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首页> 外文期刊>Hydrology and Earth System Sciences >Formulation of root water uptake in a multi-layer soil-plant model: does van den Honert's equation hold?
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Formulation of root water uptake in a multi-layer soil-plant model: does van den Honert's equation hold?

机译:多层土壤植物模型中根系水分吸收的公式:van den Honert方程是否成立?

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The withdrawal of water from soil by vegetation, which insteady state conditions is equivalent to the transpiration rate, can be written in termsof water potential in the form of an Ohm's law analogy, known as van den Honert'sequation: The difference between an effective soil water potential and the bulk canopywater potential is divided by an effective soil-plant resistance. This equation iscommonly used, but little is known about the precise definition of its parameters. Theissue of this paper is to bridge the gap between the bulk approach and a multi-layerdescription of soil-plant water transfer by interpreting the bulk parameters in terms ofthe characteristics of the multi-layer approach. Water flow through an elementary pathwithin the soil or the root is assumed to follow an Ohm's law analogy, and the soil androot characterisics are allowed to vary with depth. Starting from the basic equations ofthe multi-layer approach, it is proved that the total rate of transpiration can also beexpressed in the form of an Ohm's law analogy. This means that van den Honert's equationholds at canopy scale, insofar as the assumptions made on the physics of root water uptakehold. In the bulk formulation derived, the effective soil-plant resistance appears as acombination of the elementary resistances making up the multi-layer model; and theeffective soil water potential is a weighted mean of the water potentials in each soillayer, the weighting system involving the complete set of elementary resistances. Simplerrepresentations of soil-plant interaction leading to Ohm's law type formulations are alsoexamined: a simplified multi-layer model, in which xylem (root axial) resistance isneglected, and a bulk approach, in which soil-root interaction is represented by only onelayer. Numerical simulations performed in different standard conditions show that thesesimpler representations do not provide accurate estimates of the transpiration rate, whencompared to the values obtained by the complete algorithm.
机译:植被从土壤中抽出的水(其替代状态条件等于蒸腾速率)可以以水势的形式用欧姆定律比喻的形式表达,称为范登霍纳特方程:有效土壤之间的差异水势和大量冠层水势除以有效的土壤植物抗性。通常使用此方程,但对其参数的精确定义知之甚少。本文的目的是通过解释多层方法的特征来解释主体参数,从而弥合主体方法与土壤植物水分转移的多层描述之间的差距。假定通过土壤或根部内基本路径的水流遵循欧姆定律,并且允许土壤和根部特征随深度变化。从多层方法的基本方程出发,证明了总蒸腾速率也可以以欧姆定律比喻的形式表示。这意味着,范登·霍纳特方程式在树冠尺度上保持不变,只要其对根系水分吸收的物理性做出假设即可。在散装配方中,有效的土壤-植物抗性表现为构成多层模型的基本抗性的组合。有效土壤水势是每个土壤层中水势的加权平均值,该加权系统涉及整套基本阻力。还研究了导致欧姆定律类型公式的土壤-植物相互作用的更简单表示形式:简化的多层模型,其中忽略了木质部(根轴)抗性,以及本体法,其中土壤-根部相互作用仅由一个层表示。在不同标准条件下进行的数值模拟表明,与通过完整算法获得的值相比,这些简单的表示不能提供对蒸腾速率的准确估计。

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