地球缺少的可能不在地球核心
M Lagos1, C Ballhaus, C Münker
1Steinmann-Institut, Universität Bonn, Poppelsdorfer Schloss, 53115 Bonn, Germany. lagos@uni-bonn.de
Nature
|November 7, 2008
概括
地球 地球 地球 地球 地球 地球
科学领域:
- 地质化学 地质化学
- 行星科学 行星科学
- 同位素地质学的同位素.
背景情况:
- 地球的挥发性元素比CI的地铁更少.
- (Pb) 是挥发性的,其在地球上的耗尽是有争议的.
- 地球的地幔具有独特的同位素比率,表明积累后的Pb损失.
研究的目的:
- 研究金属硫化物-酸盐系统中的分离.
- 确定地球挥发性元素枯竭背后的机制,特别是.
- 将地球的赤字与行星形成和进化模型相协调.
主要方法:
- 在合成金属-硫化物-酸盐系统中进行分区实验.
- 在相关的行星条件下分析了分区系数.
- 利用同位素分析来限制损失模型.
主要成果:
- 不是足够的 siderophile 或 chalcophile 在核心中被隔离.
- 实验数据不支持硫化物融分离作为地球缺乏的主要机制.
- 损失不太可能仅仅通过将其分成核心来解释.
结论:
- 地球的赤字可能是由于挥发性物质的积累造成的.
- 月球形成撞击后通过脱气而导致的损失是一个合理的情景.
- 一个具有互补的同位素特征的深层地幔水库是可能的,但核心封存不太可能.
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