Abstract

Quantifying heat and mass exchanges processes of plant leaves is crucial for detailed understanding of dynamic plant-environment interactions. The two main components of these processes, convective heat transfer, and transpiration, are inevitably coupled as both processes are restricted by the leaf boundary layer. To measure leaf heat capacity and leaf heat transfer coefficient, we thoroughly tested and applied an active thermography method that uses a transient heat pulse to compute τ, the time constant of leaf cooling after release of the pulse. We validated our approach in the laboratory on intact leaves of spring barley (Hordeum vulgare) and common bean (Phaseolus vulgaris), and measured τ-changes at different boundary layer conditions.By modeling the leaf heat transfer coefficient with dimensionless numbers, we could demonstrate that τ improves our ability to close the energy budget of plant leaves and that modeling of transpiration requires considerations of convection. Applying our approach to thermal images we obtained spatio-temporal maps of τ, providing observations of local differences in thermal responsiveness of leaf surfaces. We propose that active thermography is an informative methodology to measure leaf heat transfer and derive spatial maps of thermal responsiveness of leaves contributing to improve models of leaf heat transfer processes.

Highlights

  • Plants continuously interact with their environment by heat and mass exchange and play an important role in the earth’s hydrological and carbon cycle (Foley et al, 2003)

  • We tested the relationship between t, obtained by active thermography, and leaf water content per unit area (LWC) by measuring dark-adapted leaves of both, spring barley and common bean

  • We characterized the t-response with an exponential regression and the derived wind speed at which t has decreased to 50% of its initial value (u0.5)

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Summary

Introduction

Plants continuously interact with their environment by heat and mass exchange and play an important role in the earth’s hydrological and carbon cycle (Foley et al, 2003). The most important physiological process resulting in gas and mass exchange with the atmosphere is photosynthesis accompanied by transpiration. Heat and mass exchange between plants and their environment significantly affects plant productivity, water use, and water use efficiency (Shibuya et al, 2006; Schymanski and Or, 2015). Wind affects transpiration rates by removing the water vapor within the boundary layer leading to a higher leaf-to-air water vapor pressure deficit and may induce stomatal closure (Grace, 1974; Dixon and Grace, 1983; Bunce, 1985)

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