浑水入渗机制及模拟模型研究

    Mechanism and Simulating Model for Muddy Water Infiltration

    • 摘要: 泥沙的沉积会改变土壤表面特性、影响土壤的入渗特性。但目前对此问题仅是通过实验研究,未形成具有物理机制的计算土壤入渗过程的模型,不利于根据现代土壤物理方法描述浑水入渗过程。该文通过对浑水入渗特性和浑水入渗规律的分析,对现有的Green-Ampt入渗模式进行改进,将泥沙沉积对入渗的影响归结为对湿润锋平均吸力的影响。这样有利于利用现有清水入渗模式来计算浑水入渗过程。并且利用室内模拟实验资料对模型进行检验,检验结果表明该模型是合理的。

       

      Abstract: The sediment will deposit on the surface of irrigated soils when the muddy water is used to irrigate. The deposition layer will change the surface features of irrigated soils. Therefore infiltration features of muddy water is different from that of clean water. But these problems have been only researched by the way of experiment and there are not any models with physical bases to forecast the infiltration processes of muddy water. In the paper the original Green-Ampt Equation was modified based on the analyses of infiltration features of muddy water. Effect of deposited sediment on infiltration was reflected by the average suction of wetting front. And the modified Green-Ampt Equation was convenient to calculate the infiltration process through existed infiltration data for clean water infiltration. The modified Green-Ampt Equation was checked by lab experimental data and the result indicated that the model is reasonable.

       

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