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Published online by Cambridge University Press: 05 December 2011
Non-methane hydrocarbons (NMHC), of biogenic or anthropogenic origin, are important reactants in most atmospheric environments. Oxidation of NMHC can result indirectly in the formation of ozone (Crutzen 1988). In addition to the direct toxic effects of ozone on plants, reaction of alkenes with ozone can produce organic hydroperoxides which are highly reactive and have been implicated in plant damage, especially in those species which are alkene-emitters (Hewitt et al. 1990a, b).