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Effects of water infiltration and storage in cultivated soil on surface irrigation

机译:耕地土壤水分入渗和入渗对地表灌溉的影响

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a- The irrigation functions, phases, coefficients, and soil water storage and distribution have been evaluated in a grape field. Empirical power form equations were obtained for measured advance and recession times and infiltration depths along the furrows and border lengths during the irrigation stages of advance, storage, depletion and recession. a- We concluded that the short irrigation interval using furrow irrigation with little amount of water (wet treatment) was better than far interval with large amount of water per irrigation (dry treatment). Grape yield was highly decreased due to increasing irrigation interval and insignificantly affected by increasing amount of water per irrigation. a- The partially-wetted furrow irrigation had greater water-efficiency and grape yield than dry furrow treatment and traditional border irrigation. The wet treatment achieved 11.9kg/m3 water use efficiency (WUE) with 11.9% deep seepage percentage compared with 9.9kg/m3 WUE with 18.9% deep seepage under furrow dry treatment. Surface irrigation analysis and design require the knowledge of the variation of the cumulative infiltration water Z (L) (per unit area) into the soil as a function of the infiltration time t (T). The purpose of this study is to evaluate water infiltration and storage under surface irrigation in an alluvial clay soil cultivated with grape yield, and to determine if partially wetted furrow irrigation has more efficient water storage and infiltration than traditional border irrigation. The two irrigation components considered were wet (WT) and dry (DT) treatments, at which water applied when available soil water reached 65% and 50%, and the traditional border irrigation control. Empirical power form equations were obtained for measured advance and recession times along the furrow length during the irrigation stages of advance, storage, depletion and recession. The infiltration (cumulative depth, Z and rate, I) was functioned to opportunity time (t o ) in minute for WT and DT treatments as: Z WT =0.528 t o 0.6, Z DT =1.2 t o 0.501, I WT =19 t o a degree 0.4, and I DT =36 t o a degree 0.498. The irrigation efficiency and soil water distribution have been evaluated using linear distribution and relative schedule depth. Coefficient of variation (CV) was 5.2 and 9.5% for WT and DT under furrow irrigation system comparing with 7.8% in border, respectively. Water was deeply percolated as 11.88 and 19.2% for wet and dry furrow treatments, respectively, compared with 12.8% for control, with no deficit in the irrigated area. Partially wetted furrow irrigation had greater water-efficiency and grape yield than both dry furrow and traditional border irrigations, where application efficiency achieved as 88.1% for wet furrow irrigation that achieved high grape fruit yield (30.71Mg/ha) and water use efficiency 11.9kg/m3.
机译:a-已经在葡萄田中评估了灌溉功能,阶段,系数以及土壤水的存储和分配。获得了经验的功率形式方程,用于测量提前,存储,枯竭和后退灌溉阶段沿沟和边界长度的提前和后退时间以及渗透深度。 a-我们得出的结论是,使用少量水进行沟灌(湿处理)的短灌溉间隔要好于每次灌溉中大量水的干间隔(干处理)。由于增加灌溉间隔,葡萄产量大大降低,而每次灌溉增加的水量对葡萄产量影响不大。 a-半干沟灌溉比干沟处理和传统边界灌溉具有更高的水利用效率和葡萄产量。在fur沟干法处理下,湿处理达到11.9kg / m3的水分利用效率(WUE),深层渗透率为11.9%,而9.9kg / m3的WUE为18.9%。地表灌溉分析和设计需要了解土壤中累积入渗水Z(L)(每单位面积)随入渗时间t(T)的变化。这项研究的目的是评估在表层灌溉条件下葡萄收获的冲积粘土中的水分入渗和储水,并确定部分湿润的沟灌是否比传统的边界灌溉更有效的储水和入水。考虑的两个灌溉要素是湿法(WT)和干法(DT)处理,当可用土壤水分别达到65%和50%时,要施加水,以及传统的边界灌溉控制。在前进,贮存,枯竭和后退的灌溉阶段,针对沿犁沟长度的前进和后退时间,获得了经验功率形式方程。对于WT和DT处理,渗透(累积深度,Z和速率I)的作用是每分钟机会时间(to),如:Z WT = 0.528至0.6,Z DT = 1.2至0.501,I WT = 19至0.4 ,并且I DT = 36 toa度0.498。使用线性分布和相对进度深度对灌溉效率和土壤水分分布进行了评估。在沟灌系统中,WT和DT的变异系数(CV)分别为5.2和9.5%,而边界处的变异系数(CV)分别为7.8%。湿沟和干沟处理的水渗透深度分别为11.88%和19.2%,而对照水的渗透率为12.8%,灌溉区域没有赤字。与干沟和传统边界灌溉相比,半湿沟灌溉具有更高的水效率和葡萄产量,湿沟灌溉的施用效率达到了88.1%,湿沟灌溉获得了较高的葡萄果实产量(30.71Mg / ha)和水利用效率11.9kg /立方米。

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