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Steps toward an improvement in process-based models of water use by fruit trees: A case study in olive

机译:改善基于过程的果树用水模型的步骤:以橄榄为例的研究

摘要

We applied two process-based models in a hedgerow olive orchard with the aim of understanding the limitations and mechanisms behind the control of transpiration in olive trees under drip irrigation. One model is based on the biophysics of water flow through the porous media of soil and xylem. The other is a hydromechanical model based on the observed dependence of stomatal aperture on whole-plant and epidermis water relations. The experiments were made in a hedgerow olive orchard (1667treesha -1) planted with 5-year-old 'Arbequina' trees. Measurements were made in control trees irrigated to replace 100% of the crop water needs, and in trees under regulated deficit irrigation (RDI) strategy, in which irrigation replaced ca. 30% of the control. Soil physical properties, root distribution, leaf area, sap flow, leaf osmotic pressure and key variables of leaf gas exchange and water status were measured and models were applied. Results show how in our orchard, with a shallow root distribution and very coarse soil, most of the limitation to transpiration was imposed by the hydraulics of the rhizosphere. The model shows how this limitation was related to the ratio of root to leaf area, and how this ratio can be managed by canopy pruning or by changing the number of drippers. Likewise, osmotic adjustment occurred similarly in both irrigation treatments, despite differences found on leaf water potential. Water stress largely affected plant hydraulic conductivity of RDI trees. A potential involvement of regulating signals, other than purely hydraulics, was evident in both treatments, although our data suggests that these signals were not regulated by the soil water status only.
机译:我们在树篱橄榄园中应用了两个基于过程的模型,旨在了解滴灌条件下控制橄榄树蒸腾作用的局限性和机理。一种模型是基于通过土壤和木质部的多孔介质的水的生物物理学。另一个是基于观察到的气孔孔径对整个植物和表皮水分关系的依赖性的水力力学模型。实验是在种植了5年历史的“ Arbequina”树的树篱橄榄果园(1667treesha -1)中进行的。在灌溉的对照树中进行测量,以替代100%的作物需水;在调节性缺水灌溉(RDI)策略下进行的测量中,灌溉用水替代了约200%的作物。 30%的对照。测量了土壤的物理性质,根系分布,叶面积,汁液流量,叶片渗透压以及叶片气体交换和水分状况的关键变量,并应用了模型。结果表明,在我们的果园中,根系分布较浅且土壤非常粗糙,蒸腾作用的大部分限制是由根际水力造成的。该模型显示了该限制与根与叶面积的比率如何相关,以及如何通过冠层修剪或通过改变滴头的数量来控制该比率。同样,尽管叶片水势存在差异,但两种灌溉处理的渗透调节均相似。水分胁迫在很大程度上影响了RDI树的植物水力传导率。在两种处理中,除纯水力作用外,调节信号都可能参与其中,尽管我们的数据表明这些信号不仅受土壤水分状态的调节。

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