Results of the CO2 diffuse degassing survey from the 2017 IAVCEI CCVG 13th volcanic gas workshop: Pululahua Dome Complex, Ecuador

Autores
Lamberti, María Clara Isabel; Sierra, D.; Cardellini, C.; Viveiros, F.; Vásconez Müller, A.; Vasconez, F. J.; Narváez, D. F.; Silva, C.; Melián, G.; Caliro, S.; Kis, B. M.; Ionescu, A.; Hidalgo, S.
Año de publicación
2024
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Pululahua is a potentially active andesite anddacite lava dome complex. This paper presents the results of a survey focusedon carbon dioxide (CO2) diffuse degassing at Pululahua, which wasconducted during the 2017 International Association of Volcanology andChemistry of the Earth´s Interior (IAVCEI) Commission of the Chemistry ofVolcanic Gases (CCVG) 13th Gas Workshop. Our objective was toconduct a comprehensive investigation of CO2 diffuse degassing byemploying standard methods for measuring CO2 flux and temperature,and data processing. These methods were applied to map the spatial distributionof the measured parameters, investigate the origin of CO2, andquantify the volcanic CO2 output within the surveyed area ofPululahua. We carried out a total of 350 soil CO2 flux and 329 soiltemperature measurements and collected 12 gas samples for carbon isotopiccomposition analysis, surrounding the three youngest domes in the complex. Inaddition, seventeen CO2 flux measurements over a thermal water poolwere performed. Our findings indicate that the diffuse emission at Pululahua´scrater floor is fed by both biogenic and volcanic CO2. Fluxes fromeach source are similar in magnitude, with approximately 90% of themeasurements falling into an intermediate flux range. The occurrence ofvolcanic CO2 emissions is supported by the carbon isotopiccomposition. Diffuse degassing distribution highlights a CO2 anomalysurrounding the younger domes within the crater. We estimated the CO2 diffuseemission using both statistical and geostatistical approaches over area of 3.36km2, resulting in values of 154.2 t d-1 and 126.2 t d-1respectively. Based on the geostatistical quantification of the total CO2emission from soil degassing, Pululahu´s crater volcanic CO2contribution is estimated between 59 and 97 t d-1. Finally, thepotential hazards associated with the release of cold CO2 atPululahua´s crater are also discussed.
Fil: Lamberti, María Clara Isabel. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina
Fil: Sierra, D.. Instituto Geofísico de la Escuela Politécnica Nacional; Ecuador
Fil: Cardellini, C.. Università di Perugia; Italia
Fil: Viveiros, F.. University of the Azores; Portugal
Fil: Vásconez Müller, A.. Instituto Geofísico de la Escuela Politécnica Nacional; Ecuador
Fil: Vasconez, F. J.. Instituto Geofísico de la Escuela Politécnica Nacional; Ecuador
Fil: Narváez, D. F.. Escuela Politécnica Nacional; Ecuador
Fil: Silva, C.. University Of The Azores; Portugal
Fil: Melián, G.. Instituto Tecnológico y de Energías Renovables; España
Fil: Caliro, S.. Istituto Nazionale di Geofisica e Vulcanologia; Italia
Fil: Kis, B. M.. Babeș -Bolyai University; Rumania
Fil: Ionescu, A.. Università di Perugia; Italia
Fil: Hidalgo, S.. Instituto Geofísico de la Escuela Politécnica Nacional; Ecuador
Materia
PULULAHUA_VOLCANO
CO2_DIFFUSE_DEGASSING
CO2_SOURCES
SOIL_TEMPERATURE
DIFFUSE_DEGASSING_MAP
CCVG_WORSHOP
Nivel de accesibilidad
acceso embargado
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/243436
Acceder
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oai_identifier_str oai:ri.conicet.gov.ar:11336/243436
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Results of the CO2 diffuse degassing survey from the 2017 IAVCEI CCVG 13th volcanic gas workshop: Pululahua Dome Complex, EcuadorLamberti, María Clara IsabelSierra, D.Cardellini, C.Viveiros, F.Vásconez Müller, A.Vasconez, F. J.Narváez, D. F.Silva, C.Melián, G.Caliro, S.Kis, B. M.Ionescu, A.Hidalgo, S.PULULAHUA_VOLCANOCO2_DIFFUSE_DEGASSINGCO2_SOURCESSOIL_TEMPERATUREDIFFUSE_DEGASSING_MAPCCVG_WORSHOPhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Pululahua is a potentially active andesite anddacite lava dome complex. This paper presents the results of a survey focusedon carbon dioxide (CO2) diffuse degassing at Pululahua, which wasconducted during the 2017 International Association of Volcanology andChemistry of the Earth´s Interior (IAVCEI) Commission of the Chemistry ofVolcanic Gases (CCVG) 13th Gas Workshop. Our objective was toconduct a comprehensive investigation of CO2 diffuse degassing byemploying standard methods for measuring CO2 flux and temperature,and data processing. These methods were applied to map the spatial distributionof the measured parameters, investigate the origin of CO2, andquantify the volcanic CO2 output within the surveyed area ofPululahua. We carried out a total of 350 soil CO2 flux and 329 soiltemperature measurements and collected 12 gas samples for carbon isotopiccomposition analysis, surrounding the three youngest domes in the complex. Inaddition, seventeen CO2 flux measurements over a thermal water poolwere performed. Our findings indicate that the diffuse emission at Pululahua´scrater floor is fed by both biogenic and volcanic CO2. Fluxes fromeach source are similar in magnitude, with approximately 90% of themeasurements falling into an intermediate flux range. The occurrence ofvolcanic CO2 emissions is supported by the carbon isotopiccomposition. Diffuse degassing distribution highlights a CO2 anomalysurrounding the younger domes within the crater. We estimated the CO2 diffuseemission using both statistical and geostatistical approaches over area of 3.36km2, resulting in values of 154.2 t d-1 and 126.2 t d-1respectively. Based on the geostatistical quantification of the total CO2emission from soil degassing, Pululahu´s crater volcanic CO2contribution is estimated between 59 and 97 t d-1. Finally, thepotential hazards associated with the release of cold CO2 atPululahua´s crater are also discussed.Fil: Lamberti, María Clara Isabel. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; ArgentinaFil: Sierra, D.. Instituto Geofísico de la Escuela Politécnica Nacional; EcuadorFil: Cardellini, C.. Università di Perugia; ItaliaFil: Viveiros, F.. University of the Azores; PortugalFil: Vásconez Müller, A.. Instituto Geofísico de la Escuela Politécnica Nacional; EcuadorFil: Vasconez, F. J.. Instituto Geofísico de la Escuela Politécnica Nacional; EcuadorFil: Narváez, D. F.. Escuela Politécnica Nacional; EcuadorFil: Silva, C.. University Of The Azores; PortugalFil: Melián, G.. Instituto Tecnológico y de Energías Renovables; EspañaFil: Caliro, S.. Istituto Nazionale di Geofisica e Vulcanologia; ItaliaFil: Kis, B. M.. Babeș -Bolyai University; RumaniaFil: Ionescu, A.. Università di Perugia; ItaliaFil: Hidalgo, S.. Instituto Geofísico de la Escuela Politécnica Nacional; EcuadorElsevier Science2024-07info:eu-repo/date/embargoEnd/2025-01-03info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/243436Lamberti, María Clara Isabel; Sierra, D.; Cardellini, C.; Viveiros, F.; Vásconez Müller, A.; et al.; Results of the CO2 diffuse degassing survey from the 2017 IAVCEI CCVG 13th volcanic gas workshop: Pululahua Dome Complex, Ecuador; Elsevier Science; Journal of Volcanology and Geothermal Research; 453; 7-2024; 1-430377-0273CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://linkinghub.elsevier.com/retrieve/pii/S0377027324001379info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jvolgeores.2024.108145info:eu-repo/semantics/embargoedAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:29:42Zoai:ri.conicet.gov.ar:11336/243436instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 10:29:43.097CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Results of the CO2 diffuse degassing survey from the 2017 IAVCEI CCVG 13th volcanic gas workshop: Pululahua Dome Complex, Ecuador
title Results of the CO2 diffuse degassing survey from the 2017 IAVCEI CCVG 13th volcanic gas workshop: Pululahua Dome Complex, Ecuador
spellingShingle Results of the CO2 diffuse degassing survey from the 2017 IAVCEI CCVG 13th volcanic gas workshop: Pululahua Dome Complex, Ecuador
Lamberti, María Clara Isabel
PULULAHUA_VOLCANO
CO2_DIFFUSE_DEGASSING
CO2_SOURCES
SOIL_TEMPERATURE
DIFFUSE_DEGASSING_MAP
CCVG_WORSHOP
title_short Results of the CO2 diffuse degassing survey from the 2017 IAVCEI CCVG 13th volcanic gas workshop: Pululahua Dome Complex, Ecuador
title_full Results of the CO2 diffuse degassing survey from the 2017 IAVCEI CCVG 13th volcanic gas workshop: Pululahua Dome Complex, Ecuador
title_fullStr Results of the CO2 diffuse degassing survey from the 2017 IAVCEI CCVG 13th volcanic gas workshop: Pululahua Dome Complex, Ecuador
title_full_unstemmed Results of the CO2 diffuse degassing survey from the 2017 IAVCEI CCVG 13th volcanic gas workshop: Pululahua Dome Complex, Ecuador
title_sort Results of the CO2 diffuse degassing survey from the 2017 IAVCEI CCVG 13th volcanic gas workshop: Pululahua Dome Complex, Ecuador
dc.creator.none.fl_str_mv Lamberti, María Clara Isabel
Sierra, D.
Cardellini, C.
Viveiros, F.
Vásconez Müller, A.
Vasconez, F. J.
Narváez, D. F.
Silva, C.
Melián, G.
Caliro, S.
Kis, B. M.
Ionescu, A.
Hidalgo, S.
author Lamberti, María Clara Isabel
author_facet Lamberti, María Clara Isabel
Sierra, D.
Cardellini, C.
Viveiros, F.
Vásconez Müller, A.
Vasconez, F. J.
Narváez, D. F.
Silva, C.
Melián, G.
Caliro, S.
Kis, B. M.
Ionescu, A.
Hidalgo, S.
author_role author
author2 Sierra, D.
Cardellini, C.
Viveiros, F.
Vásconez Müller, A.
Vasconez, F. J.
Narváez, D. F.
Silva, C.
Melián, G.
Caliro, S.
Kis, B. M.
Ionescu, A.
Hidalgo, S.
author2_role author
author
author
author
author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv PULULAHUA_VOLCANO
CO2_DIFFUSE_DEGASSING
CO2_SOURCES
SOIL_TEMPERATURE
DIFFUSE_DEGASSING_MAP
CCVG_WORSHOP
topic PULULAHUA_VOLCANO
CO2_DIFFUSE_DEGASSING
CO2_SOURCES
SOIL_TEMPERATURE
DIFFUSE_DEGASSING_MAP
CCVG_WORSHOP
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Pululahua is a potentially active andesite anddacite lava dome complex. This paper presents the results of a survey focusedon carbon dioxide (CO2) diffuse degassing at Pululahua, which wasconducted during the 2017 International Association of Volcanology andChemistry of the Earth´s Interior (IAVCEI) Commission of the Chemistry ofVolcanic Gases (CCVG) 13th Gas Workshop. Our objective was toconduct a comprehensive investigation of CO2 diffuse degassing byemploying standard methods for measuring CO2 flux and temperature,and data processing. These methods were applied to map the spatial distributionof the measured parameters, investigate the origin of CO2, andquantify the volcanic CO2 output within the surveyed area ofPululahua. We carried out a total of 350 soil CO2 flux and 329 soiltemperature measurements and collected 12 gas samples for carbon isotopiccomposition analysis, surrounding the three youngest domes in the complex. Inaddition, seventeen CO2 flux measurements over a thermal water poolwere performed. Our findings indicate that the diffuse emission at Pululahua´scrater floor is fed by both biogenic and volcanic CO2. Fluxes fromeach source are similar in magnitude, with approximately 90% of themeasurements falling into an intermediate flux range. The occurrence ofvolcanic CO2 emissions is supported by the carbon isotopiccomposition. Diffuse degassing distribution highlights a CO2 anomalysurrounding the younger domes within the crater. We estimated the CO2 diffuseemission using both statistical and geostatistical approaches over area of 3.36km2, resulting in values of 154.2 t d-1 and 126.2 t d-1respectively. Based on the geostatistical quantification of the total CO2emission from soil degassing, Pululahu´s crater volcanic CO2contribution is estimated between 59 and 97 t d-1. Finally, thepotential hazards associated with the release of cold CO2 atPululahua´s crater are also discussed.
Fil: Lamberti, María Clara Isabel. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina
Fil: Sierra, D.. Instituto Geofísico de la Escuela Politécnica Nacional; Ecuador
Fil: Cardellini, C.. Università di Perugia; Italia
Fil: Viveiros, F.. University of the Azores; Portugal
Fil: Vásconez Müller, A.. Instituto Geofísico de la Escuela Politécnica Nacional; Ecuador
Fil: Vasconez, F. J.. Instituto Geofísico de la Escuela Politécnica Nacional; Ecuador
Fil: Narváez, D. F.. Escuela Politécnica Nacional; Ecuador
Fil: Silva, C.. University Of The Azores; Portugal
Fil: Melián, G.. Instituto Tecnológico y de Energías Renovables; España
Fil: Caliro, S.. Istituto Nazionale di Geofisica e Vulcanologia; Italia
Fil: Kis, B. M.. Babeș -Bolyai University; Rumania
Fil: Ionescu, A.. Università di Perugia; Italia
Fil: Hidalgo, S.. Instituto Geofísico de la Escuela Politécnica Nacional; Ecuador
description Pululahua is a potentially active andesite anddacite lava dome complex. This paper presents the results of a survey focusedon carbon dioxide (CO2) diffuse degassing at Pululahua, which wasconducted during the 2017 International Association of Volcanology andChemistry of the Earth´s Interior (IAVCEI) Commission of the Chemistry ofVolcanic Gases (CCVG) 13th Gas Workshop. Our objective was toconduct a comprehensive investigation of CO2 diffuse degassing byemploying standard methods for measuring CO2 flux and temperature,and data processing. These methods were applied to map the spatial distributionof the measured parameters, investigate the origin of CO2, andquantify the volcanic CO2 output within the surveyed area ofPululahua. We carried out a total of 350 soil CO2 flux and 329 soiltemperature measurements and collected 12 gas samples for carbon isotopiccomposition analysis, surrounding the three youngest domes in the complex. Inaddition, seventeen CO2 flux measurements over a thermal water poolwere performed. Our findings indicate that the diffuse emission at Pululahua´scrater floor is fed by both biogenic and volcanic CO2. Fluxes fromeach source are similar in magnitude, with approximately 90% of themeasurements falling into an intermediate flux range. The occurrence ofvolcanic CO2 emissions is supported by the carbon isotopiccomposition. Diffuse degassing distribution highlights a CO2 anomalysurrounding the younger domes within the crater. We estimated the CO2 diffuseemission using both statistical and geostatistical approaches over area of 3.36km2, resulting in values of 154.2 t d-1 and 126.2 t d-1respectively. Based on the geostatistical quantification of the total CO2emission from soil degassing, Pululahu´s crater volcanic CO2contribution is estimated between 59 and 97 t d-1. Finally, thepotential hazards associated with the release of cold CO2 atPululahua´s crater are also discussed.
publishDate 2024
dc.date.none.fl_str_mv 2024-07
info:eu-repo/date/embargoEnd/2025-01-03
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/243436
Lamberti, María Clara Isabel; Sierra, D.; Cardellini, C.; Viveiros, F.; Vásconez Müller, A.; et al.; Results of the CO2 diffuse degassing survey from the 2017 IAVCEI CCVG 13th volcanic gas workshop: Pululahua Dome Complex, Ecuador; Elsevier Science; Journal of Volcanology and Geothermal Research; 453; 7-2024; 1-43
0377-0273
CONICET Digital
CONICET
url http://hdl.handle.net/11336/243436
identifier_str_mv Lamberti, María Clara Isabel; Sierra, D.; Cardellini, C.; Viveiros, F.; Vásconez Müller, A.; et al.; Results of the CO2 diffuse degassing survey from the 2017 IAVCEI CCVG 13th volcanic gas workshop: Pululahua Dome Complex, Ecuador; Elsevier Science; Journal of Volcanology and Geothermal Research; 453; 7-2024; 1-43
0377-0273
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://linkinghub.elsevier.com/retrieve/pii/S0377027324001379
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jvolgeores.2024.108145
dc.rights.none.fl_str_mv info:eu-repo/semantics/embargoedAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv embargoedAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Elsevier Science
publisher.none.fl_str_mv Elsevier Science
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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score 13.070432

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