Transpiration response to soil drying and vapor pressure deficit is soil texture specific

Aims Although soil water deficit is the primary constraint on transpiration globally, the mechanisms by which soil drying and soil properties impact transpiration and stomatal regulation remain elusive. This work aimed to investigate how soil textures and vapor pressure deficit (VPD) impact the rela...

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Published inPlant and soil Vol. 500; no. 1-2; pp. 129 - 145
Main Authors Cai, Gaochao, König, Maria, Carminati, Andrea, Abdalla, Mohanned, Javaux, Mathieu, Wankmüller, Fabian, Ahmed, Mutez Ali
Format Journal Article
LanguageEnglish
Published Cham Springer International Publishing 01.07.2024
Springer
Springer Nature B.V
Subjects
Agriculture
Analysis
Biomedical and Life Sciences
Canopies
canopy
Conductance
Corn
Drying
Ecology
Fluid flow
fluid mechanics
Growth
hydraulic conductivity
Hydraulics
leaf water potential
Leaves
Life Sciences
Loam
Moisture content
Plant Physiology
Plant Sciences
Plants
Research Article
Sand
Soil conductivity
Soil investigations
soil matric potential
Soil moisture
Soil properties
Soil Science & Conservation
Soil texture
Soil water
soil water deficit
species
Stomata
stomatal movement
Terrestrial ecosystems
Texture
Transpiration
Vapor pressure
vapor pressure deficit
Vapors
Water
Water deficit
Water potential
Water shortages
Zea mays
Switzerland
Germany
Stomatal regulation
Leaf water potential
Maize
VPD
Drought
Canopy conductance
Soil–plant hydraulic conductance
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Abstract Aims Although soil water deficit is the primary constraint on transpiration globally, the mechanisms by which soil drying and soil properties impact transpiration and stomatal regulation remain elusive. This work aimed to investigate how soil textures and vapor pressure deficit (VPD) impact the relationship between transpiration rate, canopy conductance, and leaf water potential of maize ( Zea mays L.) during soil drying. We hypothesize that the decrease in soil–plant hydraulic conductance ( K sp ) triggers stomatal closure and the latter is soil specific. Methods Plants were grown in two contrasting soil textures (sand and loam) and exposed to two consecutive VPD levels (1.8 and 2.8 kPa). We measured transpiration rate, canopy conductance, soil and leaf water potentials during soil drying. Results Transpiration rate decreased at higher soil matric potential in sand than in loam at both VPD levels. In sand, high VPD generated a steeper drop in canopy conductance with decreasing leaf water potential. The decrease in canopy conductance was well correlated with the drop in K sp , which was significantly affected by soil texture. Conclusions Our results demonstrated that variations in canopy conductance were not simply a function of leaf water potential but largely affected by soil hydraulics. These results reinforce a model of stomatal closure driven by a loss in soil hydraulic conductivity. Further studies will determine if soil-specific stomatal regulation exists among species.
AbstractList Aims Although soil water deficit is the primary constraint on transpiration globally, the mechanisms by which soil drying and soil properties impact transpiration and stomatal regulation remain elusive. This work aimed to investigate how soil textures and vapor pressure deficit (VPD) impact the relationship between transpiration rate, canopy conductance, and leaf water potential of maize ( Zea mays L.) during soil drying. We hypothesize that the decrease in soil–plant hydraulic conductance ( K sp ) triggers stomatal closure and the latter is soil specific. Methods Plants were grown in two contrasting soil textures (sand and loam) and exposed to two consecutive VPD levels (1.8 and 2.8 kPa). We measured transpiration rate, canopy conductance, soil and leaf water potentials during soil drying. Results Transpiration rate decreased at higher soil matric potential in sand than in loam at both VPD levels. In sand, high VPD generated a steeper drop in canopy conductance with decreasing leaf water potential. The decrease in canopy conductance was well correlated with the drop in K sp , which was significantly affected by soil texture. Conclusions Our results demonstrated that variations in canopy conductance were not simply a function of leaf water potential but largely affected by soil hydraulics. These results reinforce a model of stomatal closure driven by a loss in soil hydraulic conductivity. Further studies will determine if soil-specific stomatal regulation exists among species.
AIMS: Although soil water deficit is the primary constraint on transpiration globally, the mechanisms by which soil drying and soil properties impact transpiration and stomatal regulation remain elusive. This work aimed to investigate how soil textures and vapor pressure deficit (VPD) impact the relationship between transpiration rate, canopy conductance, and leaf water potential of maize (Zea mays L.) during soil drying. We hypothesize that the decrease in soil–plant hydraulic conductance (Kₛₚ) triggers stomatal closure and the latter is soil specific. METHODS: Plants were grown in two contrasting soil textures (sand and loam) and exposed to two consecutive VPD levels (1.8 and 2.8 kPa). We measured transpiration rate, canopy conductance, soil and leaf water potentials during soil drying. RESULTS: Transpiration rate decreased at higher soil matric potential in sand than in loam at both VPD levels. In sand, high VPD generated a steeper drop in canopy conductance with decreasing leaf water potential. The decrease in canopy conductance was well correlated with the drop in Kₛₚ, which was significantly affected by soil texture. CONCLUSIONS: Our results demonstrated that variations in canopy conductance were not simply a function of leaf water potential but largely affected by soil hydraulics. These results reinforce a model of stomatal closure driven by a loss in soil hydraulic conductivity. Further studies will determine if soil-specific stomatal regulation exists among species.
Aims Although soil water deficit is the primary constraint on transpiration globally, the mechanisms by which soil drying and soil properties impact transpiration and stomatal regulation remain elusive. This work aimed to investigate how soil textures and vapor pressure deficit (VPD) impact the relationship between transpiration rate, canopy conductance, and leaf water potential of maize (Zea mays L.) during soil drying. We hypothesize that the decrease in soil-plant hydraulic conductance (K.sub.sp) triggers stomatal closure and the latter is soil specific. Methods Plants were grown in two contrasting soil textures (sand and loam) and exposed to two consecutive VPD levels (1.8 and 2.8 kPa). We measured transpiration rate, canopy conductance, soil and leaf water potentials during soil drying. Results Transpiration rate decreased at higher soil matric potential in sand than in loam at both VPD levels. In sand, high VPD generated a steeper drop in canopy conductance with decreasing leaf water potential. The decrease in canopy conductance was well correlated with the drop in K.sub.sp, which was significantly affected by soil texture. Conclusions Our results demonstrated that variations in canopy conductance were not simply a function of leaf water potential but largely affected by soil hydraulics. These results reinforce a model of stomatal closure driven by a loss in soil hydraulic conductivity. Further studies will determine if soil-specific stomatal regulation exists among species.
AimsAlthough soil water deficit is the primary constraint on transpiration globally, the mechanisms by which soil drying and soil properties impact transpiration and stomatal regulation remain elusive. This work aimed to investigate how soil textures and vapor pressure deficit (VPD) impact the relationship between transpiration rate, canopy conductance, and leaf water potential of maize (Zea mays L.) during soil drying. We hypothesize that the decrease in soil–plant hydraulic conductance (Ksp) triggers stomatal closure and the latter is soil specific.MethodsPlants were grown in two contrasting soil textures (sand and loam) and exposed to two consecutive VPD levels (1.8 and 2.8 kPa). We measured transpiration rate, canopy conductance, soil and leaf water potentials during soil drying.ResultsTranspiration rate decreased at higher soil matric potential in sand than in loam at both VPD levels. In sand, high VPD generated a steeper drop in canopy conductance with decreasing leaf water potential. The decrease in canopy conductance was well correlated with the drop in Ksp, which was significantly affected by soil texture.ConclusionsOur results demonstrated that variations in canopy conductance were not simply a function of leaf water potential but largely affected by soil hydraulics. These results reinforce a model of stomatal closure driven by a loss in soil hydraulic conductivity. Further studies will determine if soil-specific stomatal regulation exists among species.
Audience Academic
Author Cai, Gaochao
König, Maria
Abdalla, Mohanned
Wankmüller, Fabian
Ahmed, Mutez Ali
Carminati, Andrea
Javaux, Mathieu
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  organization: School of Agriculture, Shenzhen Campus of Sun Yat-Sen University, Chair of Soil Physics, Bayreuth Center of Ecology and Environmental Research (BayCEER), University of Bayreuth
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  givenname: Maria
  surname: König
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  organization: Physics of Soils and Terrestrial Ecosystems, Institute of Terrestrial Ecosystems, Department of Environmental Systems Science, ETH Zürich
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  surname: Ahmed
  fullname: Ahmed, Mutez Ali
  email: maaahmed@ucdavis.edu
  organization: Chair of Soil Physics, Bayreuth Center of Ecology and Environmental Research (BayCEER), University of Bayreuth, Department of Land, Air and Water Resources, University of California Davis
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Issue 1-2
Keywords Stomatal regulation
Leaf water potential
Maize
VPD
Drought
Canopy conductance
Soil–plant hydraulic conductance
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content type line 23
ORCID 0000-0002-7402-1571
OpenAccessLink http://hdl.handle.net/2078.1/269535
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PublicationSubtitle An International Journal on Plant-Soil Relationships
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Springer Nature B.V
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Snippet Aims Although soil water deficit is the primary constraint on transpiration globally, the mechanisms by which soil drying and soil properties impact...
Aims Although soil water deficit is the primary constraint on transpiration globally, the mechanisms by which soil drying and soil properties impact...
AimsAlthough soil water deficit is the primary constraint on transpiration globally, the mechanisms by which soil drying and soil properties impact...
AIMS: Although soil water deficit is the primary constraint on transpiration globally, the mechanisms by which soil drying and soil properties impact...
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SubjectTerms Agriculture
Analysis
Biomedical and Life Sciences
Canopies
canopy
Conductance
Corn
Drying
Ecology
Fluid flow
fluid mechanics
Growth
hydraulic conductivity
Hydraulics
leaf water potential
Leaves
Life Sciences
Loam
Moisture content
Plant Physiology
Plant Sciences
Plants
Research Article
Sand
Soil conductivity
Soil investigations
soil matric potential
Soil moisture
Soil properties
Soil Science & Conservation
Soil texture
Soil water
soil water deficit
species
Stomata
stomatal movement
Terrestrial ecosystems
Texture
Transpiration
Vapor pressure
vapor pressure deficit
Vapors
Water
Water deficit
Water potential
Water shortages
Zea mays
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Title Transpiration response to soil drying and vapor pressure deficit is soil texture specific
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