Thermal dispersion and solute dispersion, resulting from the discrepancies of pore water velocity, are important parameters in studying water, heat, and solute transport in porous media.
由土壤孔隙水流速率差异引起的热弥散和溶质弥散对于了解水热盐耦合运移非常重要。
This method is suitable for studying the problem on the dispersion of solute matter in arbitrary fluid models where velocity distributions through a circular tube are known.
本方法适用于研究已知圆管流速分布的任意流体模型中溶质的分散问题。
The traditional method of hydrogeological calculation is to set up a solute convection-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。
应用推荐