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根据热力学平衡理论绘制了铜的硫化矿物水系Eh—pH图,以铜矿床氧化带的宏观地质特征及铜矿物的微观结构演变为依据,重点分析了铜的硫化矿物在表生环境中的地电化学行为,对交代反应的实质及潜水面问题作了初步探讨。
Based on the thermodynamic equilibrium theory, the Eh-pH diagram of copper sulphide mineral water system was drawn. Based on the macroscopic geologic characteristics of copper oxidation belt and the microstructure evolution of copper minerals, the copper sulfide minerals in the superficial environment Geochemical behavior of the reaction to explain the substance and the surface of the dive made a preliminary discussion.