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Volume 14, issue 13
Atmos. Chem. Phys., 14, 6967–6981, 2014
https://doi.org/10.5194/acp-14-6967-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 14, 6967–6981, 2014
https://doi.org/10.5194/acp-14-6967-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 09 Jul 2014

Research article | 09 Jul 2014

Fog scavenging of organic and inorganic aerosol in the Po Valley

S. Gilardoni1, P. Massoli4, L. Giulianelli1, M. Rinaldi1, M. Paglione1, F. Pollini1, C. Lanconelli1, V. Poluzzi2, S. Carbone3, R. Hillamo3, L. M. Russell5, M. C. Facchini1, and S. Fuzzi1 S. Gilardoni et al.
  • 1Italian National Research Council – Institute of Atmospheric Sciences and Climate, Bologna, Italy
  • 2Agenzia Regionale per la Prevenzione e l'Ambiente ARPA, Bologna, Italy
  • 3Finnish Meteorological Institute, Air quality, Helsinki, Finland
  • 4Aerodyne Research, Billerica, MA, USA
  • 5Scripps Institute of Oceanography, University of California-San Diego, La Jolla, CA, USA

Abstract. The interaction of aerosol with atmospheric water affects the processing and wet removal of atmospheric particles. Understanding such interaction is mandatory to improve model description of aerosol lifetime and ageing. We analyzed the aerosol–water interaction at high relative humidity during fog events in the Po Valley within the framework of the Agenzia Regionale per la Prevenzione e l'Ambiente (ARPA) – Emilia Romagna supersite project. For the first time in this area, the changes in particle chemical composition caused by fog are discussed along with changes in particle microphysics.

During the experiment, 14 fog events were observed. The average mass scavenging efficiency was 70% for nitrate, 68% for ammonium, 61% for sulfate, 50% for organics, and 39% for black carbon. After fog formation, the interstitial aerosol was dominated by particles smaller than 200 nm Dva (vacuum aerodynamic diameter) and enriched in carbonaceous aerosol, mainly black carbon and water-insoluble organic aerosol.

For each fog event, the size-segregated scavenging efficiency of nitrate and organic aerosol (OA) was calculated by comparing chemical species size distribution before and after fog formation. For both nitrate and OA, the size-segregated scavenging efficiency followed a sigmoidal curve, with values close to zero below 100 nm Dva and close to 1 above 700 nm Dva. OA was able to affect scavenging efficiency of nitrate in particles smaller than 300 nm Dva. A linear correlation between nitrate scavenging and particle hygroscopicity (κ) was observed, indicating that 44–51% of the variability of nitrate scavenging in smaller particles (below 300 nm Dva) was explained by changes in particle chemical composition.

The size-segregated scavenging curves of OA followed those of nitrate, suggesting that organic scavenging was controlled by mixing with water-soluble species. In particular, functional group composition and OA elemental analysis indicated that more oxidized OA was scavenged more efficiently than less oxidized OA. Nevertheless, the small variability of organic functional group composition during the experiment did not allow us to discriminate the effect of different organic functionalities on OA scavenging.

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