Identificador persistente para citar o vincular este elemento: http://hdl.handle.net/10553/55098
Campo DC Valoridioma
dc.contributor.authorAlonso, H.en_US
dc.contributor.authorRubiano, J. G.en_US
dc.contributor.authorGuerra, J. G.en_US
dc.contributor.authorArnedo, M. A.en_US
dc.contributor.authorTejera, A.en_US
dc.contributor.authorMartel, P.en_US
dc.date.accessioned2019-02-18T16:30:30Z-
dc.date.available2019-02-18T16:30:30Z-
dc.date.issued2019en_US
dc.identifier.issn0048-9697en_US
dc.identifier.urihttp://hdl.handle.net/10553/55098-
dc.description.abstractThe Basic Safety Standard (BSS) Directive 2013/59/EURATOM of the European Union (EU) has stated the need for member states to establish national action plans to mitigate their general population's long-term risks of exposure to radon gas. Maps of radon-prone areas provide a useful tool for the development of such plans. This paper presents the maps of radon-prone areas in the Eastern Canary Islands (Gran Canaria, Fuerteventura and Lanzarote) obtained from assessment of Geogenic Radon Potential (GRP) distribution in the territory. GRP constitutes a magnitude that is contingent on both radon activity concentration and gas permeability of soils. An extensive campaign covering all geological formations of the Eastern Canary Islands was undertaken to locally sample these parameters. Geostatistical analysis of the spatial distribution of radon concentration in soils, permeability and GRP was performed on each of the islands, and the relationship between these magnitudes and the characteristic geological formations of the volcanic islands was investigated. Areas dominated by basic volcanic and plutonic rocks (originated by both recent and ancient volcanism) exhibit relatively low levels of radon in soils, and with the exception of specific cases of very high permeability, these areas are not classified as prone to radon risk according to international criteria. Areas in which intermediate or acidic volcanic and plutonic rocks predominate are characterised by greater radon activity concentration in soils, rendering them radon-prone. Given these results, Lanzarote is classified as an island with low radon risk all over its surface; Fuerteventura presents low-medium risk; and Gran Canaria contains extensive areas in the centre and north where the risk is medium or high. This classification is consistent with the risk maps obtained by National and European agencies from indoor radon measurements conducted on these islands.en_US
dc.languageengen_US
dc.relation.ispartofScience of the Total Environmenten_US
dc.sourceScience of the Total Environment [ISSN 0048-9697], v. 664, p. 449-460, (Mayo 2019)en_US
dc.subject2207 Física atómica y nuclearen_US
dc.subject.otherEnvironmental radioactivityen_US
dc.subject.otherRadon risk mapsen_US
dc.subject.otherRadon in soilen_US
dc.subject.otherSoil gas permeabilityen_US
dc.subject.otherGeogenic Radon Potentialen_US
dc.titleAssessment of radon risk areas in the Eastern Canary Islands using soil radon gas concentration and gas permeability of soilsen_US
dc.typeinfo:eu-repo/semantics/Articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.scitotenv.2019.01.411en_US
dc.identifier.pmid30759409-
dc.identifier.scopus85061200505-
dc.identifier.isi000460245600043-
dc.contributor.orcid#NODATA#-
dc.contributor.orcid0000-0002-7763-0778-
dc.contributor.orcid#NODATA#-
dc.contributor.orcid#NODATA#-
dc.contributor.orcid#NODATA#-
dc.contributor.orcid#NODATA#-
dc.contributor.authorscopusid55820626300-
dc.contributor.authorscopusid55768891400-
dc.contributor.authorscopusid57205095259-
dc.contributor.authorscopusid56356517200-
dc.contributor.authorscopusid6602494476-
dc.contributor.authorscopusid55769220800-
dc.description.lastpage460en_US
dc.description.firstpage449en_US
dc.relation.volume664en_US
dc.investigacionIngeniería y Arquitecturaen_US
dc.type2Artículoen_US
dc.contributor.daisngid4777825-
dc.contributor.daisngid757252-
dc.contributor.daisngid9918554-
dc.contributor.daisngid6363634-
dc.contributor.daisngid3141177-
dc.contributor.daisngid177510-
dc.utils.revisionen_US
dc.contributor.wosstandardWOS:Alonso, H-
dc.contributor.wosstandardWOS:Rubiano, JG-
dc.contributor.wosstandardWOS:Guerra, JG-
dc.contributor.wosstandardWOS:Arnedo, MA-
dc.contributor.wosstandardWOS:Tejera, A-
dc.contributor.wosstandardWOS:Martel, P-
dc.date.coverdateMayo 2019en_US
dc.identifier.ulpgcen_US
dc.description.sjr1,661-
dc.description.jcr6,551-
dc.description.sjrqQ1-
dc.description.jcrqQ1-
dc.description.scieSCIE-
item.fulltextCon texto completo-
item.grantfulltextrestricted-
crisitem.author.deptGIR IUNAT: Interacción Radiación-Materia-
crisitem.author.deptIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.deptDepartamento de Física-
crisitem.author.deptGIR IUNAT: Interacción Radiación-Materia-
crisitem.author.deptIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.deptDepartamento de Física-
crisitem.author.deptGIR IUNAT: Interacción Radiación-Materia-
crisitem.author.deptIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.deptDepartamento de Física-
crisitem.author.deptGIR IUNAT: Interacción Radiación-Materia-
crisitem.author.deptIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.deptDepartamento de Física-
crisitem.author.orcid0000-0002-3479-9805-
crisitem.author.orcid0000-0002-7763-0778-
crisitem.author.orcid0000-0002-2022-8411-
crisitem.author.orcid0000-0002-2416-3053-
crisitem.author.orcid0000-0001-7883-5970-
crisitem.author.parentorgIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.parentorgIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.parentorgIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.parentorgIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.fullNameAlonso Hernández, Héctor Eulogio-
crisitem.author.fullNameGarcía Rubiano, Jesús-
crisitem.author.fullNameArnedo Ayensa, Miguel Ángel-
crisitem.author.fullNameTejera Cruz, Alicia María-
crisitem.author.fullNameMartel Escobar, Pablo-
Colección:Artículos
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