Welcome to the new version of CaltechAUTHORS. Login is currently restricted to library staff. If you notice any issues, please email coda@library.caltech.edu
Published February 25, 2011 | Published + Supplemental Material
Journal Article Open

Influence of aerosol acidity on the chemical composition of secondary organic aerosol from β-caryophyllene

Abstract

The secondary organic aerosol (SOA) yield of β-caryophyllene photooxidation is enhanced by aerosol acidity. In the present study, the influence of aerosol acidity on the chemical composition of β-caryophyllene SOA is investigated using ultra performance liquid chromatography/electrospray ionization-time-of-flight mass spectrometry (UPLC/ESI-TOFMS). A number of first-, second- and higher-generation gas-phase products having carbonyl and carboxylic acid functional groups are detected in the particle phase. Particle-phase reaction products formed via hydration and organosulfate formation processes are also detected. Increased acidity leads to different effects on the abundance of individual products; significantly, abundances of organosulfates are correlated with aerosol acidity. To our knowledge, this is the first detection of organosulfates and nitrated organosulfates derived from a sesquiterpene. The increase of certain particle-phase reaction products with increased acidity provides chemical evidence to support the acid-enhanced SOA yields. Based on the agreement between the chromatographic retention times and accurate mass measurements of chamber and field samples, three β-caryophyllene products (i.e., β-nocaryophyllon aldehyde, β-hydroxynocaryophyllon aldehyde, and β-dihydroxynocaryophyllon aldehyde) are suggested as chemical tracers for β-caryophyllene SOA. These compounds are detected in both day and night ambient samples collected in downtown Atlanta, GA and rural Yorkville, GA during the 2008 August Mini-Intensive Gas and Aerosol Study (AMIGAS).

Additional Information

© 2011 the Author(s). This work is distributed under the Creative Commons Attribution 3.0 License. Published by Copernicus Publications on behalf of the European Geosciences Union. Received: 18 November 2010. Published in Atmos. Chem. Phys. Discuss.: 30 November 2010. Revised: 10 February 2011. Accepted: 15 February 2011. Published: 25 February 2011. Edited by: H. Saathoff. This work was supported by the Electric Power Research Institute and the Southern Company, Birmingham, AL. We acknowledge all members of the AMIGAS for their support during the field campaign. The US Environmental Protection Agency through its Office of Research and Development funded and collaborated in the research described here under Contract 68-D-00-206 to Alion Science and Technology. It has been subject to Agency review and approved for publication. Mention of trade names or commercial products does not constitute an endorsement or recommendation for use.

Attached Files

Published - Chan2011p13318Atmos_Chem_Phys.pdf

Supplemental Material - acp-11-1735-2011-supplement.pdf

Files

Chan2011p13318Atmos_Chem_Phys.pdf
Files (1.3 MB)
Name Size Download all
md5:77ba6d7cbd37700ed82aca9ff0637328
1.1 MB Preview Download
md5:b935b596d2d9007a803423c906219242
252.5 kB Preview Download

Additional details

Created:
August 19, 2023
Modified:
October 23, 2023