The chemical composition of secondary organic aerosol (SOA) generated from the ozonolysis of isoprene (C5H8) in the presence of an OH scavenger was examined using high-resolution electrospray ionization mass spectrometry (ESI-MS) in the mass range m/z = 50-1000. The chemical composition of SOA is complex, with more than 1000 assigned peaks observed in the positive and negative ion mode spectra. Only a small fraction of peaks correspond to known products of isoprene oxidation, such as pyruvic acid, glycolic acid, methylglyoxal, etc. The absolute majority of the detected peaks correspond to highly oxidized oligomeric constituents of SOA, with an average OX molar ratio of 0.6. The corresponding organic mass (OM) to organic oxygen (00) ratio is 2.4. Approximately 8% of oxygen atoms in SOA are in the form of peroxides, as quantified with an iodide test. Double bond equivalency (DBE) factors, representing the sum of all double bonds and rings, increase by 1 for every 1-2 additional carbon atoms in the molecule. The number of unoxidized C=C double bonds is estimated to be less than 10%; the remaining DBE is due to C=O carbonyl groups. Kendrick analysis suggests that the prevalent oligomer building blocks are small carbonyls with a C-1-C-2 skeleton. Formaldehyde (CH2O) is identified as the most common repetitive building block in the observed oligomeric compounds. (C) 2009 Elsevier Ltd. All rights reserved.
%0 Journal Article
%1 Nguyen:2010p4080
%A Nguyen, Tran B
%A Bateman, Adam P
%A Bones, David L
%A Nizkorodov, Sergey A
%A Laskin, Julia
%A Laskin, Alexander
%D 2010
%J Atmospheric Environment
%K Accretion Aerosol, Alkene Alpha-Pinene, Biogenic Carbon, Carbonyls, Characterization, Chemical-Composition, Formation, Gas-Particle Gas-Phase Matter, Molecular Oh Oligomer Oligomers Organic Oxidation-Products, Ozonolysis, Particulate Partitioning, Peroxides, Radicals, Reactions, Soa,
%N 8
%P 1032--1042
%R 10.1016/j.atmosenv.2009.12.019
%T High-resolution mass spectrometry analysis of secondary organic aerosol generated by ozonolysis of isoprene
%U http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6VH3-4Y1NV8W-3&_user=655127&_coverDate=03%252F31%252F2010&_rdoc=1&_fmt=high&_orig=search&_sort=d&_docanchor=&view=c&_acct=C000033918&_version=1&_urlVersion=0&_userid=655127&md5=1d5fc24d558ca3e90d850f2d0a8583ac
%V 44
%X The chemical composition of secondary organic aerosol (SOA) generated from the ozonolysis of isoprene (C5H8) in the presence of an OH scavenger was examined using high-resolution electrospray ionization mass spectrometry (ESI-MS) in the mass range m/z = 50-1000. The chemical composition of SOA is complex, with more than 1000 assigned peaks observed in the positive and negative ion mode spectra. Only a small fraction of peaks correspond to known products of isoprene oxidation, such as pyruvic acid, glycolic acid, methylglyoxal, etc. The absolute majority of the detected peaks correspond to highly oxidized oligomeric constituents of SOA, with an average OX molar ratio of 0.6. The corresponding organic mass (OM) to organic oxygen (00) ratio is 2.4. Approximately 8% of oxygen atoms in SOA are in the form of peroxides, as quantified with an iodide test. Double bond equivalency (DBE) factors, representing the sum of all double bonds and rings, increase by 1 for every 1-2 additional carbon atoms in the molecule. The number of unoxidized C=C double bonds is estimated to be less than 10%; the remaining DBE is due to C=O carbonyl groups. Kendrick analysis suggests that the prevalent oligomer building blocks are small carbonyls with a C-1-C-2 skeleton. Formaldehyde (CH2O) is identified as the most common repetitive building block in the observed oligomeric compounds. (C) 2009 Elsevier Ltd. All rights reserved.
@article{Nguyen:2010p4080,
abstract = {The chemical composition of secondary organic aerosol (SOA) generated from the ozonolysis of isoprene (C5H8) in the presence of an OH scavenger was examined using high-resolution electrospray ionization mass spectrometry (ESI-MS) in the mass range m/z = 50-1000. The chemical composition of SOA is complex, with more than 1000 assigned peaks observed in the positive and negative ion mode spectra. Only a small fraction of peaks correspond to known products of isoprene oxidation, such as pyruvic acid, glycolic acid, methylglyoxal, etc. The absolute majority of the detected peaks correspond to highly oxidized oligomeric constituents of SOA, with an average OX molar ratio of 0.6. The corresponding organic mass (OM) to organic oxygen (00) ratio is 2.4. Approximately 8% of oxygen atoms in SOA are in the form of peroxides, as quantified with an iodide test. Double bond equivalency (DBE) factors, representing the sum of all double bonds and rings, increase by 1 for every 1-2 additional carbon atoms in the molecule. The number of unoxidized C=C double bonds is estimated to be less than 10%; the remaining DBE is due to C=O carbonyl groups. Kendrick analysis suggests that the prevalent oligomer building blocks are small carbonyls with a C-1-C-2 skeleton. Formaldehyde (CH2O) is identified as the most common repetitive building block in the observed oligomeric compounds. (C) 2009 Elsevier Ltd. All rights reserved.},
added-at = {2010-06-22T19:38:37.000+0200},
affiliation = {Univ Calif Irvine, Dept Chem, Irvine, CA 92697 USA},
author = {Nguyen, Tran B and Bateman, Adam P and Bones, David L and Nizkorodov, Sergey A and Laskin, Julia and Laskin, Alexander},
biburl = {https://www.bibsonomy.org/bibtex/234abbe136d607b6ee72f098d57dd611a/gsmith},
date-added = {2010-06-10 10:23:29 -0400},
date-modified = {2010-06-10 10:23:29 -0400},
doi = {10.1016/j.atmosenv.2009.12.019},
interhash = {52be58056cb683b382a077735c65c92d},
intrahash = {34abbe136d607b6ee72f098d57dd611a},
journal = {Atmospheric Environment},
keywords = {Accretion Aerosol, Alkene Alpha-Pinene, Biogenic Carbon, Carbonyls, Characterization, Chemical-Composition, Formation, Gas-Particle Gas-Phase Matter, Molecular Oh Oligomer Oligomers Organic Oxidation-Products, Ozonolysis, Particulate Partitioning, Peroxides, Radicals, Reactions, Soa,},
language = {English},
local-url = {file://localhost/Users/geoffreysmith/Documents/Papers/Atmospheric%20Environment/2010/Atmospheric%20Environment,%2044,%201032-1042%202010.pdf},
month = Jan,
number = 8,
pages = {1032--1042},
pmid = {000275512500004},
rating = {0},
timestamp = {2010-06-22T19:38:54.000+0200},
title = {High-resolution mass spectrometry analysis of secondary organic aerosol generated by ozonolysis of isoprene},
uri = {papers://E88B624E-D406-46FF-9D95-BB9C1AAE3FDC/Paper/p4080},
url = {http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6VH3-4Y1NV8W-3&_user=655127&_coverDate=03%252F31%252F2010&_rdoc=1&_fmt=high&_orig=search&_sort=d&_docanchor=&view=c&_acct=C000033918&_version=1&_urlVersion=0&_userid=655127&md5=1d5fc24d558ca3e90d850f2d0a8583ac},
volume = 44,
year = 2010
}