CCN activity and volatility of β-caryophyllene secondary organic aerosol
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Authors
Frosch, Mia
Bilde, Merete
Nenes, Athanasios
Praplan, Arnaud P.
Jurányi, Zsófia
Dommen, Josef
Baltensperger, Urs
Author (Corporation)
Publication date
2013
Typ of student thesis
Course of study
Collections
Type
01A - Journal article
Editors
Editor (Corporation)
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Parent work
Atmospheric Chemistry and Physics
Special issue
DOI of the original publication
Link
Series
Series number
Volume
13
Issue / Number
4
Pages / Duration
2283–2297
Patent number
Publisher / Publishing institution
Copernicus
Place of publication / Event location
Göttingen
Edition
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Abstract
In a series of smog chamber experiments, the cloud condensation nuclei (CCN) activity of secondary organic aerosol (SOA) generated from ozonolysis of β-caryophyllene was characterized by determining the CCN derived hygroscopicity parameter, κCCN, from experimental data. Two types of CCN counters, operating at different temperatures, were used. The effect of semi-volatile organic compounds on the CCN activity of SOA was studied using a thermodenuder. Overall, SOA was only slightly CCN active (with κCCN in the range 0.001–0.16), and in dark experiments with no OH scavenger present, κCCN decreased when particles were sent through the thermodenuder (with a temperature up to 50 °C). SOA was generated under different experimental conditions: In some experiments, an OH scavenger (2-butanol) was added. SOA from these experiments was less CCN active than SOA produced in experiments without an OH scavenger (i.e. where OH was produced during ozonolysis). In other experiments, lights were turned on, either without or with the addition of HONO (OH source). This led to the formation of more CCN active SOA. SOA was aged up to 30 h through exposure to ozone and (in experiments with no OH scavenger present) to OH. In all experiments, the derived κCCN consistently increased with time after initial injection of β-caryophyllene, showing that chemical ageing increases the CCN activity of β-caryophyllene SOA. κCCN was also observed to depend on supersaturation, which was explained either as an evaporation artifact from semi-volatile SOA (only observed in experiments lacking light exposure) or, alternatively, by effects related to chemical composition depending on dry particle size. Using the method of Threshold Droplet Growth Analysis it was also concluded that the activation kinetics of the SOA do not differ significantly from calibration ammonium sulphate aerosol for particles aged for several hours.
Keywords
Subject (DDC)
550 - Geowissenschaften
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ISBN
ISSN
1680-7324
1680-7316
1680-7316
Language
English
Created during FHNW affiliation
No
Strategic action fields FHNW
Publication status
Published
Review
Peer review of the complete publication
Open access category
Gold
Citation
FROSCH, Mia, Merete BILDE, Athanasios NENES, Arnaud P. PRAPLAN, Zsófia JURÁNYI, Josef DOMMEN, Martin GYSEL, Ernest WEINGARTNER und Urs BALTENSPERGER, 2013. CCN activity and volatility of β-caryophyllene secondary organic aerosol. Atmospheric Chemistry and Physics. 2013. Bd. 13, Nr. 4, S. 2283–2297. DOI 10.5194/acp-13-2283-2013. Verfügbar unter: https://doi.org/10.26041/fhnw-8171