Molecular distribution and compound-specific stable carbon isotopic composition of dicarboxylic acids, oxocarboxylic acids and <i>α</i>-dicarbonyls in PM<sub>2.5</sub> from Beijing, China
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Published:2018-02-27
Issue:4
Volume:18
Page:2749-2767
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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:
Zhao Wanyu, Kawamura KimitakaORCID, Yue SiyaoORCID, Wei LianfangORCID, Ren Hong, Yan Yu, Kang Mingjie, Li Linjie, Ren Lujie, Lai SenchaoORCID, Li Jie, Sun YeleORCID, Wang Zifa, Fu PingqingORCID
Abstract
Abstract. This study investigates the seasonal variation, molecular distribution and
stable carbon isotopic composition of diacids, oxocarboxylic acids and
α-dicarbonyls to better understand the sources and formation
processes of fine aerosols (PM2.5) in Beijing. The concentrations of
total dicarboxylic acids varied from 110 to 2580 ng m−3, whereas
oxoacids (9.50–353 ng m−3) and dicarbonyls (1.50–85.9 ng m−3)
were less abundant. Oxalic acid was found to be the most abundant individual
species, followed by succinic acid or occasionally by terephthalic acid
(tPh), a plastic waste burning tracer. Ambient concentrations of phthalic
acid (37.9 ± 27.3 ng m−3) and tPh (48.7 ± 51.1 ng m−3)
were larger in winter than in other seasons, illustrating that fossil fuel
combustion and plastic waste incineration contribute more to wintertime
aerosols. The year-round mass concentration ratios of malonic acid to
succinic acid (C3 ∕ C4) were relatively low by comparison with
those in other urban aerosols and remote marine aerosols. The values were
less than or equal to unity in Beijing, implying that the degree of
photochemical formation of diacids in Beijing is insignificant. Moreover,
strong correlation coefficients of major oxocarboxylic acids and α-dicarbonyls with nss-K+ suggest that biomass burning contributes
significantly to these organic acids and related precursors. The mean
δ13C value of succinic acid is the highest among all species, with
values of −17.1 ± 3.9 ‰ (winter) and −17.1 ± 2.0 ‰ (spring), while malonic acid is more enriched in
13C than others in autumn (−17.6 ± 4.6 ‰) and
summer (−18.7 ± 4.0 ‰). The δ13C values
of major species in Beijing aerosols are generally lower than those in the
western North Pacific atmosphere, the downwind region, which indicates that
stable carbon isotopic compositions of diacids depend on their precursor
sources in Beijing. Therefore, our study demonstrates that in addition to
photochemical oxidation, high abundances of diacids, oxocarboxylic acids and
α-dicarbonyls in Beijing are largely associated with anthropogenic
primary emissions, such as biomass burning, fossil fuel combustion and
plastic waste burning.
Funder
National Natural Science Foundation of China
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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