Rate constants for the reaction of NO and HO 2 with peroxy radicals formed from the reaction of OH, Cl or NO 3 with alkenes, dienes and α,β-unsaturated carbonyls. Atmospheric Environment 37 (32) 4517-4527.This is an author-produced version of a paper published in Atmospheric Environment (ISSN 1352(ISSN -2310. This version has been peer-reviewed but does not include the final publisher proof corrections, published layout or pagination.All articles available through Birkbeck ePrints are protected by intellectual property law, including copyright law. Any use made of the contents should comply with the relevant law.
AbstractRate constants for the gas-phase reaction of NO and HO 2 radicals with 33 peroxy radicals are presented. The peroxy radicals are derived from the addition of either OH, Cl, or NO 3 radicals, followed by addition of O 2 , to a series of alkenes: tetrachloroethene, ethene, 1,2−dimethyl but−2−ene, butadiene, 2,3,4,5−tetramethyl hexa−1,3−diene, 1,1,2,3,4,4−hexachlorobutadiene but−1−ene−3−one (methyl vinyl ketone) and 2,3−dimethylpen−2−ene−4−one. The rate constants were predicted using a correlation between the singly occupied molecular orbital (SOMO) energy of the peroxy radical and the logarithm of the rate constant for reaction with NO or HO 2 . A discussion of the accuracy of the method and the trends in the reactivity of the titled peroxy radicals is given. Peroxy radicals derived from halogenated alkenes have larger values of rate constants for reaction with NO relative to reaction with HO 2 , indicating that they are more likely to react with NO, rather than HO 2 , in the atmosphere. The reverse is true for peroxy radicals derived from alkylated alkenes.