Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/412
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dc.contributor.authorallCarapezza, M. L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallGranieri, D.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2005-09-25T17:40:48Zen
dc.date.available2005-09-25T17:40:48Zen
dc.date.issued2004en
dc.identifier.urihttp://hdl.handle.net/2122/412en
dc.description.abstractCarbon dioxide soil flux has been used for many years to monitor Italian active volcanoes and both the active Dynamic Concentration (DCM) and the passive Accumulation Chamber (ACM) methods are employed. These two methods have been compared by means of 218 simultaneous flux measurements carried out in the La Fossa area of Vulcano Island, where a large variation of CO2 soil release occurs. Results indicate that DCMoverestimates CO2 flux and is proportional to it only in high flux zones (flux higher than 100 gm 2 day 1). UsingACMfluxes and the Stefan–Maxwell equation, the measured CO2/depth curves in the soil could be reproduced. In high flux points CO2 is transported mostly by viscous flow up to a very shallow depth and then by diffusive flow, which is the dominant gas transport mechanism in low flux points. Carbon dioxide soil flux values are controlled by proximity to active gas releasing fractures, by changes in the barometric pressure and by variations in soil permeability.en
dc.format.extent493 bytesen
dc.format.extent596092 bytesen
dc.format.mimetypetext/htmlen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.publisher.namePergamonen
dc.relation.ispartofApplied Geochemistryen
dc.relation.ispartofseries19en
dc.subjectVulcanoen
dc.subjectCO2en
dc.subjectCarbon dioxideen
dc.titleCO2 soil flux at Vulcano (Italy): comparison between active and passive methodsen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber73-88en
dc.identifier.URLwww.elsevier.com/locate/apgeochemen
dc.subject.INGV04. Solid Earth::04.02. Exploration geophysics::04.02.07. Instruments and techniquesen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniquesen
dc.identifier.doi10.1016/S0883-2927(03)00111-2en
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dc.description.fulltextpartially_openen
dc.contributor.authorCarapezza, M. L.en
dc.contributor.authorGranieri, D.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
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.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.orcid0000-0002-0223-6012-
crisitem.author.orcid0000-0003-2831-723X-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
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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