Observations of highly oxidized molecules and particle nucleation in the atmosphere of Beijing
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Published:2019-12-10
Issue:23
Volume:19
Page:14933-14947
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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:
Brean James, Harrison Roy M.ORCID, Shi Zongbo, Beddows David C. S., Acton W. Joe F., Hewitt C. NicholasORCID, Squires Freya A.ORCID, Lee JamesORCID
Abstract
Abstract. Particle nucleation is one of the main sources of atmospheric particulate
matter by number, with new particles having great relevance for human health
and climate. Highly oxidized multifunctional organic molecules (HOMs) have
been recently identified as key constituents in the growth and, sometimes,
in initial formation of new particles. While there have been many studies of
HOMs in atmospheric chambers, flow tubes, and clean environments, analyses of
data from polluted environments are scarce. Here, measurements of HOMs and
particle size distributions down to small molecular clusters are presented
alongside volatile organic compounds (VOCs) and trace-gas data from a
campaign in June 2017, in Beijing. Many gas-phase HOMs have been
characterized and their temporal trends and behaviours analysed in the
context of new particle formation. The HOMs identified have a
degree of oxidation comparable to that seen in other, cleaner, environments, likely
due to an interplay between the higher temperatures facilitating rapid
hydrogen abstractions and the higher concentrations of NOx and other
RO2⚫ terminators ending the autoxidation sequence more rapidly.
Our data indicate that alkylbenzenes, monoterpenes, and isoprene are
important precursor VOCs for HOMs in Beijing. Many of the C5 and
C10 compounds derived from isoprene and monoterpenes have a slightly
greater degree of average oxidation state of carbon compared to those from
other precursors. Most HOMs except for large dimers have daytime peak
concentrations, indicating the importance of OH⚫ chemistry in the
formation of HOMs, as O3 tends to be lower on days with higher HOM
concentrations; similarly, VOC concentrations are lower on the days with
higher HOM concentrations. The daytime peaks of HOMs coincide with the
growth of freshly formed new particles, and their initial formation
coincides with the peak in sulfuric acid vapours, suggesting that the
nucleation process is sulfuric-acid-dependent, with HOMs contributing to
subsequent particle growth.
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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