http://www.cnr.it/ontology/cnr/individuo/prodotto/ID169843
Aerosol fine fraction in the Venice Lagoon: particle composition and sources. (Articolo in rivista)
- Type
- Label
- Aerosol fine fraction in the Venice Lagoon: particle composition and sources. (Articolo in rivista) (literal)
- Anno
- 2009-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1016/j.atmosres.2008.09.020 (literal)
- Alternative label
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Prodi F.; Belosi F.; Contini D.; Santachiara G.; Di Matteo L.; Gambaro A.; Donateo A.; Cesari D. (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Note
- ISI Web of Science (WOS) (literal)
- Scopu (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Gamabaro Andrea, Università di Venezia (literal)
- Titolo
- Aerosol fine fraction in the Venice Lagoon: particle composition and sources. (literal)
- Abstract
- The work presents a characterisation of aerosol sampled during three campaigns conducted in the Venice Lagoon from 30 June to 21 July 2004, from 15 February to 10 March 2005 and from 8 May to 25 May 2006. The results yield information about the physical-chemical characteristics of fine aerosol, the possible sources and its fate.
Sulphate (SO42-), nitrate (NO3-) and ammonium (NH4+) are identified as the main water soluble 4 3 components. The sum of these ions in the spring campaign 2006 varies from 51% to nearly 100% of PM2.5 fraction aerosol. NH4+ is found to be significantly correlated to non-sea-salt sulphate (nSS-SO42-) and NO3-, thus indicating the prevalent presence of ammonium nitrate and sulphate. The overall lack of a clear diurnal and seasonal cycle of sulphate suggests a transport from the Po Valley, while the diurnal and seasonal profile of nitrate concentrations suggests a prevalence of local generation. Sulphates from sea water through oxidation of dimethylsulfide (DMS) are not negligible (about 10% of the anthropogenic sulphate).
The marine aerosol contribution to PM1 and PM2.5 fractions, calculated using Na+ as a tracer of sea-salts. is low (range 1-6%).
In some cases chlorine depletion is observed. The content of chlorine in the aerosol particle is mostly higher than expected for marine environments (considered on the basis of Cl-/Na+ ratio). Therefore, specific sources for the element have been suggested.
Oxalic acid anion, which accounts for 55% of the organic compounds examined, presents mean values 180 ng m(-3) and 161 ng m(-3) in the winter and spring campaigns, comparable with reported values in low polluted urban areas.
In the winter campaign there is a high correlation between formate and acetate (R-2 = 0.93). suggesting that a common source makes a high contribution to the measured concentrations. (literal)
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