Abstract
It is now well established that the ozone molecules present in the lower troposphere generally undergo a downward flux through the surface layer, as a consequence of a dry deposition process at the surface. This fact was first described by Regener [1]. Rich et al. [2] studied the removal of ozone from the air by bean leaves under controlled conditions and found that its rate follows a pattern that is very similar to that of evaporation. Using the resistance analogy, they inferred from these observations that both processes are controlled by the stomatal aperture. Galbally [3] and Galbally and Roy [4] measured ozone deposition rates using enclosure techniques on various surface types, both bare and vegetated. Turner et al. [5] stated that both bare soils and vegetation are targets for ozone deposition.
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Cieslik, S., Labatut, A. (1997). Ozone Deposition on Various Surface Types. In: Slanina, S. (eds) Biosphere-Atmosphere Exchange of Pollutants and Trace Substances. Transport and Chemical Transformation of Pollutants in the Troposphere, vol 4. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-03394-4_11
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DOI: https://doi.org/10.1007/978-3-662-03394-4_11
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