高温高压下水流体中石英溶解度研究进展
A Progress on Quartz Solubility in Aqueous Fluids at High Temperature and High Pressure
查看参考文献50篇
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文摘
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高温高压水流体中矿物的溶解度是研究地球内部水流体-固体相互作用过程中元素活化、迁移和沉淀以及热液组成、性状及演化的必备参数。石英作为地壳最基本的组成矿物,其在高温高压水流体中的溶解度在地球内部热液作用研究中具有极为重要的意义,迄今已有许多学者对石英在高温高压水流体中的溶解度作过研究。本文通过系统总结前人有关研究成果,从实验技术、影响因素以及石英的赋存状态和溶解度模型等方面介绍了高温高压水流体中石英溶解度的研究进展,对目前该研究存在的问题作出了评述,并对未来该研究的发展趋势进行了预测。 |
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其他语种文摘
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As an essential parameter, solubility of minerals in aqueous fluids at high temperature under high pressure plays a key role in understanding the element activation, migration and precipitation during interaction of aqueous-solid in the internal earth. Meanwhile, it is also important to focus in the composition, property and evolution of fluids. Study on the solubility of quartz, one of the most basic minerals of the Earth, in water and aqueous solutions is important to the study on hydrothermal fluids, and has been conducted by many researchers. In this article, the research progress is reviewed on the following aspects, the experimental techniques, the composition of aqueous systems, the impact factors and other effects, as well as the further prospect. |
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来源
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矿物学报
,2013,33(1):75-82 【核心库】
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关键词
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高温高压
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水流体
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石英
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溶解度
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研究进展
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地址
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中国科学院地球化学研究所地球内部物质高温高压实验室, 贵州, 贵阳, 550002
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语种
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中文 |
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文献类型
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综述型 |
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ISSN
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1000-4734 |
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学科
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地质学 |
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基金
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国家自然科学基金项目
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中国科学院大型设备研制项目
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文献收藏号
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CSCD:4798333
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