Loading…

Elevated CO 2 concentration alleviates the negative effect of vapour pressure deficit and soil drought on juvenile poplar growth

The growth performance of short-rotation woody coppice (SRWC) is strongly influenced by successful establishment in the initial months after planting. Future climates, expected to be warmer due to elevated atmospheric CO 2 (eCO 2 ), may bring about more frequent soil droughts alongside increased vap...

Full description

Saved in:
Bibliographic Details
Published in:Central European forestry journal 2024-06, Vol.70 (2), p.51-61
Main Authors: Orság, Matěj, Berhongaray, Gonzalo, Fischer, Milan, Klem, Karel, Ceulemans, Reinhart, King, John S., Hlaváčová, Marcela, Trnka, Miroslav
Format: Article
Language:English
Citations: Items that this one cites
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:The growth performance of short-rotation woody coppice (SRWC) is strongly influenced by successful establishment in the initial months after planting. Future climates, expected to be warmer due to elevated atmospheric CO 2 (eCO 2 ), may bring about more frequent soil droughts alongside increased vapour pressure deficit (eVPD). Hence, this growth chamber experiment aimed to explore the interactive effects of eVPD, eCO 2 , and soil drought on growth and physiology traits of juvenile hybrid poplars under warmer climates. Our findings with juvenile hybrid poplar J-105 revealed that eVPD resulted in reductions in leaf area (–21%), root (–20%) and stem biomass (–9%), as well as in net assimilation (–15%), stomatal conductance (–26%), and transpiration (–13%). However, these decreases were relatively minor compared to the compensating effect of eCO 2 , which generally exerted a stronger influence than eVPD. While soil drought emerged as the primary growth-limiting factor in our study, elevated VPD is not expected to pose a significant additional threat to central European SRWC plantations of juvenile hybrid poplars under future conditions of ongoing climate change.
ISSN:2454-0358
2454-0358
DOI:10.2478/forj-2024-0017