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Esigenze idriche di Vitis vinifera L. in ambiente caldo-arido

机译:干旱环境下葡萄的水分需求

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Many important viticultural areas are located in semiarid environments where mean annual rainfall ranges between 400 and 600 mm, rains are mainly concentrated during tile vine rest period, and vineyard water use is meanly estimated between 500 and 800 mm. The daily vine water use is known to be highly related with the air temperature but, at a greater extent, with the net radiation; moreover, the vineyard water use is affected by other environmental conditions influencing the leaf transpiration, such as the air movement and tile VPD, as well as by several agronomical factors such as the vine density, the training system, the vine age, the floor management, the irrigation frequency and the vine phenological phase. The general decrement of vine water status during the growing season induces both stomatic and non stomatic limitation affecting the leaf gas exchange, the vine nutritional status and the canopy development. In order to estimate the vineyard water use, the evaluation of the water requirement and the crop coefficients has been traditionally done by lysimetry; however, some limits of this method have been pointed out in the '90s, mainly as for studies on woody species. Alternative methods more recently proposed are based on micrometeorological techniques such as Eddy Covariance, which allows the direct measurement of air temperature, water vapour and carbon dioxide, and Surface Renewal, which allows to estimate matter and energy exchange by measuring the air temperature at high frequency. The water deficit, as a limiting factor, is known to affect the canopy development more than the carbohydrate production, thus, when a performing vine leaf area has been already reached, a moderate water deficit may be imposed to reduce the rate of shoot development, and thus the transpiring leaf surface, without compromising the leaf functioning. Many factors concern the estimation of the water requirement in winegrape and tablegrape vineyards and the effect of the irrigation water supply on the berry quality. The main research carried out on this topic pointed out a post-berry set or post-veraison water deficit as the irrigation strategy more helpful to achieve the equilibrium between the vegetative and the reproductive activity and a good berry quality.
机译:许多重要的葡萄种植区都位于半干旱环境中,年平均降雨量在400至600毫米之间,雨水主要集中在瓦藤休息期间,而葡萄园用水估计在500至800毫米之间。众所周知,葡萄树的日常用水与气温高度相关,但在更大程度上与净辐射有关。此外,葡萄园的用水还受到影响叶片蒸腾作用的其他环境条件的影响,例如空气流动和瓷砖的VPD,以及多种农艺因素的影响,例如葡萄树的密度,栽培系统,葡萄树的年龄,地面管理,灌溉频率和葡萄树物候期。生长季节葡萄藤水分状况的总体下降会引起气孔和非气孔限制,从而影响叶片气体交换,葡萄藤的营养状况和冠层发育。为了估算葡萄园的用水量,传统上通过溶度测定法对需水量和作物系数进行了评估。然而,在90年代已经指出了这种方法的一些局限性,主要是针对木本物种的研究。最近提出的替代方法基于微气象技术,例如Eddy Covariance,它可以直接测量空气温度,水蒸气和二氧化碳,Surface Renewal可以通过测量高频空气温度来估计物质和能量交换。 。水分不足是限制因素,它对冠层发育的影响大于碳水化合物的产生,因此,当已经达到正常的葡萄叶面积时,可以施加适度的水分亏缺来降低枝条发育的速度,从而使叶片表面蒸腾而不会损害叶片的功能。许多因素涉及对葡萄酒葡萄和食用葡萄的葡萄园中水需求的估计以及灌溉水供应对浆果质量的影响。关于这一主题的主要研究指出,浆果定植后或水分不足后的补水作为灌溉策略,有助于实现营养和生殖活动之间的平衡以及良好的浆果品质。

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