潜水区流体pH对金属和挥发性循环的影响
Matthieu E Galvez1, James A D Connolly1, Craig E Manning2
1Earth Sciences Department, Swiss Federal Institute of Technology, CH-8092 Zurich, Switzerland.
Nature
|November 18, 2016
概括
潜水区的液体有轻微的性,pH值由岩石组成和挥发性含量控制. 这影响了金属和挥发性元素在地质时间尺度上的全球循环.
科学领域:
- 地球科学
- 地质化学
- 地动力学
背景情况:
- 水性流体化学控制着地球的金属和挥发性元素循环.
- 潜伏区是流体介导化学交换的关键设置.
- 描述潜水区流体物种和pH值是一个重要的科学挑战.
研究的目的:
- 预测潜伏区中的流体岩石平衡.
- 连接热结构,矿物学和流体物种化模型.
- 了解液体pH的控制及其对元素循环的影响.
主要方法:
- 流体岩石平衡的热力学预测.
- 潜水区的热结构和矿物学的建模.
- 在不同的岩石组成下分析流体物种化.
主要成果:
- 在地石质中,潜水区液体具有轻微的性pH值.
- 液体的pH值由岩石挥发物和含量进行调节.
- 低温降温保存氧化碳;地幔液的pH对岩石组成敏感.
结论:
- 液体的pH值变化与岩石组成,地内分化和地液体透有关.
- 岩石组成的微小变化对地幔液的pH有显著的影响.
- 大气-海洋化学和潜水区流体物种化之间存在反.
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