在地球核心中以身体为中心的立方铁合金
L Dubrovinsky1, N Dubrovinskaia, O Narygina
1Bayerisches Geoinstitut, Universität Bayreuth, D-95440 Bayreuth, Germany.
概括
地球的核心可能含有铁合金. 高压,高温实验表明,这种合金采用以身体为中心的立方体结构,支持地球深层内部的模型.
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
- 宇宙化学 宇宙化学
背景情况:
- 地质化学和地质物理证据表明,地球的核心由铁组成,含有相当大的含量 (5-15%).
- 在核心条件下了解铁合金的结构和行为对于建模行星内部至关重要.
研究的目的:
- 在极端的压力和温度下研究铁合金 (Fe{0.9) Ni{0.1)) 的现场结构和特性.
- 为了确定与地球核心组成相关的铁合金的相位行为.
主要方法:
- 在现场角度分散式X射线衍射使用内部加热的钻石天细胞 (DAC).
- 测量电阻作为压力和温度的函数.
- 在模拟核心条件下对合金行为进行实验和理论分析.
主要成果:
- 铁合金Fe ((0.9) Ni ((0.1) 在超过225 GPa的压力和超过3400 K的温度下被观察到采用身体中心立方体 (bcc) 结构.
- 实验结果与理论预测一致,并支持对纯铁的冲击波数据的解释,表明固体-固体相位过渡约为200 GPa.
结论:
- 这项研究支持这样一个假设:具有地化学可信组成的铁合金 (包括,硫或) 可能形成地球内核中观察到的以身体为中心的立方体结构.
- 这些发现完善了我们对核心组成和结构的理解,为行星形成和进化的模型做出了贡献.
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