Modelación geoquímica de los fluidos del sistema periférico del Volcán Stromboli y su relación con la actividad volcánica reciente
ilustraciones, gráficas, tablas
- Autores:
-
Copete Murillo, Iliana Karen
- Tipo de recurso:
- Fecha de publicación:
- 2021
- Institución:
- Universidad Nacional de Colombia
- Repositorio:
- Universidad Nacional de Colombia
- Idioma:
- spa
- OAI Identifier:
- oai:repositorio.unal.edu.co:unal/80951
- Palabra clave:
- 550 - Ciencias de la tierra::551 - Geología, hidrología, meteorología
Seismic zones
Intrusions (Geology)
Geology, structural
Zonas de actividad sísmica
Intrusiones (Geología)
Geotecnia
Stromboli
Acuífero termal
Mezclas
Gases disueltos
Isótopos
Intrusión marina
Stromboli
Thermal aquifer
Mixtures
Dissolved gases
Isotopes
Marine intrusion
- Rights
- openAccess
- License
- Atribución-NoComercial-SinDerivadas 4.0 Internacional
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dc.title.spa.fl_str_mv |
Modelación geoquímica de los fluidos del sistema periférico del Volcán Stromboli y su relación con la actividad volcánica reciente |
dc.title.translated.eng.fl_str_mv |
Geochemical modeling of the fluids of the peripheral system of the Stromboli Volcano and its relationship with recent volcanic activity |
title |
Modelación geoquímica de los fluidos del sistema periférico del Volcán Stromboli y su relación con la actividad volcánica reciente |
spellingShingle |
Modelación geoquímica de los fluidos del sistema periférico del Volcán Stromboli y su relación con la actividad volcánica reciente 550 - Ciencias de la tierra::551 - Geología, hidrología, meteorología Seismic zones Intrusions (Geology) Geology, structural Zonas de actividad sísmica Intrusiones (Geología) Geotecnia Stromboli Acuífero termal Mezclas Gases disueltos Isótopos Intrusión marina Stromboli Thermal aquifer Mixtures Dissolved gases Isotopes Marine intrusion |
title_short |
Modelación geoquímica de los fluidos del sistema periférico del Volcán Stromboli y su relación con la actividad volcánica reciente |
title_full |
Modelación geoquímica de los fluidos del sistema periférico del Volcán Stromboli y su relación con la actividad volcánica reciente |
title_fullStr |
Modelación geoquímica de los fluidos del sistema periférico del Volcán Stromboli y su relación con la actividad volcánica reciente |
title_full_unstemmed |
Modelación geoquímica de los fluidos del sistema periférico del Volcán Stromboli y su relación con la actividad volcánica reciente |
title_sort |
Modelación geoquímica de los fluidos del sistema periférico del Volcán Stromboli y su relación con la actividad volcánica reciente |
dc.creator.fl_str_mv |
Copete Murillo, Iliana Karen |
dc.contributor.advisor.spa.fl_str_mv |
Inguaggiato, Salvatore Cadena Sánchez, Ariel Oswaldo |
dc.contributor.author.spa.fl_str_mv |
Copete Murillo, Iliana Karen |
dc.subject.ddc.spa.fl_str_mv |
550 - Ciencias de la tierra::551 - Geología, hidrología, meteorología |
topic |
550 - Ciencias de la tierra::551 - Geología, hidrología, meteorología Seismic zones Intrusions (Geology) Geology, structural Zonas de actividad sísmica Intrusiones (Geología) Geotecnia Stromboli Acuífero termal Mezclas Gases disueltos Isótopos Intrusión marina Stromboli Thermal aquifer Mixtures Dissolved gases Isotopes Marine intrusion |
dc.subject.lemb.eng.fl_str_mv |
Seismic zones Intrusions (Geology) Geology, structural |
dc.subject.lemb.spa.fl_str_mv |
Zonas de actividad sísmica Intrusiones (Geología) Geotecnia |
dc.subject.proposal.spa.fl_str_mv |
Stromboli Acuífero termal Mezclas Gases disueltos Isótopos Intrusión marina |
dc.subject.proposal.ita.fl_str_mv |
Stromboli |
dc.subject.proposal.eng.fl_str_mv |
Thermal aquifer Mixtures Dissolved gases Isotopes Marine intrusion |
description |
ilustraciones, gráficas, tablas |
publishDate |
2021 |
dc.date.issued.none.fl_str_mv |
2021 |
dc.date.accessioned.none.fl_str_mv |
2022-02-11T18:57:05Z |
dc.date.available.none.fl_str_mv |
2022-02-11T18:57:05Z |
dc.type.spa.fl_str_mv |
Trabajo de grado - Maestría |
dc.type.driver.spa.fl_str_mv |
info:eu-repo/semantics/masterThesis |
dc.type.version.spa.fl_str_mv |
info:eu-repo/semantics/acceptedVersion |
dc.type.content.spa.fl_str_mv |
Text Workflow |
dc.type.redcol.spa.fl_str_mv |
http://purl.org/redcol/resource_type/TM |
status_str |
acceptedVersion |
dc.identifier.uri.none.fl_str_mv |
https://repositorio.unal.edu.co/handle/unal/80951 |
dc.identifier.instname.spa.fl_str_mv |
Universidad Nacional de Colombia |
dc.identifier.reponame.spa.fl_str_mv |
Repositorio Institucional Universidad Nacional de Colombia |
dc.identifier.repourl.spa.fl_str_mv |
https://repositorio.unal.edu.co/ |
url |
https://repositorio.unal.edu.co/handle/unal/80951 https://repositorio.unal.edu.co/ |
identifier_str_mv |
Universidad Nacional de Colombia Repositorio Institucional Universidad Nacional de Colombia |
dc.language.iso.spa.fl_str_mv |
spa |
language |
spa |
dc.relation.references.spa.fl_str_mv |
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Sonney, R., & Vuataz, F. D. (2010). Validation of chemical and isotopic geothermometers from low temperature deep fluids of northern Switzerland. In Proceedings World Geothermal Congress (Vol. 14, No. 1423, pp. 1-12). International Geothermal Association. Spycher, N., Peiffer, L., Sonnenthal, E. L., Saldi, G., Reed, M. H., & Kennedy, B. M. (2014). Integrated multicomponent solute geothermometry. Geothermics, 51, 113-123. Standard Methods (1992) Standard Methods for the Examinatiul1 of Water (lftd We slewater 18th edn.) American Public Health Association. Tamburello, 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. Tibaldi, 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. Vaselli, 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. Verma, M. P. (2008). Qrtzgeotherm: An ActiveX component for the quartz solubility geothermometer. Computers & Geosciences, 34(12), 1918-1925 Vita, 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. |
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xv, 124 páginas |
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Universidad Nacional de Colombia |
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Bogotá - Ciencias - Maestría en Ciencias - Geología |
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Departamento de Geociencias |
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Facultad de Ciencias |
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Bogotá, Colombia |
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Universidad Nacional de Colombia - Sede Bogotá |
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Universidad Nacional de Colombia |
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Atribución-NoComercial-SinDerivadas 4.0 Internacionalhttp://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Inguaggiato, Salvatore3ef24cbea2271d30a696971f97af1942600Cadena Sánchez, Ariel Oswaldode54fb890339f88a3a84902a66d86c76600Copete Murillo, Iliana Karen175f60656150f722d1486edca3708a102022-02-11T18:57:05Z2022-02-11T18:57:05Z2021https://repositorio.unal.edu.co/handle/unal/80951Universidad Nacional de ColombiaRepositorio Institucional Universidad Nacional de Colombiahttps://repositorio.unal.edu.co/ilustraciones, gráficas, tablasEl 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).Geochemical 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.El 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 .MaestríaMagíster en Ciencias - Geologíaxv, 124 páginasapplication/pdfspaUniversidad Nacional de ColombiaBogotá - Ciencias - Maestría en Ciencias - GeologíaDepartamento de GeocienciasFacultad de CienciasBogotá, ColombiaUniversidad Nacional de Colombia - Sede Bogotá550 - Ciencias de la tierra::551 - Geología, hidrología, meteorologíaSeismic zonesIntrusions (Geology)Geology, structuralZonas de actividad sísmicaIntrusiones (Geología)GeotecniaStromboliAcuífero termalMezclasGases disueltosIsótoposIntrusión marinaStromboliThermal aquiferMixturesDissolved gasesIsotopesMarine intrusionModelación geoquímica de los fluidos del sistema periférico del Volcán Stromboli y su relación con la actividad volcánica recienteGeochemical modeling of the fluids of the peripheral system of the Stromboli Volcano and its relationship with recent volcanic activityTrabajo de grado - Maestríainfo:eu-repo/semantics/masterThesisinfo:eu-repo/semantics/acceptedVersionTextWorkflowhttp://purl.org/redcol/resource_type/TMAiuppa, A., Moretti, R., Federico, C., Giudice, G., Gurrieri, S., Liuzzo, M., ... & Valenza, M. 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Geophys. 55, 301–308.Istituto Nazionale di Geofisica e Vulcanologia (INGV) ,ItaliaEstudiantesInvestigadoresMaestrosORIGINAL35852447.2021 .pdf35852447.2021 .pdfTesis de Maestría en Ciencias - Geologíaapplication/pdf14139119https://repositorio.unal.edu.co/bitstream/unal/80951/1/35852447.2021%20.pdfb37113b2611a66ab9a10c9353f5466c1MD51LICENSElicense.txtlicense.txttext/plain; charset=utf-84074https://repositorio.unal.edu.co/bitstream/unal/80951/2/license.txt8153f7789df02f0a4c9e079953658ab2MD52THUMBNAIL35852447.2021 .pdf.jpg35852447.2021 .pdf.jpgGenerated Thumbnailimage/jpeg5283https://repositorio.unal.edu.co/bitstream/unal/80951/3/35852447.2021%20.pdf.jpg71d5c022fee6c7898a4850bdba88438bMD53unal/80951oai:repositorio.unal.edu.co:unal/809512023-08-01 23:03:44.157Repositorio Institucional Universidad Nacional de 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