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Updated: Feb 5, 2026

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阿波罗17号火山玻璃在月球表面的长时间冷却和脱气
1Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, CA, USA. pengni@epss.ucla.edu.
Nature communications
|February 3, 2026
概括
月球上的火态沉积物显示了长时间的表面脱气,而不仅仅是喷发驱动的挥发性损失. 这表明活动延长,影响月球的大气和挥发性循环.
科学领域:
- 月球地质学 月球地质学
- 星球科学 星球科学
- 火山学 火山学是一门学科.
背景情况:
- 月球上的火热弹性火山活动提供了对地幔演变和挥发性物质含量的洞察.
- 烟雾沉积物源于更深,更原始,更富有挥发性物质的月球地幔来源.
研究的目的:
- 从阿波罗17号样本74220中合成挥发性脱气,这是一个关键的火岩沉积物.
- 调查月球火岩样本的脱气机制和热史.
主要方法:
- 模拟含有橄素的融入物,融入物和玻璃珠的挥发性脱气.
- 使用热建模来支持建议的冷却和脱气场景.
主要成果:
- 样本中的挥发性物质耗尽不能仅仅由自由飞行脱气来解释.
- 证据表明,在月球表面,玻璃珠的冷却速度缓慢,并长时间脱气,持续了多年.
- 需要扩展的热史来解释观察到的挥发性物质耗尽.
结论:
- 月球上的火态沉积物作为持续的挥发性来源,超越了最初的喷发.
- 这种长时间的活动可能会维持月球短暂的大气层.
- 这些发现对了解月球的长期波动周期具有重要意义.
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