dor_id: 4132787

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

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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

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

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270.#.#.d: MX

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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/785/777

100.1.#.a: Armienta, M. A.; Varley, N.; Ramos, E.

524.#.#.a: Armienta, M. A., et al. (2002). Radon and hydrogeochemical monitoring at Popocatépetl volcano, Mexico. Geofísica Internacional; Vol. 41 Núm. 3: Julio 1, 2002; 271-276. Recuperado de https://repositorio.unam.mx/contenidos/4132787

245.1.0.a: Radon and hydrogeochemical monitoring at Popocatépetl volcano, Mexico

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2002

264.#.1.c: 2002-07-01

653.#.#.a: Radón; Popocatépetl; monitoreo geoquímico; manantiales; suelos; Radon; Popocatépetl; geochemical monitoring; springs; soils

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/785

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041.#.7.h: spa

520.3.#.a: Measurements of radon in soil gas were carried out around Popocatépetl volcano during the period from September 1997 to April 1999. Soil gas was sampled using a stainless steel probe, and measured in the field with an alpha scintillation counter. At one location concentration variations of Rn in soil have been related with changes in the volcanic activity. In addition, chemical variations of spring waters at active volcanoes may be useful for volcano monitoring. In 1993 an increased period of volcanic activity began at Popocatépetl volcano. Since 1995, the chemical analyses of springs have been carried out as part of the surveil-lance of the volcanic activity. Conductivity, pH, and temperature were measured in the field. Concentration of the major ions: HCO -, Cl- , SO 2-, Mg2+, Na+, K+, Ca2+ have been determined in the laboratory by standard methods. The minor species boron, sulfide and fluoride were analyzed by colorimetry and potentiometry. Concentration increases of B, SO 2-, and Cl-, have been observed preceding some changes in volcanic activity during the studied period in some of the springs. Radon anomalies were found to approximately coincide with some of the chemical variations. The highest Rn levels at one location were measured during the period that preceded the eruption that occurred on December 24, 1997, which included the emission of relatively large tephra fragments.doi: https://doi.org/10.22201/igeof.00167169p.2002.41.3.342

773.1.#.t: Geofísica Internacional; Vol. 41 Núm. 3: Julio 1, 2002; 271-276

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: 271-276

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

doi: https://doi.org/10.22201/igeof.00167169p.2002.41.3.342

handle: 10f8743dfa109f19

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

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file_creation_date: 2002-08-02 11:32:40.0

file_modification_date: 2022-07-15 17:00:09.0

file_creator: M.A. Armienta

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245.1.0.b: Radon and hydrogeochemical monitoring at Popocatépetl volcano, Mexico

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

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Artículo

Radon and hydrogeochemical monitoring at Popocatépetl volcano, Mexico

Armienta, M. A.; Varley, N.; Ramos, E.

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

Armienta, M. A., et al. (2002). Radon and hydrogeochemical monitoring at Popocatépetl volcano, Mexico. Geofísica Internacional; Vol. 41 Núm. 3: Julio 1, 2002; 271-276. Recuperado de https://repositorio.unam.mx/contenidos/4132787

Descripción del recurso

Autor(es)
Armienta, M. A.; Varley, N.; Ramos, E.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Radon and hydrogeochemical monitoring at Popocatépetl volcano, Mexico
Fecha
2002-07-01
Resumen
Measurements of radon in soil gas were carried out around Popocatépetl volcano during the period from September 1997 to April 1999. Soil gas was sampled using a stainless steel probe, and measured in the field with an alpha scintillation counter. At one location concentration variations of Rn in soil have been related with changes in the volcanic activity. In addition, chemical variations of spring waters at active volcanoes may be useful for volcano monitoring. In 1993 an increased period of volcanic activity began at Popocatépetl volcano. Since 1995, the chemical analyses of springs have been carried out as part of the surveil-lance of the volcanic activity. Conductivity, pH, and temperature were measured in the field. Concentration of the major ions: HCO -, Cl- , SO 2-, Mg2+, Na+, K+, Ca2+ have been determined in the laboratory by standard methods. The minor species boron, sulfide and fluoride were analyzed by colorimetry and potentiometry. Concentration increases of B, SO 2-, and Cl-, have been observed preceding some changes in volcanic activity during the studied period in some of the springs. Radon anomalies were found to approximately coincide with some of the chemical variations. The highest Rn levels at one location were measured during the period that preceded the eruption that occurred on December 24, 1997, which included the emission of relatively large tephra fragments.doi: https://doi.org/10.22201/igeof.00167169p.2002.41.3.342
Tema
Radón; Popocatépetl; monitoreo geoquímico; manantiales; suelos; Radon; Popocatépetl; geochemical monitoring; springs; soils
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces