Root hydraulic phenotypes impacting water uptake in drying soils

Soil drying is a limiting factor for crop production worldwide. Yet, it is not clear how soil drying impacts water uptake across different soils, species, and root phenotypes. Here we ask (1) what root phenotypes improve the water use from drying soils? and (2) what root hydraulic properties impact...

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Published inPlant, cell and environment Vol. 45; no. 3; pp. 650 - 663
Main Authors Cai, Gaochao, Ahmed, Mutez A., Abdalla, Mohanned, Carminati, Andrea
Format Journal Article
LanguageEnglish
Published United States Wiley Subscription Services, Inc 01.03.2022
John Wiley and Sons Inc
Subjects
Conductance
Crop production
Desiccation
drought
Drying
environment
hydraulic conductivity
Hydraulic properties
Hydraulics
Invited Review
Invited Reviews
leaf water potential
leaves
Moisture content
Phenotype
Phenotypes
Plant Roots - chemistry
Plant Transpiration
Root hairs
root hydraulic conductance
root length
root water uptake
Soil
soil hydraulic conductivity
Soil investigations
Soil properties
Soil texture
Soil water
Soil water potential
Soils
Transpiration
Water - analysis
Water flow
Water potential
Water uptake
Water use
soil texture
soil hydraulic conductivity
root hydraulic conductance
drought
leaf water potential
root water uptake
root hairs
root length
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Abstract Soil drying is a limiting factor for crop production worldwide. Yet, it is not clear how soil drying impacts water uptake across different soils, species, and root phenotypes. Here we ask (1) what root phenotypes improve the water use from drying soils? and (2) what root hydraulic properties impact water flow across the soil–plant continuum? The main objective is to propose a hydraulic framework to investigate the interplay between soil and root hydraulic properties on water uptake. We collected highly resolved data on transpiration, leaf and soil water potential across 11 crops and 10 contrasting soil textures. In drying soils, the drop in water potential at the soil–root interface resulted in a rapid decrease in soil hydraulic conductance, especially at higher transpiration rates. The analysis reveals that water uptake was limited by soil within a wide range of soil water potential (−6 to −1000 kPa), depending on both soil textures and root hydraulic phenotypes. We propose that a root phenotype with low root hydraulic conductance, long roots and/or long and dense root hairs postpones soil limitation in drying soils. The consequence of these root phenotypes on crop water use is discussed. Summary statement During soil drying, the drop in soil–plant hydraulic conductance causes a decline in root water uptake, which is impacted by soil and root hydraulic phenotypes. Lower root conductance, longer root length and longer root hairs would allow plants to maintain water uptake at lower soil matric potential.
AbstractList Soil drying is a limiting factor for crop production worldwide. Yet, it is not clear how soil drying impacts water uptake across different soils, species, and root phenotypes. Here we ask (1) what root phenotypes improve the water use from drying soils? and (2) what root hydraulic properties impact water flow across the soil–plant continuum? The main objective is to propose a hydraulic framework to investigate the interplay between soil and root hydraulic properties on water uptake. We collected highly resolved data on transpiration, leaf and soil water potential across 11 crops and 10 contrasting soil textures. In drying soils, the drop in water potential at the soil–root interface resulted in a rapid decrease in soil hydraulic conductance, especially at higher transpiration rates. The analysis reveals that water uptake was limited by soil within a wide range of soil water potential (−6 to −1000 kPa), depending on both soil textures and root hydraulic phenotypes. We propose that a root phenotype with low root hydraulic conductance, long roots and/or long and dense root hairs postpones soil limitation in drying soils. The consequence of these root phenotypes on crop water use is discussed. Summary statement During soil drying, the drop in soil–plant hydraulic conductance causes a decline in root water uptake, which is impacted by soil and root hydraulic phenotypes. Lower root conductance, longer root length and longer root hairs would allow plants to maintain water uptake at lower soil matric potential.
Soil drying is a limiting factor for crop production worldwide. Yet, it is not clear how soil drying impacts water uptake across different soils, species, and root phenotypes. Here we ask (1) what root phenotypes improve the water use from drying soils? and (2) what root hydraulic properties impact water flow across the soil–plant continuum? The main objective is to propose a hydraulic framework to investigate the interplay between soil and root hydraulic properties on water uptake. We collected highly resolved data on transpiration, leaf and soil water potential across 11 crops and 10 contrasting soil textures. In drying soils, the drop in water potential at the soil–root interface resulted in a rapid decrease in soil hydraulic conductance, especially at higher transpiration rates. The analysis reveals that water uptake was limited by soil within a wide range of soil water potential (−6 to −1000 kPa), depending on both soil textures and root hydraulic phenotypes. We propose that a root phenotype with low root hydraulic conductance, long roots and/or long and dense root hairs postpones soil limitation in drying soils. The consequence of these root phenotypes on crop water use is discussed.
Soil drying is a limiting factor for crop production worldwide. Yet, it is not clear how soil drying impacts water uptake across different soils, species, and root phenotypes. Here we ask (1) what root phenotypes improve the water use from drying soils? and (2) what root hydraulic properties impact water flow across the soil–plant continuum? The main objective is to propose a hydraulic framework to investigate the interplay between soil and root hydraulic properties on water uptake. We collected highly resolved data on transpiration, leaf and soil water potential across 11 crops and 10 contrasting soil textures. In drying soils, the drop in water potential at the soil–root interface resulted in a rapid decrease in soil hydraulic conductance, especially at higher transpiration rates. The analysis reveals that water uptake was limited by soil within a wide range of soil water potential (−6 to −1000 kPa), depending on both soil textures and root hydraulic phenotypes. We propose that a root phenotype with low root hydraulic conductance, long roots and/or long and dense root hairs postpones soil limitation in drying soils. The consequence of these root phenotypes on crop water use is discussed. During soil drying, the drop in soil–plant hydraulic conductance causes a decline in root water uptake, which is impacted by soil and root hydraulic phenotypes. Lower root conductance, longer root length and longer root hairs would allow plants to maintain water uptake at lower soil matric potential.
Soil drying is a limiting factor for crop production worldwide. Yet, it is not clear how soil drying impacts water uptake across different soils, species, and root phenotypes. Here we ask (1) what root phenotypes improve the water use from drying soils? and (2) what root hydraulic properties impact water flow across the soil-plant continuum? The main objective is to propose a hydraulic framework to investigate the interplay between soil and root hydraulic properties on water uptake. We collected highly resolved data on transpiration, leaf and soil water potential across 11 crops and 10 contrasting soil textures. In drying soils, the drop in water potential at the soil-root interface resulted in a rapid decrease in soil hydraulic conductance, especially at higher transpiration rates. The analysis reveals that water uptake was limited by soil within a wide range of soil water potential (-6 to -1000 kPa), depending on both soil textures and root hydraulic phenotypes. We propose that a root phenotype with low root hydraulic conductance, long roots and/or long and dense root hairs postpones soil limitation in drying soils. The consequence of these root phenotypes on crop water use is discussed.
Soil drying is a limiting factor for crop production worldwide. Yet, it is not clear how soil drying impacts water uptake across different soils, species, and root phenotypes. Here we ask (1) what root phenotypes improve the water use from drying soils? and (2) what root hydraulic properties impact water flow across the soil-plant continuum? The main objective is to propose a hydraulic framework to investigate the interplay between soil and root hydraulic properties on water uptake. We collected highly resolved data on transpiration, leaf and soil water potential across 11 crops and 10 contrasting soil textures. In drying soils, the drop in water potential at the soil-root interface resulted in a rapid decrease in soil hydraulic conductance, especially at higher transpiration rates. The analysis reveals that water uptake was limited by soil within a wide range of soil water potential (-6 to -1000 kPa), depending on both soil textures and root hydraulic phenotypes. We propose that a root phenotype with low root hydraulic conductance, long roots and/or long and dense root hairs postpones soil limitation in drying soils. The consequence of these root phenotypes on crop water use is discussed.Soil drying is a limiting factor for crop production worldwide. Yet, it is not clear how soil drying impacts water uptake across different soils, species, and root phenotypes. Here we ask (1) what root phenotypes improve the water use from drying soils? and (2) what root hydraulic properties impact water flow across the soil-plant continuum? The main objective is to propose a hydraulic framework to investigate the interplay between soil and root hydraulic properties on water uptake. We collected highly resolved data on transpiration, leaf and soil water potential across 11 crops and 10 contrasting soil textures. In drying soils, the drop in water potential at the soil-root interface resulted in a rapid decrease in soil hydraulic conductance, especially at higher transpiration rates. The analysis reveals that water uptake was limited by soil within a wide range of soil water potential (-6 to -1000 kPa), depending on both soil textures and root hydraulic phenotypes. We propose that a root phenotype with low root hydraulic conductance, long roots and/or long and dense root hairs postpones soil limitation in drying soils. The consequence of these root phenotypes on crop water use is discussed.
Author Cai, Gaochao
Abdalla, Mohanned
Ahmed, Mutez A.
Carminati, Andrea
AuthorAffiliation 3 Department of Environmental Systems Science, Physics of Soils and Terrestrial Ecosystems Institute of Terrestrial Ecosystems, ETH Zürich Zurich Switzerland
2 Department of Land, Air and Water Resources University of California Davis Davis California United States
1 Chair of Soil Physics, Bayreuth Center of Ecology and Environmental Research (BayCEER) University of Bayreuth Bayreuth Germany
AuthorAffiliation_xml – name: 2 Department of Land, Air and Water Resources University of California Davis Davis California United States
– name: 3 Department of Environmental Systems Science, Physics of Soils and Terrestrial Ecosystems Institute of Terrestrial Ecosystems, ETH Zürich Zurich Switzerland
– name: 1 Chair of Soil Physics, Bayreuth Center of Ecology and Environmental Research (BayCEER) University of Bayreuth Bayreuth Germany
Author_xml – sequence: 1
  givenname: Gaochao
  orcidid: 0000-0003-4484-1146
  surname: Cai
  fullname: Cai, Gaochao
  organization: University of Bayreuth
– sequence: 2
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  orcidid: 0000-0002-7402-1571
  surname: Ahmed
  fullname: Ahmed, Mutez A.
  organization: University of California Davis
– sequence: 3
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  orcidid: 0000-0002-4220-8761
  surname: Abdalla
  fullname: Abdalla, Mohanned
  organization: University of Bayreuth
– sequence: 4
  givenname: Andrea
  orcidid: 0000-0001-7415-0480
  surname: Carminati
  fullname: Carminati, Andrea
  email: andrea.carminati@usys.ethz.ch
  organization: Institute of Terrestrial Ecosystems, ETH Zürich
BackLink https://www.ncbi.nlm.nih.gov/pubmed/35037263$$D View this record in MEDLINE/PubMed
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IsDoiOpenAccess true
IsOpenAccess true
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IsScholarly true
Issue 3
Keywords soil texture
soil hydraulic conductivity
root hydraulic conductance
drought
leaf water potential
root water uptake
root hairs
root length
Language English
License Attribution-NonCommercial
2022 The Authors. Plant, Cell & Environment published by John Wiley & Sons Ltd.
This is an open access article under the terms of the http://creativecommons.org/licenses/by-nc/4.0/ License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited and is not used for commercial purposes.
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Snippet Soil drying is a limiting factor for crop production worldwide. Yet, it is not clear how soil drying impacts water uptake across different soils, species, and...
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SourceType Open Access Repository
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StartPage 650
SubjectTerms Conductance
Crop production
Desiccation
drought
Drying
environment
hydraulic conductivity
Hydraulic properties
Hydraulics
Invited Review
Invited Reviews
leaf water potential
leaves
Moisture content
Phenotype
Phenotypes
Plant Roots - chemistry
Plant Transpiration
Root hairs
root hydraulic conductance
root length
root water uptake
Soil
soil hydraulic conductivity
Soil investigations
Soil properties
Soil texture
Soil water
Soil water potential
Soils
Transpiration
Water - analysis
Water flow
Water potential
Water uptake
Water use
Title Root hydraulic phenotypes impacting water uptake in drying soils
URI https://onlinelibrary.wiley.com/doi/abs/10.1111%2Fpce.14259
https://www.ncbi.nlm.nih.gov/pubmed/35037263
https://www.proquest.com/docview/2633228641
https://www.proquest.com/docview/2620785987
https://www.proquest.com/docview/2661040054
https://pubmed.ncbi.nlm.nih.gov/PMC9303794
Volume 45
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