Organic peroxy radicals (RO 2 ), formed from the degradation of hydrocarbons and other volatile organic compounds (VOCs), play a key role in tropospheric oxidation mechanisms. Several competing reactions may be available for a given RO 2 radical, the relative rates of which depend on both the structure of RO 2 and the ambient conditions. Published kinetics and branching ratio data are reviewed for the bimolecular reactions of RO 2 with NO, NO 2 , NO 3 , OH and HO 2 ; and for their self-reactions and cross-reactions with other RO 2 radicals. This information is used to define generic rate coefficients and structure-activity relationship (SAR) methods that can be applied to the bimolecular reactions of a series of important classes of hydrocarbon and oxygenated RO 2 radicals. Information for selected unimolecular isomerization reactions (i.e. H-atom shift and ring-closure reactions) is also summarized and discussed. The methods presented here are intended to guide the representation of RO 2 radical chemistry in the next generation of explicit detailed chemical mechanisms.Under tropospheric conditions, a given RO 2 radical may have several competing reactions available, the relative rates of which are dependent both on the prevailing ambient conditions and on the structure of RO 2 . These include a series of bimolecular reactions (i.e. with NO, NO 2 , NO 3 , OH and HO 2 ; and the self-reaction and cross-reactions with the multitude of other RO 2 radicals present in the atmosphere), which are generally available for all RO 2 radicals; and specific unimolecular isomerization reactions (i.e. H-atom shiftPublished by Copernicus Publications on behalf of the European Geosciences Union.