Online gas- and particle-phase measurements of organosulfates, organosulfonates and nitrooxy organosulfates in Beijing utilizing a FIGAERO ToF-CIMS

A time-of-flight chemical ionization mass spectrometer (CIMS) utilizing the Filter Inlet for Gas and Aerosol (FIGAERO) was deployed at a regional site 40 km north-west of Beijing and successfully identified and measured 17 sulfur-containing organics (SCOs are organo/nitrooxy organosulfates and sulf...

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Veröffentlicht in:Atmospheric chemistry and physics 2018-07, Vol.18 (14), p.10355-10371
Hauptverfasser: Le Breton, Michael, Wang, Yujue, Hallquist, Åsa M, Pathak, Ravi Kant, Zheng, Jing, Yang, Yudong, Shang, Dongjie, Glasius, Marianne, Bannan, Thomas J, Liu, Qianyun, Chan, Chak K, Percival, Carl J, Zhu, Wenfei, Lou, Shengrong, Topping, David, Wang, Yuchen, Yu, Jianzhen, Lu, Keding, Guo, Song, Hu, Min, Hallquist, Mattias
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Sprache:eng
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Zusammenfassung:A time-of-flight chemical ionization mass spectrometer (CIMS) utilizing the Filter Inlet for Gas and Aerosol (FIGAERO) was deployed at a regional site 40 km north-west of Beijing and successfully identified and measured 17 sulfur-containing organics (SCOs are organo/nitrooxy organosulfates and sulfonates) with biogenic and anthropogenic precursors. The SCOs were quantified using laboratory-synthesized standards of lactic acid sulfate and nitrophenol organosulfate (NP OS). The variation in field observations was confirmed by comparison to offline measurement techniques (orbitrap and high-performance liquid chromatography, HPLC) using daily averages. The mean total (of the 17 identified by CIMS) SCO particle mass concentration was 210 ± 110 ng m.sup.-3 and had a maximum of 540 ng m.sup.-3, although it contributed to only 2 ± 1 % of the organic aerosol (OA). The CIMS identified a persistent gas-phase presence of SCOs in the ambient air, which was further supported by separate vapour-pressure measurements of NP OS by a Knudsen Effusion Mass Spectrometer (KEMS). An increase in relative humidity (RH) promoted partitioning of SCO to the particle phase, whereas higher temperatures favoured higher gas-phase concentrations.
ISSN:1680-7324
1680-7316
1680-7324
DOI:10.5194/acp-18-10355-2018