在地球核心地幔边界的FeHx和运输的稳定性
Yu He1, Duck Young Kim2, Viktor V Struzhkin3
1Key Laboratory of High-Temperature and High-Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China; Center for High Pressure Science and Technology Advanced Research, Shanghai 201203, China.
铁化物 (FeH) 在地球深层内部是稳定的,在较低的地幔条件下形成超离子状态. 这促进了气的运输,可能会在核心-地幔边界附近创造一个核心储库和富含氧气的斑块.
科学领域:
- 地质物理学 地质物理学
- 高压矿物物理 高压矿物物理
- 计算材料科学 计算材料科学
背景情况:
- 铁化物是由地球内部的水和铁反应形成的.
- 了解FeH对于模拟地球深处的运输至关重要.
研究的目的:
- 研究铁化物 (FeH) 在极端压力下的稳定性和性能.
- 确定地球深层内部的气运输潜力.
主要方法:
- 高压实验可以达到165 GPa.
- 最初的分子动力学模拟.
- 密度和化温度的计算.
主要成果:
- 面中心立方体 (fcc) FeH在165 GPa之前是稳定的.
- 在下层地幔条件下,fcc FeH 转化为超离子状态.
- 超离子FeH表现出高度扩散的离子,与液体Fe-H相比.
结论:
- 铁的稳定性和超离子性质有助于将运输到外核.
- 这一过程可能会在地球内部建立一个水库.
- 富含氧气的斑块可能会在核心-地幔边界上方形成,这是由于这种气运输.
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