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The atmospheric oxidation of ethyl formate and ethyl acetate over a range of temperatures and oxygen partial pressures
Author(s) -
Orlando John J.,
Tyndall Geoffrey S.
Publication year - 2010
Publication title -
international journal of chemical kinetics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.341
H-Index - 68
eISSN - 1097-4601
pISSN - 0538-8066
DOI - 10.1002/kin.20493
Subject(s) - chemistry , radical , ethyl formate , medicinal chemistry , methyl formate , atmospheric pressure , formate , ethyl acetate , oxygen , atmospheric temperature range , organic chemistry , methanol , catalysis , oceanography , physics , meteorology , geology
The Cl‐atom‐initiated oxidation of two esters, ethyl formate [HC(O)OCH 2 CH 3 ] and ethyl acetate [CH 3 C(O)OCH 2 CH 3 ], has been studied at pressures close to 1 atm as a function of temperature (249–325 K) and O 2 partial pressure (50–700 Torr), using an environmental chamber technique. In both cases, Cl‐atom attack at the CH 2 group is most important, leading in part to the formation of radicals of the type RC(O)OCH(O • )CH 3 [R = H, CH 3 ]. The atmospheric fate of these radicals involves competition between reaction with O 2 to produce an anhydride compound, RC(O)OC(O)CH 3 , and the so‐called α‐ester rearrangement that produces an organic acid, RC(O)OH, and an acetyl radical, CH 3 C(O). For both species studied, the α‐ester rearrangement is found to dominate in air at 1 atm and 298 K. Barriers to the rearrangement of 7.7 ± 1.5 and 8.4 ± 1.5 kcal/mole are estimated for CH 3 C(O)OCH(O • )CH 3 and HC(O)OCH(O • )CH 3 , respectively, leading to increased occurrence of the O 2 reaction at reduced temperature. The data are combined with those obtained from similar studies of other simple esters to provide a correlation between the rate of occurrence of the α‐ester rearrangement and the structure of the reacting radical. © 2010 Wiley Periodicals, Inc. Int J Chem Kinet 42: 397–413, 2010