Modelación geoquímica de los fluidos del sistema periférico del Volcán Stromboli y su relación con la actividad volcánica reciente

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dc.contributor.advisorInguaggiato, Salvatorespa
dc.contributor.advisorCadena Sánchez, Ariel Oswaldospa
dc.contributor.authorCopete Murillo, Iliana Karenspa
dc.date.accessioned2022-02-11T18:57:05Z
dc.date.available2022-02-11T18:57:05Z
dc.date.issued2021
dc.descriptionilustraciones, gráficas, tablasspa
dc.description.abstractEl área periférica de la isla de Stromboli cuenta con distintos ambientes naturales idóneos para la evaluación y monitoreo del sistema volcánico activo; en este caso el agua del acuífero termal se caracteriza por presentar temperaturas hasta de 50°C y altas concentraciones de CO2 disuelto como resultado de desgasificación del magma. Estos aspectos permitieron modelar el sistema hidrotermal, evaluar la composición química y la temperatura del sistema geotérmico que alimenta los fluidos superficiales a partir de pozos termales localizados sobre el acuifero. El sistema hidrotermal en general es una mezcla de agua de mar y agua geotérmica en diferentes porcentajes. El estudio de la composición química e isotópica de las aguas de los pozos ha permitido estimar los diferentes porcentajes de mezcla, la temperatura del sistema geotérmico en profundidad y evaluar la interaccion del agua del acuífero con las rocas del reservorio. La temperatura del sistema geotérmico es alrededor de 180°C ±10°C y la composición química de los iones mayores es gobernada por agua de mar modificada con porcentajes de Cl- de 150 meq/l aproximadamente y con altos contenidos de K+ y de HCO3- entre (8 y 13 meq/l respectivamente), debido a procesos de interacción agua/roca y disolución de CO2 en el agua termal. (Texto tomado de la fuente).spa
dc.description.abstractGeochemical modeling of the fluids of the peripheral system of the Stromboli Volcano and its relationship with recent volcanic activity The peripheral area of the island of Stromboli has different natural environments suitable for the evaluation and monitoring of the active volcanic system, in this case the thermal aquifer is characterized by presenting wells that capture water with temperatures up to 50°C and high concentrations of CO2 dissolved as a result of magma degassing. These aspects allowed modeling the hydrothermal system and evaluating the chemical composition and temperature of the geothermal system that feeds the surface fluids. The hydrothermal system in general is a mixture of seawater and geothermal water in different percentages. The study of the chemical and isotopic composition of the water from the wells has made it possible to estimate the different percentages and the temperature of the deep geothermal system, characterizing and evaluating the seawater modified by interaction with the rocks of the reservoir. The temperature of the deep geothermal system is around 180°C ±10°C and the chemical composition of the major ions is governed by modified seawater with Cl- percentages of approximately 150 meq/l and with high K+ and HCO3- contents, (between 8 and 13 meq/l respectively), due to water/rock interaction processes and dissolution of CO2 in the thermal water.eng
dc.description.degreelevelMaestríaspa
dc.description.degreenameMagíster en Ciencias - Geologíaspa
dc.description.sponsorshipEl Istituto Nazionale di Geofisica e Vulcanologia (INGV) ,es una de las mayores instituciones europeas de investigación en el campo de las ciencias de la Tierra. Es responsable del estudio de los fenómenos geofísicos y vulcanológicos y de la gestión de las respectivas redes nacionales de monitoreo de fenómenos sísmicos y volcánicos .spa
dc.format.extentxv, 124 páginasspa
dc.format.mimetypeapplication/pdfspa
dc.identifier.instnameUniversidad Nacional de Colombiaspa
dc.identifier.reponameRepositorio Institucional Universidad Nacional de Colombiaspa
dc.identifier.repourlhttps://repositorio.unal.edu.co/spa
dc.identifier.urihttps://repositorio.unal.edu.co/handle/unal/80951
dc.language.isospaspa
dc.publisherUniversidad Nacional de Colombiaspa
dc.publisher.branchUniversidad Nacional de Colombia - Sede Bogotáspa
dc.publisher.departmentDepartamento de Geocienciasspa
dc.publisher.facultyFacultad de Cienciasspa
dc.publisher.placeBogotá, Colombiaspa
dc.publisher.programBogotá - Ciencias - Maestría en Ciencias - Geologíaspa
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dc.relation.referencesTamburello, G., Aiuppa, A., Kantzas, E. P., McGonigle, A. J. S., & Ripepe, M. (2012). Passive vs. active degassing modes at an open-vent volcano (Stromboli, Italy). Earth and Planetary Science Letters, 359, 106-116.spa
dc.relation.referencesTibaldi, A. (2010). A new geological map of Stromboli volcano (Tyrrhenian Sea, Italy) based on application of lithostratigraphic and unconformity-bounded stratigraphic (UBS) units. GSA Spec. Pap, 464, 33-49.spa
dc.relation.referencesVaselli, O., Tassi, F., Duarte, E., Fernandez, E., Poreda, R. J., & Huertas, A. D. (2010). Evolution of fluid geochemistry at the Turrialba volcano (Costa Rica) from 1998 to 2008. Bulletin of Volcanology, 72(4), 397-410.spa
dc.relation.referencesVerma, M. P. (2008). Qrtzgeotherm: An ActiveX component for the quartz solubility geothermometer. Computers & Geosciences, 34(12), 1918-1925spa
dc.relation.referencesVita, F., Inguaggiato, S., Bobrowski, N., Calderone, L., Galle, B., Parello, F., 2012. Continuous SO2 flux measurements at Vulcano Island, Italy. Ann. Geophys. 55, 301–308.spa
dc.rights.accessrightsinfo:eu-repo/semantics/openAccessspa
dc.rights.licenseAtribución-NoComercial-SinDerivadas 4.0 Internacionalspa
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/spa
dc.subject.ddc550 - Ciencias de la tierra::551 - Geología, hidrología, meteorologíaspa
dc.subject.lembSeismic zoneseng
dc.subject.lembZonas de actividad sísmicaspa
dc.subject.lembIntrusions (Geology)eng
dc.subject.lembIntrusiones (Geología)spa
dc.subject.lembGeology, structuraleng
dc.subject.lembGeotecniaspa
dc.subject.proposalStrombolispa
dc.subject.proposalStromboliita
dc.subject.proposalAcuífero termalspa
dc.subject.proposalMezclasspa
dc.subject.proposalGases disueltosspa
dc.subject.proposalIsótoposspa
dc.subject.proposalIntrusión marinaspa
dc.subject.proposalThermal aquifereng
dc.subject.proposalMixtureseng
dc.subject.proposalDissolved gaseseng
dc.subject.proposalIsotopeseng
dc.subject.proposalMarine intrusioneng
dc.titleModelación geoquímica de los fluidos del sistema periférico del Volcán Stromboli y su relación con la actividad volcánica recientespa
dc.title.translatedGeochemical modeling of the fluids of the peripheral system of the Stromboli Volcano and its relationship with recent volcanic activityeng
dc.typeTrabajo de grado - Maestríaspa
dc.type.coarhttp://purl.org/coar/resource_type/c_bdccspa
dc.type.coarversionhttp://purl.org/coar/version/c_ab4af688f83e57aaspa
dc.type.contentTextspa
dc.type.contentWorkflowspa
dc.type.driverinfo:eu-repo/semantics/masterThesisspa
dc.type.redcolhttp://purl.org/redcol/resource_type/TMspa
dc.type.versioninfo:eu-repo/semantics/acceptedVersionspa
dcterms.audience.professionaldevelopmentEstudiantesspa
dcterms.audience.professionaldevelopmentInvestigadoresspa
dcterms.audience.professionaldevelopmentMaestrosspa
oaire.accessrightshttp://purl.org/coar/access_right/c_abf2spa
oaire.fundernameIstituto Nazionale di Geofisica e Vulcanologia (INGV) ,Italiaspa

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