2020
DOI: 10.1021/acs.jpca.0c02867
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Unraveling Conformer-Specific Sources of Hydroxyl Radical Production from an Isoprene-Derived Criegee Intermediate by Deuteration

Abstract: Ozonolysis of isoprene, the most abundant volatile organic compounds emitted into the Earth's troposphere after methane, yields three distinct Criegee intermediates. Among these, methyl vinyl ketone oxide (MVK-oxide) is predicted to be the major source of atmospheric hydroxyl radicals (OH) from isoprene ozonolysis. Previously, Barber et al. [J. Am. Chem. Soc., 2018, 140, pp 10866−10880] demonstrated that syn-MVK-oxide conformers undergo unimolecular decay via 1,4-hydrogen (H) transfer from the methyl group t… Show more

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Cited by 10 publications
(9 citation statements)
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“…Criegee intermediates 1 (carbonyl oxides) are formed in the ozonolysis of unsaturated compounds in the atmosphere, [2][3][4][5][6][7][8][9][10][11] and they are very important in the atmosphere because they contribute to the formation of OH radicals [12][13][14][15][16][17][18][19][20][21][22][23][24][25][26][27] and secondary organic aerosols. [28][29][30][31][32][33][34][35][36][37] Criegee intermediates act as oxidants, and their kinetics provide key parameters [38][39][40][41][42] for estimating the oxidative capacity of the atmosphere.…”
Section: Introductionmentioning
confidence: 99%
“…Criegee intermediates 1 (carbonyl oxides) are formed in the ozonolysis of unsaturated compounds in the atmosphere, [2][3][4][5][6][7][8][9][10][11] and they are very important in the atmosphere because they contribute to the formation of OH radicals [12][13][14][15][16][17][18][19][20][21][22][23][24][25][26][27] and secondary organic aerosols. [28][29][30][31][32][33][34][35][36][37] Criegee intermediates act as oxidants, and their kinetics provide key parameters [38][39][40][41][42] for estimating the oxidative capacity of the atmosphere.…”
Section: Introductionmentioning
confidence: 99%
“…Criegee intermediates (CIs) are carbonyl oxides that play vital roles in the Earth’s troposphere, where they are formed via a [3 + 2]-cycloaddition reaction involving volatile alkenes and ozone. CIs are implicated in enhancing the oxidizing capacity of the troposphere and in the formation of less volatile species that may condense to form secondary organic aerosols (SOAs). …”
Section: Introductionmentioning
confidence: 99%
“…Because of the different relative orientations of the CQO and CQC bonds (anti/syn), MVK-OO and MACR-OO have four different configurations and the syn (CO) configuration has a much larger proportion. [21][22][23] In previous work, Lester has proposed the thermal unimolecular decay paths for the MVK-OO and MACR-OO with a combination of experiments and theoretical calculations. It was found that, for MVK-OO, the anti (CO) configurations prefer to have an H-transfer from methyl to the terminal oxygen, while the syn (CO) configuration is more likely to have a three-membered ring-closure; there exists another different rule for MACR-OO, where the syn (CO) -syn (CC) configuration (SS configuration) is predicted to form the 5-membered ring of dioxole.…”
Section: Introductionmentioning
confidence: 99%