Litcius/Paper detail

Soil‐plant hydraulics explain stomatal efficiency‐safety tradeoff

Gaochao Cai, Andrea Carminati, Sean M. Gleason, Mathieu Javaux, Mutez Ali Ahmed

2023Plant Cell & Environment15 citationsDOIOpen Access PDF

Abstract

Abstract The efficiency‐safety tradeoff has been thoroughly investigated in plants, especially concerning their capacity to transport water and avoid embolism. Stomatal regulation is a vital plant behaviour to respond to soil and atmospheric water limitation. Recently, a stomatal efficiency‐safety tradeoff was reported where plants with higher maximum stomatal conductance ( g max ) exhibited greater sensitivity to stomatal closure during soil drying, that is, less negative leaf water potential at 50% g max ( ψ gs50 ). However, the underlying mechanism of this g max ‐ ψ gs50 tradeoff remains unknown. Here, we utilized a soil‐plant hydraulic model, in which stomatal closure is triggered by nonlinearity in soil‐plant hydraulics, to investigate such tradeoff. Our simulations show that increasing g max is aligned with less negative ψ gs50 . Plants with higher g max (also higher transpiration) require larger quantities of water to be moved across the rhizosphere, which results in a precipitous decrease in water potential at the soil‐root interface, and therefore in the leaves. We demonstrated that the g max ‐ ψ gs50 tradeoff can be predicted based on soil‐plant hydraulics, and is impacted by plant hydraulic properties, such as plant hydraulic conductance, active root length and embolism resistance. We conclude that plants may therefore adjust their growth and/or their hydraulic properties to adapt to contrasting habitats and climate conditions.

Topics & Concepts

TranspirationEnvironmental scienceStomatal conductanceHydraulicsSoil waterHydraulic conductivityXylemRhizosphereWater flowSoil scienceWater potentialAgronomyBotanyGeologyBiologyEngineeringPhotosynthesisBacteriaAerospace engineeringPaleontologyPlant Water Relations and Carbon DynamicsIrrigation Practices and Water ManagementSoil and Unsaturated Flow