由Chang'E-5任务返回的月球规石颗粒的融化和快速固化
Xian Zhang1, Yiwei Liu1, Shaofan Zhao1
1Qian Xuesen Laboratory of Space Technology, China Academy of Space Technology (CAST), Beijing 100094, China.
Research (Washington, D.C.)
|September 24, 2024
概括
研究人员观察到来自岩的月球规流岩的融化和快速固化.
科学领域:
- 月球地质学和火山活动
- 在现场资源利用 (ISRU)
- 材料科学是一种材料科学.
背景情况:
- 了解月球规格岩的行为对于月球科学和ISRU至关重要.
- 之前的研究缺乏直接观察化和固化动态.
研究的目的:
- 直接观察和分析月球正岩粒子的融化和快速固化.
- 为了确定融温度,序列和结晶过程.
- 为了研究融化和固化过程中挥发性物质的释放.
主要方法:
- 直接观察Chang'E 5月球粒子的融化和固化.
- 测量化温度和化的顺序.
- 对泡形成和释放的分析.
- 使用显微镜确定晶体生长速度.
- 使用扫描电子显微镜 (SEM) 和能量分散式X射线光谱 (EDS) 的化学分析.
主要成果:
- 确定了月球颗粒的融化温度和序列.
- 观察到气泡产生,生长和释放 (直径最大5微米),归因于挥发性释放.
- 结晶发生在固化过程中,其生长速度约为27nm/s.
- 富含铁的矿物被确定为第一个结晶的矿物.
结论:
- 直接观测提供了关于月球 regolith 阶段过渡的关键数据.
- 这些发现提高了对月球火山活动,地质学和影响历史的理解.
- 结果支持开发用于月球应用的现场资源利用技术.
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