Spring water and CO2 interaction at Popocatépetl volcano, Mexico

Six years of monitoring HCO3- and pH at selected springs at Popocatépetl during the present eruptive period are presented.Small peaks in HCO3- concentration and PCO2 in springs are associated with small magmatic pulses at Popocatépetl volcano. Themagma provides CO2-rich fluids into the water system...

Descripción completa

Detalles Bibliográficos
Autores: A. L. Martin Del Pozzo, S. Inguaggiato, F. Aceves, H. Saenz, A. Aguayo
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2002
País:México
Institución:Universidad Nacional Autónoma de México
Repositorio:Redalyc-UNAM
OAI Identifier:oai:redalyc.org:56841323
Acceso en línea:https://www.redalyc.org/articulo.oa?id=56841323
Access Level:acceso abierto
Palabra clave:Ciencias de la Tierra
Spring Water
CO2 interaction
Popocatépetl volcano
id MX_0bab710a7678e1163efcecdcbfa4fca3
oai_identifier_str oai:redalyc.org:56841323
network_acronym_str MX
network_name_str México
repository_id_str
spelling Spring water and CO2 interaction at Popocatépetl volcano, MexicoA. L. Martin Del PozzoS. InguaggiatoF. AcevesH. SaenzA. AguayoCiencias de la TierraSpring WaterCO2 interactionPopocatépetl volcanoSix years of monitoring HCO3- and pH at selected springs at Popocatépetl during the present eruptive period are presented.Small peaks in HCO3- concentration and PCO2 in springs are associated with small magmatic pulses at Popocatépetl volcano. Themagma provides CO2-rich fluids into the water system controlled by meteoric recharge. The PCO2 in equilibrium with the springsis two to four orders of magnitude higher than air-saturated water. The high partial pressure of CO2 also suggests a direct interactionwith the magmatic fluids. The isotopic signature of carbon as well, supports a magmatic origin for dissolved CO2.Universidad Nacional Autónoma de México2002info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdf0016-7169https://www.redalyc.org/articulo.oa?id=56841323Geofísica Internacional (México) Num.3 Vol.41reponame:Redalyc-UNAMinstname:Universidad Nacional Autónoma de Méxicoinstacron:UNAMenhttp://www.redalyc.org/revista.oa?id=568Geofísica Internacionalinfo:eu-repo/semantics/openAccessoai:redalyc.org:568413232025-09-03T18:07:50Z
dc.title.none.fl_str_mv Spring water and CO2 interaction at Popocatépetl volcano, Mexico
title Spring water and CO2 interaction at Popocatépetl volcano, Mexico
spellingShingle Spring water and CO2 interaction at Popocatépetl volcano, Mexico
A. L. Martin Del Pozzo
Ciencias de la Tierra
Spring Water
CO2 interaction
Popocatépetl volcano
title_short Spring water and CO2 interaction at Popocatépetl volcano, Mexico
title_full Spring water and CO2 interaction at Popocatépetl volcano, Mexico
title_fullStr Spring water and CO2 interaction at Popocatépetl volcano, Mexico
title_full_unstemmed Spring water and CO2 interaction at Popocatépetl volcano, Mexico
title_sort Spring water and CO2 interaction at Popocatépetl volcano, Mexico
dc.creator.none.fl_str_mv A. L. Martin Del Pozzo
S. Inguaggiato
F. Aceves
H. Saenz
A. Aguayo
author A. L. Martin Del Pozzo
author_facet A. L. Martin Del Pozzo
S. Inguaggiato
F. Aceves
H. Saenz
A. Aguayo
author_role author
author2 S. Inguaggiato
F. Aceves
H. Saenz
A. Aguayo
author2_role author
author
author
author
dc.subject.none.fl_str_mv Ciencias de la Tierra
Spring Water
CO2 interaction
Popocatépetl volcano
topic Ciencias de la Tierra
Spring Water
CO2 interaction
Popocatépetl volcano
description Six years of monitoring HCO3- and pH at selected springs at Popocatépetl during the present eruptive period are presented.Small peaks in HCO3- concentration and PCO2 in springs are associated with small magmatic pulses at Popocatépetl volcano. Themagma provides CO2-rich fluids into the water system controlled by meteoric recharge. The PCO2 in equilibrium with the springsis two to four orders of magnitude higher than air-saturated water. The high partial pressure of CO2 also suggests a direct interactionwith the magmatic fluids. The isotopic signature of carbon as well, supports a magmatic origin for dissolved CO2.
publishDate 2002
dc.date.none.fl_str_mv 2002
dc.type.none.fl_str_mv info:eu-repo/semantics/publishedVersion
info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv 0016-7169
https://www.redalyc.org/articulo.oa?id=56841323
identifier_str_mv 0016-7169
url https://www.redalyc.org/articulo.oa?id=56841323
dc.language.none.fl_str_mv en
language_invalid_str_mv en
dc.relation.none.fl_str_mv http://www.redalyc.org/revista.oa?id=568
dc.rights.none.fl_str_mv Geofísica Internacional
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Geofísica Internacional
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Universidad Nacional Autónoma de México
publisher.none.fl_str_mv Universidad Nacional Autónoma de México
dc.source.none.fl_str_mv Geofísica Internacional (México) Num.3 Vol.41
reponame:Redalyc-UNAM
instname:Universidad Nacional Autónoma de México
instacron:UNAM
instname_str Universidad Nacional Autónoma de México
instacron_str UNAM
institution UNAM
reponame_str Redalyc-UNAM
collection Redalyc-UNAM
repository.name.fl_str_mv
repository.mail.fl_str_mv
_version_ 1858174361888882688
score 14,965156

Similares en LA Referencia