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dc.contributor.authorGastmans, Didier [UNESP]
dc.contributor.authorMenegário, Amauri Antônio [UNESP]
dc.contributor.authorHutcheon, Ian
dc.date.accessioned2018-12-11T17:31:28Z
dc.date.available2018-12-11T17:31:28Z
dc.date.issued2017-02-01
dc.identifierhttp://dx.doi.org/10.1007/s12665-017-6468-1
dc.identifier.citationEnvironmental Earth Sciences, v. 76, n. 4, 2017.
dc.identifier.issn1866-6299
dc.identifier.issn1866-6280
dc.identifier.urihttp://hdl.handle.net/11449/178646
dc.description.abstractThe Cretaceous Serra Geral Aquifer (SGA) is contained within one of the largest continental flood basalts in the world, reaching a thickness up to 1700 m in the center of the Paraná Basin. The SGA is one of the most important groundwater reservoirs in northeastern São Paulo State (Brazil), responsible for water supply to cities and agriculture. In order to evaluate the geochemical and isotopic evolution of SGA, as well as to determine the mean residence time, a groundwater sampling campaign was carried out over the SGA in São Paulo State (Brazil) from January to April 2013. Two main hydrochemical facies were recognized: Ca–Mg–HCO3 related to water–rock interaction reactions in basaltic outcrop, such as mineral dissolution due to atmospheric CO2 uptake, and alkaline Na–HCO3 groundwater, evolved from mixing with groundwater from the underlying Guarani Aquifer System. Stable isotope (δ18O and δ2H) ratios range from −8.87 to −5.32‰ VSMOW and −61.31 to −31.64‰ VSMOW, respectively, closely following the GMWL. Spatial and temporal variations in isotope ratios are associated with the South Atlantic convergence zone activities and the type of rain responsible for recharge. Values for δ13C vary from −21.53 to −7.11‰ VPDB, while 14C activities vary from 1.2 pcm to more than 100 pcm, presenting a trend to enrichment and decrease in 14C activities westward, concordant with the regional groundwater flow direction. Most recent groundwaters have δ13C ratio contents mostly consistent with C3 plants.en
dc.description.sponsorshipFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
dc.language.isoeng
dc.relation.ispartofEnvironmental Earth Sciences
dc.sourceScopus
dc.subjectBrazil
dc.subjectGroundwater age
dc.subjectHydrochemistry
dc.subjectSerra Geral Aquifer
dc.subjectStable isotopes
dc.titleStable isotopes, carbon-14 and hydrochemical composition from a basaltic aquifer in São Paulo State, Brazilen
dc.typeArtigo
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)
dc.contributor.institutionUniversity of Calgary
dc.description.affiliationEnvironmental Studies Center São Paulo State University (UNESP), Av. 24A, 1515 – Bela Vista
dc.description.affiliationApplied Geochemistry Group Department of Geoscience University of Calgary, 2500 University Drive NW
dc.description.affiliationUnespEnvironmental Studies Center São Paulo State University (UNESP), Av. 24A, 1515 – Bela Vista
dc.identifier.doi10.1007/s12665-017-6468-1
dc.rights.accessRightsAcesso aberto
dc.description.sponsorshipIdFAPESP: 2012/00241-5
dc.identifier.scopus2-s2.0-85012867110
unesp.author.orcid0000-0002-1340-3373[1]
dc.relation.ispartofsjr0,552
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