随着时间的推移而增加的地球材料的同位素性质
1Origins Laboratory, Department of the Geophysical Sciences and Enrico Fermi Institute, The University of Chicago, 5734 South Ellis Avenue, Chicago, Illinois 60637, USA.
Nature
|January 28, 2017
概括
地球
科学领域:
- 星球科学
- 同位素地化学
- 宇宙化学
背景情况:
- 地球是由未知的同位素组成的行星胚胎形成的.
- 地球和月球的同位素相似性挑战了异质积累的模型.
- 石与地球和月球具有同位素的相似性.
研究的目的:
- 解读地球积聚物质的同位素性质, 使用具有不同金属亲和力的元素.
- 为了使地球和月球的同位素相似性与积累模型相协调.
- 研究恩斯塔石的起源及其与地球形成的关系.
主要方法:
- 地球,月球和石的高精度同位素测量.
- 对石质 (O,Ca,Ti,Nd),中度 siderophile (Cr,Ni,Mo) 和高度 siderophile (Ru) 元素的分析.
- 积累过程和同位素进化的建模.
主要成果:
- 具有明显的金属亲和度的元素显示出不同的增积阶段.
- 所有分析的元素都显示出同位素与石的相似性.
- 地球的积累涉及到大量的石类型的物质,特别是在其形成的后期.
结论:
- 地球和静态石起源于同一个同位素储库.
- 月球形成的撞击体可能具有与地球相似的同位素组成.
- 化学进化因随后的星云和行星分离过程而分离.
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