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Evaluation of surface irrigation as a function of water infiltration in cultivated soils in the Nile Delta.

机译:评估尼罗河三角洲耕地土壤中地表灌溉与水分渗透的关系。

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As sources of irrigation water are decreasing, efficient use of surface irrigation is essential. The purpose of this study is to determine if partially-wetted furrow irrigation has more efficient water storage and infiltration than traditional border irrigation in an alluvial clay soil under cultivated grape production. The two irrigation components considered were wet (WT) and dry (DT) treatments, at which water was 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. 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 11.9 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 dry furrow and traditional border irrigation, where application efficiency achieved as 88.1% for wet furrow irrigation that achieved high grape fruit yield (30.71 Mg /ha). The infiltration (cumulative depth, Z and rate, I) was functioned to opportunity time (t0) in minute for WT and DT treatments as: ZWT=0.528t00.6, ZDT=1.2t00.501, IWT=19t0-0.4, IDT=36t0-0.498. 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 irrigation parameters and coefficients, and soil water distribution have been also evaluated.Digital Object Identifier http://dx.doi.org/10.1007/s10795-012-9130-9
机译:随着灌溉水源的减少,有效利用地表灌溉至关重要。这项研究的目的是确定在葡萄栽培条件下的冲积粘土中,部分湿润的沟渠灌溉是否比传统的边界灌溉具有更有效的储水和入渗作用。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。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11.9%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,部分湿润的沟灌溉具有更高的水利用效率和葡萄产量,湿沟灌溉的施肥效率达到了葡萄果实高产量(30.71 Mg / ha)的88.1%。 WT和DT处理的渗透量(累积深度,Z和速率I)以分钟为单位的机会时间(t 0 )起作用:Z WT = 0.528t < sub> 0 0.6 ,Z DT = 1.2t 0 0.501 ,I WT = 19t 0 -0.4 ,I DT = 36t 0 -0.498 。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。还对灌溉参数和系数以及土壤水分分布进行了评估。数字对象标识符http://dx.doi.org/10.1007/s10795-012-9130-9

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