Estimates of tree root water uptake from soil moisture profile dynamics
<p>Root water uptake (RWU), as an important process in the terrestrial water cycle, can help us to better understand the interactions in the soil–plant–atmosphere continuum. We conducted a field study monitoring soil moisture profiles in the rhizosphere of beech trees at two sites with differe...
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2020-11-01
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doaj-64de6a1bec824cddb4508cd9008ea4042020-11-25T04:12:29ZengCopernicus PublicationsBiogeosciences1726-41701726-41892020-11-01175787580810.5194/bg-17-5787-2020Estimates of tree root water uptake from soil moisture profile dynamicsC. Jackisch0C. Jackisch1C. Jackisch2S. Knoblauch3S. Knoblauch4T. Blume5E. Zehe6S. K. Hassler7Institute of Water and River Basin Management, Karlsruhe Institute of Technology (KIT), Kaiserstraße 12, 76131 Karlsruhe, GermanyDepartment of Landscape Ecology and Environmental Systems Analysis, Institute of Geoecology, Technische Universität Braunschweig, Langer Kamp 19c, 38106 Braunschweig, GermanyFaculty of Geosciences, Geoengineering and Mining, Technische Universität Bergakademie Freiberg, Agricolastraße 22, 09599 Freiberg, GermanyInstitute of Water and River Basin Management, Karlsruhe Institute of Technology (KIT), Kaiserstraße 12, 76131 Karlsruhe, GermanyDepartment of Biology, University of Greifswald, Friedrich-Ludwig-Jahn-Straße 15, 17489 Greifswald, GermanyHydrology Section, GFZ German Research Centre for Geosciences, Helmholtz Centre Potsdam, Telegrafenberg C4, 14473 Potsdam, GermanyInstitute of Water and River Basin Management, Karlsruhe Institute of Technology (KIT), Kaiserstraße 12, 76131 Karlsruhe, GermanyInstitute of Water and River Basin Management, Karlsruhe Institute of Technology (KIT), Kaiserstraße 12, 76131 Karlsruhe, Germany<p>Root water uptake (RWU), as an important process in the terrestrial water cycle, can help us to better understand the interactions in the soil–plant–atmosphere continuum. We conducted a field study monitoring soil moisture profiles in the rhizosphere of beech trees at two sites with different soil conditions. We present an algorithm to infer RWU from step-shaped, diurnal changes in soil moisture.</p> <p>While this approach is a feasible, easily implemented method for moderately moist and homogeneously textured soil conditions, limitations were identified during drier states and for more heterogeneous soil settings. A comparison with the time series of xylem sap velocity underlines that RWU and sap flow (SF) are complementary measures in the transpiration process. The high correlation between the SF time series of the two sites, but lower correlation between the RWU time series, suggests that soil characteristics affect RWU of the trees but not SF.</p>https://bg.copernicus.org/articles/17/5787/2020/bg-17-5787-2020.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
C. Jackisch C. Jackisch C. Jackisch S. Knoblauch S. Knoblauch T. Blume E. Zehe S. K. Hassler |
spellingShingle |
C. Jackisch C. Jackisch C. Jackisch S. Knoblauch S. Knoblauch T. Blume E. Zehe S. K. Hassler Estimates of tree root water uptake from soil moisture profile dynamics Biogeosciences |
author_facet |
C. Jackisch C. Jackisch C. Jackisch S. Knoblauch S. Knoblauch T. Blume E. Zehe S. K. Hassler |
author_sort |
C. Jackisch |
title |
Estimates of tree root water uptake from soil moisture profile dynamics |
title_short |
Estimates of tree root water uptake from soil moisture profile dynamics |
title_full |
Estimates of tree root water uptake from soil moisture profile dynamics |
title_fullStr |
Estimates of tree root water uptake from soil moisture profile dynamics |
title_full_unstemmed |
Estimates of tree root water uptake from soil moisture profile dynamics |
title_sort |
estimates of tree root water uptake from soil moisture profile dynamics |
publisher |
Copernicus Publications |
series |
Biogeosciences |
issn |
1726-4170 1726-4189 |
publishDate |
2020-11-01 |
description |
<p>Root water uptake (RWU), as an important process in the terrestrial water cycle, can help us to better understand the interactions in the soil–plant–atmosphere continuum. We conducted a field study monitoring soil moisture profiles in the rhizosphere of beech trees at two sites with different soil conditions. We present an algorithm to infer RWU from step-shaped, diurnal changes in soil moisture.</p>
<p>While this approach is a feasible, easily implemented method for moderately moist and homogeneously textured soil conditions, limitations were identified during drier states and for more heterogeneous soil settings. A comparison with the time series of xylem sap velocity underlines that RWU and sap flow (SF) are complementary measures in the transpiration process. The high correlation between the SF time series of the two sites, but lower correlation between the RWU time series, suggests that soil characteristics affect RWU of the trees but not SF.</p> |
url |
https://bg.copernicus.org/articles/17/5787/2020/bg-17-5787-2020.pdf |
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