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Effect of parameter choice in root water uptake models – the arrangement of root hydraulic properties within the root architecture affects dynamics and efficiency of root water uptake

机译:参数选择对根系吸水模型的影响-根系内部根系水力特性的排列会影响根系吸水的动力学和效率

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Detailed three-dimensional models of root water uptake have become increasingly popular for investigating the process of root water uptake. However, they suffer from a lack of information on important parameters, particularly on the spatial distribution of root axial and radial conductivities, which vary greatly along a root system. In this paper we explore how the arrangement of those root hydraulic properties and branching within the root system affects modelled uptake dynamics, xylem water potential and the efficiency of root water uptake. We first apply a simple model to illustrate the mechanisms at the scale of single roots. By using two efficiency indices based on (i) the collar xylem potential ("effort") and (ii) the integral amount of unstressed root water uptake ("water yield"), we show that an optimal root length emerges, depending on the ratio between roots axial and radial conductivity. Young roots with high capacity for radial uptake are only efficient when they are short. Branching, in combination with mature transport roots, enables soil exploration and substantially increases active young root length at low collar potentials. Second, we investigate how this shapes uptake dynamics at the plant scale using a comprehensive three-dimensional root water uptake model. Plant-scale dynamics, such as the average uptake depth of entire root systems, were only minimally influenced by the hydraulic parameterization. However, other factors such as hydraulic redistribution, collar potential, internal redistribution patterns and instantaneous uptake depth depended strongly on the arrangement on the arrangement of root hydraulic properties. Root systems were most efficient when assembled of different root types, allowing for separation of root function in uptake (numerous short apical young roots) and transport (longer mature roots). Modelling results became similar when this heterogeneity was accounted for to some degree (i.e. if the root systems contained between 40 and 80% of young uptake roots). The average collar potential was cut to half and unstressed transpiration increased by up to 25% in composed root systems, compared to homogenous ones. Also, the least efficient root system (homogenous young root system) was characterized by excessive bleeding (hydraulic lift), which seemed to be an artifact of the parameterization. We conclude that heterogeneity of root hydraulic properties is a critical component for efficient root systems that needs to be accounted for in complex three-dimensional root water uptake models.
机译:用于研究根系吸水过程的详细的根系吸水三维模型已变得越来越受欢迎。然而,它们缺乏关于重要参数的信息的缺乏,特别是关于根轴向和径向电导率的空间分布的信息,这些信息在根系统中变化很大。在本文中,我们探讨了根系内水力特性和分支的排列方式如何影响模拟的吸收动力学,木质部水势和根系吸收效率。我们首先应用一个简单的模型来说明单根尺度的机制。通过使用基于(i)衣领木质部潜力(“努力”)和(ii)无胁迫根系吸水量(“水产量”)的总量的两个效率指数,我们表明出现了最佳根系长度,具体取决于根的轴向和径向电导率之比。具有高径向吸收能力的幼根仅在短时才有效。分支结合成熟的运输根,可以进行土壤勘探,并在低领势下显着增加活跃幼根的长度。其次,我们使用全面的三维根系吸水模型研究这如何在植物规模上塑造吸收动态。植物尺度的动力学,例如整个根系的平均吸收深度,受水力参数设置的影响很小。但是,其他因素(例如水力重新分配,项圈电位,内部重新分配模式和瞬时吸收深度)在很大程度上取决于根部水力特性的排列。当根系组装成不同的根类型时,根系是最有效的,可将吸收(大量短尖幼根)和运输(较长成熟根)中的根功能分开。当在某种程度上解释了这种异质性时,建模结果变得相似(即,如果根系包含40%至80%的年轻吸收根)。与同质的根系相比,在组成的根系中,平均领势降低了一半,无压力蒸腾提高了25%。同样,效率最低的根系(均质的年轻根系)的特征是出血过多(液压升力),这似乎是参数化的产物。我们得出结论,根系水力特性的不均匀性是有效根系的关键组成部分,需要在复杂的三维根系吸水模型中加以考虑。

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