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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。
The solubility of minerals in high-temperature and high-pressure water is a necessary parameter to study the activation, migration and deposition of elements and the composition, properties and evolution of hydrothermal fluids in the fluid-solid interaction. Quartz, as the most basic component of the crust, its solubility in high temperature and high pressure water fluids is of great significance in the study of the hydrothermal effect inside the Earth. So far, many scholars have studied the solubility of quartz in high temperature and pressure water fluids . This paper summarizes the previous research results systematically, and introduces the research progress of quartz solubility in high temperature and high pressure water fluid from the aspects of experimental techniques, influencing factors, the occurrence state and solubility model of quartz, and reviews the existing problems in this research , And forecast the development trend of this research in the future.