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« Previous AbstractInsights into secondary organic aerosol formation mechanisms from measured gas/particle partitioning of specific organic tracer compounds    Next AbstractIntermediate-volatility organic compounds: a large source of secondary organic aerosol »

Environ Sci Technol


Title:Hydrogen peroxide enhances the oxidation of oxygenated volatile organic compounds on mineral dust particles: a case study of methacrolein
Author(s):Zhao Y; Huang D; Huang L; Chen Z;
Address:"State Key Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University , Beijing 100871, People's Republic of China"
Journal Title:Environ Sci Technol
Year:2014
Volume:20140821
Issue:18
Page Number:10614 - 10623
DOI: 10.1021/es5023416
ISSN/ISBN:1520-5851 (Electronic) 0013-936X (Linking)
Abstract:"Heterogeneous oxidation of oxygenated volatile organic compounds (OVOCs) serves as an important sink of OVOCs as well as a source of secondary organic material. However, the roles of gas phase oxidants in these reactions are poorly understood. In this work, we present the first laboratory study of the heterogeneous reactions of methacrolein (MACR) on various mineral dust particles in the presence of gaseous H2O2. It is found that the presence of gaseous H2O2 significantly promotes both the uptake and oxidation of MACR on kaolinite, alpha-Al2O3, alpha-Fe2O3, and TiO2, but not on CaCO3. The oxidation of MACR produces organic acids as its major low-molecular-weight product, whose yields are enhanced by a factor of 2-6 in the presence of H2O2. In addition, organic peroxides such as methyl hydroperoxide, peroxyformic acid, and peroxyacetic acid are only formed in the presence of H2O2, and the formation of methyl hydroperoxide indicates that MACR oxidation on the surface involves reaction with OH radicals. A probe reaction using salicylic acid verifies the production of OH radicals from H2O2 decomposition on kaolinite, alpha-Al2O3, alpha-Fe2O3, and TiO2, which rationalizes the enhanced MACR oxidation observed on these particles. The uptake coefficients of MACR on kaolinite, alpha-Fe2O3, and TiO2 in the presence of H2O2 are on the order of 10(-5)-10(-4). Our results provide new insights into the formation and chemical evolution of organic species in the atmosphere"
Keywords:Acrolein/*analogs & derivatives/chemistry Air Pollutants/*chemistry Aluminum Oxide/chemistry Atmosphere/chemistry Dust/*analysis Ferric Compounds/chemistry Hydrogen Peroxide/*chemistry Kaolin/chemistry Oxidants/*chemistry Oxidation-Reduction Volatile Orga;
Notes:"MedlineZhao, Yue Huang, Dao Huang, Liubin Chen, Zhongming eng Research Support, Non-U.S. Gov't 2014/08/12 Environ Sci Technol. 2014 Sep 16; 48(18):10614-23. doi: 10.1021/es5023416. Epub 2014 Aug 21"

 
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