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http://hdl.handle.net/2122/7212
DC Field | Value | Language |
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dc.contributor.authorall | Caliro, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
dc.contributor.authorall | Chiodini, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
dc.contributor.authorall | Avino, R.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
dc.contributor.authorall | Minopoli, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
dc.contributor.authorall | Bocchino, B.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
dc.date.accessioned | 2011-11-29T14:58:18Z | en |
dc.date.available | 2011-11-29T14:58:18Z | en |
dc.date.issued | 2011 | en |
dc.identifier.uri | http://hdl.handle.net/2122/7212 | en |
dc.description.abstract | Long time-series of chemical and isotopic compositions of Vesuvius fumaroles were acquired in the framework of the volcanic surveillance in the 1998-2010 period. These allow the identification of processes that occur at shallow levels in the hydrothermal system, and variations that are induced by deep changes in volcanic activity. Partial condensation processes of fumarolic water under near-discharge conditions can explain the annual 18O and deuterium variabilities that are observed at Vesuvius fumaroles. Significant variations in the chemical compositions of fumaroles occurred over the 1999-2002 period, which accompanied the seismic crisis of autumn 1999, when Vesuvius was affected by the most energetic earthquakes of its last quiescence period. A continuous increase in the relative concentrations of CO2 and He and a general decrease in the CH4 concentrations are interpreted as the consequence of an increment in the relative amount of magmatic fluids in the hydrothermal system. Gas equilibria support this hypothesis, showing a PCO2 peak that culminated in 2002, increasing from values of ~40 bar in 1998 to ~55-60 bar in 2001- 2002. We propose that the seismic crisis of 1999 marked the arrival of the magmatic fluids into the hydrothermal system, which caused the observed geochemical variations that started in 1999 and culminated in 2002. | en |
dc.language.iso | English | en |
dc.publisher.name | Istituto Nazionale di Geofisica e Vulcanologia | en |
dc.relation.ispartof | Annals of Geophysics | en |
dc.relation.ispartofseries | 2/54(2011) | en |
dc.subject | Vesuvius | en |
dc.subject | Hydrothermal system | en |
dc.subject | Geochemical monitoring | en |
dc.subject | Stable isotopes. | en |
dc.title | Long time-series of chemical and isotopic compositions of Vesuvius fumaroles: evidence for deep and shallow processes | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.description.pagenumber | 137-149 | en |
dc.subject.INGV | 03. Hydrosphere::03.02. Hydrology::03.02.04. Measurements and monitoring | en |
dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.12. Fluid Geochemistry | en |
dc.subject.INGV | 04. Solid Earth::04.08. Volcanology::04.08.01. Gases | en |
dc.subject.INGV | 04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniques | en |
dc.identifier.doi | 10.4401/ag-5034 | en |
dc.relation.references | Aprile, F. and F. Ortolani (1979). Sulla struttura profonda della Piana Campana. Deep structure of the Campana Plain, Boll. Soc. Nat. Napoli, 88, 243-261. Arnò, V., C. Principe, M. Rosi, R. Santacroce, A. Sbrana and M.F. Sheridan (1987). Eruptive history, In: R. Santacroce (Editor), Somma Vesuvius, Quaderni de "La Ricerca Scientifica", CNR, Roma, 114-8, 53-103. Barberi, F., H. Bizouard, R. Clocchiatti, N. Metrich, R. Santacroce and A. Sbrana (1981). The Somma-Vesuvius magma chamber; a petrological and volcanological approach, Bull. Volcanol., 44, 295-315. Barberi, F. and L. Leoni (1980). Metamorphic carbonate ejecta from Vesuvius Plinian eruptions: evidence of the occurrence of shallow magma chambers, Bull. Volcanol., 43, 107-120. Berrino, G., G. Corrado and U. Riccardi (1998). Sea gravity data in the Gulf of Naples; a contribution to delineating the structural pattern of the Vesuvian area, J. Volcanol. Geotherm. Res., 82, 139-150. Caliro, S., G. Chiodini, R. Avino, C. Cardellini and F. Frondini (2005). Volcanic degassing at Somma-Vesuvio (Italy) inferred by chemical and isotopic signatures of LONG TIME-SERIES OF VESUVIUS FUMAROLES groundwater, Appl. Geochem., 20, 1060-1076. Caliro, S., C. Panichi and D. Stanzione (1998). Baseline study of the isotopic and chemical composition of waters associated with the Somma-Vesuvio volcanic system, Acta Vulcanol., 10, 19-25. Chiodini, G. (2009). CO2/CH4 ratio in fumaroles a powerful tool to detect magma degassing episodes at quiescent volcanoes, Geophys. Res. Lett., 36, L02302. Chiodini, G., P. Allard, S. Caliro and F. Parello (2000). 18O exchange between steam and carbon dioxide in volcanic and hydrothermal gases: implications for the source of water, Geochim. Cosmochim. Acta, 64, 2479-2488. 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., L. Marini and M. Russo (2001). Geochemical evidence for the existence of high-temperature hydrothermal brines at Vesuvio volcano, Italy, Geochim. Cosmochim. Acta, 65, 2129-2147. Cioni, R. and E. Corazza (1981). Medium-temperature fumarolic gas sampling, Bull. Volcanol., 44, 23-29. Cioni, R., R. Santacroce and A. Sbrana (1999). Pyroclastic deposits as a guide for reconstruction the multi-stage evolution of the Somma Vesuvius Caldera, Bull. Volcanol., 61, 207-222. Coleman, M.L., T.J. Shepherd, J.J. Durham, J.E. Rouse and G.R. Moore (1982). Reduction of water with zinc for hydrogen isotope analysis, Anal. Chem., 54, 993-995. Del Pezzo, E., F. Bianco and G. Saccorotti (2004). Seismic source dynamics at Vesuvius volcano, Italy, J. Volcanol. Geotherm. Res., 133, 23-39. Epstein, S. and T. Mayeda (1953). Variation of O-18 content of waters from natural sources, Geochim. Cosmochim. Acta, 4, 213-224. Federico, C., A. Aiuppa, P. Allard, S. Bellomo, P. Jean-Baptiste, F. Parello and M. Valenza (2002). Magma-derived gas influx and water-rock interactions in the volcanic aquifer of Mt. Vesuvius, Italy, Geochim. Cosmochim. Acta, 66, 963-981. Federico, C., A. Aiuppa, R. Favara, S. Gurrieri and M. Valenza (2004). Geochemical monitoring of groundwaters (1998- 2001) at Vesuvius volcano (Italy), J. Volcanol. Geotherm. Res., 133, 81-104; doi: 10.1016/S0377-0273(03)00392-5. Federico, C., G. Capasso, A. Paonita and R. Favara (2010). Effects of steam-heating processes on a stratified volcanic aquifer: stable isotopes and dissolved gases in thermal waters of Vulcano Island (Aeolian archipelago), J. Volcanol. Geotherm. Res., 192, 178-190; doi: 10.1016/ j.jvolgeores.2010.02.020. Fiebig, J., G. Chiodini, S. Caliro, A. Rizzo, J. Spangenberg and J.C. Hunziker (2004). Chemical and isotopic equilibrium between CO2 and CH4 in fumarolic gas discharges: generation of CH4 in arc magmatic-hydrothermal systems, Geochim. Cosmochim. Acta, 68, 2321-2334. Frondini, F., G. Chiodini, S. Caliro, C. Cardellini, D. Granieri and G. Ventura (2004). Diffuse CO2 degassing at Vesuvio, Italy, Bull. Volcanol., 66, 642-651. Giggenbach, W.F. (1975A simple method for the collection and analysis of volcanic gas samples, Bull.Volcanol., 39, 132-145. Giggenbach, W.F. (1987). Redox processes governing the chemistry of fumarolic gas discharges from White Island, New Zealand, Appl. Geochem., 2, 143-161. Giggenbach, W.F. and R.L. Goguel (1989) Collection and analysis of geothermal and volcanic water and gas discharges, Department of Scientific and Industrial Research Chemistry Division, Petone, New Zealand. Giggenbach, W.F. and S. Matsuo (1991). Evaluation of results from Second and Third IAVCEI field workshops on Volcanic gases, Mt. Usu, Japan, and White Island, New Zealand, Appl. Geochem., 6, 125-141. Giggenbach, W.F. and M.K. Stewart (1982). Processes controlling the isotopic composition of steam and water discharges from steam vents and steam-heated pools in geothermal areas, Geothermics, 11, 71. Giudicepietro, F., M. Orazi, G. Scarpato, R. Peluso, L. D'Auria, P. Ricciolino, D. Lo Bascio, A.M. Esposito, G. Borriello, M. Capello, A. Caputo, C. Buonocunto, W. De Cesare, G. Vilardo and M. Martini (2010). Seismological monitoring of Mount Vesuvius (Italy): more than a century of observations, Seism. Res. Lett., 81-4. Henley, R.W. and M.K. Stewart (1983). Chemical and isotopic changes in the hydrology of the Tauhara geothermal field due to exploitation at Wairakei., J. Volcanol. Geotherm. Res., 15, 285-314. Horita, J. and D.J. Wesolowski (1994). Liquid-vapor fractionation of oxygen and hydrogen isotopes of water from the freezing to the critical temperature, Geochim. Cosmochim. Acta, 58, 3425-3437. Iacono-Marziano, G., F. Gaillard, B. Scaillet, M. Pichavant and G. Chiodini (2009). Role of non-mantle CO2 in the dynamics of volcano degassing: the Mount Vesuvius example, Geology, 37, 319-322. Ippolito, F., F. Ortolani and M. Russo (1973). Struttura marginale tirrenica dell'Appennino Campano; reinterpretazione di dati di antiche ricerche di idrocarburi / The structure of the Tyrrhenian border of the Campania Apennines; reinterpretation of old data obtained during the hydrocarbon exploration program, Società Geologica Italiana, Rome, Italy. Joron, J.L., N. Metrich, M. Rosi, R. Santacroce and A. Sbrana (1987). Chemistry and petrography, In: R. Santacroce (Editor), Somma-Vesuvius, Quaderni de "La Ricerca Scientifica", CNR, Roma, 105-174. Madonia, P., C. Federico, P. Cusano, S. Petrosino, A. Aiuppa and S. Gurrieri (2008). Crustal dynamics of Mount Vesuvius from 1998 to 2005: Effects on seismicity and fluid circulation, J. Geophys. Res., 113, B05206; doi: 10.1029/ 2007JB005210. Pescatore, T.S. and I. Sgrosso (1973). I rapporti tra la piattaforma campano-lucana e la piattaforma abruzzese-campana nel casertano, Boll. Soc. Geol. It., 92, 925-938. Principe, C., D. Brocchini and M. Perillo (1999). The "Cognoli di Trocchia" volcano and Monte Somma growth, Plinius, 22, 316-317. Richet, P., Y. Bottinga and M. Javoy (1977). Review of hydrogen, carbon, nitrogen, oxygen, sulfur, and chlorine stable isotope fractionation among gaseous molecules, Ann. Rev. Earth Planet. Sci., 5, 65-110. Rosi, M., C. Principe and R. Vecci (1993). The 1631 Vesuvius eruption – a reconstruction based on historical and stratigraphical data, J. Volcanol. Geotherm. Res., 58, 151-182. Saccorotti, G., G. Ventura, G. Vilardo (2002). Seismic swarms related to diffusive processes; the case of Somma-Vesuvius Volcano, Italy, Geophysics, 67, 199-203. Santacroce, R. (1983). A general model for the behavior of the Somma-Vesuvius volcanic complex, J. Volcanol. Geotherm. Res., 17, 237-248. Ventura, G., G. Vilardo and P.P. Bruno (1999). The role of flank failure in modifying the shallow plumbing system of volcanoes: an example from Somma-Vesuvius, Italy, Geophys. Res. Lett., 26, 3681-3684. Zollo, A., W. Marzocchi, P. Capuano, A. Lomax and G. Iannaccone (2002). Space and time behavior of seismic activity at Mt. Vesuvius volcano, southern Italy, Bull. Seismol. Soc. Am., 92, 625-640. | en |
dc.description.obiettivoSpecifico | 1.2. TTC - Sorveglianza geochimica delle aree vulcaniche attive | en |
dc.description.obiettivoSpecifico | 2.4. TTC - Laboratori di geochimica dei fluidi | en |
dc.description.obiettivoSpecifico | 4.5. Studi sul degassamento naturale e sui gas petroliferi | en |
dc.description.journalType | JCR Journal | en |
dc.description.fulltext | open | en |
dc.contributor.author | Caliro, S. | en |
dc.contributor.author | Chiodini, G. | en |
dc.contributor.author | Avino, R. | en |
dc.contributor.author | Minopoli, C. | en |
dc.contributor.author | Bocchino, B. | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | open | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia | - |
crisitem.author.orcid | 0000-0002-8522-6695 | - |
crisitem.author.orcid | 0000-0002-0628-8055 | - |
crisitem.author.orcid | 0000-0003-2686-220X | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 03. Hydrosphere | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
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