Effects of SO 2 oxidation on ambient aerosol growth in water and ethanol vapours

Hygroscopicity (i.e. water vapour affinity) of atmospheric aerosol particles is one of the key factors in defining their impacts on climate. Condensation of sulphuric acid onto less hygroscopic particles is expected to increase their hygrocopicity and hence their cloud condensation nuclei formation...

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Main Authors: T. Petäjä, V.-M. Kerminen, K. Hämeri, P. Vaattovaara, J. Joutsensaari, W. Junkermann, A. Laaksonen, M. Kulmala
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2005
Subjects:
Online Access:https://doaj.org/article/28a12600362b4187a1e870eb96050e49
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spelling ftdoajarticles:oai:doaj.org/article:28a12600362b4187a1e870eb96050e49 2023-05-15T15:08:17+02:00 Effects of SO 2 oxidation on ambient aerosol growth in water and ethanol vapours T. Petäjä V.-M. Kerminen K. Hämeri P. Vaattovaara J. Joutsensaari W. Junkermann A. Laaksonen M. Kulmala 2005-01-01T00:00:00Z https://doaj.org/article/28a12600362b4187a1e870eb96050e49 EN eng Copernicus Publications http://www.atmos-chem-phys.net/5/767/2005/acp-5-767-2005.pdf https://doaj.org/toc/1680-7316 https://doaj.org/toc/1680-7324 1680-7316 1680-7324 https://doaj.org/article/28a12600362b4187a1e870eb96050e49 Atmospheric Chemistry and Physics, Vol 5, Iss 3, Pp 767-779 (2005) Physics QC1-999 Chemistry QD1-999 article 2005 ftdoajarticles 2022-12-31T15:07:47Z Hygroscopicity (i.e. water vapour affinity) of atmospheric aerosol particles is one of the key factors in defining their impacts on climate. Condensation of sulphuric acid onto less hygroscopic particles is expected to increase their hygrocopicity and hence their cloud condensation nuclei formation potential. In this study, differences in the hygroscopic and ethanol uptake properties of ultrafine aerosol particles in the Arctic air masses with a different exposure to anthropogenic sulfur pollution were examined. The main discovery was that Aitken mode particles having been exposed to polluted air were more hygroscopic and less soluble to ethanol than after transport in clean air. This aging process was attributed to sulphur dioxide oxidation and subsequent condensation during the transport of these particle to our measurement site. The hygroscopicity of nucleation mode aerosol particles, on the other hand, was approximately the same in all the cases, being indicative of a relatively similar chemical composition despite the differences in air mass transport routes. These particles had also been produced closer to the observation site typically 3–8 h prior to sampling. Apparently, these particles did not have an opportunity to accumulate sulphuric acid on their way to the site, but instead their chemical composition (hygroscopicity and ethanol solubility) resembled that of particles produced in the local or semi-regional ambient conditions. Article in Journal/Newspaper Arctic Directory of Open Access Journals: DOAJ Articles Aitken ENVELOPE(-44.516,-44.516,-60.733,-60.733) Arctic
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Physics
QC1-999
Chemistry
QD1-999
spellingShingle Physics
QC1-999
Chemistry
QD1-999
T. Petäjä
V.-M. Kerminen
K. Hämeri
P. Vaattovaara
J. Joutsensaari
W. Junkermann
A. Laaksonen
M. Kulmala
Effects of SO 2 oxidation on ambient aerosol growth in water and ethanol vapours
topic_facet Physics
QC1-999
Chemistry
QD1-999
description Hygroscopicity (i.e. water vapour affinity) of atmospheric aerosol particles is one of the key factors in defining their impacts on climate. Condensation of sulphuric acid onto less hygroscopic particles is expected to increase their hygrocopicity and hence their cloud condensation nuclei formation potential. In this study, differences in the hygroscopic and ethanol uptake properties of ultrafine aerosol particles in the Arctic air masses with a different exposure to anthropogenic sulfur pollution were examined. The main discovery was that Aitken mode particles having been exposed to polluted air were more hygroscopic and less soluble to ethanol than after transport in clean air. This aging process was attributed to sulphur dioxide oxidation and subsequent condensation during the transport of these particle to our measurement site. The hygroscopicity of nucleation mode aerosol particles, on the other hand, was approximately the same in all the cases, being indicative of a relatively similar chemical composition despite the differences in air mass transport routes. These particles had also been produced closer to the observation site typically 3–8 h prior to sampling. Apparently, these particles did not have an opportunity to accumulate sulphuric acid on their way to the site, but instead their chemical composition (hygroscopicity and ethanol solubility) resembled that of particles produced in the local or semi-regional ambient conditions.
format Article in Journal/Newspaper
author T. Petäjä
V.-M. Kerminen
K. Hämeri
P. Vaattovaara
J. Joutsensaari
W. Junkermann
A. Laaksonen
M. Kulmala
author_facet T. Petäjä
V.-M. Kerminen
K. Hämeri
P. Vaattovaara
J. Joutsensaari
W. Junkermann
A. Laaksonen
M. Kulmala
author_sort T. Petäjä
title Effects of SO 2 oxidation on ambient aerosol growth in water and ethanol vapours
title_short Effects of SO 2 oxidation on ambient aerosol growth in water and ethanol vapours
title_full Effects of SO 2 oxidation on ambient aerosol growth in water and ethanol vapours
title_fullStr Effects of SO 2 oxidation on ambient aerosol growth in water and ethanol vapours
title_full_unstemmed Effects of SO 2 oxidation on ambient aerosol growth in water and ethanol vapours
title_sort effects of so 2 oxidation on ambient aerosol growth in water and ethanol vapours
publisher Copernicus Publications
publishDate 2005
url https://doaj.org/article/28a12600362b4187a1e870eb96050e49
long_lat ENVELOPE(-44.516,-44.516,-60.733,-60.733)
geographic Aitken
Arctic
geographic_facet Aitken
Arctic
genre Arctic
genre_facet Arctic
op_source Atmospheric Chemistry and Physics, Vol 5, Iss 3, Pp 767-779 (2005)
op_relation http://www.atmos-chem-phys.net/5/767/2005/acp-5-767-2005.pdf
https://doaj.org/toc/1680-7316
https://doaj.org/toc/1680-7324
1680-7316
1680-7324
https://doaj.org/article/28a12600362b4187a1e870eb96050e49
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