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Scheduling peach orchard irrigation in water stress conditions: use of relative transpiration and predawn leaf water potential

机译:在缺水条件下安排桃园灌溉:利用相对蒸腾作用和黎明前的叶片水势

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Plant water stress indicators have become valuable for moving towards deficit irrigation strategies and saving water. In this case evapotranspiration (ET) is below its maximum value for the crop and stage (ETc), and a stress coefficient (Ks) is applied to obtain actual ET(ETd). Predawn leaf water potential (Wp) can be related to relative transpiration (RT), the ratio between transpiration of a stressed plot (T) and transpiration of a well-irrigated plot (7m). Estimating RT from Wp allows calculatingETa for determination of irrigation amounts, if deficit irrigation practices are used, as RT corresponds approximately to Ks. Materials and methods. i?7"and Wp were measured with the aim of establishing a relationship to estimate RTunder moderate water stress for irrigation scheduling, in a peach orchard in south Portugal. RT was calculated using sap flow measurements (heat balance method) in two plots, one well-irrigated (daily drip irrigation amounts calculated for 7m) and another temporarily withoutirrigation. Results and discussion. A high correlation was found between RTand Wp, allowing the estimation of RTior the studied conditions. Significant differences regarding the relationship RT- Wp obtained for another peach orchard in the same region and similar soil conditions were found for Wp in the range between -0.11 and -0.45 MPa. The results suggest that the differences resulted from the different irrigation systems: drip and micro-sprinkling, as they determine different temporal and spatial water distribution and therefore different geometry of root systems. A formerly proposed equation to estimate 77rrom Wp with a general form for different fruit tree species was tested, proving to be adequate within some limits: when RTis lowered to 0.7, theerror was below 9%. The threshold value RT= 0.7 was considered a minimum as it was successfully tested in deficit irrigation practices for peach orchards.
机译:植物水分胁迫指标对于转向亏缺灌溉策略和节水非常有价值。在这种情况下,蒸散量(ET)低于作物和生长阶段的最大值(ETc),并应用应力系数(Ks)以获得实际的ET(ETd)。黎明前的叶片水势(Wp)可能与相对蒸腾量(RT),胁迫样地的蒸腾量(T)和灌溉良好的样地的蒸腾量(7m)之间的比率有关。从Wp估算RT可以计算ETa,以确定灌溉量(如果使用亏水灌溉的话),因为RT大约等于Ks。材料和方法。在葡萄牙南部的一个桃园中,测量i?7“和Wp的目的是建立一种关系,以估算适度水分胁迫下的RT,以进行灌溉计划。RT是在两个样地中使用树液流量测量(热平衡法)来计算的良好的灌溉条件(计算出的每日滴灌量为7m)和另一次暂时不进行灌溉的结果和讨论:RT和Wp之间存在高度相关性,可以估算RTi或研究条件。在相同区域和相似土壤条件下,桃园的Wp在-0.11和-0.45 MPa之间,结果表明差异是由于不同的灌溉系统造成的:滴灌和微滴,因为它们决定了不同的时间和空间水分布,因此根系的几何形状也不同。以前提出的方程用一般的fo估计77rrom Wp测试了不同果树种类的均方根值,证明在一定范围内是足够的:当RT降低到0.7时,误差低于9%。阈值RT = 0.7被认为是最小值,因为它已在桃园的缺水灌溉实践中成功测试。

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