Size, morphology, and composition of lunar samples returned by Chang'E-5 mission

被引:5
|
作者
Hui Zhang [1 ]
Xian Zhang [1 ]
Guang Zhang [1 ]
Keqi Dong [1 ]
Xiangjin Deng [2 ]
Xiaosong Gao [3 ]
Yaodong Yang [3 ]
Yuan Xiao [1 ]
Xiao Bai [1 ]
Kaixin Liang [1 ]
Yiwei Liu [1 ]
Wenbin Ma [1 ]
Shaofan Zhao [1 ]
Ce Zhang [1 ]
Xiaojing Zhang [1 ]
Jian Song [1 ]
Wei Yao [1 ]
Hong Chen [4 ]
Weihua Wang [1 ,5 ]
Zhigang Zou [1 ,6 ]
Mengfei Yang [1 ,4 ]
机构
[1] Qian Xuesen Laboratory of Space Technology, China Academy of Space Technology (CAST)
[2] Beijing Institute of Spacecraft System Engineering, China Academy of Space Technology (CAST)
[3] Materials and Processes Assurance Center of Beijing Spacecrafts, China Academy of Space Technology (CAST)
[4] China Academy of Space Technology (CAST)
[5] Institute of Physics, Chinese Academy of Sciences
[6] College of Engineering and Applied Sciences, Nanjing University
关键词
D O I
暂无
中图分类号
V476.3 [月球探测器];
学科分类号
082503 ;
摘要
This study focuses on the physical and chemical properties of surficial lunar regolith(LR) samples returned from the Moon by the Chang’E-5(CE-5) mission. Insights regarding the effect of a new sampling geological site on the surficial lunar sample CE5 C0400 were illustrated using nondestructive techniques such as laser diffractometry coupled with image analysis, X-ray computed tomography, and field emission scanning electron microscopy equipped with energy dispersive spectroscopy, and Xray diffraction combined with Rietveld refinement. From the characterization analyses, the CE-5 sampling site in the northeastern Oceanus Procellarum on the Moon yields a unique collection of relatively regular-shaped and fine basalt-dominated particles. The median grain size D50 is(55.24±0.96) μm, falling within the relatively low end of the range of the Apollo lunar returned samples. The coefficient of uniformity Cuof 15.1 and the coefficient of curvature Ccof 1.7 could classify CE5 C0400 to be well-graded. The minerals in CE5 C0400 comprise approximately 44.5% pyroxene, 30.4% plagioclase, 3.6% olivine, and6.0% ilmenite. There is a relatively low content of approximately 15.5% glass phase in the CE-5 lunar sample. From the results,we deduce that the CE-5 LR structure could have mainly resulted from micrometeoroid impacts to achieve such a high level of maturity.
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页码:110 / 117
页数:8
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