ArticleResearch (Washington, D.C.)2024
Melting and Rapid Solidification of Lunar Regolith Particles Returned by Chang'E-5 Mission.
Article in Research (Washington, D.C.), 2024. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 5 papers.
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Who cites it
5 citing papers in PubMed.
- Progress and Bottlenecks in Large-Scale Commercial Space Transportation Systems.Research (Washington, D.C.) · 2026Review
- Future Model for Efficient and Advanced Space Transportation: Exploration and Perspectives.Research (Washington, D.C.) · 2026Review
- Zhuque Base for Martian Habitation: Conceptual Design and Performance Analysis of Cave Dwellings and In Situ Construction.Research (Washington, D.C.) · 2025Article
- Massive Water Production from Cryogenic Icy Lunar Regolith by a Microwave Heating Method.Research (Washington, D.C.) · 2025Article
- The Formation Mechanisms of np-Fe in Lunar Regolith: A Review.Materials (Basel, Switzerland) · 2024Review
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Authors and funding
8 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
Melting and solidification of lunar regolith are pivotal for comprehending the evolutionary dynamics of lunar volcanism, geology, and impact history. Additionally, insights gained from these processes can contribute to the advancement of in situ resource utilization technologies, for instance additive manufacturing and resource extraction systems. Herein, we conduct the direct observation of the melting and rapid solidification of lunar particles returned by the Chang'E 5 mission. The melting temperature and melting sequence were obtained. Bubble generation, growth, and release were clearly observed, with a maximum bubble diameter of 5 µm, which is supposed to be according to the release of volatiles that embedded in the particles. During the solidification process, evident crystallization occurred with incremental crystal growth rate approximately of 27 nm/s. Scanning electron microscopy and energy-dispersive x-ray spectroscopy results verified that the Fe-rich mineral crystalizes first. These results would improve the understanding of the evolution of lunar volcanism, geology, and impact history.
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Registered trials
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