Phase, composition, and growth mechanism for secondary organic aerosol from the ozonolysis of <i>α</i>-cedrene

Sesquiterpenes are an important class of biogenic volatile organic compounds (BVOCs) and have a high secondary organic aerosol (SOA) forming potential. However, SOA formation from sesquiterpene oxidation has received less attention compared to other BVOCs such as monoterpenes, and the underlying...

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Main Authors: Y. Zhao, L. M. Wingen, V. Perraud, B. J. Finlayson-Pitts
Format: Article
Language:English
Published: Copernicus Publications 2016-03-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/16/3245/2016/acp-16-3245-2016.pdf
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spelling doaj-9ddab588d2524a25a55634107810106b2020-11-24T22:26:00ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242016-03-01163245326410.5194/acp-16-3245-2016Phase, composition, and growth mechanism for secondary organic aerosol from the ozonolysis of <i>α</i>-cedreneY. Zhao0L. M. Wingen1V. Perraud2B. J. Finlayson-Pitts3Department of Chemistry, University of California, Irvine, CA 92697, USADepartment of Chemistry, University of California, Irvine, CA 92697, USADepartment of Chemistry, University of California, Irvine, CA 92697, USADepartment of Chemistry, University of California, Irvine, CA 92697, USASesquiterpenes are an important class of biogenic volatile organic compounds (BVOCs) and have a high secondary organic aerosol (SOA) forming potential. However, SOA formation from sesquiterpene oxidation has received less attention compared to other BVOCs such as monoterpenes, and the underlying mechanisms remain poorly understood. In this work, we present a comprehensive experimental investigation of the ozonolysis of <i>α</i>-cedrene both in a glass flow reactor (27–44 s reaction times) and in static Teflon chambers (30–60 min reaction times). The SOA was collected by impaction or filters, followed by analysis using attenuated total reflectance Fourier transform infrared (ATR-FTIR) spectroscopy and electrospray ionization mass spectrometry (ESI-MS), or measured online using direct analysis in real-time mass spectrometry (DART-MS) and aerosol mass spectrometry (AMS). The slow evaporation of 2-ethylhexyl nitrate that was incorporated into the SOA during its formation and growth gives an estimated diffusion coefficient of 3  ×  10<sup>−15</sup> cm<sup>2</sup> s<sup>−1</sup> and shows that SOA is a highly viscous semisolid. Possible structures of four newly observed low molecular weight (MW  ≤  300 Da) reaction products with higher oxygen content than those previously reported were identified. High molecular weight (HMW) products formed in the early stages of the oxidation have structures consistent with aldol condensation products, peroxyhemiacetals, and esters. The size-dependent distributions of HMW products in the SOA, as well as the effects of stabilized Criegee intermediate (SCI) scavengers on HMW products and particle formation, confirm that HMW products and reactions of SCI play a crucial role in early stages of particle formation. Our studies provide new insights into mechanisms of SOA formation and growth in <i>α</i>-cedrene ozonolysis and the important role of sesquiterpenes in new particle formation as suggested by field measurements.https://www.atmos-chem-phys.net/16/3245/2016/acp-16-3245-2016.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Y. Zhao
L. M. Wingen
V. Perraud
B. J. Finlayson-Pitts
spellingShingle Y. Zhao
L. M. Wingen
V. Perraud
B. J. Finlayson-Pitts
Phase, composition, and growth mechanism for secondary organic aerosol from the ozonolysis of <i>α</i>-cedrene
Atmospheric Chemistry and Physics
author_facet Y. Zhao
L. M. Wingen
V. Perraud
B. J. Finlayson-Pitts
author_sort Y. Zhao
title Phase, composition, and growth mechanism for secondary organic aerosol from the ozonolysis of <i>α</i>-cedrene
title_short Phase, composition, and growth mechanism for secondary organic aerosol from the ozonolysis of <i>α</i>-cedrene
title_full Phase, composition, and growth mechanism for secondary organic aerosol from the ozonolysis of <i>α</i>-cedrene
title_fullStr Phase, composition, and growth mechanism for secondary organic aerosol from the ozonolysis of <i>α</i>-cedrene
title_full_unstemmed Phase, composition, and growth mechanism for secondary organic aerosol from the ozonolysis of <i>α</i>-cedrene
title_sort phase, composition, and growth mechanism for secondary organic aerosol from the ozonolysis of <i>α</i>-cedrene
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2016-03-01
description Sesquiterpenes are an important class of biogenic volatile organic compounds (BVOCs) and have a high secondary organic aerosol (SOA) forming potential. However, SOA formation from sesquiterpene oxidation has received less attention compared to other BVOCs such as monoterpenes, and the underlying mechanisms remain poorly understood. In this work, we present a comprehensive experimental investigation of the ozonolysis of <i>α</i>-cedrene both in a glass flow reactor (27–44 s reaction times) and in static Teflon chambers (30–60 min reaction times). The SOA was collected by impaction or filters, followed by analysis using attenuated total reflectance Fourier transform infrared (ATR-FTIR) spectroscopy and electrospray ionization mass spectrometry (ESI-MS), or measured online using direct analysis in real-time mass spectrometry (DART-MS) and aerosol mass spectrometry (AMS). The slow evaporation of 2-ethylhexyl nitrate that was incorporated into the SOA during its formation and growth gives an estimated diffusion coefficient of 3  ×  10<sup>−15</sup> cm<sup>2</sup> s<sup>−1</sup> and shows that SOA is a highly viscous semisolid. Possible structures of four newly observed low molecular weight (MW  ≤  300 Da) reaction products with higher oxygen content than those previously reported were identified. High molecular weight (HMW) products formed in the early stages of the oxidation have structures consistent with aldol condensation products, peroxyhemiacetals, and esters. The size-dependent distributions of HMW products in the SOA, as well as the effects of stabilized Criegee intermediate (SCI) scavengers on HMW products and particle formation, confirm that HMW products and reactions of SCI play a crucial role in early stages of particle formation. Our studies provide new insights into mechanisms of SOA formation and growth in <i>α</i>-cedrene ozonolysis and the important role of sesquiterpenes in new particle formation as suggested by field measurements.
url https://www.atmos-chem-phys.net/16/3245/2016/acp-16-3245-2016.pdf
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