Fog scavenging of organic and inorganic aerosol in the Po Valley

TitleFog scavenging of organic and inorganic aerosol in the Po Valley
Publication TypeJournal Article
Year of Publication2014
AuthorsGilardoni S., Massoli P., Giulianelli L., Rinaldi M., Paglione M., Pollini F., Lanconelli C., Poluzzi V., Carbone S., Hillamo R., Russell LM, Facchini M.C, Fuzzi S.
JournalAtmospheric Chemistry and Physics
Date Published2014/07
Type of ArticleArticle
ISBN Number1680-7316
Accession NumberWOS:000339244600030
Keywordsambient aerosol; chemical-characterization; cloud droplets; condensation nucleus activity; high-resolution; hygroscopic growth; mass-spectrometer; particulate matter; positive matrix factorization; single-parameter representation

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 D-va (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 D-va and close to 1 above 700 nm D-va. OA was able to affect scavenging efficiency of nitrate in particles smaller than 300 nm D-va. A linear correlation between nitrate scavenging and particle hygroscopicity (kappa) was observed, indicating that 44-51% of the variability of nitrate scavenging in smaller particles (below 300 nm D-va) 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.

Short TitleAtmos. Chem. Phys.
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