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The contribution of new particle formation and subsequent growth to haze formation.
Kulmala, Markku; Cai, Runlong; Stolzenburg, Dominik; Zhou, Ying; Dada, Lubna; Guo, Yishuo; Yan, Chao; Petäjä, Tuukka; Jiang, Jingkun; Kerminen, Veli-Matti.
Afiliación
  • Kulmala M; Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Sciences and Engineering, Beijing University of Chemical Technology (BUCT) Beijing China.
  • Cai R; Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki Finland markku.kulmala@helsinki.fi.
  • Stolzenburg D; Joint International Research Laboratory of Atmospheric and Earth System Sciences, School of Atmospheric Sciences, Nanjing University Nanjing China.
  • Zhou Y; Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki Finland markku.kulmala@helsinki.fi.
  • Dada L; Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki Finland markku.kulmala@helsinki.fi.
  • Guo Y; Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Sciences and Engineering, Beijing University of Chemical Technology (BUCT) Beijing China.
  • Yan C; Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki Finland markku.kulmala@helsinki.fi.
  • Petäjä T; Laboratory of Atmospheric Chemistry, Paul Scherrer Institute Villigen Switzerland.
  • Jiang J; Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Sciences and Engineering, Beijing University of Chemical Technology (BUCT) Beijing China.
  • Kerminen VM; Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Sciences and Engineering, Beijing University of Chemical Technology (BUCT) Beijing China.
Environ Sci Atmos ; 2(3): 352-361, 2022 May 19.
Article en En | MEDLINE | ID: mdl-35694136
ABSTRACT
We investigated the contribution of atmospheric new particle formation (NPF) and subsequent growth of the newly formed particles, characterized by high concentrations of fine particulate matter (PM2.5). In addition to having adverse effects on visibility and human health, these haze particles may act as cloud condensation nuclei, having potentially large influences on clouds and precipitation. Using atmospheric observations performed in 2019 in Beijing, a polluted megacity in China, we showed that the variability of growth rates (GR) of particles originating from NPF depend only weakly on low-volatile vapor - highly oxidated organic molecules (HOMs) and sulphuric acid - concentrations and have no apparent connection with the strength of NPF or the level of background pollution. We then constrained aerosol dynamic model simulations with these observations. We showed that under conditions typical for the Beijing atmosphere, NPF is capable of contributing with more than 100 µg m-3 to the PM2.5 mass concentration and simultaneously >103 cm-3 to the haze particle (diameter > 100 nm) number concentration. Our simulations reveal that the PM2.5 mass concentration originating from NPF, strength of NPF, particle growth rate and pre-existing background particle population are all connected with each other. Concerning the PM pollution control, our results indicate that reducing primary particle emissions might not result in an effective enough decrease in total PM2.5 mass concentrations until a reduction in emissions of precursor compounds for NPF and subsequent particle growth is imposed.

Texto completo: 1 Bases de datos: MEDLINE Idioma: En Revista: Environ Sci Atmos Año: 2022 Tipo del documento: Article

Texto completo: 1 Bases de datos: MEDLINE Idioma: En Revista: Environ Sci Atmos Año: 2022 Tipo del documento: Article