• The surface soil water content was close with different mineralization degree levels water, which approached saturated water content.

    不同矿化度入渗后,土壤表层含水率基本相近接近饱和含水率

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  • The coefficient of variation of saturated water content 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

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  • Sensitivity analysis of model parameters showed: Saturated hydraulic conductivity is the most sensitive factor for two soil groups, and saturated water content takes second place.

    模型参数敏感性分析表明饱和水力传导度敏感参数,饱和含水量的敏感性次之

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  • Sensitivity analysis of model parameters showed: Saturated hydraulic conductivity is the most sensitive factor for two soil groups, and saturated water content takes second place.

    模型参数敏感性分析表明饱和水力传导度敏感参数,饱和含水量的敏感性次之

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