Please use this identifier to cite or link to this item: http://hdl.handle.net/10773/26994
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dc.contributor.authorAlves, Céliapt_PT
dc.contributor.authorVicente, Anapt_PT
dc.contributor.authorPio, Casimiropt_PT
dc.contributor.authorKiss, Gyulapt_PT
dc.contributor.authorHoffer, Andraspt_PT
dc.contributor.authorDecesari, Stefanopt_PT
dc.contributor.authorPrevôt, André S. H.pt_PT
dc.contributor.authorMinguillón, María Cruzpt_PT
dc.contributor.authorQuerol, Xavierpt_PT
dc.contributor.authorHillamo, Ristopt_PT
dc.contributor.authorSpindler, Geraldpt_PT
dc.contributor.authorSwietlicki, Erikpt_PT
dc.date.accessioned2019-11-20T16:36:50Z-
dc.date.available2019-11-20T16:36:50Z-
dc.date.issued2012-
dc.identifier.issn1352-2310pt_PT
dc.identifier.urihttp://hdl.handle.net/10773/26994-
dc.description.abstractAtmospheric aerosol samples from a boreal forest (Hyytiälä, April 2007), a rural site in Hungary (K-puszta, summer 2008), a polluted rural area in Italy (San Pietro Capofiume, Po Valley, April 2008), a moderately polluted rural site in Germany located on a meadow (Melpitz, May 2008), a natural park in Spain (Montseny, March 2009) and two urban background locations (Zurich, December 2008, and Barcelona, February/March 2009) were collected. Aliphatics, polycyclic aromatic hydrocarbons, carbonyls, sterols, n-alkanols, acids, phenolic compounds and anhydrosugars in aerosols were chemically characterised by gas chromatography–mass spectrometry, along with source attribution based on the carbon preference index (CPI), the ratios between the unresolved and the chromatographically resolved aliphatics, the contribution of wax n-alkanes, n-alkanols and n-alkanoic acids from plants, diagnostic ratios of individual target compounds and source-specific markers to organic carbon ratios. In spite of transboundary pollution episodes, Hyytiälä registered the lowest levels among all locations. CPI values close to 1 for the aliphatic fraction of the Montseny aerosol suggest that the anthropogenic input may be associated with the transport of aged air masses from the surrounding industrial/urban areas, which superimpose the locally originated hydrocarbons with biogenic origin. Aliphatic and aromatic hydrocarbons in samples from San Pietro Capofiume reveal that fossil fuel combustion is a major source influencing the diel pattern of concentrations. This source contributed to 25–45% of the ambient organic carbon (OC) at the Po Valley site. Aerosols from the German meadow presented variable contributions from both biogenic and anthropogenic sources. The highest levels of vegetation wax components and biogenic secondary organic aerosol (SOA) products were observed at K-puszta, while anthropogenic SOA compounds predominated in Barcelona. The primary vehicular emissions in the Spanish city accounted for around 25–30% of the OC in aerosols. Besides the traffic input (10% of OC), residential wood burning was found to be another dominant emission source contributing to the atmospheric aerosol (up to 38% of OC) at the Swiss urban location. It was estimated that around 10% of the OC mass in the urban sites originates from cooking emissions. Aerosols from the urban area of Zurich presented a much higher PAH content, and benzo(a)pyrene equivalent concentrations sometimes exceeding the mandatory limit.pt_PT
dc.language.isoengpt_PT
dc.publisherElsevierpt_PT
dc.relationinfo:eu-repo/grantAgreement/FCT/SFRH/SFRH%2FBD%2F48535%2F2008/PTpt_PT
dc.rightsrestrictedAccesspt_PT
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/pt_PT
dc.subjectEuropean aerosolpt_PT
dc.subjectOrganic compoundspt_PT
dc.subjectTracerspt_PT
dc.subjectDiagnostic ratiospt_PT
dc.subjectBenzo(a)pyrene equivalent carcinogenicitypt_PT
dc.subjectSourcespt_PT
dc.titleOrganic compounds in aerosols from selected European sites – Biogenic versus anthropogenic sourcespt_PT
dc.typearticlept_PT
dc.description.versionpublishedpt_PT
dc.peerreviewedyespt_PT
degois.publication.firstPage243pt_PT
degois.publication.lastPage255pt_PT
degois.publication.titleAtmospheric Environmentpt_PT
degois.publication.volume59pt_PT
dc.identifier.doi10.1016/j.atmosenv.2012.06.013pt_PT
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DAO - Artigos

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