硫物种和黄金在弧形磁流体中的运输
Stefan Farsang1, Zoltán Zajacz1
1Department of Earth Sciences, University of Geneva, Geneva, Switzerland.
概括
岩石流体中硫的特异化影响地球的氧化还原循环和矿石形成. 这项研究揭示了硫化 (HS-) 和硫化 (H2S) 是关键的,影响水热系统中的黄金溶解度.
科学领域:
- 地质化学 地质化学
- 矿物学是什么?矿物学是什么?
- 石化学 石化学是一门学科.
背景情况:
- 磁性流体中的硫种对全球氧化还原循环,气候和关键金属矿石沉积物形成至关重要.
- 了解上层地岩中的硫分类是必不可少的,但仍然不清楚.
研究的目的:
- 在地质上相关的压力-温度-氧化还原条件下,在弧形磁性流体类似物中确定硫分类.
- 为了研究不同硫种在岩热水流体内黄金溶解度中的作用.
主要方法:
- 在现场分析使用原型压力容器装置.
- 拉曼光谱法用于在实验液体中识别硫物种.
主要成果:
- 硫化 (HS-),硫化 (H2S) 和二氧化硫 (SO2) 被确定为主要的硫物种.
- 发现S6+物种和硫基离子 (S2−,S3−) 的度可以忽略不计.
- 当硫主要是HS-和H2S时,测量的黄金溶解度最高,超过了热力学预测.
结论:
- HS-和H2S,而不是硫基,是导致岩热水流体中的高金溶度的原因.
- 磁性硫除气是氧化条件下的氧化还原过程,可能会增加磁性氧化.
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