参考文献:
[1] Criegee R and Wenner G. Die Ozonisierung des 9,10-Oktalins. Justus Liebigs Ann. Chem., 1949, 564, 9–15.
[2] Criegee R. Mecranism of Ozondysis. Angew. Chem. Int. Ed. Engl., 1975, 14: 745–752.
[3] Welz O, Savee J D, Osborn D L, et al. Direct kinetic measurements of Criegee Intermediate (CH2OO) formed by reaction of CH2I with O2. Science, 2012, 335: 204–207.
[4] Anglada J M, Aplincourt P, Bofill J M, et al. Formation of OH radicals and H2O2 from alkene ozonolysis under humid conditions. Chem. Phys. Chem., 2002, 3: 215–221.
[5] Harrison R M, Yin J, Tilling R M, et al. Sci. Measurement and modelling of air pollution and atmospheric chemistry in the U.K. West Midlands conurbation: Overview of the PUMA Consortium project. Total Environ., 2006, 360, 5–25.
[6] Gutbrod R, Schindler R N, Kraka E, et al. Formation of OH radicals in the gas phase ozonolysis of alkenes, the unexpected role of carbonyl oxides.Chemical Physics Letters,1996, 252: 221–229.
[7] Taatjes C A, Shallcross D E, Percival C J. Research frontiers in the chemistry of Criegee intermediates and tropospheric ozonolysis. Phys. Chem. Chem. Phys.,2014, 16: 1704–18.
[8] Ryzhkov A B, Ariya P A. Reactions of substituted Criegee biradical with water dimer. Phys. Chem. Chem. Phys., 2004, 6: 5042–5050.
[9] Anglada J M, Gonzalez J, Torrent-Sucarrat M. A theoretical study on the reaction of substituted carbonyl oxides with water. Phys. Chem. Chem. Phys., 2011, 13: 13034–13045.
[10] Vereecken L and Francisco J S. Theoretical studies of atmospheric reaction mechanisms in the troposphere. Chem. Soc. Rev., 2012, 41, 6259–6293.
[11] Aplincourt P and Anglada J M. Theoretical studies of the isoprene ozonolysis under tropospheric conditions. 2. Unimolecular and water-assisted decompos- ition of the α-hydroxy hydroperoxides. J. Phys. Chem. A, 2003, 107: 5812–5820.
[12] Bonn B, Schuster G, Moortgat G K. Influence of water vapor on the process of new particle formation during monoterpene ozonolysis. J. Phys. Chem. A, 2002, 106: 2869–2881.
[13] Bonn B, Schuster G, Moortgat G K. Sesquiterpene ozonolysis: Origin of atmospheric new particle formation from biogenic hydrocarbons. Geophys. Res. Lett., 2003, 30: 1585.
[14] Atkinson R and Arey J. Atmospheric degradation of volatile organic compounds. Chem. Rev., 2003, 103: 4605–4638.
[15] Li J Y, Ying Q, Yi B Q,et al. Role of stabilized Criegee intermediates in the formation of atmospheric sulfate in eastern United States. Atmos. Environ., 2013, 79: 442–447.
[16] Carlsson P T, Keunecke C, Krüger B C, et al. Sulfur dioxide oxidation induced mechanistic branching and particle formation during the ozonolysis of β-pinene and 2-butene. Phys. Chem. Chem. Phys., 2012, 14: 15637–15640.
[17] Cox R A and Penkett S A. Oxidation of Atmospheric SO2 by Products of the Ozone–Olefin Reaction. Nature, 1971, 230: 321–322.
[18] Cox R A and Penkett S A. Aerosol formation from sulphur dioxide in the presence of ozone and olefinic hydrocarbons. J. Chem. Soc., Faraday Trans. 1, 1972, 68: 1735–1753.
[19] Calvert J G and Stockwell W R. Acid generation in the troposphere by gas-phase chemistry. Environ. Sci. Technol., 1983, 17, 428–443.
[20] Ouyang B, McLeod M W, Jones R L, et al. NO3 radical production from the reaction between the Criegee intermediate CH2OO and NO2. Phys. Chem. Chem. Phys., 2013, 15, 17070–17075.
[21] Taatjes C A, Welz O, Eskola A J, et al. Direct Measurements of Conformer-Dependent Reactivity of the Criegee Intermediate CH3CHOO. Science, 2013, 340: 177–180.
[22] Su Y T, Huang Y H, Witek, et al. Infrared Absorption Spectrum of the simplest Criegee intermediate CH2OO. Science, 2013, 340: 174–176.
[23] Sakamoto Y, Inomata S, Hirokawa J. Oligomerization reaction of the Criegee intermediate leads to secondary organic aerosol formation in ethylene ozonolysis. J. Phys. Chem. A, 2013, 117, 12912?12921
[24] Vereecken L, Harder H, Novelli A. The reaction of Criegee intermediates with NO, RO2, and SO2, and their fate in the atmosphere. Phys. Chem. Chem. Phys., 2012, 14: 14682?14695.
[25] Kuwata K T, Valin L C, Converse, A D. Quantum chemical and master equation studies of the methyl vinyl carbonyl oxides formed in isoprene ozonolysis. J. Phys. Chem. A, 2005, 109: 10710?10725.
[26] Long B, Tan X F, Long Z W, et al. Theoretical studies on reactions of the stabilized H2COO with HO2 and the HO2...H2O complex. J. Phys. Chem. A, 2011, 115: 6559?6567.
[27] Boyd A A, Canosa-Mas C E, King A D, et al. Use of a Stopped-flow Technique to measure the Rate Constants at Room Temperature for Reactions between the Nitrate Radical and Various Organic Species. J. Chem. Soc., Faraday Trans., 1991, 87, 2913–2919.
[28] Winterhalter R, Neeb P, Grossmann Dirk, et al. Products and Mechanism of the Gas Phase Reaction of Ozone with β-Pinene. J. Atmos. Chem., 2000, 35: 165-197.
[29] Ahrens J, Carlsson P T, Hertl N, et al. Infrared Detection of Criegee Intermediates Formed during the Ozonolysis of β-Pinene and Their Reactivity towards Sulfur Dioxide. Angew. Chem. Int. Ed. Engl., 2014, 53: 715-719. |