Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/507
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dc.contributor.authorallAiuppa, A.; Dipartimento CFTA, Universita` di Palermo, Palermo, Italy.en
dc.contributor.authorallFederico, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallGiudice, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallGurrieri, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.date.accessioned2005-10-31T11:47:28Zen
dc.date.available2005-10-31T11:47:28Zen
dc.date.issued2005en
dc.identifier.urihttp://hdl.handle.net/2122/507en
dc.description.abstractThe performance of a newly-developed portable gas analyzer, capable of real-time measurement of CO2, SO2 and H2S concentrations in volcanic gases, was tested at La Fossa Crater, Vulcano Island. The gas analyzer was used to acquire about 3000 determinations over the fumarolic field, allowing the definition of its chemical structure and heterogeneity. Our high-resolution analysis reveals that, in December 2004, the La Fossa fumarolic field was characterized by an oxidized inner core (SO2/H2S ratios of 3), and by more reducing conditions on its northern edge (SO2/H2S ratios of 1; range: 0.2–3.3). CO2/(SO2+H2S) molar ratios averaged 35 ± 21, with overlapping compositions for rim and inner crater fumaroles. S-poor compositions (CO2/(SO2+H2S) 50) characterized the field margins, probably due to deposition of native sulfur. Based on the above data and an SO2 flux of 18 ± 3 t.d-1, we estimate CO2 and H2S output rates from the volcano of 420 ± 250 and 4 ± 2 t.d-1, respectively.en
dc.format.extent503 bytesen
dc.format.extent253439 bytesen
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dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.publisher.nameAmerican Geophysical Unionen
dc.relation.ispartofGeophysical Research Lettersen
dc.relation.ispartofseries32(2005)en
dc.subjectelectrochemical sensorsen
dc.subjectfumarolic gasesen
dc.titleChemical mapping of a fumarolic field: La Fossa Crater, Vulcano Island (Aeolian Islands, Italy)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumberL13309en
dc.identifier.URLhttp://www.agu.org/en
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.01. Gasesen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoringen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniquesen
dc.identifier.doi10.1029/2005GL023207en
dc.relation.referencesAiuppa, A., S. Inguaggiato, A. J. S. McGonigle, M. O’Dwyer, C. Oppenheimer, M. J. Padgett, D. Rouwet, and M. Valenza (2005), H2S fluxes from Mt. Etna, Stromboli and Vulcano (Italy) and implications for the global volcanic sulfur budget, Geochim. Cosmochim. Acta, 69, 1861–1871. Allard, P., et al. (1991), Eruptive and diffuse emissions of CO2 from Mount Etna, Nature, 351, 387–391. Allard, P., M. Burton, and F. Murè (2004), Spectroscopic evidence for a lava fountain driven by previously accumulated magmatic gases, Nature, 433, 407–410. Bluth, G. J. S., C. C. Schnetzler, A. J. Kreuger, and L. S. Walter (1993), The contribution of explosive volcanism to global sulfur dioxide concentrations, Nature, 366, 327–329. Capasso, G., R. Favara, and S. Inguaggiato (1997), Chemical features and isotopic gaseous manifestation on Vulcano Island (Aeolian Island): An interpretative model of fluid circulation, Geochim. Cosmochim. Acta, 61, 3425–3442. Carroll, M. R., and J. R. Holloway (1994), Volatiles in Magmas, Rev. Mineral., vol. 30, 500 pp., Am. Mineral. Soc., Washington, D.C. Chiodini, G., R. Cioni, and L. Marini (1993), Reactions governing the chemistry of crater fumaroles from Vulcano Island, Italy, and implications for volcanic surveillance, Appl. Geochem., 8, 357–371. Chiodini, G., F. Frondini, and B. Raco (1996), Diffuse emission of CO2 from the Fossa crater, Vulcano Island (Italy), Bull. Volcanol., 58, 41–50. Diliberto, I. S., S. Gurrieri, and M. Valenza (2002), Relationships between diffuse CO2 emissions and volcanic activity on the island of Vulcano (Aeolian Islands, Italy) during the period 1984– 1994, Bull. Volcanol., 64, 219–228. Di Liberto, V., P. M. Nuccio, and A. Paonita (2002), Genesis of chlorine and sulphur in fumarolic emissions at Vulcano Island (Italy): Assessment of pH and redox conditions in the hydrothermal system, J. Volcanol. Geotherm. Res., 116, 137–150. Francis, P., M. R. Burton, and C. Oppenheimer (1998), Remote measurements of volcanic gas compositions by solar occultation spectroscopy, Nature, 396, 567–570. Galle, B., C. Oppenheimer, A. Geyer, A. J. S. McGonigle, M. Edmonds, and L. A. Horrocks (2003), A miniaturised ultraviolet spectrometer for remote sensing of SO2 fluxes: A new tool for volcano surveillance, J. Volcanol. Geotherm. Res., 119, 241–254. Giggenbach, W. F. (1975), A simple method for the collection and analysis of volcanic gas samples, Bull. Volcanol., 39, 132–145. Giggenbach,W. F., D. Tedesco, Y. Sulistiyo, A. Caprai, R. Cioni, R. Favara, and T. P. Fischer (2001), Evaluation of results from the fourth and fifth IAVCEI field workshops on volcanic gases, Vulcano island, Italy and Java, Indonesia, J. Volcanol. Geotherm. Res., 108, 157–172. Nuccio, P. M., A. Paonita, and F. Sortino (1999), Geochemical modeling of mixing between magmatic and hydrothermal gases: The case of Vulcano Island (Italy), Earth Planet. Sci. Lett., 167, 321–333. Stoiber, R. E., L. L. Malinconico, and S. N. Williams (1980), Use of the correlation spectrometer at volcanoes, in Forecasting Volcanic Events, edited by H. Tazieff and J.-C. Sabroux, pp. 425–444, Elsevier, New York. Symonds, R. B., W. I. Rose, G. J. S. Bluth, and T. M. Gerlach (1994), Volcanic-gas studies: Methods, results and applications, Rev. Mineral., 30, 1–66. Wallace, P. J. (2001), Volcanic SO2 emissions and the abundance and distribution of exsolved gas in magma bodies, J. Volcanol. Geotherm. Res., 108, 85–106.en
dc.description.fulltextpartially_openen
dc.contributor.authorAiuppa, A.en
dc.contributor.authorFederico, C.en
dc.contributor.authorGiudice, G.en
dc.contributor.authorGurrieri, S.en
dc.contributor.departmentDipartimento CFTA, Universita` di Palermo, Palermo, Italy.en
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.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, 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 Palermo, Palermo, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.orcid0000-0002-0254-6539-
crisitem.author.orcid0000-0001-8887-2580-
crisitem.author.orcid0000-0002-9410-4139-
crisitem.author.orcid0000-0003-4085-0440-
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.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-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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