根据水流推进过程预测Horton入渗公式参数和田面平均糙率系数

    Estimation of Horton infiltration equation parameters and field-averaged roughness coefficient by surface irrigation advance

    • 摘要: 通过分析畦田水流特征,结合Horton入渗公式,在满宁公式的基础上,根据水量平衡原理建立了利用水流推进过程确定土壤入渗参数和田面糙率系数的方法。同时,利用实验资料对所提出的方法进行了检验,结果表明利用该方法所推求的入渗参数和糙率系数,零惯量模型预测的推进过程和消退过程与实测数据相一致。

       

      Abstract: Based on the analyses of water stream and irrigation advance, two functions were given to describe irrigation advance and water depth profile. A method for estimation of Manning roughness coefficient was developed through adopting Manning equation for water flow. Combining with Horton infiltration equation, the solution for estimation of infiltration properties was established based on the water volume balance. The method was evaluated by the field experimental data, and the results indicate that the predicted irrigation advance and recession of SRFR4.06 with the parameters obtained by the new method go well with the observed.

       

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