Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6028
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dc.contributor.authorallD'Alessandro, W.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallCalabrese, S.; Università di Palermo, Dipartimento CFTAen
dc.contributor.authorallBellomo, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallBrusca, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallDi Maio, G.; Università di Palermo, Dipartimento CFTAen
dc.contributor.authorallParello, F.; Università di Palermo, Dipartimento CFTAen
dc.contributor.authorallSaiano, F.; Università di Palermo, Dipartimento ITAFen
dc.date.accessioned2010-06-07T16:38:49Zen
dc.date.available2010-06-07T16:38:49Zen
dc.date.issued2010-05-02en
dc.identifier.urihttp://hdl.handle.net/2122/6028en
dc.description.abstractA biomonitoring survey, above tree line level, using two endemic species (Senecio aethnensis and Rumex aethnensis) was performed on Mt. Etna, in order to evaluate the dispersion and the impact of volcanic atmospheric emissions. Samples of leaves were collected in summer 2008 from 30 sites in the upper part of the volcano (1500- 3000 m a.s.l). Acid digestion of samples was carried out with a microwave oven, and 44 elements were analyzed by using plasma spectrometry (ICP-MS and ICP-OES). The highest concentrations of all investigated elements were found in the samples collected closest to the degassing craters, and in the downwind sector, confirming that the eastern flank of Mt. Etna is the most impacted by volcanic emissions. Leaves collected along two radial transects from the active vents on the eastern flank, highlight that the levels of metals decrease one or two orders of magnitude with increasing distance from the source. This variability is higher for volatile elements (As, Bi, Cd, Cs, Pb, Sb, Tl) than for more refractory elements (Al, Ba, Sc, Si, Sr, Th, U). The two different species of plants do not show significant differences in the bioaccumulation of most of the analyzed elements, except for lanthanides, which are systematically enriched in Rumex leaves. The high concentrations of many toxic elements in the leaves allow us to consider these plants as highly tolerant species to the volcanic emissions, and suitable for biomonitoring researches in the Mt. Etna area.en
dc.language.isoEnglishen
dc.publisher.nameCopernicusen
dc.relation.ispartofEGU General Assembly 2010en
dc.subjectMt. Etnaen
dc.subjectbiomonitoringen
dc.subjectTrace elementsen
dc.titleEnvironmental impact of Mt. Etna’s degassing: volcanogenic trace elements bioaccumulation in two endemic plant species (Senecio aethnensis and Rumex aethnensis)en
dc.typePoster sessionen
dc.description.statusPublisheden
dc.subject.INGV01. Atmosphere::01.01. Atmosphere::01.01.03. Pollutionen
dc.subject.INGV01. Atmosphere::01.01. Atmosphere::01.01.07. Volcanic effectsen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.01. Gasesen
dc.subject.INGV05. General::05.02. Data dissemination::05.02.01. Geochemical dataen
dc.subject.INGV05. General::05.08. Risk::05.08.01. Environmental risken
dc.description.ConferenceLocationVienna, Austriaen
dc.description.obiettivoSpecifico4.4. Scenari e mitigazione del rischio ambientaleen
dc.description.fulltextopenen
dc.contributor.authorD'Alessandro, W.en
dc.contributor.authorCalabrese, S.en
dc.contributor.authorBellomo, S.en
dc.contributor.authorBrusca, L.en
dc.contributor.authorDi Maio, G.en
dc.contributor.authorParello, F.en
dc.contributor.authorSaiano, F.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentUniversità di Palermo, Dipartimento CFTAen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentUniversità di Palermo, Dipartimento CFTAen
dc.contributor.departmentUniversità di Palermo, Dipartimento ITAFen
item.openairetypePoster session-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
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.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptUniversità di Palermo, Dipartimento CFTA-
crisitem.author.deptUniversità di Palermo, DiSTeM, Italy-
crisitem.author.deptDip. Itaf, UNIPA-
crisitem.author.orcid0000-0003-1724-0388-
crisitem.author.orcid0000-0003-0249-6663-
crisitem.author.orcid0000-0002-6570-9673-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent01. Atmosphere-
crisitem.classification.parent01. Atmosphere-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent05. General-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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