. In snow, two-dimensional (2D) stereological data can be obtained by analyzing planar sections. In this paper the authors calculate the volume 3D pair distribution functions from the 2D stereological data by solving Hanisch's integral equation. They first use Monte Carlo simulations for multisize particles to verify the procedure. Next they apply the procedure to available planar snow sections. A log-normal distribution of particle sizes is assumed for the ice grains in snow. To derive multisize pair functions, a least squares fit is used to recover pair functions for particles with sufficient number density and the hole correction approximation is assumed for the larger particles. A family of 3D pair distribution functions are derived. These are then substituted into dense media scattering theory to calculate scattering. It is found that the computed scattering rates are comparable to those calculated under the Percus-Yevick approximation of pair distribution functions of multiple sizes.
机译:在诸如雪之类的稠密介质中的电磁波散射取决于粒子位置的三维(3D)对分布函数。在雪中,可以通过分析平面截面来获取二维(2D)立体数据。在本文中,作者通过求解Hanisch积分方程,从2D立体数据计算体积3D对分布函数。他们首先使用蒙特卡洛模拟法对多尺寸颗粒进行验证。接下来,他们将该程序应用于可用的平面积雪部分。假定雪中冰粒的对数正态分布。为了导出多尺寸对函数,使用最小二乘拟合恢复具有足够数密度的粒子的对函数,并假设较大粒子的空穴校正近似值。导出了一系列3D对分布函数。然后将它们代入稠密介质散射理论以计算散射。可以发现,所计算的散射率与多种尺寸的成对分布函数的Percus-Yevick近似计算的散射率相当。

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