CO2 flux from the volcanic lake of El Chichón (Mexico)

Carbon dioxide flux was measured in March 2007 at the surface of the volcanic lake of El Chichón volcano, Mexico using the floating accumulation chamber method. The results of 162 measurements and the application of a standard statistical approach developed for these studies showed that the total CO...

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Detalles Bibliográficos
Autores: Mazot, A., Taran, Y.
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2009
País:México
Institución:UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO
Repositorio:Geofísica Internacional
Idioma:español
inglés
OAI Identifier:oai:revistagi.geofisica.unam.mx:article/333
Acceso en línea:http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/333
Access Level:acceso abierto
Palabra clave:Flujo de CO2
cámara de acumulación
lagos cratéricos
El Chichón
CO2 flux
accumulation chamber
crater lakes
Descripción
Sumario:Carbon dioxide flux was measured in March 2007 at the surface of the volcanic lake of El Chichón volcano, Mexico using the floating accumulation chamber method. The results of 162 measurements and the application of a standard statistical approach developed for these studies showed that the total CO2 flux from the crater lake is relatively high. The total emission rate calculated by sequential Gaussian simulation was 164 ± 9.5 t.d-1 from the 138,000 m2 area of the lake. Two different mechanisms of degassing (diffusion through the water-air interface and bubbling) are well resolved by a graphical statistical approach (GSA). The highest fluxes were observed along inferred fault traces. Elevated degassing was also observed along main basement faults in the area. The average flux of CO2 over the entire crater floor of El Chichón (~ 308,000 m2) is inferred to exceed 370 t.d-1. Thus the total emission rate of CO2 from El Chichón crater is five times higher than at Kelud volcanic lake, Indonesia, but is similar to emission rates from other passively degassing active volcanoes worldwide.