Molecular composition of fresh and aged secondary organic aerosol from a mixture of biogenic volatile compounds: a high-resolution mass spectrometry study

Field observations over the past decade indicate that a significant fraction of organic aerosol in remote areas may contain highly oxidized molecules. Aerosol processing or further oxidation (aging) of organic aerosol has been suggested to be responsible for their formation through heterogeneous rea...

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Main Authors: I. Kourtchev, J.-F. Doussin, C. Giorio, B. Mahon, E. M. Wilson, N. Maurin, E. Pangui, D. S. Venables, J. C. Wenger, M. Kalberer
Format: Article
Language:English
Published: Copernicus Publications 2015-05-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/15/5683/2015/acp-15-5683-2015.pdf
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author I. Kourtchev
J.-F. Doussin
C. Giorio
B. Mahon
E. M. Wilson
N. Maurin
E. Pangui
D. S. Venables
J. C. Wenger
M. Kalberer
author_facet I. Kourtchev
J.-F. Doussin
C. Giorio
B. Mahon
E. M. Wilson
N. Maurin
E. Pangui
D. S. Venables
J. C. Wenger
M. Kalberer
author_sort I. Kourtchev
collection DOAJ
description Field observations over the past decade indicate that a significant fraction of organic aerosol in remote areas may contain highly oxidized molecules. Aerosol processing or further oxidation (aging) of organic aerosol has been suggested to be responsible for their formation through heterogeneous reaction with oxidants and multigenerational oxidation of vapours by OH radicals. In this study we investigated the influence of several aging processes on the molecular composition of secondary organic aerosols (SOA) using direct infusion and liquid chromatography high-resolution mass spectrometry. SOA was formed in simulation chamber experiments from ozonolysis of a mixture of four biogenic volatile organic compounds (BVOC): α-pinene, β-pinene, &Delta;<sub>3</sub>-carene and isoprene. The SOA was subsequently aged under three different sets of conditions: in the dark in the presence of residual ozone, with UV irradiation and OH radicals, and using UV light only. Among all studied conditions, only OH radical-initiated aging was found to influence the molecular composition of the aerosol and showed an increase in carbon oxidation state (OS<sub>C</sub>) and elemental O / C ratios of the SOA components. None of the aging processes produced an observable effect on the oligomers formed from ozonolysis of the BVOC mixture, which were found to be equally abundant in both "fresh" and "aged" SOA. Additional experiments using α-pinene as the sole precursor demonstrated that oligomers are an important group of compounds in SOA produced from both ozonolysis and OH radical-initiated oxidation processes; however, a completely different set of oligomers is formed under these two oxidation regimes. SOA from the OH-initiated oxidation of α-pinene had a significantly higher overall OS<sub>C</sub> and O / C compared to that from pure ozonolysis experiments confirming that the OH radical reaction is more likely to be responsible for the occurrence of highly oxidized species in ambient biogenic SOA.
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spelling doaj.art-5dca5a8298db4eddba40d5fb798f06162022-12-21T18:53:25ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242015-05-0115105683569510.5194/acp-15-5683-2015Molecular composition of fresh and aged secondary organic aerosol from a mixture of biogenic volatile compounds: a high-resolution mass spectrometry studyI. Kourtchev0J.-F. Doussin1C. Giorio2B. Mahon3E. M. Wilson4N. Maurin5E. Pangui6D. S. Venables7J. C. Wenger8M. Kalberer9Department of Chemistry, University of Cambridge, Cambridge, CB2 1EW, United KingdomLISA, Universités Paris-Est-Créteil et Paris Diderot, CNRS UMR 7583, 61 Avenue du Général de Gaulle, 94010, Créteil, FranceDepartment of Chemistry, University of Cambridge, Cambridge, CB2 1EW, United KingdomDepartment of Chemistry, University of Cambridge, Cambridge, CB2 1EW, United KingdomDepartment of Chemistry and Environmental Research Institute, University College Cork, Cork, IrelandLISA, Universités Paris-Est-Créteil et Paris Diderot, CNRS UMR 7583, 61 Avenue du Général de Gaulle, 94010, Créteil, FranceLISA, Universités Paris-Est-Créteil et Paris Diderot, CNRS UMR 7583, 61 Avenue du Général de Gaulle, 94010, Créteil, FranceDepartment of Chemistry and Environmental Research Institute, University College Cork, Cork, IrelandDepartment of Chemistry and Environmental Research Institute, University College Cork, Cork, IrelandDepartment of Chemistry, University of Cambridge, Cambridge, CB2 1EW, United KingdomField observations over the past decade indicate that a significant fraction of organic aerosol in remote areas may contain highly oxidized molecules. Aerosol processing or further oxidation (aging) of organic aerosol has been suggested to be responsible for their formation through heterogeneous reaction with oxidants and multigenerational oxidation of vapours by OH radicals. In this study we investigated the influence of several aging processes on the molecular composition of secondary organic aerosols (SOA) using direct infusion and liquid chromatography high-resolution mass spectrometry. SOA was formed in simulation chamber experiments from ozonolysis of a mixture of four biogenic volatile organic compounds (BVOC): α-pinene, β-pinene, &Delta;<sub>3</sub>-carene and isoprene. The SOA was subsequently aged under three different sets of conditions: in the dark in the presence of residual ozone, with UV irradiation and OH radicals, and using UV light only. Among all studied conditions, only OH radical-initiated aging was found to influence the molecular composition of the aerosol and showed an increase in carbon oxidation state (OS<sub>C</sub>) and elemental O / C ratios of the SOA components. None of the aging processes produced an observable effect on the oligomers formed from ozonolysis of the BVOC mixture, which were found to be equally abundant in both "fresh" and "aged" SOA. Additional experiments using α-pinene as the sole precursor demonstrated that oligomers are an important group of compounds in SOA produced from both ozonolysis and OH radical-initiated oxidation processes; however, a completely different set of oligomers is formed under these two oxidation regimes. SOA from the OH-initiated oxidation of α-pinene had a significantly higher overall OS<sub>C</sub> and O / C compared to that from pure ozonolysis experiments confirming that the OH radical reaction is more likely to be responsible for the occurrence of highly oxidized species in ambient biogenic SOA.http://www.atmos-chem-phys.net/15/5683/2015/acp-15-5683-2015.pdf
spellingShingle I. Kourtchev
J.-F. Doussin
C. Giorio
B. Mahon
E. M. Wilson
N. Maurin
E. Pangui
D. S. Venables
J. C. Wenger
M. Kalberer
Molecular composition of fresh and aged secondary organic aerosol from a mixture of biogenic volatile compounds: a high-resolution mass spectrometry study
Atmospheric Chemistry and Physics
title Molecular composition of fresh and aged secondary organic aerosol from a mixture of biogenic volatile compounds: a high-resolution mass spectrometry study
title_full Molecular composition of fresh and aged secondary organic aerosol from a mixture of biogenic volatile compounds: a high-resolution mass spectrometry study
title_fullStr Molecular composition of fresh and aged secondary organic aerosol from a mixture of biogenic volatile compounds: a high-resolution mass spectrometry study
title_full_unstemmed Molecular composition of fresh and aged secondary organic aerosol from a mixture of biogenic volatile compounds: a high-resolution mass spectrometry study
title_short Molecular composition of fresh and aged secondary organic aerosol from a mixture of biogenic volatile compounds: a high-resolution mass spectrometry study
title_sort molecular composition of fresh and aged secondary organic aerosol from a mixture of biogenic volatile compounds a high resolution mass spectrometry study
url http://www.atmos-chem-phys.net/15/5683/2015/acp-15-5683-2015.pdf
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