Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5114
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dc.contributor.authorallFloor, G.H.; University of Girona, Spainen
dc.contributor.authorallCalabrese, S.; Dip. CFTA, Università di Palermoen
dc.contributor.authorallRoman-Ross, G.; University of Girona, Spainen
dc.contributor.authorallD'Alessandro, W.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallAiuppa, A.; Dip. CFTA, Università di Palermoen
dc.date.accessioned2009-07-05T16:57:51Zen
dc.date.available2009-07-05T16:57:51Zen
dc.date.issued2009-06-21en
dc.identifier.urihttp://hdl.handle.net/2122/5114en
dc.description.abstractActive volcanoes emit considerable amounts of contaminants such as As, Se and V. Mount Etna is the biggest volcano of Europe and an excellent geochemical site to study water-soil processes. Due to its volcanic activity, the rainwater has a strong compositional gradient, both in time and space. At present, the behaviour of trace elements in the soils around Mt Etna is poorly understood. To determine the influence of the rainwater pH on the potential mobilization of geogenic pollutants, batch experiments have been performed with synthetic rainwater for 25 soils collected along the flanks of the volcano. Our results show that: i) The maximum concentrations in the leaching solutions are higher for acid rain than for neutral rain (e.g. 7.7 vs 1.3 mg/L for Se). ii) With neutral rain conditions the soils upwind from the volcano have higher concentrations of Se than those downwind (up to 1.3 mg/L compared to ≤0.3 mg/L for the other samples). This trend is less clear for As and V. iii) For soils collected from 2 to 10 km downwind of the craters, Se concentrations in acid rain leachates decrease one order of magnitude with increasing distance. A similar pattern is also observed upwind from the volcano. For As and V no clear relationship between concentrations and location with respect to the volcanic craters is observed. Both i) and ii) result in a low pH dependence for samples upwind from the volcano. The biggest difference between acid and neutral leaching for As and V is observed for a sample 2 km downwind from the craters. The observed patterns are influenced by potential controlling factors, such as organic matter content, total concentrations, mineralogy, influence of the volcanic plume, etc. Our results have implications for the chemical composition of the Etnean aquifer, the only water resource to the one million inhabitants around Mt Etna, as well as for the bioavailability and potential toxicity through agricultural activities, essential to the local economy.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofGoldschmidt 2009en
dc.subjectvolcanic soilsen
dc.subjectseleniumen
dc.subjectarsenicen
dc.subjectvanadiumen
dc.titleRainwater-induced leaching of selenium, arsenic and vanadium from Etnean volcanic soilsen
dc.typeOral presentationen
dc.description.statusPublisheden
dc.subject.INGV01. Atmosphere::01.01. Atmosphere::01.01.07. Volcanic effectsen
dc.subject.INGV03. Hydrosphere::03.03. Physical::03.03.01. Air/water/earth interactionsen
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.ConferenceLocationDavos, Switzerlanden
dc.description.obiettivoSpecifico4.4. Scenari e mitigazione del rischio ambientaleen
dc.description.fulltextopenen
dc.contributor.authorFloor, G.H.en
dc.contributor.authorCalabrese, S.en
dc.contributor.authorRoman-Ross, G.en
dc.contributor.authorD'Alessandro, W.en
dc.contributor.authorAiuppa, A.en
dc.contributor.departmentUniversity of Girona, Spainen
dc.contributor.departmentDip. CFTA, Università di Palermoen
dc.contributor.departmentUniversity of Girona, Spainen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentDip. CFTA, Università di Palermoen
item.openairetypeOral presentation-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversity of Girona, Dep. Chemistry, Spain-
crisitem.author.deptDipartimento C.F.T.A., Palermo University, Palermo/Italy-
crisitem.author.deptUniversity of Girona, Spain-
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.orcid0000-0003-0249-6663-
crisitem.author.orcid0000-0003-1724-0388-
crisitem.author.orcid0000-0002-0254-6539-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent01. Atmosphere-
crisitem.classification.parent03. Hydrosphere-
crisitem.classification.parent05. General-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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