Formation and aging of secondary organic aerosol from toluene: changes in chemical composition, volatility, and hygroscopicity

Secondary organic aerosol (SOA) is transformed after its initial formation, but this chemical aging of SOA is poorly understood. Experiments were conducted in the Carnegie Mellon environmental chamber to form secondary organic aerosol (SOA) from the photo-oxidation of toluene and other small aromati...

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Main Authors: L. Hildebrandt Ruiz, A. L. Paciga, K. M. Cerully, A. Nenes, N. M. Donahue, S. N. Pandis
Format: Article
Language:English
Published: Copernicus Publications 2015-07-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/15/8301/2015/acp-15-8301-2015.pdf
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spelling doaj-49f6294c6c7a4fb59532ecf642e130eb2020-11-24T22:10:34ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242015-07-0115148301831310.5194/acp-15-8301-2015Formation and aging of secondary organic aerosol from toluene: changes in chemical composition, volatility, and hygroscopicityL. Hildebrandt Ruiz0A. L. Paciga1K. M. Cerully2A. Nenes3N. M. Donahue4S. N. Pandis5The University of Texas at Austin, Austin, Texas, USACarnegie Mellon University, Pittsburgh, Pennsylvania, USAGeorgia Institute of Technology, Atlanta, Georgia, USAGeorgia Institute of Technology, Atlanta, Georgia, USACarnegie Mellon University, Pittsburgh, Pennsylvania, USACarnegie Mellon University, Pittsburgh, Pennsylvania, USASecondary organic aerosol (SOA) is transformed after its initial formation, but this chemical aging of SOA is poorly understood. Experiments were conducted in the Carnegie Mellon environmental chamber to form secondary organic aerosol (SOA) from the photo-oxidation of toluene and other small aromatic volatile organic compounds (VOCs) in the presence of NO<sub><i>x</i></sub> under different oxidizing conditions. The effects of the oxidizing condition on organic aerosol (OA) composition, mass yield, volatility, and hygroscopicity were explored. Higher exposure to the hydroxyl radical resulted in different OA composition, average carbon oxidation state (OS<sub>c</sub>), and mass yield. The OA oxidation state generally increased during photo-oxidation, and the final OA OS<sub>c</sub> ranged from −0.29 to 0.16 in the performed experiments. The volatility of OA formed in these different experiments varied by as much as a factor of 30, demonstrating that the OA formed under different oxidizing conditions can have a significantly different saturation concentration. There was no clear correlation between hygroscopicity and oxidation state for this relatively hygroscopic SOA.http://www.atmos-chem-phys.net/15/8301/2015/acp-15-8301-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author L. Hildebrandt Ruiz
A. L. Paciga
K. M. Cerully
A. Nenes
N. M. Donahue
S. N. Pandis
spellingShingle L. Hildebrandt Ruiz
A. L. Paciga
K. M. Cerully
A. Nenes
N. M. Donahue
S. N. Pandis
Formation and aging of secondary organic aerosol from toluene: changes in chemical composition, volatility, and hygroscopicity
Atmospheric Chemistry and Physics
author_facet L. Hildebrandt Ruiz
A. L. Paciga
K. M. Cerully
A. Nenes
N. M. Donahue
S. N. Pandis
author_sort L. Hildebrandt Ruiz
title Formation and aging of secondary organic aerosol from toluene: changes in chemical composition, volatility, and hygroscopicity
title_short Formation and aging of secondary organic aerosol from toluene: changes in chemical composition, volatility, and hygroscopicity
title_full Formation and aging of secondary organic aerosol from toluene: changes in chemical composition, volatility, and hygroscopicity
title_fullStr Formation and aging of secondary organic aerosol from toluene: changes in chemical composition, volatility, and hygroscopicity
title_full_unstemmed Formation and aging of secondary organic aerosol from toluene: changes in chemical composition, volatility, and hygroscopicity
title_sort formation and aging of secondary organic aerosol from toluene: changes in chemical composition, volatility, and hygroscopicity
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2015-07-01
description Secondary organic aerosol (SOA) is transformed after its initial formation, but this chemical aging of SOA is poorly understood. Experiments were conducted in the Carnegie Mellon environmental chamber to form secondary organic aerosol (SOA) from the photo-oxidation of toluene and other small aromatic volatile organic compounds (VOCs) in the presence of NO<sub><i>x</i></sub> under different oxidizing conditions. The effects of the oxidizing condition on organic aerosol (OA) composition, mass yield, volatility, and hygroscopicity were explored. Higher exposure to the hydroxyl radical resulted in different OA composition, average carbon oxidation state (OS<sub>c</sub>), and mass yield. The OA oxidation state generally increased during photo-oxidation, and the final OA OS<sub>c</sub> ranged from −0.29 to 0.16 in the performed experiments. The volatility of OA formed in these different experiments varied by as much as a factor of 30, demonstrating that the OA formed under different oxidizing conditions can have a significantly different saturation concentration. There was no clear correlation between hygroscopicity and oxidation state for this relatively hygroscopic SOA.
url http://www.atmos-chem-phys.net/15/8301/2015/acp-15-8301-2015.pdf
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