Interactive effects of elevated CO<inf>2</inf>and drought on nocturnal water fluxes in Eucalyptus saligna
- Publication Type:
- Journal Article
- Tree Physiology, 2011, 31 (9), pp. 932 - 944
- Issue Date:
Nocturnal water flux has been observed in trees under a variety of environmental conditions and can be a significant contributor to diel canopy water flux. Elevated atmospheric CO2(elevated [CO2]) can have an important effect on day-time plant water fluxes, but it is not known whether it also affects nocturnal water fluxes. We examined the effects of elevated [CO2] on nocturnal water flux of field-grown Eucalyptus saligna trees using sap flux through the tree stem expressed on a sapwood area (Js) and leaf area (Et) basis. After 19 months growth under well-watered conditions, drought was imposed by withholding water for 5 months in the summer, ending with a rain event that restored soil moisture. Reductions in Jsand Etwere observed during the severe drought period in the dry treatment under elevated [CO2], but not during moderate- and post-drought periods. Elevated [CO2] affected night-time sap flux density which included the stem recharge period, called 'total night flux' (19:00 to 05:00, Js,r), but not during the post-recharge period, which primarily consisted of canopy transpiration (23:00 to 05:00, Js,c). Elevated [CO2] wet (EW) trees exhibited higher Js,rthan ambient [CO2] wet trees (AW) indicating greater water flux in elevated [CO2] under well-watered conditions. However, under drought conditions, elevated [CO2] dry (ED) trees exhibited significantly lower Js,rthan ambient [CO2] dry trees (AD), indicating less water flux during stem recharge under elevated [CO2]. Js,cdid not differ between ambient and elevated [CO2]. Vapour pressure deficit (D) was clearly the major influence on night-time sap flux. D was positively correlated with Js,rand had its greatest impact on Js,rat high D in ambient [CO2]. Our results suggest that elevated [CO2] may reduce night-time water flux in E. saligna when soil water content is low and D is high. While elevated [CO2] affected Js,r, it did not affect day-time water flux in wet soil, suggesting that the responses of Js,rto environmental factors cannot be directly inferred from day-time patterns. Changes in Js,rare likely to influence pre-dawn leaf water potential, and plant responses to water stress. Nocturnal fluxes are clearly important for predicting effects of climate change on forest physiology and hydrology. © 2011 The Author. Published by Oxford University Press. All rights reserved.
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