dor_id: 4132428

506.#.#.a: Público

590.#.#.d: Los artículos enviados a la revista "Geofísica Internacional", se juzgan por medio de un proceso de revisión por pares

510.0.#.a: Consejo Nacional de Ciencia y Tecnología (CONACyT); Scientific Electronic Library Online (SciELO); SCOPUS, Dialnet, Directory of Open Access Journals (DOAJ); Geobase

561.#.#.u: https://www.geofisica.unam.mx/

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

336.#.#.b: article

336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

351.#.#.6: http://revistagi.geofisica.unam.mx/index.php/RGI

351.#.#.b: Geofísica Internacional

351.#.#.a: Artículos

harvesting_group: RevistasUNAM

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

590.#.#.c: Open Journal Systems (OJS)

270.#.#.d: MX

270.1.#.d: México

590.#.#.b: Concentrador

883.#.#.u: https://revistas.unam.mx/catalogo/

883.#.#.a: Revistas UNAM

590.#.#.a: Coordinación de Difusión Cultural

883.#.#.1: https://www.publicaciones.unam.mx/

883.#.#.q: Dirección General de Publicaciones y Fomento Editorial

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

856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/324/318

100.1.#.a: Tassi, F.; Capaccioni, B.; Capecchiacci, F.; Vaselli, O.

524.#.#.a: Tassi, F., et al. (2009). Non-methane Volatile Organic Compounds (VOCs) at El Chichón volcano (Chiapas, México): Geochemical features, origin and behavior. Geofísica Internacional; Vol. 48 Núm. 1: Enero 1, 2009; 85-95. Recuperado de https://repositorio.unam.mx/contenidos/4132428

245.1.0.a: Non-methane Volatile Organic Compounds (VOCs) at El Chichón volcano (Chiapas, México): Geochemical features, origin and behavior

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2009

264.#.1.c: 2009-01-01

653.#.#.a: VOC; El Chichón; fluidos termales; química orgánica; VOC; El Chichón volcano; thermal fluid; organic chemistry

506.1.#.a: La titularidad de los derechos patrimoniales de esta obra pertenece a las instituciones editoras. Su uso se rige por una licencia Creative Commons BY-NC-SA 4.0 Internacional, https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es, para un uso diferente consultar al responsable jurídico del repositorio por medio del correo electrónico revistagi@igeofisica.unam.mx

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/324

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/324

041.#.7.h: spa

520.3.#.a: Geochemical features of the organic gas fraction in fumarolic fluids at El Chichón volcano (Chiapas State, Mexico) are studied to investigate the origin of non-methane volatile organic compounds (VOCs) and the processes governing their behavior. VOCs from fumaroles and bubbling pools mainly consist of C2-C5 alkanes, with total abundance one order of magnitude less than that of methane, and relatively high concentrations of aromatics (benzene and toluene) and C2-C3 alkenes (mainly propene and iso-butene). Significant concentrations of S-bearing compounds, mostly of the heterocyclic group, are also detected. This composition is similar to that of gas emissions of geothermal systems. The production of organic gases at El Chichón may be due to thermogenic processes. Total VOC abundance is relatively low when compared with typical hydrothermal gas discharges, and may be attributed to magmatic-related fluids in the main reservoir feeding the thermal manifestations of the crater. As absence of O-bearing compounds seems to indicate that the hydrothermal fluids are not significantly affected by organic species produced at shallow depth by decomposing vegetation, such as that buried by the volcanic products of the 1982 eruption.doi: https://doi.org/10.22201/igeof.00167169p.2009.48.1.101

773.1.#.t: Geofísica Internacional; Vol. 48 Núm. 1: Enero 1, 2009; 85-95

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: 85-95

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

doi: https://doi.org/10.22201/igeof.00167169p.2009.48.1.101

handle: 00ffd2ec7cfc0034

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

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file_creation_date: 2009-01-21 15:47:22.0

file_modification_date: 2022-05-30 14:21:18.0

file_creator: Tassi F., Capaccioni B., Capecchiacci F., Vaselli O.

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245.1.0.b: Non-methane Volatile Organic Compounds (VOCs) at El Chichón volcano (Chiapas, México): Geochemical features, origin and behavior

last_modified: 2023-06-20 16:00:00

license_url: https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es

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Artículo

Non-methane Volatile Organic Compounds (VOCs) at El Chichón volcano (Chiapas, México): Geochemical features, origin and behavior

Tassi, F.; Capaccioni, B.; Capecchiacci, F.; Vaselli, O.

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

Tassi, F., et al. (2009). Non-methane Volatile Organic Compounds (VOCs) at El Chichón volcano (Chiapas, México): Geochemical features, origin and behavior. Geofísica Internacional; Vol. 48 Núm. 1: Enero 1, 2009; 85-95. Recuperado de https://repositorio.unam.mx/contenidos/4132428

Descripción del recurso

Autor(es)
Tassi, F.; Capaccioni, B.; Capecchiacci, F.; Vaselli, O.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Non-methane Volatile Organic Compounds (VOCs) at El Chichón volcano (Chiapas, México): Geochemical features, origin and behavior
Fecha
2009-01-01
Resumen
Geochemical features of the organic gas fraction in fumarolic fluids at El Chichón volcano (Chiapas State, Mexico) are studied to investigate the origin of non-methane volatile organic compounds (VOCs) and the processes governing their behavior. VOCs from fumaroles and bubbling pools mainly consist of C2-C5 alkanes, with total abundance one order of magnitude less than that of methane, and relatively high concentrations of aromatics (benzene and toluene) and C2-C3 alkenes (mainly propene and iso-butene). Significant concentrations of S-bearing compounds, mostly of the heterocyclic group, are also detected. This composition is similar to that of gas emissions of geothermal systems. The production of organic gases at El Chichón may be due to thermogenic processes. Total VOC abundance is relatively low when compared with typical hydrothermal gas discharges, and may be attributed to magmatic-related fluids in the main reservoir feeding the thermal manifestations of the crater. As absence of O-bearing compounds seems to indicate that the hydrothermal fluids are not significantly affected by organic species produced at shallow depth by decomposing vegetation, such as that buried by the volcanic products of the 1982 eruption.doi: https://doi.org/10.22201/igeof.00167169p.2009.48.1.101
Tema
VOC; El Chichón; fluidos termales; química orgánica; VOC; El Chichón volcano; thermal fluid; organic chemistry
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces