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首页> 外文期刊>Soil Science Society of America Journal >Microdrip Irrigation of Field Crops: Effect on Yield, Water Uptake, and Drainage in Sweet Corn
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Microdrip Irrigation of Field Crops: Effect on Yield, Water Uptake, and Drainage in Sweet Corn

机译:田间作物微滴灌对甜玉米产量,水分吸收和排水的影响

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摘要

Microdrip irrigation supplies water at a rate close to that of plant water uptake. It is thus expected to improve yields and reduce water losses from drainage below the root zone. To test this assumption, four drip irrigation treatments were applied on corn (Zea mays L.) at Bet Dagan, Israel: (i) daily irrigation with 2 L h-1 emitters (2-D); (ii) twice-weekly irrigation with 2 L h-1 emitters (2-TW); (iii) weekly irrigation with 2 L h-1 emitters (2-W); (iv) daily microdrip irrigation with 0.25 L h-1 emitters (0.25-D). Total irrigation was similar for all treatments. Soil water content depth distribution was monitored by the neutron scattering method. Total water uptake (sap flow, SF) was measured using the heat pulse method for two consecutive periods of 2 wk. Relative drying of the 0.60- to 0.90-m soil layer was observed only in the microdrip treatment. These might indicate different root structure or water uptake patterns because of the low application rate. Highest estimated drainage fluxes were obtained for the 2-D treatment and lowest for the 0.25-D treatment, especially at the end of the growing period. The SF/ETp ratio was the steadiest for the 0.25-D treatment. The relationship of canopy conductance to vapor pressure difference for 0.25-D was not different from those of 2-D and 2-TW. Lower conductance values were obtained for 2-W at the end of the irrigation cycle. Daily irrigation led to the highest yield, while weekly irrigation led to the lowest. The results indicate that microdrip irrigation might improve yields and reduce water losses from drainage below the root zone.
机译:微滴灌的供水速率与植物吸水量的 接近。因此,有望提高产量 并减少根部区域下方排水带来的水分流失。为了 检验此假设,对以色列贝塔干(Bet Dagan)的玉米(Zea mays L.)进行了四种滴灌处理:(i)每日灌溉 具有2个L h -1 发射器(2-D); (ii)每周两次用 2 L h -1 辐射器(2-TW)灌溉; (iii)每周灌溉2 L h -1 发射器(2-W); (iv)每天用0.25 L h -1 发射器(0.25-D)进行微滴灌。所有 处理的总灌溉量相似。用中子散射法监测土壤含水量深度分布 。使用热脉冲法在两个连续的2 wk的 期间测量总吸水量(树液流量, SF)。仅在微滴处理中才观察到0.60至0.90-m的土壤 层的相对干燥。这些可能 表示不同的根系结构或吸水方式,因为 的施用量较低。二维处理获得的最高估计排水通量 ,而0.25-D 处理则最低,尤其是在生长期结束时。对于0.25-D处理, SF / ET p 比最稳定。 0.25-D的冠层电导率与蒸汽压差 的关系与2-D和2-TW的无差异。在灌溉 周期结束时获得2-W的更低的 电导值。每日灌溉导致最高产量,而每周 灌溉导致最低产量。结果表明,微滴 灌溉可能会提高产量,并减少根区以下 排水造成的水分流失。

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  • 来源
    《Soil Science Society of America Journal 》 |2002年第1期| 228-234| 共7页
  • 作者单位

    Dep. of Environmental Physics and Irrigation, Institute of Soil, Water and Environmental Sciences, Volcani Center, ARO, Bet Dagan 50250, Israel;

    Dep. of Environmental Physics and Irrigation, Institute of Soil, Water and Environmental Sciences, Volcani Center, ARO, Bet Dagan 50250, Israel;

    Dep. of Environmental Physics and Irrigation, Institute of Soil, Water and Environmental Sciences, Volcani Center, ARO, Bet Dagan 50250, Israel;

    Dep. of Environmental Physics and Irrigation, Institute of Soil, Water and Environmental Sciences, Volcani Center, ARO, Bet Dagan 50250, Israel;

    Dep. of Environmental Physics and Irrigation, Institute of Soil, Water and Environmental Sciences, Volcani Center, ARO, Bet Dagan 50250, Israel;

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