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Updated: Dec 3, 2025

Scattering And Absorption of Light in Planetary Regoliths
Published on: July 1, 2019
菲拉探测器发现彗星岩石内部的低强度原始冰
Laurence O'Rourke1, Philip Heinisch2, Jürgen Blum2
1European Space Agency (ESA), European Space Astronomy Centre (ESAC), Madrid, Spain. lorourke@esa.int.
菲莱登陆器在67P/Churyumov-Gerasimenko彗星上的第二次着陆暴露了古老的水冰. 这种与有机物质混合的原始冰具有较低的压力和较高的孔隙性,
科学领域:
- * 星球科学
- * 天体生物学
- * 彗星科学
背景情况:
- 菲莱登陆器的任务是对67P/Churyumov-Gerasimenko彗星进行研究.
- 之前的数据提供了对彗星表面的初步见解.
- 菲拉的第二次着陆地点的确切位置和性质尚未完全理解.
研究的目的:
- 为了调查之前未被发现的菲莱号在67P彗星上的第二次着陆地点.
- 分析暴露的原始水冰和相关材料的特性.
- * 确定彗星核的物理特征,包括压力强度和孔隙性.
主要方法:
- 在第二次着陆和随后的表面相互作用期间分析了菲拉的仪器数据.
- * 在登陆后19个月进行多仪器观测.
- * 在现场测量冰的压力强度和孔隙性.
主要成果:
- 菲拉的第二次着陆地点揭示了彗星岩石中的原始水冰.
- 暴露的冰与含有有机物质的深色物质混合在一起,具有特定的尘埃/冰质量比.
- 在现场测量显示原始冰的压力强度很低 (< 12 Pa) 和高孔径 (75 ± 7%).
结论:
- 彗星核的物理特性,特别是其冰冷的内部,已经受到限制.
- 这些发现为了解彗星的组成和演变提供了至关重要的数据.
- 结果为设计未来的着陆器提供了有价值的见解,
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