首页> 外文期刊>Irrigation Science >Influence of soil water content and atmospheric conditions on leaf water potential in cv. 'Touriga Nacional' deep-rooted vineyards. (Special Issue: Water management in grapevines.)
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Influence of soil water content and atmospheric conditions on leaf water potential in cv. 'Touriga Nacional' deep-rooted vineyards. (Special Issue: Water management in grapevines.)

机译:土壤水分和大气条件对简历叶片水势的影响。 “ Touriga Nacional”根深蒂固的葡萄园。 (特刊:葡萄中的水管理。)

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摘要

In this study, the influence of soil and atmosphere conditions on noon and basal leaf water potential of vines "Touriga Nacional" in the Dao region submitted to different irrigation treatments is analysed. Both indicators showed to be dependent on environmental conditions at the time of measurement. Leaf water potential at noon of fully watered plants was linearly related with atmospheric conditions, with values registered when vapour pressure deficit (VPD) was higher than approximately 3 kPa being no different from the values registered in stressed plants. Therefore, this indicator cannot be reliably used to distinguish different plant water stress levels when atmospheric conditions induce high evaporative demands. The basal leaf water potential ( psi b) was also influenced by VPD at the time of measurement for all soil water conditions. In well irrigated plants, it was even possible to establish a baseline that can therefore be used to identify nonwater stressed conditions ( psi b (MPa)=-0.062-0.0972 VPD (kPa), r2=0.78). A good correlation was found between soil humidity and psi b. However, more than the average value of the whole thickness of soil monitored, the psi b values were dependent on the distribution of soil humidity, with the plants responding to the presence of wet layers.
机译:在这项研究中,分析了土壤和大气条件对在不同灌溉处理下的Dao地区“ Touriga Nacional”葡萄藤中午和基叶水势的影响。在测量时,两个指标都显示出与环境条件有关。充分浇水的植物在中午时的叶片水势与大气条件呈线性关系,当蒸气压亏缺(VPD)高于大约3 kPa时记录的值与胁迫植物中记录的值没有差异。因此,当大气条件引起高蒸发需求时,该指标不能可靠地用于区分不同的植物水分胁迫水平。在测量所有土壤水分条件时,基础叶片水势(psi b )也受VPD影响。在灌溉良好的植物中,甚至有可能建立一个基线,因此可以用来确定非水分胁迫条件(psi b (MPa)=-0.062-0.0972 VPD(kPa),r 2 = 0.78)。土壤湿度与psi b 之间具有良好的相关性。但是,psi b 值比监测的土壤总厚度的平均值要高,这取决于土壤湿度的分布,而植物对湿层的存在有反应。

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