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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7415
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dc.contributor.authorallCarapezza, M. L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallBarberi, F.; Univ. Roma Treen
dc.contributor.authorallRanaldi, M.; Univ. Roma Treen
dc.contributor.authorallRicci, T.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallTarchini, L.; Univ. Roma Treen
dc.date.accessioned2012-01-19T10:20:59Zen
dc.date.available2012-01-19T10:20:59Zen
dc.date.issued2011en
dc.identifier.urihttp://hdl.handle.net/2122/7415en
dc.description.abstractLa Fossa crater on Vulcano Island is quiescent since 1890. Periodically it undergoes “crises” characterized by marked increase of temperature (T), gas output and concentration of magmatic components in the crater fumaroles (T may exceed 600 °C). During these crises, which so far did not lead to any eruptive reactivation, the diffuse CO2 soil degassing also increases and in December 2005 an anomalous CO2 flux of 1350 tons/day was estimated by 1588 measurements over a surface of 1.66 km2 extending from La Fossa crater to the inhabited zone of Vulcano Porto. The crater area and two other anomalously degassing sites (Levante Beach and Palizzi) have been periodically investigated from December 2004 to August 2010 for diffuse CO2 soil flux. They show a marked variation with time of the degassing rate, with synchronous maxima in December 2005. Carbon dioxide soil flux and environmental parameters have been also continuously monitored for over one year by an automatic station at Vulcano Porto. In order to assess the hazard of the endogenous gas emissions, CO2 and H2S air concentrations have been measured by Tunable Diode Laser profiles near the fumaroles of the crater rim and of the Levante Beach area, where also the viscous gas flux has been estimated. In addition, CO2 air concentration has been measured both indoor and outdoor in an inhabited sector of Vulcano Porto. Results show that in some sites usually frequented by tourists there is a dangerous H2S air concentration and CO2 exceeds the hazardous thresholds in some Vulcano houses. These zones should be immediately monitored for gas hazard should a new crisis arise.en
dc.description.sponsorshipINGV-DPC programme - Project V5-Diffuse degassing in Italy; Airplane FIRB project of the Italian Ministry of the University and Researchen
dc.language.isoEnglishen
dc.publisher.nameelsevieren
dc.relation.ispartofJournal of Volcanology and Geothermal Researchen
dc.relation.ispartofseries3-4/207(2011)en
dc.subjectVulcano Islanden
dc.subjectdiffuse degassingen
dc.titleDiffuse CO2 soil degassing and CO2 and H2S air concentration and related hazard at Vulcano Island (Aeolian arc, Italy).en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber130-144en
dc.identifier.URLhttp://www.sciencedirect.com/science/article/pii/S0377027311001764en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.12. Fluid Geochemistryen
dc.identifier.doi10.1016/j.jvolgeores.2011.06.010en
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dc.description.obiettivoSpecifico1.2. TTC - Sorveglianza geochimica delle aree vulcaniche attiveen
dc.description.journalTypeJCR Journalen
dc.description.fulltextpartially_openen
dc.contributor.authorCarapezza, M. L.en
dc.contributor.authorBarberi, F.en
dc.contributor.authorRanaldi, M.en
dc.contributor.authorRicci, T.en
dc.contributor.authorTarchini, L.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentUniv. Roma Treen
dc.contributor.departmentUniv. Roma Treen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentUniv. Roma Treen
item.openairetypearticle-
item.cerifentitytypePublications-
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item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptUniversità Roma Tre-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0002-0223-6012-
crisitem.author.orcid0000-0001-6464-6298-
crisitem.author.orcid0000-0002-0553-5384-
crisitem.author.orcid0000-0001-6045-0802-
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.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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