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Green-Ampt Model for Layered Soils with Nonuniform Initial Water Content Under Unsteady Infiltration

机译:非恒定入渗条件下初始含水量不均匀的层状土壤的绿色安培模型

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摘要

The Green-Ampt equation is often used to estimate infiltration in hydrologic modeling. Only a few of the currently used simulation models, however, can simulate infiltration into a heterogeneous soil with nonuniform initial soil water content by the Green-Ampt equation during nonsteady rainfall. In this study, we derived an infiltration model for layered soils under nonsteady infiltration based on the Green-Ampt method (Green-Ampt for Layered Soils, or GALS). In the GALS model, a formula for estimating average suction (S) was derived to include initial soil water effect, and the soil profile was divided into several layers to consider both soil texture and initial soil moisture effects on infiltration. The new model can predict infiltration capacity, ponding time, and cumulative infiltration. Three infiltration experiments, steady-state infiltration into a layered soil with nonuniform initial soil water content, nonsteady infiltration into a layered soil with uniform soil water content; and nonsteady-state infiltration into a layered soil with nonuniform soil water content, were conducted for model testing. Comparison showed that the GALS model was in good agreement with another Green-Ampt-based model and the measured data.
机译:Green-Ampt方程通常用于估算水文模型中的入渗量。但是,目前只有少数几个模拟模型可以通过非稳定降雨过程中的Green-Ampt方程模拟初始土壤水含量不均匀的非均质土壤的入渗。在这项研究中,我们基于Green-Ampt方法(层状土壤的Green-Ampt或GALS)导出了非稳态渗透下的层状土壤入渗模型。在GALS模型中,推导了估算平均吸力(S)的公式,其中包括初始土壤水分效应,并将土壤剖面分为几层,以考虑土壤质地和初始土壤水分对入渗的影响。新模型可以预测渗透能力,蓄水时间和累积渗透。三个渗透实验,稳态渗入初始含水量不均匀的层状土壤,非稳定渗入均匀水含量的层状土壤;进行了非稳态渗入土壤含水量不均匀的层状土壤中进行模型测试。比较表明,GALS模型与另一个基于Green-Ampt的模型和实测数据非常吻合。

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