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Interactions between Ozone and Plant Cuticles. I. Ozone Deposition and Permeability
Gerhard Kerstiens and Klaus J. Lendzian
The New Phytologist
Vol. 112, No. 1 (May, 1989), pp. 13-19
Stable URL: http://www.jstor.org/stable/2556750
Page Count: 7
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The flux of ozone to plant surfaces results in its decomposition at the surface and its uptake through the cuticle. Ozone deposition velocity and ozone permeance were determined for a variety of isolated plant cuticles. Ozone deposition velocity was lower than determined with whole plants kept in darkness. It declined continuously during exposure to the gas and showed a 'recovery' effect after an interruption of the fumigation. It increased with the moisture content of the cuticles and decreased when the ozone concentration in the surrounding air was raised. The deposition velocity was much higher than cuticular ozone permeance at equivalent ozone concentrations. Due to the ozone decay in the cuticle, ozone permeance was much lower in thick than in thin cuticles. Even with the most permeable cuticles, ozone uptake under natural conditions is smaller than the flux through open stomata by a factor of at least 10 000.
The New Phytologist © 1989 New Phytologist Trust