Experimental and Theoretical Determination of Solubilities of Rock-Forming Minerals

首席研究员将通过实验确定几种具有重要地质意义的硅酸盐矿物在高温和高压下的平衡溶解度。测量将在含有盐、氩或二氧化碳的水溶液中进行。所得数据将用于模拟地壳变质过程中发生的流体-岩石相互作用。

The principal investigator will experimentally determine the equilibrium solubilities of several geologically important silicate minerals at elevated temperatures and pressures. Measurements will be made in aqueous solutions containing either salt, argon, or carbon dioxide. Resulting data will be used to model fluid-rock interactions that occur during metamorphism of the Earth's crust.