This article discusses the hydrogeochemical differences among four pouring water aquifers and the causes.

探讨了四个突水含水层水文地球化学特征差异及原因.

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Simulation experiments based on hydrogeochemical thermodynamics analysis are the basic research methods of the subject.

其研究方法是在水文地球化学热力学分析基础上的模拟实验方法.

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Moreover this apper studies hydrogeochemical critical value of solute precipitation according to compute saturation index.

通过计算饱和指数,确定溶质水解沉淀的水文地球化学条件临界值.

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