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Photosynthetic Response of European Beech to Atmospheric and Soil Drought

机译:欧洲山毛榉对大气和土壤干旱的光合响应

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Physiological response of European beech under soil and atmospheric drought conditions was investigated in this study. A group of six beech trees was irrigated during the growing season 2012, while the second group of non-irrigated (control) beech trees was treated under natural soil drought. During the experiment, we observed more than 45-day long period when no precipitation fell on the soil surface. The relationship of PN (CO2 assimilation rate) to gS (stomatal conductance) was very tight in both groups, which indicates that stomatal opening was the main factor limiting PN. The statistically significant differences in gS between the groups of trees were revealed only on the last measuring day. The significant differences in PN were confirmed on the days when the differences in soil water potential (ΨS) appeared. On these measurement days, the PN values of irrigated individuals were approximately 1.9 or 3.3 times greater than the values of non-irrigated individuals. At the level of primary photosynthetic processes (chlorophyll fluorescence parameters) we did not observe lower values of the control individuals in comparison with the irrigated trees in any of the evaluated parameters. Long-term soil water deficit caused strong decrease of leaf water potential (ΨL) in the control trees, but ΨL values of the irrigated trees were also rather low due to diurnal dynamics in higher parts of crown. Close relationship between ΨL and gS was confirmed for the control (non-irrigated) trees, but could not be confirmed for the irrigated trees. We revealed significant influence of VPD (vapour pressure deficit of the air) on gS only in the control group. On the days when ΨS decreased, the stomata of the non-irrigated trees were closed in spite of the low VPD values. Almost complete stomatal closure in both groups of trees was caused by the increase of VPD to 1.2 kPa.
机译:研究了欧洲山毛榉在土壤和大气干旱条件下的生理响应。在2012年的生长季节期间,对六棵山毛榉树进行了灌溉,而第二组非灌溉(对照)山毛榉树则在自然土壤干旱条件下进行了处理。在实验过程中,我们观察到超过45天的长时间没有土壤表面沉淀。两组的PN(CO 2 同化率)与gS(气孔导度)之间的关系非常紧密,这表明气孔开放是限制PN的主要因素。仅在最后一个测量日才显示出树木组之间的g S 的统计学显着差异。在出现土壤水势(ΨS)差异的那几天,便确认了PN的显着差异。在这些测量天中,灌溉个体的PN值大约是非灌溉个体的PN值的1.9或3.3倍。在初级光合作用水平(叶绿素荧光参数)方面,与任何评估参数中的灌溉树木相比,我们没有观察到对照个体的较低值。长期的土壤水分亏缺导致对照树的叶片水势(Ψ L )大大降低,但灌溉树的Ψ L 值也很低,原因是冠的较高部分的昼夜动力学。对照(非灌溉)树确认了Ψ L 和g S 之间的密切关系,但灌溉树无法确认。我们仅在对照组中揭示了VPD(空气蒸气压不足)对g S 的显着影响。在ΨS降低的那一天,尽管VPD值低,但未灌溉的树木的气孔仍然关闭。两组树木中几乎完全的气孔关闭是由VPD增加到1.2 kPa引起的。

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