Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4547
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dc.contributor.authorallTaran, Y.; Instituto de Geofísica, Universidad Nacional Autónoma de México, 04510, Méxicoen
dc.contributor.authorallRouwet, D.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.date.accessioned2008-12-09T15:11:48Zen
dc.date.available2008-12-09T15:11:48Zen
dc.date.issued2008-04-16en
dc.identifier.urihttp://hdl.handle.net/2122/4547en
dc.description.abstractEl Chichón crater lake appeared immediately after the 1982 catastrophic eruption in a newly formed, 1-km wide, explosive crater. During the first 2 years after the eruption the lake transformed from hot and ultraacidic caused by dissolution of magmatic gases, to a warm and less acidic lake due to a rapid “magmatic-tohydrothermal transition” — input of hydrothermal fluids and oxidation of H2S to sulfate. Chemical composition of the lake water and other thermal fluids discharging in the crater, stable isotope composition (δD and δ18O) of lake water, gas condensates and thermal waters collected in 1995–2006 were used for the mass-balance calculations (Cl, SO4 and isotopic composition) of the thermal flux from the crater floor. The calculated fluxes of thermal fluid by different mass-balance approaches become of the same order of magnitude as those derived from the energy-budget model if values of 1.9 and 2 mmol/mol are taken for the catchment coefficient and the average H2S concentration in the hydrothermal vapors, respectively. The total heat power from the crater is estimated to be between 35 and 60 MW and the CO2 flux is not higher than 150 t/day or ~200 gm−2 day−1.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofJournal of Volcanology and Geothermal Researchen
dc.relation.ispartofseries4/175(2008)en
dc.subjectEl Chichónen
dc.subjectcrater lakeen
dc.subjectmass-energy budgeten
dc.subjectCO2 fluxen
dc.titleEstimating thermal inflow to El Chichón crater lake using the energy-budget, chemical and isotope balance approachesen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber472-481en
dc.identifier.URLhttp://www.elsevier.com/wps/find/homepage.cws_homeen
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.12. Fluid Geochemistryen
dc.subject.INGV05. General::05.02. Data dissemination::05.02.01. Geochemical dataen
dc.subject.INGV05. General::05.02. Data dissemination::05.02.04. Hydrogeological dataen
dc.identifier.doi10.1016/j.jvolgeores.2008.02.019en
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dc.description.obiettivoSpecifico1.2. TTC - Sorveglianza geochimica delle aree vulcaniche attiveen
dc.description.obiettivoSpecifico2.4. TTC - Laboratori di geochimica dei fluidien
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorTaran, Y.en
dc.contributor.authorRouwet, D.en
dc.contributor.departmentInstituto de Geofísica, Universidad Nacional Autónoma de México, 04510, Méxicoen
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.deptInstitute of Geophysics, Universidad Nacional Autonoma de Mexico, Ciudad Universitario, Del. Coyocan, 04510 Mexico, DF, Mexico-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.orcid0000-0003-3390-4316-
crisitem.author.orcid0000-0003-3366-3882-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent05. General-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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