铁铁稳定在深层岩海洋条件下
Hongluo L Zhang1, Marc M Hirschmann2, Oliver T Lord3
1State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China.
Science advances
|October 16, 2024
概括
早期的地球地球.
科学领域:
- 行星科学 行星科学
- 地质化学 地质化学
- 高压地质物理学 高压地质物理学
背景情况:
- 早期地球上的岩海洋影响了它的氧化还原状态和大气.
- 之前对岩海洋中铁氧化物的研究产生了相互矛盾的结果.
研究的目的:
- 为了确定铁的氧化状态 (Fe3+/ΣFe) 在深海的岩海洋.
- 了解对地球早期大气和氧化还原预算的影响.
主要方法:
- 在高压 (38-71 GPa) 和高温 (3600-4400 K) 下,对与铁合金平衡的融体进行实验.
- 使用同步子Mössbauer光谱学分析灭的玻璃.
主要成果:
- 在28-53GPa时,Fe3+/ΣFe比率从0.056到0.112不等.
- 这些值表明足够的Fe2O3产量可以解释地球的大规模酸盐氧化还原预算.
结论:
- 深海的岩海洋条件形成了氧化环境.
- 这支持了富含一氧化碳和水的原始大气.
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