4.7 Article

Quantifying the relative contributions of aqueous phase and photochemical processes to water-soluble organic carbon formation in winter in a megacity of South China

Journal

CHEMOSPHERE
Volume 300, Issue -, Pages -

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.chemosphere.2022.134598

Keywords

Nitrate; Condensation mode; Droplet mode; Photochemical processes; Aqueous phase chemical processes

Funding

  1. National Natural Science Foundation of China [41875160]
  2. Science and Technology Program of Guangdong Province (Science and Technology Innovation Platform Category) [2019B121201002]
  3. Guangzhou Science and Technology Program key projects [201904010152]
  4. Central Research Institute's Basic Scientific Special Funds [PM-zx703-202004-148]

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This study investigated the potential formation mechanisms and contributions of water-soluble organic carbon (WSOC) in urban Guangzhou of south China. The results revealed that WSOC formation is mainly influenced by photochemical and aqueous phase chemical processes.
To identify potential formation mechanisms of water-soluble organic carbon (WSOC) and quantify their contributions to WSOC in urban Guangzhou of south China, a comprehensive campaign was carried out in winter of 2019-2020. During the campaign, WSOC, total carbon (TC), black carbon (BC), water-soluble inorganic ions (WSIIs) and fourteen elements in PM2.5 were collected using inline instruments. Bulk PM2.5 and size-segregated particle samples were also synchronously collected using offline instruments for analyzing the dominant chemical components including WSOC, organic carbon (OC), elemental carbon (EC) and WSIIs. In addition, gaseous pollutants (e.g., NH3, SO2, HNO3, NO2, O-3) and meteorological parameters were also measured during the same period. PM2.5 pollution episodes during the campaign period were mainly driven by increased nitrate concentrations. The mass concentration of WSOC increased from 3.9 & PLUSMN; 1.1 mu gm(-3) on non-episode days to 6.8 +/- 0.6 mu gm(-3) on episode days, although the mass ratio of WSOC to OC in PM2.5 changed little (< 4%). Photochemical processes dominated WSOC formation in the afternoon and aqueous phase chemical processes played

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