4.2 Article

Atmospheric photochemistry and secondary aerosol formation of urban air in Lyon, France

Journal

JOURNAL OF ENVIRONMENTAL SCIENCES
Volume 99, Issue -, Pages 311-323

Publisher

SCIENCE PRESS
DOI: 10.1016/j.jes.2020.06.037

Keywords

Urban air; Oxidation Flow Reactor (OFR); Secondary Organic Aerosol (SOA); Volatile Organic Compounds (VOC); Photochemistry; Lyon

Funding

  1. Institute for Research on Catalysis and the Environment of Lyon (IRCELYON)
  2. Investissement d'Avenir PEPS Program Project (ASTRAL) of the University of Lyon
  3. French National center for Scientific Research (French: center national de la recherche scientifique, CNRS) [ANR-11-IDEX-0007]
  4. European Research Council under the Horizon 2020 Research and Innovation Program Project of the European Union [690958]

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Through an atmospheric experiment conducted in Lyon, it was found that urban air has a high potential to form secondary organic aerosol (SOA), primarily influenced by OH radical photochemical oxidation rather than ozonolysis. The correlation between SOA formation and ambient environment conditions was also observed during the study.
Photochemical aging of volatile organic compounds (VOCs) in the atmosphere is an important source of secondary organic aerosol (SOA). To evaluate the formation potential of SOA at an urban site in Lyon (France), an outdoor experiment using a Potential Aerosol Mass (PAM) oxidation flow reactor (OFR) was conducted throughout entire days during JanuaryFebruary 2017. Diurnal variation of SOA formations and their correlation with OH radical exposure (OHexp), ambient pollutants (VOCs and particulate matters, PM), Relative Humid-ity (RH), and temperature were explored in this study. Ambient urban air was exposed to high concentration of OH radicals with OHexp in range of (0.2-1.2)x10(12) molecule/(cm(3).sec), corresponding to several days to weeks of equivalent atmospheric photochemical aging. The results informed that urban air at Lyon has high potency to contribute to SOA, and these SOA productions were favored from OH radical photochemical oxidation rather than via ozonolysis. Maximum SOA formation (36 mu g/m(3)) was obtained at OHexp of about 7.4 x 10(11) molecule/(cm(3).sec), equivalent to approximately 5 days of atmospheric oxidation. The correlation between SOA formation and ambient environment conditions (RH & temperature, VOCs and PM) was observed. It was the first time to estimate SOA formation potential from ambient air over a long period in urban environment of Lyon. (C) 2020 The Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences. Published by Elsevier B.V.

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