Influence of seed aerosol surface area and oxidation rate on vapor wall deposition and SOA mass yields: a case study with <i>α</i>-pinene ozonolysis

Laboratory chambers, invaluable in atmospheric chemistry and aerosol formation studies, are subject to particle and vapor wall deposition, processes that need to be accounted for in order to accurately determine secondary organic aerosol (SOA) mass yields. Although particle wall deposition is re...

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Main Authors: T. Nah, R. C. McVay, X. Zhang, C. M. Boyd, J. H. Seinfeld, N. L. Ng
Format: Article
Language:English
Published: Copernicus Publications 2016-07-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/16/9361/2016/acp-16-9361-2016.pdf
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spelling doaj-7be1202e831647869431c2aba63d20bc2020-11-24T22:17:44ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242016-07-01169361937910.5194/acp-16-9361-2016Influence of seed aerosol surface area and oxidation rate on vapor wall deposition and SOA mass yields: a case study with <i>α</i>-pinene ozonolysisT. Nah0R. C. McVay1X. Zhang2X. Zhang3C. M. Boyd4J. H. Seinfeld5J. H. Seinfeld6N. L. Ng7N. L. Ng8School of Chemical and Biomolecular Engineering, Georgia Institute of Technology, Atlanta, GA, USADivision of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, USADivision of Engineering and Applied Science, California Institute of Technology, Pasadena, CA, USAnow at: Center for Aerosol and Cloud Chemistry, Aerodyne Research, Billerica, MA, USASchool of Chemical and Biomolecular Engineering, Georgia Institute of Technology, Atlanta, GA, USADivision of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, USADivision of Engineering and Applied Science, California Institute of Technology, Pasadena, CA, USASchool of Chemical and Biomolecular Engineering, Georgia Institute of Technology, Atlanta, GA, USASchool of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA, USALaboratory chambers, invaluable in atmospheric chemistry and aerosol formation studies, are subject to particle and vapor wall deposition, processes that need to be accounted for in order to accurately determine secondary organic aerosol (SOA) mass yields. Although particle wall deposition is reasonably well understood and usually accounted for, vapor wall deposition is less so. The effects of vapor wall deposition on SOA mass yields in chamber experiments can be constrained experimentally by increasing the seed aerosol surface area to promote the preferential condensation of SOA-forming vapors onto seed aerosol. Here, we study the influence of seed aerosol surface area and oxidation rate on SOA formation in <i>α</i>-pinene ozonolysis. The observations are analyzed using a coupled vapor–particle dynamics model to interpret the roles of gas–particle partitioning (quasi-equilibrium vs. kinetically limited SOA growth) and <i>α</i>-pinene oxidation rate in influencing vapor wall deposition. We find that the SOA growth rate and mass yields are independent of seed surface area within the range of seed surface area concentrations used in this study. This behavior arises when the condensation of SOA-forming vapors is dominated by quasi-equilibrium growth. Faster <i>α</i>-pinene oxidation rates and higher SOA mass yields are observed at increasing O<sub>3</sub> concentrations for the same initial <i>α</i>-pinene concentration. When the <i>α</i>-pinene oxidation rate increases relative to vapor wall deposition, rapidly produced SOA-forming oxidation products condense more readily onto seed aerosol particles, resulting in higher SOA mass yields. Our results indicate that the extent to which vapor wall deposition affects SOA mass yields depends on the particular volatility organic compound system and can be mitigated through the use of excess oxidant concentrations.https://www.atmos-chem-phys.net/16/9361/2016/acp-16-9361-2016.pdf
collection DOAJ
language English
format Article
sources DOAJ
author T. Nah
R. C. McVay
X. Zhang
X. Zhang
C. M. Boyd
J. H. Seinfeld
J. H. Seinfeld
N. L. Ng
N. L. Ng
spellingShingle T. Nah
R. C. McVay
X. Zhang
X. Zhang
C. M. Boyd
J. H. Seinfeld
J. H. Seinfeld
N. L. Ng
N. L. Ng
Influence of seed aerosol surface area and oxidation rate on vapor wall deposition and SOA mass yields: a case study with <i>α</i>-pinene ozonolysis
Atmospheric Chemistry and Physics
author_facet T. Nah
R. C. McVay
X. Zhang
X. Zhang
C. M. Boyd
J. H. Seinfeld
J. H. Seinfeld
N. L. Ng
N. L. Ng
author_sort T. Nah
title Influence of seed aerosol surface area and oxidation rate on vapor wall deposition and SOA mass yields: a case study with <i>α</i>-pinene ozonolysis
title_short Influence of seed aerosol surface area and oxidation rate on vapor wall deposition and SOA mass yields: a case study with <i>α</i>-pinene ozonolysis
title_full Influence of seed aerosol surface area and oxidation rate on vapor wall deposition and SOA mass yields: a case study with <i>α</i>-pinene ozonolysis
title_fullStr Influence of seed aerosol surface area and oxidation rate on vapor wall deposition and SOA mass yields: a case study with <i>α</i>-pinene ozonolysis
title_full_unstemmed Influence of seed aerosol surface area and oxidation rate on vapor wall deposition and SOA mass yields: a case study with <i>α</i>-pinene ozonolysis
title_sort influence of seed aerosol surface area and oxidation rate on vapor wall deposition and soa mass yields: a case study with <i>α</i>-pinene ozonolysis
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2016-07-01
description Laboratory chambers, invaluable in atmospheric chemistry and aerosol formation studies, are subject to particle and vapor wall deposition, processes that need to be accounted for in order to accurately determine secondary organic aerosol (SOA) mass yields. Although particle wall deposition is reasonably well understood and usually accounted for, vapor wall deposition is less so. The effects of vapor wall deposition on SOA mass yields in chamber experiments can be constrained experimentally by increasing the seed aerosol surface area to promote the preferential condensation of SOA-forming vapors onto seed aerosol. Here, we study the influence of seed aerosol surface area and oxidation rate on SOA formation in <i>α</i>-pinene ozonolysis. The observations are analyzed using a coupled vapor–particle dynamics model to interpret the roles of gas–particle partitioning (quasi-equilibrium vs. kinetically limited SOA growth) and <i>α</i>-pinene oxidation rate in influencing vapor wall deposition. We find that the SOA growth rate and mass yields are independent of seed surface area within the range of seed surface area concentrations used in this study. This behavior arises when the condensation of SOA-forming vapors is dominated by quasi-equilibrium growth. Faster <i>α</i>-pinene oxidation rates and higher SOA mass yields are observed at increasing O<sub>3</sub> concentrations for the same initial <i>α</i>-pinene concentration. When the <i>α</i>-pinene oxidation rate increases relative to vapor wall deposition, rapidly produced SOA-forming oxidation products condense more readily onto seed aerosol particles, resulting in higher SOA mass yields. Our results indicate that the extent to which vapor wall deposition affects SOA mass yields depends on the particular volatility organic compound system and can be mitigated through the use of excess oxidant concentrations.
url https://www.atmos-chem-phys.net/16/9361/2016/acp-16-9361-2016.pdf
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