Measuring and Modeling Hydraulic Lift of Lolium multiflorum Using Stable Water Isotopes

This study tested a method to quantify and locate hydraulic lift (HL, defined as the passive upward water flow from wetter to dryer soil zones through the plant root system) by combining an experiment using the stable water isotope HO as a tracer with a soil–plant water flow model. Our methodology c...

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Main Authors: Félicien Meunier, Youri Rothfuss, Thierry Bariac, Philippe Biron, Patricia Richard, Jean-Louis Durand, Valentin Couvreur, Jan Vanderborght, Mathieu Javaux
Format: Article
Language:English
Published: Wiley 2018-02-01
Series:Vadose Zone Journal
Online Access:https://dl.sciencesocieties.org/publications/vzj/articles/17/1/160134
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author Félicien Meunier
Youri Rothfuss
Thierry Bariac
Philippe Biron
Patricia Richard
Jean-Louis Durand
Valentin Couvreur
Jan Vanderborght
Mathieu Javaux
author_facet Félicien Meunier
Youri Rothfuss
Thierry Bariac
Philippe Biron
Patricia Richard
Jean-Louis Durand
Valentin Couvreur
Jan Vanderborght
Mathieu Javaux
author_sort Félicien Meunier
collection DOAJ
description This study tested a method to quantify and locate hydraulic lift (HL, defined as the passive upward water flow from wetter to dryer soil zones through the plant root system) by combining an experiment using the stable water isotope HO as a tracer with a soil–plant water flow model. Our methodology consisted in (i) establishing the initial conditions for HL in a large rhizobox planted with Italian ryegrass ( Lam.), (ii) labeling water in the deepest soil layer with an O-enriched solution, (iii) monitoring the water O isotopic composition in soil layers to find out changes in the upper layers that would reflect redistribution of O-enriched water from the bottom layers by the roots, and (iv) comparing the observed soil water O isotopic composition to simulation results of a three-dimensional model of water flow and isotope transport in the soil–root system. Our main findings were that (i) the depth and strength of the observed changes in soil water O isotopic composition could be well reproduced with a modeling approach (RMSE = 0.2‰, i.e., equivalent to the precision of the isotopic measurements), (ii) the corresponding water volume involved in HL was estimated to account for 19% of the plant transpiration of the following day, i.e., 0.45 mm of water, and was in agreement with the observed soil water content changes, and (iii) the magnitude of the simulated HL was sensitive to both plant and soil hydraulic properties.
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spelling doaj.art-b3521f8a7ba4430ab346a354b1b023202022-12-21T18:46:14ZengWileyVadose Zone Journal1539-16632018-02-0117110.2136/vzj2016.12.0134Measuring and Modeling Hydraulic Lift of Lolium multiflorum Using Stable Water IsotopesFélicien MeunierYouri RothfussThierry BariacPhilippe BironPatricia RichardJean-Louis DurandValentin CouvreurJan VanderborghtMathieu JavauxThis study tested a method to quantify and locate hydraulic lift (HL, defined as the passive upward water flow from wetter to dryer soil zones through the plant root system) by combining an experiment using the stable water isotope HO as a tracer with a soil–plant water flow model. Our methodology consisted in (i) establishing the initial conditions for HL in a large rhizobox planted with Italian ryegrass ( Lam.), (ii) labeling water in the deepest soil layer with an O-enriched solution, (iii) monitoring the water O isotopic composition in soil layers to find out changes in the upper layers that would reflect redistribution of O-enriched water from the bottom layers by the roots, and (iv) comparing the observed soil water O isotopic composition to simulation results of a three-dimensional model of water flow and isotope transport in the soil–root system. Our main findings were that (i) the depth and strength of the observed changes in soil water O isotopic composition could be well reproduced with a modeling approach (RMSE = 0.2‰, i.e., equivalent to the precision of the isotopic measurements), (ii) the corresponding water volume involved in HL was estimated to account for 19% of the plant transpiration of the following day, i.e., 0.45 mm of water, and was in agreement with the observed soil water content changes, and (iii) the magnitude of the simulated HL was sensitive to both plant and soil hydraulic properties.https://dl.sciencesocieties.org/publications/vzj/articles/17/1/160134
spellingShingle Félicien Meunier
Youri Rothfuss
Thierry Bariac
Philippe Biron
Patricia Richard
Jean-Louis Durand
Valentin Couvreur
Jan Vanderborght
Mathieu Javaux
Measuring and Modeling Hydraulic Lift of Lolium multiflorum Using Stable Water Isotopes
Vadose Zone Journal
title Measuring and Modeling Hydraulic Lift of Lolium multiflorum Using Stable Water Isotopes
title_full Measuring and Modeling Hydraulic Lift of Lolium multiflorum Using Stable Water Isotopes
title_fullStr Measuring and Modeling Hydraulic Lift of Lolium multiflorum Using Stable Water Isotopes
title_full_unstemmed Measuring and Modeling Hydraulic Lift of Lolium multiflorum Using Stable Water Isotopes
title_short Measuring and Modeling Hydraulic Lift of Lolium multiflorum Using Stable Water Isotopes
title_sort measuring and modeling hydraulic lift of lolium multiflorum using stable water isotopes
url https://dl.sciencesocieties.org/publications/vzj/articles/17/1/160134
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