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Laboratory light scattering from regolith surface and simulation of data by Hapke model

机译:实验室从灰泥岩表面散射光并通过Hapke模型模拟数据

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The small atmosphereless objects of our solar system, such as asteroids and the moon, are covered by layer of dust particles known as regolith, formed by meteoritic impact. The light scattering studies of such dust layer by laboratory experiment and numerical simulation are two important tools to investigate their physical properties. In the present work, the light scattered from a layer of dust particles, containing 0.3 mu m Al2O3 at wavelength 632.8 nm, is analysed. This work has been performed by using a light scattering instrument 'ellipsometer', at the Department of Physics, Assam University, Silchar, India. Through this experiment, we generated in laboratory the photometric and polarimetric phase curves of light scattered from such a layer. In order to numerically simulate this data, we used Hapke's model combined with Mie's single particle scattering properties. The perpendicular and parallel components of single particle albedo and the phase function were derived from Mie theory. By using Hapke's model combined with Mie theory, the physical properties of the dust grain such as grain size, optical constant (n,k) and wavelength can be studied through this scheme. In the literature, till today no theoretical model to represent polarisation caused due to scattering from rough surface is available, which can successfully explain the scattering process. So the main objective of this work is to develop a model which can theoretically estimate polarisation as caused due to scattering from rough surface and also to validate our model with the laboratory data generated in the present work. (C) 2016 Elsevier Ltd. All rights reserved.
机译:我们太阳系中小的无大气层的物体,例如小行星和月球,被陨石撞击形成的尘埃颗粒层覆盖,该尘埃颗粒称为雷格石。通过实验室实验和数值模拟研究这种粉尘层的光散射是研究其物理性质的两个重要工具。在本工作中,分析了从粉尘颗粒层散射的光,该粉尘颗粒包含0.3μm的Al2O3,波长为632.8 nm。这项工作是通过使用印度锡尔恰尔阿萨姆大学物理系的光散射仪器“椭圆仪”完成的。通过该实验,我们在实验室中生成了从该层散射的光的光度和偏振相位曲线。为了对这些数据进行数值模拟,我们使用了Hapke模型和Mie的单粒子散射特性。单粒子反照率的垂直分量和平行分量以及相位函数均来自Mie理论。通过使用Hapke模型与Mie理论相结合,可以通过该方案研究粉尘颗粒的物理性质,例如粒度,光学常数(n,k)和波长。在文献中,直到今天,还没有可用的理论模型来表示由于粗糙表面的散射而引起的极化,它可以成功地解释散射过程。因此,这项工作的主要目的是开发一个模型,该模型可以从理论上估计由于粗糙表面的散射而引起的极化,并且还可以使用本工作中生成的实验室数据来验证我们的模型。 (C)2016 Elsevier Ltd.保留所有权利。

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