在高压下将硫分离到水性流体和性溶液之间:对潜水带中的硫迁移的影响
Lanqin Li1,2, Xingcheng Liu3,4, Ting Xu1
1State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, 510640, China.
Scientific reports
|February 5, 2025
概括
硫主要溶解在水性流体中,而不是在潜水区的化物中. 岩中的这种硫运输是形成巨大的矿石沉积物和推动火山爆发的关键.
科学领域:
- 地质化学 地质化学
- 石化学 石化学是一门学科.
- 火山学 火山学是一门学科.
背景情况:
- 硫是潜伏区 magmaism 中的一个必不可少的挥发物.
- 硫在水性液体中的溶解度超过了酸溶液中的溶解度.
- 了解硫分离对于岩生成和演化至关重要.
研究的目的:
- 研究水性流体和酸溶液之间的硫分区.
- 确定压力,氧气流动性,融化和流体组成对硫分区的影响.
主要方法:
- 在950°C和1-2 GPa下进行的活塞气实验.
- 多样化的氧气流动性 (Ni-NiO,Re-ReO2缓冲器),融成分和液体盐度.
- 测量的硫分区系数 (DS流体/融化).
主要成果:
- 硫分区系数 (DS流体/融化) 始终高 (>1),有利于水性流体.
- DS流体/融体随着压力从1到2 GPa的增加而下降.
- 在还原条件下,DS流体/溶液从147±40下降到20±2;在氧化条件下,从27±1下降到20±2.2.
结论:
- 硫在潜水带的高压下对水性流体表现出强烈的亲和力.
- 和液体的岩岩能有效地运输硫,影响矿石矿床的形成和火山气体的释放.
- 这项研究阐明了硫在潜水区过程和相关地质现象中的作用.
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