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Emitter selection and operation strategies for drip irrigation based on three-dimensional soil wetting patterns

机译:基于三维土壤润湿模式的滴灌滴头选择及运行策略

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摘要

Distance between consecutive emitters along the irrigation lateral, and irrigation frequency for trickle irrigation systems, are defined in relation to 3-dimensional soil wetting patterns, obtained from infiltration curves based on a modified Green-Ampt approach. Soil wetting patterns developing under a water surface point source located at the soil surface with unlimited supply, is represented by the time-soil infiltrability distribution function. After an extended period of water supply, soil infiltrability rates usually described for one and two dimensional infiltration; this is a result of the continuous expansion of the hemispherical wetting front, that can offset the effect of diminshing soil water potential gradients on water flow rates inside the wetted soil volume. This consideration may explain the differences in wetted soil volumes obtained under field conditions, when 100 % ETc is provided to a crop on a daily basis, as compared with irrigation events taking place every, third or fourth day. Adjusting emitter discharge to match average soil infiltrability, enables an accurate description of the soil wetting process for the case of a constant discharge emitter. Thus, for different soils and irrigation frequency strategies, soil wetted patterns (maximum wetting depth and wetted radius) can be predicted. Several examples are analyzed to compare wetting patterns and volumes, in order to define more accurately the best: emitter density on the irrigation lateral, application time, emitter discharge, and irrigation frequency, when 100 % ETc accumulated from the last irrigation event is supplied to the crop.
机译:相对于3维土壤润湿模式,定义了沿滴灌灌溉系统的连续排放源之间的距离以及滴灌系统的灌溉频率,这些模式是根据改进的Green-Ampt方法从入渗曲线获得的。时间-土壤渗透性分布函数代表了位于土壤表层的水面点源在无限供应下的土壤润湿模式。长期供水后,通常描述的一维和二维渗透的土壤渗透率;这是半球形湿润锋面持续扩张的结果,可以抵消土壤水势梯度减小对湿润土壤体积内水流速的影响。与每天,第三天或第四天发生的灌溉事件相比,每天向作物提供100%ETc时,这种考虑可以解释在田间条件下获得的湿润土壤量的差异。调整发射器的排放量以匹配平均土壤渗透性,可以在排放恒定的情况下准确描述土壤的润湿过程。因此,对于不同的土壤和灌溉频率策略,可以预测出土壤的湿润模式(最大湿润深度和湿润半径)。分析了几个例子,比较了润湿模式和数量,以便更准确地定义最佳方案:从上次灌溉事件中累积的100%ETc被提供给灌溉侧的喷头密度,施用时间,喷头排放和灌溉频率。庄稼。

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