二氧化的结晶和地球核心的组成演变
Kei Hirose1, Guillaume Morard2, Ryosuke Sinmyo1
1Earth-Life Science Institute, Tokyo Institute of Technology, 2-12-1 Ookayama, Meguro, Tokyo 152-8550, Japan.
地球的核心含有和氧的杂质. 实验表明这种Fe-Si-O合金结晶了二氧化 (SiO2),可能导致早期的核心对流和发动机生成.
科学领域:
- 地质学
- 高压矿物物理
- 星球科学
背景情况:
- 地球的核心密度表明除了铁之外的轻元素杂质.
- 之前的研究集中在二进制Fe-Si和Fe-O系统上,使Fe-Si-O三进制在核心条件下缺乏研究.
研究的目的:
- 在地球核心压力和温度下调查Fe-Si-O三元合金的行为.
- 确定结晶产物和对核心形成和动态的影响.
主要方法:
- 在液体Fe-Si-O合金上进行化实验.
- 使用激光加热的钻石芯来实现高压 (40-60 GPa) 和高温 (~3,500 K).
主要成果:
- 在富含铁的Fe-Si-O三元系统中,二氧化 (SiO2) 的液体场异常宽.
- 一个初始的Fe-Si-O核心组成结晶SiO2随着冷却.
结论:
- SiO2的结晶释放了浮力,足以为哈迪时代的核心对流和发电机产生动力.
- SiO2和对外核当前的和氧度造成了约束.
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