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650.#.4.x: Físico Matemáticas y Ciencias de la Tierra

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336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

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351.#.#.b: Geofísica Internacional

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270.1.#.p: Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

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850.#.#.a: Universidad Nacional Autónoma de México

856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/859/815

100.1.#.a: Koh, Yongkwon; Kim, Chunsoo; Bae, Daeseok; Han, Kyeongwon

524.#.#.a: Koh, Yongkwon, et al. (2002). The isotopic and chemical compositions of the CO. Geofísica Internacional; Vol. 41 Núm. 4: Octubre 1, 2002; 491-498. Recuperado de https://repositorio.unam.mx/contenidos/4132363

245.1.0.a: The isotopic and chemical compositions of the CO

502.#.#.c: Universidad Nacional Autónoma de México

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2002

264.#.1.c: 2002-10-01

653.#.#.a: Aguas ricas en CO2; química; isotopía; interacción agua-roca; mezcla; geotermometría; CO2-rich water; chemistry; isotope; water/rock interaction; mixing; geothermometry

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041.#.7.h: spa

520.3.#.a: The chemical and isotopic compositions of CO2-rich water (Pco2 â‰ˆ 1 atm) in Korea mainly occurring in granitic terrain were investigated. CO2-rich waters can be divided into three types based on chemical compositions: Na-HCO3, Ca-Na-HCO3 and Ca-HCO3 types. Water chemistry indicates that these waters were evolved through a strong reaction of the host rocks with a supply of deep-seated CO2 during deep circulation. The dissolution process of plagioclase is important in water/granite interactions and its solubility changes with reaction temperature played an important role in the determination of chemical composition. Multi-com-ponent mineral/water equilibrium calculations indicate that the CO2-rich water reaches temperature of 115-140°C.δ18O and δD data indicate that CO2-rich waters were derived from local meteoric water and have a lighter isotope composition than other natural waters. The tritium contents show a long residence time and the possibility of CO2 flux in an aquifer at great depth. There is a strong indication of mixing between deep CO2-rich water and recent fresh water during ascent to the surface. Carbon isotope analysis reveals that the carbon composition is associated with mantle-derived CO2. The preliminary helium isotope ratio also supports that the CO2 gas was derived from mantle origin. The strontium isotope ratios indicate that the chemistry of the CO2-rich water is determined by reaction with local granite.doi: https://doi.org/10.22201/igeof.00167169p.2002.41.4.500

773.1.#.t: Geofísica Internacional; Vol. 41 Núm. 4: Octubre 1, 2002; 491-498

773.1.#.o: http://revistagi.geofisica.unam.mx/index.php/RGI

022.#.#.a: ISSN-L: 2954-436X; ISSN impreso: 0016-7169

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300.#.#.a: Páginas: 491-498

264.#.1.b: Instituto de Geofísica, UNAM

doi: https://doi.org/10.22201/igeof.00167169p.2002.41.4.500

handle: 009f2f8aaf9e6a75

harvesting_date: 2023-06-20 16:00:00.0

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file_modification_date: 2022-07-18 16:34:26.0

file_creator: Yongkwon Koh

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245.1.0.b: The isotopic and chemical compositions of the CO2-rich waters in Korea

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Artículo

The isotopic and chemical compositions of the CO

Koh, Yongkwon; Kim, Chunsoo; Bae, Daeseok; Han, Kyeongwon

Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM

Licencia de uso

Procedencia del contenido

Entidad o dependencia
Instituto de Geofísica, UNAM
Revista
Repositorio
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

Koh, Yongkwon, et al. (2002). The isotopic and chemical compositions of the CO. Geofísica Internacional; Vol. 41 Núm. 4: Octubre 1, 2002; 491-498. Recuperado de https://repositorio.unam.mx/contenidos/4132363

Descripción del recurso

Autor(es)
Koh, Yongkwon; Kim, Chunsoo; Bae, Daeseok; Han, Kyeongwon
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
The isotopic and chemical compositions of the CO
Fecha
2002-10-01
Resumen
The chemical and isotopic compositions of CO2-rich water (Pco2 â‰ˆ 1 atm) in Korea mainly occurring in granitic terrain were investigated. CO2-rich waters can be divided into three types based on chemical compositions: Na-HCO3, Ca-Na-HCO3 and Ca-HCO3 types. Water chemistry indicates that these waters were evolved through a strong reaction of the host rocks with a supply of deep-seated CO2 during deep circulation. The dissolution process of plagioclase is important in water/granite interactions and its solubility changes with reaction temperature played an important role in the determination of chemical composition. Multi-com-ponent mineral/water equilibrium calculations indicate that the CO2-rich water reaches temperature of 115-140°C.δ18O and δD data indicate that CO2-rich waters were derived from local meteoric water and have a lighter isotope composition than other natural waters. The tritium contents show a long residence time and the possibility of CO2 flux in an aquifer at great depth. There is a strong indication of mixing between deep CO2-rich water and recent fresh water during ascent to the surface. Carbon isotope analysis reveals that the carbon composition is associated with mantle-derived CO2. The preliminary helium isotope ratio also supports that the CO2 gas was derived from mantle origin. The strontium isotope ratios indicate that the chemistry of the CO2-rich water is determined by reaction with local granite.doi: https://doi.org/10.22201/igeof.00167169p.2002.41.4.500
Tema
Aguas ricas en CO2; química; isotopía; interacción agua-roca; mezcla; geotermometría; CO2-rich water; chemistry; isotope; water/rock interaction; mixing; geothermometry
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces