The ozone transfer between atmosphere and vegetation. A study on Scots pine in the field
Altimir N. (2006). The ozone transfer between atmosphere and vegetation. A study on Scots pine in the field. https://doi.org/10.14214/df.28
Abstract
This thesis analysed the controlling processes of the transfer of ozone at the air-plant interface. Improvement in the knowledge of these processes benefits the prediction of both atmospheric removal of O³ and its impact on vegetation. This study was based on the measurement and analysis of multi-year field measurements of O³ flux to Scots pine (Pinus sylvestris L.) foliage with a shoot-scale gas-exchange enclosure system. In addition, the analyses made use of simultaneous CO² and H²O exchange, canopy-scale O³, CO² and H²O exchange, foliage surface wetness, and environmental variables. All data was gathered at the SMEAR measuring station (southern Finland). Enclosure gas-exchange techniques can be applied to the measure of O³ gas-exchange in the field with consideration of artefacts arising from O³ reactivity and low concentration. The O³ wall-loss was corrected with information from simultaneous and continuous measurements, and was included the mass balance formulation of O³ concentration inside the chamber. The flux of ozone to the Scots pine foliage was generated in equal proportions by stomatal and non-stomatal controlled processes. The temporal pattern of total flux was an overlap of the patterns of biological activity and presence of wetness in the environment. The stomatal uptake was estimated from models of stomatal behaviours and the non-stomatal portion of the flux was analysed further. The observed moisture enhancement was related to the presence of liquid films on the foliage surface. Theoretical simulation of the diffusive transfer at one-stoma-scale showed that O³ scavenging reactions located before or near the stomatal aperture can prevent or diminish the diffusion of ozone towards the intercellular air space of the mesophyll. The discussion covers the methodological developments of this study, the relevance of the different controlling factors of ozone flux, the partition amongst its component, and the possible mechanisms of non-stomatal uptake.
Keywords
gas-exchange;
deposition;
shoot-scale chambers;
stomatal and non-stomatal;
uptake;
SMEAR
Published 20 September 2006
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Available at https://doi.org/10.14214/df.28 | Download PDF
Original articles
Altimir, N., Vesala, T., Keronen, P., Kulmala, M., & Hari, P. 2002. Methodology for direct field measurements of ozone flux to foliage with shoot chambers. Atmospheric Environment, 36:1, 19-29.
https://doi.org/10.1016/S1352-2310(01)00478-2
Altimir, N., Tuovinen, J-P., Vesala, T., Kulmala, M., & Hari, P. 2004. Measurements of ozone removal by Scots pine shoots: calibration of a stomatal uptake model including the non-stomatal component. Atmospheric Environment, 38:15, 2387-2398, Special Issue on New methods of risk assessment for ozone impacts on vegetation.
https://doi.org/10.1016/j.atmosenv.2003.09.077
Altimir, N., Kolari, P., Tuovinen, J.-P., Vesala, T., Bäck, J., Suni, T., Kulmala, M. & Hari, P. 2006. Foliage surface ozone deposition: a role for surface moisture?, Biogeosciences, 3, 1-20.
http://www.biogeosciences.net/3/209/2006/
Altimir, N., Vesala, T., Aalto, T, Bäck, J., & Hari, P. Competition between ozone sinks at the air-leaf interface.(Manuscript).