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灌溉葡萄树冠导度和蒸腾作用的调控及其建模

Regulation of canopy conductance and transpiration and their modelling in irrigated grapevines.

作者信息

Lu Ping, Yunusa Isa A M, Walker Rob R, Müller Warren J

机构信息

CSIRO Plant Industry, Darwin Laboratory, PMB 44, Winnellie, NT 0822, Australia. Corresponding author; email:

CSIRO Plant Industry, Horticulture Unit, PMB, Merbein, Vic. 3505, Australia. Agriculture Victoria, RMB 1145, Rutherglen, Vic. 3685, Australia.

出版信息

Funct Plant Biol. 2003 Jul;30(6):689-698. doi: 10.1071/FP02181.

Abstract

Whole-vine transpiration was estimated for well-watered nine-year-old Sultana grapevines (Vitis vinifera L. cv. Sultana) from xylem sap flow measured with Granier's heat-dissipation probes. Canopy conductance of the grapevine was calculated by inverting the Penman-Monteith equation. Transpiration from grapevine canopies was strongly controlled by the canopy conductance. Canopy conductance decreased exponentially with increasing vapour pressure deficit (VPD) except in the morning when solar radiation was less than 200 W m and the canopy conductance was predominantly limited by the solar radiation. A non-linear model of canopy conductance as a function of the solar radiation and VPD explained > 90% of the variation observed in canopy conductance. Under contrasting VPD conditions (daytime maximum of 3 kPa vs 8 kPa), grapevines were able to regulate their canopy conductance from 0.006 to 0.001 m s to maintain a near constant transpiration. Whole-canopy transpiration calculated from modelled canopy conductance using the Penman-Monteith equation was highly correlated with the measured transpiration (sap flow) values over the range of 0-0.20 mm h (R > 0.85). Cross-validation shows that these mechanistic models based on solar radiation and VPD provide good predictions of canopy conductance and transpiration under the conditions of the study.

摘要

利用Granier热消散探针测量木质部液流,估算了充分灌溉的9年生无核白葡萄(Vitis vinifera L. cv. Sultana)整株葡萄的蒸腾作用。通过对Penman-Monteith方程求逆来计算葡萄树冠层导度。葡萄树冠层的蒸腾作用受树冠层导度的强烈控制。树冠层导度随蒸汽压亏缺(VPD)的增加呈指数下降,但在太阳辐射小于200 W m且树冠层导度主要受太阳辐射限制的早晨除外。作为太阳辐射和VPD函数的树冠层导度非线性模型解释了树冠层导度观测变化的90%以上。在对比的VPD条件下(白天最大值分别为3 kPa和8 kPa),葡萄能够将其树冠层导度从0.006调节到0.001 m s,以维持近乎恒定的蒸腾作用。使用Penman-Monteith方程从模拟的树冠层导度计算出的整株树冠层蒸腾作用与0-0.20 mm h范围内实测的蒸腾作用(液流)值高度相关(R>0.85)。交叉验证表明,这些基于太阳辐射和VPD的机理模型在研究条件下能够很好地预测树冠层导度和蒸腾作用。

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