The surface soilwatercontent was close with different mineralization degree levels water, which approached saturated water content.
不同矿化度的水入渗后,土壤表层含水率基本相近,接近饱和含水率。
2
The coefficient of variation of saturatedwatercontent decreased with the depth of profile. The coefficient of variation of bulk density and field capacity fluctuate with depth of soil.
饱和含水量的变异系数都随深度的增加逐渐降低,含水量、容重和田闷持水量的变异系数随深度的呈波动变化。
3
Sensitivity analysis of model parameters showed: Saturated hydraulic conductivity is the most sensitive factor for two soil groups, and saturatedwatercontent takes second place.