在地球的深层地幔中保留了大量的水
Wenhua Lu1,2, Ya-Nan Yang1,2, Tao Long3
1State Key Laboratory of Deep Earth Processes and Resources, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences (CAS), Guangzhou, China.
概括
地球的早期
科学领域:
- 地质化学
- 矿物物理
- 星球科学
背景情况:
- 地球的水获取发生在早期,化的阶段通过冲击.
- 在结晶地中保持和分配水的机制是未知的.
研究的目的:
- 在高压下调查桥石和融之间的水分离.
- 确定温度如何影响水融入主要地幔矿物质.
主要方法:
- 系统的高压实验.
- 水分系数的分析.
主要成果:
- 随着温度的增加,水分离成桥石显著增加.
- 暗示下层地幔在结晶后存在大量的水留.
结论:
- 下层地幔中早期储存的水可能会影响地幔对流.
- 在地球向宜居星球的转变中发挥了潜在的作用.
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