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

被引:45
作者
Asatryan, Rubik [1 ]
Bozzelli, Joseph W. [1 ]
机构
[1] New Jersey Inst Technol, Dept Chem & Environm Sci, Newark, NJ 07102 USA
关键词
D O I
10.1039/b716179d
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
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(=O)CH2OO center dot]*, predominantly undergoes simple dissociation to a methylsulfinyl radical CH3S center dot(=O) and a Criegee intermediate, CH2OO, with the barrier to dissociation 11.3 kcal mol(-1) below the energy of the CH3S(=QO)CH2 center dot + O-2 reactants. The well depth for addition of O-2 to the CH3S(=O)CH2 center dot 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)-C-center dot(=O)CH2OOH over a low barrier of activation. The initial H-transfer reaction is similar and common in analogous hydrocarbon radical + O-2 reactions; but the subsequent very low (3-6 kcal mol(-1)) barrier ( 14 kcal mol(-1) below the initial reagents) to beta-scission products is not common in HC systems. The low energy reaction of the hydroperoxide radical is a b-scission elimination of (CH2S)-C-center dot(=O)CH2OOH into the CH2=S=O + CH2O + (OH)-O-center dot product set. This beta-scission barrier is low, because of the delocalization of the (CH2)-C-center dot radical center through the -S(=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 center dot(=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 center dot(=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 center dot 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.
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收藏
页码:1769 / 1780
页数:12
相关论文
共 81 条
[21]   THE REACTION OF OH RADICALS WITH DIMETHYL-SULFOXIDE - A COMPARATIVE-STUDY OF FENTON REAGENT AND THE RADIOLYSIS OF AQUEOUS DIMETHYL-SULFOXIDE SOLUTIONS [J].
EBERHARDT, MK ;
COLINA, R .
JOURNAL OF ORGANIC CHEMISTRY, 1988, 53 (05) :1071-1074
[22]   Thermochemistry of acetonyl and related radicals [J].
El-Nahas, Ahmed M. ;
Bozzelli, Joseph W. ;
Simmie, John M. ;
Navarro, Maria V. ;
Black, Grainne ;
Curran, Henry J. .
JOURNAL OF PHYSICAL CHEMISTRY A, 2006, 110 (50) :13618-13623
[23]  
ELNAHAS AM, 2006, P 19 INT S GAS KIN O, P225
[24]   DIMETHYL DULFOXIDE OXIDATIONS [J].
EPSTEIN, WW ;
SWEAT, FW .
CHEMICAL REVIEWS, 1967, 67 (03) :247-&
[25]   Measurements and modeling of DO2 formation in the reactions of C2D5 and C3D7 radicals with O2 [J].
Estupinan, Edgar G. ;
Smith, Jared D. ;
Tezaki, Atsumu ;
Klippenstein, Stephen J. ;
Taatjes, Craig A. .
JOURNAL OF PHYSICAL CHEMISTRY A, 2007, 111 (19) :4015-4030
[26]   Atmospheric gas-phase reactions of dimethylsulphoxide and dimethylsulphone with ON and NO3 radicals, Cl atoms and ozone [J].
Falbe-Hansen, H ;
Sorensen, S ;
Jensen, NR ;
Pedersen, T ;
Hjorth, J .
ATMOSPHERIC ENVIRONMENT, 2000, 34 (10) :1543-1551
[27]   CASSCF and CAS+1+2 studies on the potential energy surface and the rate constants for the reactions between CH2 and O2 [J].
Fang, DC ;
Fu, XY .
JOURNAL OF PHYSICAL CHEMISTRY A, 2002, 106 (12) :2988-2993
[28]  
Finlayson-Pitts B. J., 2000, Chemistry of the Upper and Lower Atmosphere
[29]   Sulfur atom exchange in the reaction of SH radicals with S atoms [J].
Francisco, Joseph S. .
JOURNAL OF CHEMICAL PHYSICS, 2007, 126 (21)
[30]  
Frisch M., 2016, Gaussian, V16