非均质含水层中渗流与溶质运移研究进展*
覃荣高1,2, 曹广祝2, 仵彦卿1,*

Review of Study on Groundwater Flow and Solute Transport in Heterogeneous Aquifer
Qin Ronggao1,2, Cao Guangzhu2, Wu Yanqing1
图1 不同类型渗流场及其相关渗流特性 K eff 为有效渗透系数, K a 为渗透系数算术平均值, K h 为渗透系数调和平均值（据文献[103]修改）
Fig. 1 Illustration of various types of fields and some results concerning their flow properties K eff is the effective conductivity, K a the arithmetic mean and K h the harmonic one modified from reference[103]