Transpiration response to soil drying versus increasing vapor pressure deficit in crops : physical and physiological mechanisms and key plant traits

© The Author(s) 2023. Published by Oxford University Press on behalf of the Society for Experimental Biology.

Bibliographische Detailangaben
Veröffentlicht in:Journal of experimental botany. - 1985. - 74(2023), 16 vom: 02. Sept., Seite 4789-4807
1. Verfasser: Koehler, Tina (VerfasserIn)
Weitere Verfasser: Wankmüller, Fabian J P, Sadok, Walid, Carminati, Andrea
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2023
Zugriff auf das übergeordnete Werk:Journal of experimental botany
Schlagworte:Journal Article Research Support, Non-U.S. Gov't Plant traits root water uptake soil drying soil–plant hydraulics stomatal regulation transpiration rate vapor pressure deficit Soil mehr... Water 059QF0KO0R
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520 |a © The Author(s) 2023. Published by Oxford University Press on behalf of the Society for Experimental Biology. 
520 |a The water deficit experienced by crops is a function of atmospheric water demand (vapor pressure deficit) and soil water supply over the whole crop cycle. We summarize typical transpiration response patterns to soil and atmospheric drying and the sensitivity to plant hydraulic traits. We explain the transpiration response patterns using a soil-plant hydraulic framework. In both cases of drying, stomatal closure is triggered by limitations in soil-plant hydraulic conductance. However, traits impacting the transpiration response differ between the two drying processes and act at different time scales. A low plant hydraulic conductance triggers an earlier restriction in transpiration during increasing vapor pressure deficit. During soil drying, the impact of the plant hydraulic conductance is less obvious. It is rather a decrease in the belowground hydraulic conductance (related to soil hydraulic properties and root length density) that is involved in transpiration down-regulation. The transpiration response to increasing vapor pressure deficit has a daily time scale. In the case of soil drying, it acts on a seasonal scale. Varieties that are conservative in water use on a daily scale may not be conservative over longer time scales (e.g. during soil drying). This potential independence of strategies needs to be considered in environment-specific breeding for yield-based drought tolerance 
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650 4 |a Research Support, Non-U.S. Gov't 
650 4 |a Plant traits 
650 4 |a root water uptake 
650 4 |a soil drying 
650 4 |a soil–plant hydraulics 
650 4 |a stomatal regulation 
650 4 |a transpiration rate 
650 4 |a vapor pressure deficit 
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700 1 |a Wankmüller, Fabian J P  |e verfasserin  |4 aut 
700 1 |a Sadok, Walid  |e verfasserin  |4 aut 
700 1 |a Carminati, Andrea  |e verfasserin  |4 aut 
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