Micro-CT Characterization of the Chang'e-5 Lunar Regolith Samples

IF 4 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Journal of Geophysical Research: Planets Pub Date : 2025-02-27 DOI:10.1029/2024JE008787
Huanyu Wu, Yuan Zou, Chi Zhang, Wei Yang, Bo Wu, Kai-Leung Yung, Qi Zhao
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Abstract

Chang'e-5 (CE-5) lunar regolith samples were scanned using X-ray micro-computed tomography (micro-CT), and over 0.7 million particles were extracted from the images through machine learning-based segmentation. This is the largest three-dimensional (3D) image data set on lunar regolith particles to date, offering a unique opportunity to study the key characteristics of the lunar regolith. The image intensity was correlated with mineral density, allowing for the assessment of the bulk density (1.58 g/cm3), true density (3.17 g/cm3), and mineralogy of the lunar regolith. Glass and plagioclase contributed 45.6 wt.% of the samples, while pyroxene and olivine made up 49.7 wt.%, and ilmenite accounted for 4.7 wt.%. The median grain size of CE-5 was 57.5 μm, smaller than the Apollo 11, 16 and Luna 16, 20 and 24 samples. Spherical harmonic (SH) analysis and aspect ratio (AR) measurement revealed that the CE-5 lunar regolith particles have more complex shapes than two common terrestrial soils and exhibit less spherical shapes than Apollo 11, 16 and Luna 16, 20 and 24 samples. We recommend using size and shape characteristics cautiously when inferring the lunar regolith maturity because the intrinsic crystal size of the protolith and complex lunar surface weathering can cause significant size and shape variations. Additionally, characterizing particle shapes requires a large sample size (>1,000) to prevent skewed results from outliers. Our non-destructive examination method offers a novel and appealing approach for analyzing critical physical, mineralogical, and morphological properties of million-scale extraterrestrial soil particles, paving the way for future deep space explorations.

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嫦娥五号月球风化层样品的微ct表征
使用x射线微计算机断层扫描(micro-CT)扫描嫦娥五号(CE-5)月球表层样品,并通过基于机器学习的分割从图像中提取了70多万个颗粒。这是迄今为止最大的月球风化层颗粒三维(3D)图像数据集,为研究月球风化层的关键特征提供了独特的机会。图像强度与矿物密度相关,从而可以评估月球风化层的体积密度(1.58 g/cm3)、真密度(3.17 g/cm3)和矿物学。玻璃和斜长石占45.6%,辉石和橄榄石占49.7%,钛铁矿占4.7%。CE-5的中位晶粒尺寸为57.5 μm,小于阿波罗11号、16号和月球16号、20号和24号样品。球谐(SH)分析和长宽比(AR)测量结果表明,CE-5月球风化层颗粒的形状比两种常见的陆地土壤更复杂,比阿波罗11号、16号和月球16号、20号和24号样品的形状更小。我们建议在推断月球风化层成熟度时谨慎使用尺寸和形状特征,因为原岩的固有晶体尺寸和复杂的月球表面风化会导致显着的尺寸和形状变化。此外,表征粒子形状需要较大的样本量(1,000),以防止异常值导致的结果偏斜。我们的无损检测方法为分析百万级地外土壤颗粒的关键物理、矿物学和形态学特性提供了一种新颖而有吸引力的方法,为未来的深空探测铺平了道路。
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来源期刊
Journal of Geophysical Research: Planets
Journal of Geophysical Research: Planets Earth and Planetary Sciences-Earth and Planetary Sciences (miscellaneous)
CiteScore
8.00
自引率
27.10%
发文量
254
期刊介绍: The Journal of Geophysical Research Planets is dedicated to the publication of new and original research in the broad field of planetary science. Manuscripts concerning planetary geology, geophysics, geochemistry, atmospheres, and dynamics are appropriate for the journal when they increase knowledge about the processes that affect Solar System objects. Manuscripts concerning other planetary systems, exoplanets or Earth are welcome when presented in a comparative planetology perspective. Studies in the field of astrobiology will be considered when they have immediate consequences for the interpretation of planetary data. JGR: Planets does not publish manuscripts that deal with future missions and instrumentation, nor those that are primarily of an engineering interest. Instrument, calibration or data processing papers may be appropriate for the journal, but only when accompanied by scientific analysis and interpretation that increases understanding of the studied object. A manuscript that describes a new method or technique would be acceptable for JGR: Planets if it contained new and relevant scientific results obtained using the method. Review articles are generally not appropriate for JGR: Planets, but they may be considered if they form an integral part of a special issue.
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