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« Previous AbstractSilencing a Simple Extracellular Leucine-Rich Repeat Gene OsI-BAK1 Enhances the Resistance of Rice to Brown Planthopper Nilaparvata lugens    Next AbstractUsing Ionic Liquids To Study the Migration of Semivolatile Organic Vapors in Smog Chamber Experiments »

J Phys Chem A


Title:Uptake of Semivolatile Secondary Organic Aerosol Formed from alpha-Pinene into Nonvolatile Polyethylene Glycol Probe Particles
Author(s):Ye P; Ding X; Ye Q; Robinson ES; Donahue NM;
Address:"Center for Atmospheric Particle Studies, Carnegie Mellon University , 5000 Forbes Avenue, Pittsburgh, Pennsylvania 15213, United States. State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry , Chinese Academy of Sciences , Guangzhou 510640, China"
Journal Title:J Phys Chem A
Year:2016
Volume:20160106
Issue:9
Page Number:1459 - 1467
DOI: 10.1021/acs.jpca.5b07435
ISSN/ISBN:1520-5215 (Electronic) 1089-5639 (Linking)
Abstract:"Semivolatile organic compounds (SVOCs) play an essential role in secondary organic aerosol (SOA) formation, chemical aging, and mixing of organic aerosol (OA) from different sources. Polyethylene glycol (PEG400) particles are liquid, polar, and nearly nonvolatile; they provide a new vehicle to study the interaction between SVOCs with OA. With a unique fragment ion C4H9O2(+) (m/z 89), PEG400 can be easily separated from alpha-pinene SOA in aerosol mass spectra. By injecting separately prepared PEG probe particles into a chamber containing SOA coated on ammonium sulfate seeds, we show that a substantial pool of SVOCs exists in equilibrium with the original SOA particles. Quantitative findings are based on bulk mass spectra, size-dependent composition, and the evolution of individual particle mass spectra, which we use to separate the two particle populations. We observed a larger fraction of SVOC vapors with increased amounts of reacted alpha-pinene. For the same amount of reacted alpha-pinene, the SOA formed from alpha-pinene oxidized by OH radicals had a higher fraction of SOA vapors than SOA formed by alpha-pinene ozonolysis. Compared to the PEG400 probe particles, we observed a lower mass fraction of SVOCs in poly(ethylene glycol) dimethyl ether (MePEG500) probe particles under otherwise identical conditions; this may be due to the lower polarity of the MePEG500 or caused by esterification reactions between the PEG400 and organic acids in the SOA"
Keywords:Aerosols/*chemistry Bicyclic Monoterpenes Molecular Probes/*chemistry Monoterpenes/*chemistry Organic Chemicals/*chemistry Polyethylene Glycols/*chemistry Volatilization;
Notes:"MedlineYe, Penglin Ding, Xiang Ye, Qing Robinson, Ellis S Donahue, Neil M eng Research Support, Non-U.S. Gov't Research Support, U.S. Gov't, Non-P.H.S. 2015/12/23 J Phys Chem A. 2016 Mar 10; 120(9):1459-67. doi: 10.1021/acs.jpca.5b07435. Epub 2016 Jan 6"

 
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