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Simple model of a polarized bidirectional scattering cross section at 10.6μm: application to Si0↓(2) sand

机译:极化双向散射截面为10.6μm的简单模型:在Si0↓(2)砂中的应用

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A model is proposed to interpret the polarized scattering behavior for natural soils. The model is based on the vector radiative transfer equation and is developed to the second order. Higher orders are modeled with a simple expression. The particles are assumed to have a large dimension with respect to the wavelength, allowing for the light to be locally specularly reflected. Apart from the complex refractive index, the model has only one extra parameter directly related to the compactness of the medium. Predicted values are compared with carefully calibrated measurements of the polarized bidirectional scattering cross section obtained with coarse SiO↓(2) sand. The model parameters retrieved from the fit are quite realistic. Good agreement is obtained between model-computed and experimental data for the angular behavior and the amplitude, without further adjustment. Comparison between model-computed total unpolarized bidirectional scattering cross section, Hapke's nonpolarized model, and measurements also shows good agreement.# 1997 Optical Society of America
机译:提出了一个模型来解释天然土壤的极化散射行为。该模型基于矢量辐射传递方程,并发展为二阶。使用简单的表达式对高阶建模。假定粒子相对于波长具有较大的尺寸,从而允许光被局部镜面反射。除了复折射率之外,该模型仅具有一个与介质紧密度直接相关的额外参数。将预测值与通过粗SiO↓(2)砂获得的极化双向散射横截面的仔细校准测量值进行比较。从拟合中检索的模型参数是很实际的。在模型计算和实验数据之间,对于角行为和振幅,无需进一步调整即可获得良好的一致性。模型计算的总非偏振双向散射截面,Hapke的非偏振模型与测量值之间的比较也显示出良好的一致性。#1997美国光学学会

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