Issue 13, 2008

Formation of a Criegee intermediate in the low-temperature oxidation of dimethyl sulfoxide

Abstract

Dimethyl sulfoxide (DMSO) is the major sulfur-containing constituent of the Marine Boundary Layer. It is a significant source of H2SO4 aerosol/particles and methane sulfonic acid via atmospheric oxidation processes, where the mechanism is not established. In this study, several new, low-temperature pathways are revealed in the oxidation of DMSO using CBS-QB3 and G3MP2 multilevel and B3LYP hybrid density functional quantum chemical methods. Unlike analogous hydrocarbon peroxy radicals the chemically activated DMSO peroxy radical, [CH3S([double bond, length as m-dash]O)CH2OO˙]*, predominantly undergoes simple dissociation to a methylsulfinyl radical CH3S˙([double bond, length as m-dash]O) and a Criegee intermediate, CH2OO, with the barrier to dissociation 11.3 kcal mol−1 below the energy of the CH3S([double bond, length as m-dash]O)CH2˙ + O2 reactants. The well depth for addition of O2 to the CH3S([double bond, length as m-dash]O)CH2˙ precursor radical is 29.6 kcal mol−1 at the CBS-QB3 level of theory. We believe that this reaction may serve an important role in atmospheric photochemical and irradiated biological (oxygen-rich) media where formation of initial radicals is facilitated even at lower temperatures. The Criegee intermediate (carbonyl oxide, peroxymethylene) and sulfinyl radical can further decompose, resulting in additional chain branching. A second reaction channel important for oxidation processes includes formation (via intramolecular H atom transfer) and further decomposition of hydroperoxide methylsulfoxide radical, ˙CH2S([double bond, length as m-dash]O)CH2OOH over a low barrier of activation. The initial H-transfer reaction is similar and common in analogous hydrocarbon radical + O2 reactions; but the subsequent very low (3–6 kcal mol−1) barrier (14 kcal mol−1 below the initial reagents) to β-scission products is not common in HC systems. The low energy reaction of the hydroperoxide radical is a β-scission elimination of ˙CH2S([double bond, length as m-dash]O)CH2OOH into the CH2[double bond, length as m-dash]S[double bond, length as m-dash]O + CH2O + ˙OH product set. This β-scission barrier is low, because of the delocalization of the ˙CH2 radical center through the –S([double bond, length as m-dash]O) group, to the –CH2OOH fragment in the transition state structure. The hydroperoxide methylsulfoxide radical can also decompose via a second reaction channel of intramolecular OH migration, yielding formaldehyde and a sulfur-centered hydroxymethylsulfinyl radical HOCH2S˙([double bond, length as m-dash]O). The barrier of activation relative to initial reagents is 4.2 kcal mol−1. Heats of formation for DMSO, DMSO carbon-centered radical and Criegee intermediate are evaluated at 298 K as −35.97 ± 0.05, 13.0 ± 0.2 and 25.3 ± 0.7 kcal mol−1 respectively using isodesmic reaction analysis. The [CH3S˙([double bond, length as m-dash]O) + CH2OO] product set is shown to form a van der Waals complex that results in O-atom transfer reaction and the formation of new products CH3SO2˙ radical and CH2O. Proper orientation of the Criegee intermediate and methylsulfinyl radical, as a pre-stabilized pre-reaction complex, assist the process. The DMSO radical reaction is also compared to that of acetonyl radical.

Graphical abstract: Formation of a Criegee intermediate in the low-temperature oxidation of dimethyl sulfoxide

Supplementary files

Article information

Article type
Paper
Submitted
19 Oct 2007
Accepted
15 Jan 2008
First published
19 Feb 2008

Phys. Chem. Chem. Phys., 2008,10, 1769-1780

Formation of a Criegee intermediate in the low-temperature oxidation of dimethyl sulfoxide

R. Asatryan and J. W. Bozzelli, Phys. Chem. Chem. Phys., 2008, 10, 1769 DOI: 10.1039/B716179D

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