Aliphatic carbonyl compounds (C<sub>8</sub>–C<sub>26</sub>) in wintertime atmospheric aerosol in London, UK
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Published:2019-02-20
Issue:4
Volume:19
Page:2233-2246
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Lyu RuiheORCID, Alam Mohammed S., Stark Christopher, Xu Ruixin, Shi Zongbo, Feng Yinchang, Harrison Roy M.ORCID
Abstract
Abstract. Three groups of aliphatic carbonyl compounds, the n-alkanals
(C8–C20), n-alkan-2-ones (C8–C26), and
n-alkan-3-ones (C8–C19), were measured in both particulate
and vapour phases in air samples collected in London from January to
April 2017. Four sites were sampled including two rooftop background sites,
one ground-level urban background site, and a street canyon location on
Marylebone Road in central London. The n-alkanals showed the highest
concentrations, followed by the n-alkan-2-ones and the n-alkan-3-ones, the
latter having appreciably lower concentrations. It seems likely that all
compound groups have both primary and secondary sources and these are
considered in light of published laboratory work on the oxidation
products of high-molecular-weight n-alkanes. All compound groups show
a relatively low correlation with black carbon and NOx in the
background air of London, but in street canyon air heavily impacted by
vehicle emissions, stronger correlations emerge, especially for the
n-alkanals. It appears that vehicle exhaust is likely to be a major
contributor for concentrations of the n-alkanals, whereas it is a much smaller
contributor to the n-alkan-2-ones and n-alkan-3-ones. Other primary sources
such as cooking or wood burning may be contributors for the ketones but were
not directly evaluated. It seems likely that there is also a significant
contribution from the photo-oxidation of n-alkanes and this would be consistent
with the much higher abundance of n-alkan-2-ones relative to
n-alkan-3-ones if the formation mechanism were through the oxidation of
condensed-phase alkanes. Vapour–particle partitioning fitted the Pankow model
well for the n-alkan-2-ones but less well for the other compound groups,
although somewhat stronger relationships were seen at the Marylebone Road
site than at the background sites. The former observation gives support to
the n-alkane-2-ones being a predominantly secondary product, whereas primary
sources of the other groups are more prominent.
Funder
European Research Council Natural Environment Research Council
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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