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LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00004652naa a2200481 4500
001oai:lup.lub.lu.se:6d6ddbe7-1cef-44f5-bab3-ab93bd9c14f0
003SwePub
008160401s2012 | |||||||||||000 ||eng|
024a https://lup.lub.lu.se/record/31895932 URI
024a https://doi.org/10.1016/j.atmosenv.2012.06.0132 DOI
040 a (SwePub)lu
041 a engb eng
042 9 SwePub
072 7a art2 swepub-publicationtype
072 7a ref2 swepub-contenttype
100a Alves, Celia4 aut
2451 0a Organic compounds in aerosols from selected European sites - Biogenic versus anthropogenic sources
264 1b Elsevier BV,c 2012
520 a Atmospheric aerosol samples from a boreal forest (Hyytiala, 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 rations 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, Hyytiala 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. (C) 2012 Elsevier Ltd. All rights reserved.
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskapx Meteorologi och atmosfärforskning0 (SwePub)105082 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Meteorology and Atmospheric Sciences0 (SwePub)105082 hsv//eng
653 a European aerosol
653 a Organic compounds
653 a Tracers
653 a Diagnostic ratios
653 a Benzo(a)pyrene equivalent carcinogenicity
653 a Sources
700a Vicente, Ana4 aut
700a Pio, Casimiro4 aut
700a Kiss, Gyula4 aut
700a Hoffer, Andras4 aut
700a Decesari, Stefano4 aut
700a Prevot, Andre S. H.4 aut
700a Cruz Minguillon, Maria4 aut
700a Querol, Xavier4 aut
700a Hillamo, Risto4 aut
700a Spindler, Gerald4 aut
700a Swietlicki, Eriku Lund University,Lunds universitet,Kärnfysik,Fysiska institutionen,Institutioner vid LTH,Lunds Tekniska Högskola,Nuclear physics,Department of Physics,Departments at LTH,Faculty of Engineering, LTH4 aut0 (Swepub:lu)nucl-esw
710a Kärnfysikb Fysiska institutionen4 org
773t Atmospheric Environmentd : Elsevier BVg 59, s. 243-255q 59<243-255x 1352-2310
856u http://dx.doi.org/10.1016/j.atmosenv.2012.06.013y FULLTEXT
8564 8u https://lup.lub.lu.se/record/3189593
8564 8u https://doi.org/10.1016/j.atmosenv.2012.06.013

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