Atmospheric degradation of n -butyl formate in the presence of O 2 and NO 2

Atmospheric Photo-oxidation of Diethyl Carbonate: Kinetics, Products, and Reaction Mechanism

The rate coefficient for the gas phase of diethyl carbonate with chlorine atoms has been determined at 298 K using a relative method, employing ethyl formate and ethyl acetate as reference compounds. The experimental value, (1.0 ± 0.2) × 10^-11 cm³ molecule^-1 s^-1, is in good correlation with the one estimated by the SAR (Structure-Activity Relationship) method. The photo-oxidation mechanism of diethyl carbonate initiated by chlorine atoms was also studied at 298 K and atmospheric pressure as a function of the oxygen partial pressure. The main products identified by infrared spectroscopy were CH₃CH₂OC(O)OCHO, CH₃CH₂OC(O)OCH₂CHO, CH₃CH₂OC(O)OC(O)CH₃, CO₂, CO, HCOOH, and CH₃COOH. The results reveal that the oxidation process occurs by the abstraction of a hydrogen atom from the methyl (43%) and methylene (57%) groups. The relative importance of each reaction path from the primary radicals formed in photo-oxidation and the identity of CH₃CH₂OC(O)OCHO, CH₃CH₂OC(O)OC(O)CH₃, and CH₃CH₂OC(O)OCH₂CHO were determined using computational methods. The activation energy of reaction paths for the main oxygenated radicals formed during photo-oxidation was determined using Gaussian09 Program.