Dependence of particle nucleation and growth on high-molecular-weight gas-phase products during ozonolysis of α-pinene

We report the first time-dependent measurements of high-molecular-weight (up to 700 amu) gas-phase oxidation products from α-pinene ozonolysis in an aerosol chamber under dry and low-NO<sub>x</sub> conditions. Measurements of products having mole fractions ranging from 10<sup>&...

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Main Authors: J. Zhao, J. Ortega, M. Chen, P. H. McMurry, J. N. Smith
Format: Article
Language:English
Published: Copernicus Publications 2013-08-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/13/7631/2013/acp-13-7631-2013.pdf
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spelling doaj-bcc0983b04bc4f4db43c4b0c7a7b9a402020-11-25T01:15:43ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242013-08-0113157631764410.5194/acp-13-7631-2013Dependence of particle nucleation and growth on high-molecular-weight gas-phase products during ozonolysis of α-pineneJ. ZhaoJ. OrtegaM. ChenP. H. McMurryJ. N. SmithWe report the first time-dependent measurements of high-molecular-weight (up to 700 amu) gas-phase oxidation products from α-pinene ozonolysis in an aerosol chamber under dry and low-NO<sub>x</sub> conditions. Measurements of products having mole fractions ranging from 10<sup>&minus;14</sup> to 10<sup>&minus;11</sup> were carried out with a chemical ionization mass spectrometer (the Cluster CIMS). Most products that were correlated with number concentrations of the smallest particles measured (10–20 nm) had molecular weights in the 430–560 amu range. Those products are proposed to be likely responsible for the initial nuclei formation and the early growth of the freshly nucleated particles based on their high molecular weights and chemical identities, both of which suggest low-volatility compounds. Another group of oxidation products in the lower mass range of 140–380 amu was well correlated with particles larger than 20 nm. We postulate that those products contributed to the later growth of particles (i.e., larger than 20 nm in diameter). Although particle nucleation in this study was primarily due to condensation of oxidation products from α-pinene ozonolysis, the involvement of residual sulfuric acid vapor in particle nucleation cannot be totally excluded.http://www.atmos-chem-phys.net/13/7631/2013/acp-13-7631-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. Zhao
J. Ortega
M. Chen
P. H. McMurry
J. N. Smith
spellingShingle J. Zhao
J. Ortega
M. Chen
P. H. McMurry
J. N. Smith
Dependence of particle nucleation and growth on high-molecular-weight gas-phase products during ozonolysis of α-pinene
Atmospheric Chemistry and Physics
author_facet J. Zhao
J. Ortega
M. Chen
P. H. McMurry
J. N. Smith
author_sort J. Zhao
title Dependence of particle nucleation and growth on high-molecular-weight gas-phase products during ozonolysis of α-pinene
title_short Dependence of particle nucleation and growth on high-molecular-weight gas-phase products during ozonolysis of α-pinene
title_full Dependence of particle nucleation and growth on high-molecular-weight gas-phase products during ozonolysis of α-pinene
title_fullStr Dependence of particle nucleation and growth on high-molecular-weight gas-phase products during ozonolysis of α-pinene
title_full_unstemmed Dependence of particle nucleation and growth on high-molecular-weight gas-phase products during ozonolysis of α-pinene
title_sort dependence of particle nucleation and growth on high-molecular-weight gas-phase products during ozonolysis of α-pinene
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2013-08-01
description We report the first time-dependent measurements of high-molecular-weight (up to 700 amu) gas-phase oxidation products from α-pinene ozonolysis in an aerosol chamber under dry and low-NO<sub>x</sub> conditions. Measurements of products having mole fractions ranging from 10<sup>&minus;14</sup> to 10<sup>&minus;11</sup> were carried out with a chemical ionization mass spectrometer (the Cluster CIMS). Most products that were correlated with number concentrations of the smallest particles measured (10–20 nm) had molecular weights in the 430–560 amu range. Those products are proposed to be likely responsible for the initial nuclei formation and the early growth of the freshly nucleated particles based on their high molecular weights and chemical identities, both of which suggest low-volatility compounds. Another group of oxidation products in the lower mass range of 140–380 amu was well correlated with particles larger than 20 nm. We postulate that those products contributed to the later growth of particles (i.e., larger than 20 nm in diameter). Although particle nucleation in this study was primarily due to condensation of oxidation products from α-pinene ozonolysis, the involvement of residual sulfuric acid vapor in particle nucleation cannot be totally excluded.
url http://www.atmos-chem-phys.net/13/7631/2013/acp-13-7631-2013.pdf
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