The traditional method of hydrogeological calculation is to set up a soluteconvection-dispersion model.
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。
2
A graphing method is proposed in this paper for estimating parameters of solute transport in soils based on the convection-dispersion equation (CDE).
基于土壤中溶质运移的对流弥散方程(CDE)提出了溶质运移参数估计的图解方法。
3
Due to the effects of convection, the solute will be washed from upstream to downstream, resulting in the upstream concentration lower than the downstream one in the liquid alloy.