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024 7 _ |2 DOI
|a 10.1007/s11104-010-0639-0
024 7 _ |2 WOS
|a WOS:000288455300019
037 _ _ |a PreJuSER-18204
041 _ _ |a eng
082 _ _ |a 570
084 _ _ |2 WoS
|a Agronomy
084 _ _ |2 WoS
|a Plant Sciences
084 _ _ |2 WoS
|a Soil Science
100 1 _ |0 P:(DE-HGF)0
|a Janott, M.
|b 0
245 _ _ |a A one-dimensional model of water flow in soil-plant systems based on plant architecture
260 _ _ |a Dordrecht [u.a.]
|b Springer Science + Business Media B.V
|c 2011
300 _ _ |a 233 - 256
336 7 _ |a Journal Article
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336 7 _ |a ARTICLE
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336 7 _ |a JOURNAL_ARTICLE
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336 7 _ |a article
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440 _ 0 |0 9161
|a Plant and Soil
|v 341
|x 0032-079X
|y 1-2
500 _ _ |3 POF3_Assignment on 2016-02-29
500 _ _ |a We are grateful to the Deutsche Forschungsgemeinschaft which funded this study within the frame of Forschergruppe 788 'Competitive mechanisms of water and nitrogen partitioning in beech-dominated deciduous forests'. We also want to thank an anonymous reviewer whose comments helped to considerably improve the manuscript and we thank Sebastian Bittner for his help during the revision of the manuscript.
520 _ _ |a 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.
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653 2 0 |2 Author
|a Transpiration
653 2 0 |2 Author
|a Plant hydro-dynamics model
653 2 0 |2 Author
|a Root water uptake
653 2 0 |2 Author
|a European beech
653 2 0 |2 Author
|a Porous media equation
700 1 _ |0 P:(DE-HGF)0
|a Gayler, S.
|b 1
700 1 _ |0 P:(DE-HGF)0
|a Gessler, A.
|b 2
700 1 _ |0 P:(DE-Juel1)129477
|a Javaux, M.
|b 3
|u FZJ
700 1 _ |0 P:(DE-HGF)0
|a Klier, C.
|b 4
700 1 _ |0 P:(DE-HGF)0
|a Priesack, E.
|b 5
773 _ _ |0 PERI:(DE-600)1478535-3
|a 10.1007/s11104-010-0639-0
|g Vol. 341, p. 233 - 256
|p 233 - 256
|q 341<233 - 256
|t Plant and soil
|v 341
|x 0032-079X
|y 2011
856 7 _ |u http://dx.doi.org/10.1007/s11104-010-0639-0
909 C O |o oai:juser.fz-juelich.de:18204
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