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

被引:53
|
作者
Zhang, Hui [1 ]
Zhang, Xian [1 ]
Zhang, Guang [1 ]
Dong, Keqi [1 ]
Deng, Xiangjin [2 ]
Gao, Xiaosong [3 ]
Yang, Yaodong [3 ]
Xiao, Yuan [1 ]
Bai, Xiao [1 ]
Liang, Kaixin [1 ]
Liu, Yiwei [1 ]
Ma, Wenbin [1 ]
Zhao, Shaofan [1 ]
Zhang, Ce [1 ]
Zhang, Xiaojing [1 ]
Song, Jian [1 ]
Yao, Wei [1 ]
Chen, Hong [4 ]
Wang, Weihua [1 ,5 ]
Zou, Zhigang [1 ,6 ]
Yang, Mengfei [1 ,4 ]
机构
[1] China Acad Space Technol CAST, Qian Xuesen Lab Space Technol, Beijing 100094, Peoples R China
[2] China Acad Space Technol CAST, Beijing Inst Spacecraft Syst Engn, Beijing 100094, Peoples R China
[3] China Acad Space Technol CAST, Mat & Proc Assurance Ctr Beijing Spacecrafts, Beijing 100094, Peoples R China
[4] China Acad Space Technol CAST, Beijing 100094, Peoples R China
[5] Chinese Acad Sci, Inst Phys, Beijing 100190, Peoples R China
[6] Nanjing Univ, Coll Engn & Appl Sci, Nanjing 210093, Peoples R China
关键词
the Moon; surface microscopy; meteoroid; SOIL; PETROLOGY; SURFACE; MINERALOGY; CHEMISTRY; REGOLITH; REGION;
D O I
10.1007/s11433-021-1818-1
中图分类号
O4 [物理学];
学科分类号
0702 ;
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 CE5C0400 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 X-ray 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 D-50 is (55.24 +/- 0.96) mu m, falling within the relatively low end of the range of the Apollo lunar returned samples. The coefficient of uniformity C-u of 15.1 and the coefficient of curvature C-c of 1.7 could classify CE5C0400 to be well-graded. The minerals in CE5C0400 comprise approximately 44.5% pyroxene, 30.4% plagioclase, 3.6% olivine, and 6.0% 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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页数:8
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