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

机译:来自风化层表面的实验室光散射和数据模拟   通过Hapke模型

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摘要

The small atmosphereless objects of our solar system, such as asteroids, themoon are covered by layer of dust particles known as regolith, formed bymeteoritic impact. The light scattering studies of such dust layer bylaboratory experiment and numerical simulation are two important tools toinvestigate their physical properties. In the present work, the light scatteredfrom a layer of dust particles, containing 0.3{\mu}m Al2O3 at wavelength 632.8nm is analysed. This work has been performed by using a light scatteringinstrument 'ellipsometer', at the Department of Physics, Assam Universiy,Silchar, India. Through this experiment, we generated in laboratory thephotometric and polarimetric phase curves of light scattered from such a layer.In order to numerically simulate this data, we used Hapke's model combined withMie's single particle scattering properties. The perpendicular and parallelcomponents of single particle albedo and the phase function were derived fromMie theory. By using the Hapke's model combined with Mie theory, the physicalproperties of the dust grain such as grain size, optical constant (n,k) andwavelength can be studied through this scheme. In literature, till today notheoretical model to represent polarisation caused due to scattering from roughsurface is available, which can successfully explain the scattering process. Sothe main objective of this work is to develop a model which can theoreticallyestimate polarisation as caused due to scattering from rough surface and alsoto validate our model with the laboratory data generated in the present work.
机译:太阳系中小的无大气层的物体,例如小行星,小行星,被气象撞击形成的尘埃颗粒层覆盖。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,该粉尘颗粒包含波长为632.8nm的0.3μmAl2O3。这项工作是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。通过此实验,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函数均来自米理论。通过结合Hapke模型和Mie理论,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,还没有可用非理论模型来表示由于从粗糙表面散射而引起的极化,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。

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    Deb, S.; Sen, A. K.;

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  • 年度 2015
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