|
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 Ronggao 1,2 , Cao Guangzhu 2, Wu Yanqing 1
|
|
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] |
|
|
 |
|
|