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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/964
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dc.contributor.authorallBarquero, J.; Observatorio Vulcanológico y Sismológico de Costa Rica, Universidad Nacional (OVSICORI-UNA), Heredia, Costa Ricaen
dc.contributor.authorallFernandez, E.; Observatorio Vulcanológico y Sismológico de Costa Rica, Universidad Nacional (OVSICORI-UNA), Heredia, Costa Ricaen
dc.contributor.authorallMonnin, M.; Hydrosciences, Université Montpellier 2 (UM2) - CNRS, Montpellier, Franceen
dc.contributor.authorallSeidel, J. L.; Hydrosciences, Université Montpellier 2 (UM2) - CNRS, Montpellier, Franceen
dc.contributor.authorallSegovia, N.; Instituto Nacional de Investigaciones Nucleares (ININ), México D.F., Méxicoen
dc.date.accessioned2006-02-23T09:50:16Zen
dc.date.available2006-02-23T09:50:16Zen
dc.date.issued2005en
dc.identifier.urihttp://hdl.handle.net/2122/964en
dc.description.abstractRadon-in-soil monitoring at the Poas volcano (Costa Rica) has been performed together with water chemistry from the hot crater lake since 1981 and 1983 respectively. The results are discussed as a function of the eruptive evolution of the volcano over a 13 years period (1981-1994). It is shown that no definitely clear precursory radon signals have been recorded. On the contrary, ionic species concentrations are likely to be considered good precursors, together with the temperature variations of the crater lake water.en
dc.format.extent992032 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.publisher.nameINGVen
dc.relation.ispartofAnnals of Geophysicsen
dc.relation.ispartofseries1/48 (2005)en
dc.subjectPoas volcanoen
dc.subjectgeochemistryen
dc.subjectradonen
dc.subjectprecursoren
dc.titleWater chemistry and soil radon survey at the Poas volcano (Costa Rica)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.12. Fluid Geochemistryen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorBarquero, J.en
dc.contributor.authorFernandez, E.en
dc.contributor.authorMonnin, M.en
dc.contributor.authorSeidel, J. L.en
dc.contributor.authorSegovia, N.en
dc.contributor.departmentObservatorio Vulcanológico y Sismológico de Costa Rica, Universidad Nacional (OVSICORI-UNA), Heredia, Costa Ricaen
dc.contributor.departmentObservatorio Vulcanológico y Sismológico de Costa Rica, Universidad Nacional (OVSICORI-UNA), Heredia, Costa Ricaen
dc.contributor.departmentHydrosciences, Université Montpellier 2 (UM2) - CNRS, Montpellier, Franceen
dc.contributor.departmentHydrosciences, Université Montpellier 2 (UM2) - CNRS, Montpellier, Franceen
dc.contributor.departmentInstituto Nacional de Investigaciones Nucleares (ININ), México D.F., Méxicoen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptObservatorio Vulcanológico y Sismológico de Costa Rica, Universidad Nacional (OVSICORI-UNA), Heredia, Costa Rica-
crisitem.author.deptVolcanological and Seismological Observatory, Universidad Nacional, Heredia, Costa Rica-
crisitem.author.deptHydrosciences, Université Montpellier 2 (UM2) - CNRS, Montpellier, France-
crisitem.author.deptHydrosciences, Université Montpellier 2 (UM2) - CNRS, Montpellier, France-
crisitem.author.deptInstituto de Geofisica, Universidad Nacional Autónoma de Mexico (UNAM), México D.F., México-
crisitem.classification.parent04. Solid Earth-
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