将超临界流体视为膨胀液体，根据溶液理论，建立了计算溶质在超临界流体中溶解度的膨胀液体模型。
An expanded liquid model (ELM) for solid solute solubility in supercritical fluids was proposed based on the assumption that the supercritical fluid was considered as an expanded liquid.
解决该问题传统的水文地质计算方法就是建立一个溶质对流—弥散模型。
The traditional method of hydrogeological calculation is to set up a solute convection-dispersion model.
计算结果与实验结果比较表明此数学模型是可行的，有可能用于测量和研究水流速度、泥沙含量及溶质在水流中的分布。
Comparing the calculated and experiment results show that the mathematical model is feasible and may be used to measure and study the velocity of sheet flow, sediment and the distribution of solute.
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