在地球深层内部的挥发性元素的铁合金
Yifan Tian1,2, Peiyu Zhang1,2, Wei Zhang1,2
1Key Laboratory of Material Simulation Methods and Software of Ministry of Education, College of Physics, Jilin University, Changchun, 130012, China.
Nature communications
|April 18, 2024
概括
和等挥发性元素可能被隔离在地球的核心. 第一原则的模拟表明,这些元素可以与铁合金形成,解释了它们在酸盐地球上的枯竭.
科学领域:
- 地化学和行星科学 地球化学和行星科学
- 计算材料科学科学 计算材料科学
背景情况:
- 地球的酸盐部分不典型的挥发性元素度是理解行星演变的关键.
- "挥发性趋势"解释了一些挥发性元素的耗尽,但 (Se) 和 (Br) 仍然无法解释.
- 了解挥发性元素的行为对于准确的地球组成模型至关重要.
研究的目的:
- 为了研究挥发性元素 (Se, Br) 在地球核心中的潜在结合.
- 探索六角密封铁 (hcp-Fe) 中替代合金的形成,这是一个假定的核心成分.
- 为了确定对隔离的挥发性元素的潜在的地球深层储库.
主要方法:
- 利用第一原则模拟来模拟挥发性元素的行为.
- 研究了挥发性元素和hcp-Fe.Fe.之间形成的合金的热力学稳定性.
- 分析了地球核心中替代合金形成的潜力.
主要成果:
- 第一个原则的模拟证明了Se和Br在hcp-Fe中整合的潜力.
- 这些合金的热力学稳定性表明,在地球核心内封存是合理的.
- 这些发现挑战了仅仅依赖"波动性趋势"来解释Se和Br的枯竭.
结论:
- 挥发性元素,包括Se和Br,可能部分被隔离在地球的核心.
- 核心中的替代合金代表了这些元素的重要,以前被低估的储备库.
- 这项研究增强了我们对地球深层构成和挥发性元素循环的理解.
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