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
dor_id: 4132363
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336.#.#.b: article
336.#.#.3: Artículo de Investigación
336.#.#.a: Artículo
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351.#.#.b: Geofísica Internacional
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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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001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/859
041.#.7.h: spa
520.3.#.a: The chemical and isotopic compositions of CO2-rich water (Pco2 ≈ 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
310.#.#.a: Trimestral
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
856.#.0.q: application/pdf
file_creation_date: 2002-10-21 16:43:44.0
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
last_modified: 2023-06-20 16:00:00
license_url: https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es
license_type: by-nc-sa
Koh, Yongkwon; Kim, Chunsoo; Bae, Daeseok; Han, Kyeongwon
Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM
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