韩用德, 罗毅, 于强, 张海林. 非均匀土壤剖面的Green-Ampt模型[J]. 中国生态农业学报(中英文), 2001, 9(1): 31-33.
引用本文: 韩用德, 罗毅, 于强, 张海林. 非均匀土壤剖面的Green-Ampt模型[J]. 中国生态农业学报(中英文), 2001, 9(1): 31-33.
HAN Yong-De, LUO Yi, YU Qiang, ZHANG Hai-Lin. Green-Ampt model of non-uniform layered soil profile[J]. Chinese Journal of Eco-Agriculture, 2001, 9(1): 31-33.
Citation: HAN Yong-De, LUO Yi, YU Qiang, ZHANG Hai-Lin. Green-Ampt model of non-uniform layered soil profile[J]. Chinese Journal of Eco-Agriculture, 2001, 9(1): 31-33.

非均匀土壤剖面的Green-Ampt模型

Green-Ampt model of non-uniform layered soil profile

  • 摘要: 给出了相应条件下的Green-Ampt模型,入渗量、入渗速率、湿润层深度以及入渗时间的具体表达式,并对1次实测灌水入渗过程进行了模拟。结果表明,Green-Ampt模型计算的入渗时土壤水分剖面与水流连续方程的计算结果存在较大差别,但这种差别经过再分布后逐渐消失。在作较长时段的土壤水分动态模拟时利用Green-Ampt模型模拟入渗过程是适用的,特别是在已知入渗总量而未知入渗强度过程的情况下具有优越性。

     

    Abstract: The Green-Ampt model, formulas of infiltration rate and time under the condition of the layered soil profile were given in this paper. Both the equation and the continuity equation of soil water flow were used to simulate a field infiltration case and the simulated soil profiles were compared. The result show that there existed a great difference between the soil profiles simulated by the Green-Ampt equation and the continuity equation, but the difference disappeared quickly after some hours of redistribution of soil moisture. This indicates that the Green-Ampt equation can simulate the soil moisture profile of infiltration for the long-term simulation of soil moisture dynamics. Especially, when the infiltration water amount is available only, it is more advantageous than other methods.

     

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