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首页> 外文期刊>Journal of Hydrology >Radial water infiltration-advance-evaporation processes during irrigation using point source emitters in rigid and swelling soils
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Radial water infiltration-advance-evaporation processes during irrigation using point source emitters in rigid and swelling soils

机译:在刚性和膨胀土壤中使用点源辐射器灌溉期间的径向水渗透-提前蒸发过程

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In this paper we investigate the dynamic water balance of radial flows during irrigation using point source emitters. The components of radial flows of this kind include infiltration simultaneously coupled to the storage and advance on the soil surface, and evaporation into the air while the source continuously supplies water. The soils we consider here can be rigid or swelling. Because the infiltration equations reported for both rigid and swelling soils have an identical mathematical structure, the analysis for rigid soils using Philip's two-term infiltration equation applies to both swelling and rigid soils. As such, we emphasise that our analysis is applicable to both rigid and swelling soils. We first extend the radial Lewis-Milne equation (RLME) given by Rasmussen to analyse the radial flow mechanics by incorporating evaporation as a key component in the radial dynamic water balance. Then we present a set of four solutions of the RLME using Philip's two-parameter infiltration equation and two-term and three-term equations for cumulative evaporation. With the two-term cumulative evaporation equation, we show that the three solutions yield a simple identical asymptotic formulae at large times, which can be used to design the area to be irrigated, or to derive the final infiltration rate, A, and the final evaporation rate, E-2. Analyses show that evaporation plays an important role in the radial dynamic water balance at large times, and as expected it plays a minor role during the early stage of irrigation (small time solutions). (c) 2007 Elsevier B.V. All rights reserved.
机译:在本文中,我们使用点源发射器研究了灌溉过程中径向流的动态水平衡。此类径向流的组成部分包括同时与存储耦合并在土壤表面前进的渗透,以及在水源不断供应水的同时蒸发到空气中。我们在这里考虑的土壤可能是刚性的或膨胀的。由于所报告的针对刚性土壤和膨胀土壤的渗透方程具有相同的数学结构,因此使用Philip的两项渗透方程对刚性土壤进行的分析适用于膨胀土壤和刚性土壤。因此,我们强调我们的分析适用于刚性和膨胀性土壤。我们首先扩展Rasmussen给出的径向Lewis-Milne方程(RLME),通过将蒸发作为径向动态水平衡的关键组成部分来分析径向流力学。然后,我们使用Philip的两参数渗透方程以及两,三项方程对累积蒸发提出了RLME的四个解。利用两项累积蒸发方程,我们证明了这三种解决方案在大量时间内产生了一个简单的相同渐近公式,可用于设计要灌溉的面积,或得出最终的入渗率A和最终的蒸发速率,E-2。分析表明,蒸发在很大的时间里对径向动态水平衡起着重要的作用,并且正如所预期的,在灌溉的早期阶段(小的时间解决方案),蒸发起着很小的作用。 (c)2007 Elsevier B.V.保留所有权利。

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