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Remote determination of small-scale three-dimensional surface properties based on imaging photometry and polarimetry: an introduction

机译:基于成像光度法和偏光法的远程确定小尺度三维表面性质:简介

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摘要

The remote sensing analysis of planetary surfaces is a field in which photopolarimetric techniques allow the estimation of the average small-scale 3D properties of the examined surfaces (i.e. on millimeter or sub-millimeter scales) from large distances. This work provides an overview of image-based photometric and polarimetric methods for the remote determination of small-scale 3D properties of planetary regolith surfaces. Specifically, the surface porosity governs the phase angle dependence of the reflectance function of the surface material for near-zero phase angles, while the reflectance behavior at large phase angles between around 90° and 180° allows to estimate the surface roughness on sub-millimeter and millimeter scales. For the lunar regolith, a calibration of the phase angle dependence of the polarization behavior of the light reflected from the surface based on returned lunar sample material provides a framework to determine the median regolith grain size based on measurements of the polarization degree. In this work, the corresponding methodologies as well as their application to specific planetary bodies are discussed. Where deemed favorable, new photometric and polarimetric measurements of prototypical areas of the lunar surface are provided to exemplify the described approaches in an illustrative manner.
机译:行星表面的遥感分析是一个领域,其中光偏光技术可以从远处估算被检查表面的平均小尺度3D特性(即毫米或亚毫米尺度)。这项工作概述了基于图像的光度法和旋光法,用于远程确定行星重石表面的小规模3D特性。具体而言,表面孔隙率控制着表面材料的反射函数对接近零相位角的相位角依赖性,而在大约90°和180°之间的大相位角下的反射行为可以估计亚毫米级的表面粗糙度和毫米刻度。对于月球巨石,基于返回的月球样本材料对从表面反射的光的偏振行为的相位角依赖性进行校准提供了一个框架,该框架可基于偏振度的测量来确定中值角砾石晶粒尺寸。在这项工作中,讨论了相应的方法及其在特定行星体上的应用。在认为有利的地方,提供了月球表面原型区域的新的光度和偏振测量,以示例性方式例示了所描述的方法。

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  • 来源
    《3D Research》 |2010年第4期|p.1-15|共15页
  • 作者

    Christian Wöhler;

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  • 正文语种 eng
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