Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9141
DC FieldValueLanguage
dc.contributor.authorallBoatta, F.; Università di Palermo, Dip. DiSTeMen
dc.contributor.authorallCalabrese, S.; Università di Palermo, Dip. DiSTeMen
dc.contributor.authorallD'Alessandro, W.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallParello, F.; Università di Palermo, Dip. DiSTeMen
dc.contributor.editorallVoudouris, K.; Aristotele University, Thessaloniki, Greeceen
dc.contributor.editorallStamatis, G.; Hellenic Committee of Hydrogeologyen
dc.contributor.editorallMattas, C.; Aristotele University, Thessaloniki, Greeceen
dc.contributor.editorallKaklis, T.; Aristotele University, Thessaloniki, Greeceen
dc.contributor.editorallKazakis, N.; Aristotele University, Thessaloniki, Greeceen
dc.date.accessioned2014-10-23T13:38:07Zen
dc.date.available2014-10-23T13:38:07Zen
dc.date.issued2014-10-08en
dc.identifier.urihttp://hdl.handle.net/2122/9141en
dc.description.abstractBulk deposition has been collected at six sampling sites in area of Gela plain (Italy) in the period from February 2008 to May 2009. Samples collected each two weeks were analysed for the major ion and trace elements content. Preliminary results allow identifying three different sources that control the abundance of the elements in atmospheric deposition: (1) sea spray, (2) geogenic dust, and (3) anthropogenic pollution. Due to the closeness of the coast, clear evidence of sea spray input is detectable for most of the samples. The high excess of non sea-salt sulphate (50 - 90% of the total) is prevailingly ascribable to the abundant SO2 emissions of the refinery. The pH values of the collected samples range from 4.2 to 8.6, with 80% of them above pH 6.5, indicating an extensive neutralization. This is due to NH3 coming from widespread agricultural activities in the plain of Gela, and geogenic CaCO3 either from local or from regional (desert dust) sources. Elevated levels of trace metals (Zn, V, Sb, Ni, Cr, Ni and Cu) can be observed in the samples collected close to the industrial area. All these elements can be identified as “anthropogenic” and attributed to the human activities, mainly to the industrial emissions, but a contribution could also derive from the intensive vehicular traffic.en
dc.language.isoEnglishen
dc.relation.ispartof10th International Hydrogeological Congress of Greeceen
dc.subjectRainwateren
dc.subjectTrace elementsen
dc.subjectPetroleum refineryen
dc.subjectSea sprayen
dc.subjectSaharan dusten
dc.titleCHEMICAL COMPOSITION OF ATMOSPHERIC BULK DEPOSITION AT THE INDUSTRIAL AREA OF GELA (SICILY, ITALY)en
dc.typeConference paperen
dc.description.statusPublisheden
dc.subject.INGV01. Atmosphere::01.01. Atmosphere::01.01.03. Pollutionen
dc.subject.INGV03. Hydrosphere::03.04. Chemical and biological::03.04.03. Chemistry of watersen
dc.description.ConferenceLocationThessaloniki, Greeceen
dc.description.obiettivoSpecifico6A. Monitoraggio ambientale, sicurezza e territorioen
dc.publisherAristotele University of Thessalonikien
dc.description.fulltextopenen
dc.contributor.authorBoatta, F.en
dc.contributor.authorCalabrese, S.en
dc.contributor.authorD'Alessandro, W.en
dc.contributor.authorParello, F.en
dc.contributor.departmentUniversità di Palermo, Dip. DiSTeMen
dc.contributor.departmentUniversità di Palermo, Dip. DiSTeMen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.editorVoudouris, K.en
dc.contributor.editorStamatis, G.en
dc.contributor.editorMattas, C.en
dc.contributor.editorKaklis, T.en
dc.contributor.editorKazakis, N.en
dc.contributor.editordepartmentAristotele University, Thessaloniki, Greeceen
dc.contributor.editordepartmentHellenic Committee of Hydrogeologyen
dc.contributor.editordepartmentAristotele University, Thessaloniki, Greeceen
dc.contributor.editordepartmentAristotele University, Thessaloniki, Greeceen
dc.contributor.editordepartmentAristotele University, Thessaloniki, Greeceen
item.openairetypeConference paper-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversità di Palermo, Dip. DiSTeM-
crisitem.author.deptDipartimento C.F.T.A., Palermo University, Palermo/Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptUniversità di Palermo, DiSTeM, Italy-
crisitem.author.orcid0000-0003-0249-6663-
crisitem.author.orcid0000-0003-1724-0388-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent01. Atmosphere-
crisitem.classification.parent03. Hydrosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
Appears in Collections:Conference materials
Files in This Item:
File Description SizeFormat
07b_Boatta.pdfmain article1.04 MBAdobe PDFView/Open
Show simple item record

Page view(s) 10

381
checked on Apr 17, 2024

Download(s) 50

254
checked on Apr 17, 2024

Google ScholarTM

Check