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Molecular Characterization and Seasonal Variation in Primary and Secondary Organic Aerosols in Beijing, China
Author(s) -
Li Linjie,
Ren Lujie,
Ren Hong,
Yue Siyao,
Xie Qiaorong,
Zhao Wanyu,
Kang Mingjie,
Li Jie,
Wang Zifa,
Sun Yele,
Fu Pingqing
Publication year - 2018
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1029/2018jd028527
Subject(s) - levoglucosan , environmental chemistry , aerosol , arabitol , chemistry , isoprene , total organic carbon , particulates , organic matter , environmental science , biomass burning , organic chemistry , fermentation , copolymer , xylitol , polymer
Biomass burning (BB) aerosols, primary biological aerosol particles, and secondary organic aerosols, are critical components of particulate matter in the atmosphere. In this study, saccharides, lignin/resin acids, biogenic secondary organic aerosols tracers, aromatic acids, and hydroxyacids/polyacids were measured in total suspended particles collected from April 2012 to March 2013 at an urban site in Beijing using gas chromatography/mass spectrometry. The concentration of levoglucosan was elevated during 18–20 June. The high ratio of levoglucosan to mannosan and low ratio of galactosan to mannosan in June demonstrated the influence of wheat straw combustion in the North China Plain via long‐rang transport. Sucrose, glucose, and fructose were more abundant in April, the spring bloom season. The maximum trehalose content (298 ng/m 3 ) occurred during a dust storm (27–29 April) with the highest stable carbon isotope ratio ( δ 13 C, −21.2‰) of total carbon. Fungal spore tracers (arabitol and mannitol) peaked in summer. The largest concentrations of the oxidization products of isoprene and α/β‐pinene also occurred in summer. However, the β‐caryophyllene tracer was much more abundant on long‐lasting haze days in winter and was positively related to levoglucosan. The contributions of biogenic primary sources (plant debris, fungal spores, and BB) to organic carbon were estimated to be in range of 2.64–35.2% (11.8%), with BB being the predominant source. Biogenic secondary sources (isoprene, α‐pinene, and β‐caryophyllene) and anthropogenic secondary source (naphthalene) accounted for 0.23–10.9% (3.36%) of organic carbon with large contributions in summer and winter, respectively.