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首页> 外文期刊>Irrigation Science >Modeling irrigated cotton with shallow groundwater in the Aral Sea Basin of Uzbekistan: I. Water dynamics
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Modeling irrigated cotton with shallow groundwater in the Aral Sea Basin of Uzbekistan: I. Water dynamics

机译:乌兹别克斯坦咸海盆地浅水灌溉棉花的建模:I.水动力学

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In Khorezm, a region located in the Aral Sea basin of Uzbekistan, water use for irrigation of predominantly cotton is high whereas water use efficiency is low. To quantify the seasonal water and salt balance, water application, crop growth, soil water, and groundwater dynamics were studied on a sandy, sandy loam and loamy cotton field in the years 2003 and 2005. To simulate and quantify improved management strategies and update irrigation standards, the soil water model Hydrus-1D was applied. Results showed that shallow groundwater contributed a substantial share (up to 399 mm) to actual evapotranspiration of cotton (estimated at 488–727 mm), which alleviated water stress in response to suboptimal quantities of water applied for irrigation, but enhanced concurrently secondary soil salinization. Thus, pre-season salt leaching becomes a necessity. Nevertheless, as long as farmers face high uncertainty in irrigation water supply, maintaining shallow groundwater tables can be considered as a safety-net against unreliable water delivery. Simulations showed that in 2003 around 200 mm would have been sufficient during pre-season leaching, whereas up to 300 mm of water was applied in reality amounting to an overuse of almost 33%. Using some of this water during the irrigation season would have alleviated season crop-water stress such as in June 2003. Management strategy analyses revealed that crop water uptake would only marginally benefit from a permanent crop residue layer, often recommended as part of conservation agriculture. Such a mulch layer, however, would substantially reduce soil evaporation, capillary rise of groundwater, and consequently secondary soil salinization. The simulations furthermore demonstrated that not relying on the contribution of shallow groundwater to satisfy crop water demand is possible by implementing timely and soil-specific irrigation scheduling. Water use would then not be higher than the current Uzbek irrigation standards. It is argued that if furrow irrigation is to be continued, pure sandy soils, which constitute <5% of the agricultural soils in Khorezm, are best to be taken out of annual cotton production.
机译:在位于乌兹别克斯坦咸海盆地的Khorezm地区,灌溉棉花的用水量很高,而用水效率却很低。为了量化季节性的水和盐分平衡,在2003年和2005年对沙质,沙质壤土和壤土棉田中的水分利用,作物生长,土壤水分和地下水动力学进行了研究。模拟和量化改进的管理策略并更新灌溉根据标准,应用土壤水模型Hydrus-1D。结果表明,浅层地下水在棉花的实际蒸散量(估计为488-727 mm)中占很大比例(最大399毫米),这缓解了灌溉用水量不足时的水分胁迫,但同时又增强了土壤次生盐渍化。因此,季前的盐浸变得必要。然而,只要农民在灌溉水供应方面面临高度不确定性,保持地下水浅水位可被视为防止供水不可靠的安全网。模拟显示,在2003年的季前浸出过程中,大约200毫米就足够了,而实际上最多可使用300毫米的水,这几乎导致了33%的过度使用。在灌溉季节使用一些这种水可以减轻季节的作物水分压力,例如在2003年6月。管理策略分析表明,作物水分的吸收仅会从永久性作物残渣层中获得少量收益,通常建议将其作为保护性农业的一部分。然而,这样的覆盖层将大大减少土壤蒸发,地下水的毛细上升以及因此导致的二次土壤盐渍化。模拟进一步表明,通过实施及时且针对特定土壤的灌溉计划,可以不依靠浅层地下水来满足作物需水。用水量将不会高于当前的乌兹别克斯坦灌溉标准。有人认为,如果要继续进行沟灌,最好在年度棉花生产中去除纯砂土,最好在哈罗兹姆(Khorezm)的农业土壤中占5%。

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