多点源滴灌条件下土壤水分运动的数值模拟

    Numerical simulation of soil water movement with drip irrigation of multiple point source

    • 摘要: 为了摸清多点源滴灌条件下的土壤水分运动规律,为密植作物滴灌系统的合理设计提供依据,本文根据非饱和土壤水动力学理论和多点源滴灌条件下土壤水分运动特征,建立了多点源滴灌条件下土壤水分运动数学模型,利用商业化软件Hydrus对模型进行了求解。模拟结果与实测情况对照表明,模拟的入渗过程与实测的入渗过程基本吻合,均遵循点源入渗、湿润区交汇和最终形成湿润带的演变规律;模拟的交汇时间和入渗深度与实测的相比,偏差均在10%以内;在湿润锋交汇前,湿润区内部土壤含水率模拟值与实测值的差异较小,吻合较好,在湿润锋交汇后,湿润区上部土壤含水率的模拟值要比实测值小一些。总体而言,模拟结果还是能比较真实地反映多点源滴灌条件下的土壤水分运动规律,可为滴灌系统的合理设计及运行提供一定的理论依据。

       

      Abstract: In order to provide the theory guidance for drip system design to the high density planting crop, based on the theory of unsaturated soil water dynamics and the character of soil water movement with drip irrigation from multiple point sources, the mathematic model was established and solved numerically by using the Hydrus software. Compared with the actual infiltration process, the simulated infiltration process is in agreement with actual infiltration process. The infiltration processes include three stages which are infiltration from point source, wetting front overlapped and forming wetting belt. The deviation of time of wetting front overlapped and infiltration depth between simulated and actual processes is less than 10%. There is a little difference between simulated and actual soil water content before wetting front overlapped. After wetting front overlapped, simulated soil water content is less than actual soil water content in the upper part of wetting zone. Generally speaking, simulated results can reflect the regulation of soil water movement with drip irrigation from line source, and it can provide the theory guidance for drip system design.

       

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