在酸盐中Cu的氧化状态在上层地幔条件下融化
Xingcheng Liu1,2, Lei Zhang3,4, Sanyuan Zhu5
1State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, 510640, China. Liuxingcheng@gig.ac.cn.
酸盐中的铜 (Cu) 即使在氧化条件下也主要是Cu+,这限制了其作为氧气逃逸性代理物的使用. 相反,同位素在地球深层追踪了岩石硫化物的演变.
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:
- 铜 (Cu) 在经济上具有重要意义,是深层岩过程的关键标记物.
- Cu的行为与岩硫化物演变和氧气流动性 (fO2) 有关.
- 确定酸盐融中的Cu氧化状态 (Cu+或Cu2+) 对于了解地球内部至关重要,但具有挑战性.
研究的目的:
- 研究铜 (Cu) 在水性性酸盐中的氧化状态.
- 评估Cu对氧气流动性 (fO2),温度和压力的敏感性.
- 评估Cu在地球深层岩系统中作为氧气计的实用性.
主要方法:
- 使用的X射线吸收近边缘结构 (XANES) 光谱.
- 在受控的fO2,温度和压力下分析的氧化状态.
- 在与上层地幔相关的条件下 (11501300 °C,1.02.5 GPa) 均衡地化.
主要成果:
- 铜主要以Cu+的形式存在于酸盐中,在一系列的fO2条件下 (-1.8到3.1日志单位) 融化.
- 观察到较小的Cu2+成分,但Cu+即使在相对氧化的化物中仍然占主导地位.
- 在研究的上层地幔条件下,Cu的氧化状态对fO2的敏感性有限.
结论:
- +的占主导地位限制了使用作为氧气计在来自地球深层的水性酸盐化物中.
- 同位素似乎对硫化物分离和积累在岩分化过程中更敏感.
- 这项研究提供了对地球深层岩过程和友元素行为的洞察.
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