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首页> 外文期刊>Irrigation and Drainage >Rainfall intensity and soil physical properties influence on infiltration and runoff under in-field rainwater harvesting conditions. (Special Issue: Rainwater harvesting and conservation techniques for improving household food security.)
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Rainfall intensity and soil physical properties influence on infiltration and runoff under in-field rainwater harvesting conditions. (Special Issue: Rainwater harvesting and conservation techniques for improving household food security.)

机译:在田间雨水收集条件下,降雨强度和土壤物理特性会影响入渗和径流。 (特刊:雨水收集和养护技术,以改善家庭粮食安全。)

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摘要

The objective of this study was to quantify the combined influence of rainfall intensity and soil physical properties on infiltration and runoff under in-field rainwater harvesting (IRWH). Rainfall intensities and soil physical properties were mathematically related to time to runoff, time to final infiltration rate and final infiltration rate. The influence of rainfall intensity and soil physical factors on rainwater harvesting under IRWH was demonstrated. A commercial field, divided into 75 plots and under IRWH located near Bloemfontein, South Africa, was used. Nine plots were selected to obtain the widest range of clay plus silt content possible. Three rainfall intensity treatments were applied using a mobile rainfall simulator. Before the start of the simulations soil samples were taken to determine the soil's physical properties. A multiple regression analysis showed that the infiltration and runoff process depended primarily on rainfall intensity and soil physical conditions. The in-field runoff analysis showed that for every 1 mm of rain that infiltrated in the runoff strip, between 2.18 and 6.48 mm would infiltrate in the basin strips. Thus, the soil types tested had a huge potential for water harvesting practices.
机译:这项研究的目的是量化降雨强度和土壤物理特性对田间雨水收集(IRWH)下入渗和径流的综合影响。降雨强度和土壤物理性质在数学上与径流时间,最终渗透率和最终渗透率有关。证明了降雨强度和土壤物理因素对IRWH条件下雨水收集的影响。使用了一个商业区域,该区域被划分为75个地块,位于南非布隆方丹附近的IRWH下。选择了九个样地以获得最大范围的粘土加粉砂含量。使用移动式降雨模拟器进行了三种降雨强度处理。在开始模拟之前,先采集土壤样品以确定土壤的物理性质。多元回归分析表明,入渗和径流过程主要取决于降雨强度和土壤物理条件。田间径流分析表明,径流带中每渗透1毫米雨水,盆地带中就会渗透2.18至6.48毫米。因此,测试的土壤类型在集水实践中具有巨大的潜力。

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