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A one-dimensional model of water flow in soil-plant systems based on plant architecture

机译:基于植物结构的土壤-植物系统中水流的一维模型

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摘要

The estimation of root water uptake and water flow in plants is crucial to quantify transpiration and hence the water exchange between land surface and atmosphere. In particular the soil water extraction by plant roots which provides the water supply of plants is a highly dynamic and non-linear process interacting with soil transport processes that are mainly determined by the natural soil variability at different scales. To better consider this root-soil interaction we extended and further developed a finite element tree hydro-dynamics model based on the one-dimensional (1D) porous media equation. This is achieved by including in addition to the explicit three-dimensional (3D) architectural representation of the tree crown a corresponding 3D characterisation of the root system. This 1D xylem water flow model was then coupled to a soil water flow model derived also from the 1D porous media equation. We apply the new model to conduct sensitivity analysis of root water uptake and transpiration dynamics and compare the results to simulation results obtained by using a 3D model of soil water flow and root water uptake. Based on data from lysimeter experiments with young European beech trees (Fagus silvatica L.) is shown, that the model is able to correctly describe transpiration and soil water flow. In conclusion, compared to a fully 3D model the 1D porous media approach provides a computationally efficient alternative, able to reproduce the main mechanisms of plant hydro-dynamics including root water uptake from soil.
机译:估算植物的根系吸水量和水流量对于量化蒸腾作用以及陆地表面与大气之间的水交换至关重要。特别是,通过植物根系提取的土壤水为植物提供了水,是一个高度动态且非线性的过程,与土壤运输过程相互作用,而土壤运输过程主要由不同规模的自然土壤变异性决定。为了更好地考虑这种根-土相互作用,我们扩展并进一步开发了基于一维(1D)多孔介质方程的有限元树流体动力学模型。这是通过除树冠的显式三维(3D)结构表示之外还包括根系统的相应3D表征来实现的。然后将此一维木质部水流模型与同样从一维多孔介质方程式导出的土壤水流模型耦合。我们将新模型应用于根系吸水和蒸腾动力学的敏感性分析,并将结果与​​使用土壤水流和根系吸水的3D模型获得的模拟结果进行比较。基于对欧洲年轻山毛榉树(Fagus silvatica L.)的溶渗仪实验数据,该模型能够正确描述蒸腾作用和土壤水流。总之,与完全3D模型相比,一维多孔介质方法提供了一种计算有效的替代方法,能够重现植物流体动力学的主要机理,包括从土壤吸收根系水分。

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