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In situ optical measurements of Chang'E-3 landing site in Mare Imbrium: 2. Photometric properties of the regolith

机译:母马Imbrium Chang娥三号着陆点的原位光学测量:2.重石的光度特性

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The panorama cameras onboard the Yutu Rover of the Chang'E-3 lunar mission acquired hundreds of high-resolution color images of the lunar surface and captured the first in situ lunar opposition effect (OE) since the Apollo era. We extracted the phase curve and the color ratio in three bands with the phase angle range from 2 degrees to 141 degrees. Photometric inversions using the Hapke model reveal that submicroscopic dusts are present in the landing area and both the coherent backscattering and the shadow hiding are responsible for the strong OE. Compared with spaceborne measurements, the grains in the landing site are brighter, more transparent, and appear to be better crystallized than the average maria basaltic grains. The results show that the phase-reddening effect appears to be present in the in situ phase curves. The current phase curve can be used as the ground-truth validations of any future spaceborne phase curve measurement over the landing site region.
机译:'娥三号登月任务的雨图漫游车上的全景摄像机获取了数百张月球表面的高分辨率彩色图像,并捕获了自阿波罗时代以来的第一个原位月球对立效应(OE)。我们提取了三个相位角在2度至141度范围内的相位曲线和色彩比率。使用Hapke模型进行的光度反演表明,着陆区存在亚微米级的粉尘,并且相干的反向散射和阴影遮盖都是强OE的原因。与星载测量相比,着陆点的颗粒比普通玛丽亚玄武岩颗粒更亮,更透明且结晶更好。结果表明,相变红效应似乎存在于原位相曲线中。当前的相位曲线可以用作着陆点区域上任何未来星载相位曲线测量的地面真实性验证。

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