Plant leaf temperatures can differ from ambient air temperatures. A temperature gradient in a gas mixture gives rise to a phenomenon known as thermodiffusion, which operates in addition to ordinary diffusion. Whilst transpiration is generally understood to be driven solely by the ordinary diffusion of water vapour along a concentration gradient, we consider the implications of thermodiffusion for transpiration. We develop a new modelling framework that introduces the effects of thermodiffusion on the transpiration rate, E. By applying this framework, we quantify the proportion of E attributable to thermodiffusion for a set of physiological and environmental conditions, varied over a wide range. Thermodiffusion is found to be most significant (in some cases > 30% of E) when a leaf-to-air temperature difference coincides with a relatively small water vapour concentration difference across the boundary layer; a boundary layer conductance that is large as compared to the stomatal conductance; or a relatively low transpiration rate. Thermodiffusion also alters the conditions required for the onset of reverse transpiration, and the rate at which this water vapour uptake occurs.
Details
Title
The role of thermodiffusion in transpiration
Creators
Danielle S Griffani - Southern Cross University
Pierre Rognon - University of Sydney
Graham D Farquhar - Australian National University
Publication Details
The New phytologist, Vol.243(4), pp.1301-1311
Publisher
Wiley-Blackwell Publishing Ltd.
Grant note
CE140100015 / Australian Research Council
Identifiers
991013173907002368
Copyright
(c) 2024 The Authors.
This is an open access article under the terms of the Creative Commons Attribution License.