Articles | Volume 21, issue 12
https://doi.org/10.5194/hess-21-6519-2017
https://doi.org/10.5194/hess-21-6519-2017
Research article
 | 
21 Dec 2017
Research article |  | 21 Dec 2017

Water movement through plant roots – exact solutions of the water flow equation in roots with linear or exponential piecewise hydraulic properties

Félicien Meunier, Valentin Couvreur, Xavier Draye, Mohsen Zarebanadkouki, Jan Vanderborght, and Mathieu Javaux

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Cited articles

Alm, D. M., Cavelier, J., and Nobel, P. S.: A Finite-element Model of Radial and Axial Conductivities for Individual Roots: Development and Validation for Two Desert Succulents, Ann. Bot.-London, 69, 87–92, 1992.
Ariyaratna, R.: An extension to the Landsberg and Fowkes' Model, PhD thesis, Texas Tech University, https://ttu-ir.tdl.org/ttu-ir/handle/2346/19780, 1990.
Bechmann, M., Schneider, C., Carminati, A., Vetterlein, D., Attinger, S., and Hildebrandt, A.: 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, Hydrol. Earth Syst. Sci., 18, 4189–4206, https://doi.org/10.5194/hess-18-4189-2014, 2014.
Biondini, M.: Allometric scaling laws for water uptake by plant roots, J. Theor. Biol., 251, 35–59, https://doi.org/10.1016/j.jtbi.2007.11.018, 2008.
Bramley, H., Turner, N. C., Turner, D. W., and Tyerman, S. D.: Comparison between gradient-dependent hydraulic conductivities of roots using the root pressure probe: the role of pressure propagations and implications for the relative roles of parallel radial pathways, Plant Cell Environ., 30, 861–874, https://doi.org/10.1111/j.1365-3040.2007.01678.x, 2007.
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Short summary
To maintain its yield, a plant needs to transpire water that it acquires from the soil. A deep understanding of the mechanisms that lead to water uptake location and intensity is required to correctly simulate the water transfer in the soil to the atmosphere. This work presents novel and general solutions of the water flow equation in roots with varying hydraulic properties that deeply affect the uptake pattern and the transpiration rate and can be used in ecohydrological models.
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