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Modeling effects of partial rootzone irrigation on stomatal conductance and transpiration of young citrus trees

机译:根系局部灌溉对柑橘幼树气孔导度和蒸腾作用的模拟作用

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Partial rootzone irrigation has been proposed for decreasing the amount of water applied to citrus. The computer model WATFLO was developed to investigate how environmental, plant and soil factors influence water use of young citrus trees with all or only part of their root systems irrigated. Solar radiation, dry-bulb temperature, dewpoint temperature, leaf area, root length density, soil volume, and soil water-holding characteristics are specified. Soil water movement to roots is computed using microscopic-scale radial flow to individual roots. Leaf stomatal conductance regulates actual transpiration in response to solar radiation, atmospheric evaporative demand, and soil water potential in the immediate vicinity of the roots, which is compatible with concepts of root-to-shoot abscisic acid signals that control leaf stomatal conductance. Three methods of calculating the effective soil water potential for governing leaf stomatal conductance were investigated. Partial rootzone irrigation is accomplished by dividing the rooting volume into four compartments and specifying the initial soil water content of each compartment. Predicted transpiration rates of young citrus trees with all or three-quarters of the compartments irrigated were in good agreement with measured values for young irrigated citrus trees in controlled-environment chambers. Predicted transpiration of trees with one-half or one-quarter of the compartments irrigated decreased during the afternoon due to reduced stomatal conductance in response to simulated depletion of soil water adjacent to the roots. The model indicates that partial rootzone irrigation may limit plant transpiration (with implicit plant water stress), especially if rooting volumes are small and soils are sandy with low water-holding capacity.
机译:已经提出了局部根区灌溉以减少柑桔上的水量。开发了计算机模型WATFLO,以研究环境,植物和土壤因素如何影响全部或仅部分根系灌溉的柑桔幼树的水分利用。规定了太阳辐射,干球温度,露点温度,叶面积,根长密度,土壤体积和土壤持水特性。土壤水向根的运动是使用微观尺度的向单个根的径向流来计算的。叶片气孔电导率调节实际的蒸腾量,以响应太阳辐射,大气蒸发需求和根系附近的土壤水势,这与控制叶片气孔电导率的根茎脱落酸信号的概念兼容。研究了三种计算土壤有效气势以调节叶片气孔导度的方法。通过将生根量分成四个隔间并指定每个隔间的初始土壤水分来完成部分根区灌溉。灌溉了所有或四分之三的车厢的柑橘幼树的预计蒸腾速率与环境受控室内的柑橘灌溉的实测值非常吻合。下午灌溉了一半或四分之一车厢的树木,预计的蒸腾作用在下午降低了,这是由于模拟根部附近土壤水的枯竭导致气孔导度降低。该模型表明,局部根区灌溉可能会限制植物的蒸腾作用(带有隐含的植物水分胁迫),尤其是在生根量少且土壤沙质且持水能力低的情况下。

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