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Please use this identifier to cite or link to this item: http://acervodigital.unesp.br/handle/11449/76231
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dc.contributor.authorHöyng, Dominik-
dc.contributor.authorD'Affonseca, Fernando Mazo-
dc.contributor.authorBayer, Peter-
dc.contributor.authorde Oliveira, Edson Gomes-
dc.contributor.authorPerinotto, José Alexandre de Jesus-
dc.contributor.authorReis, Fábio-
dc.contributor.authorWeiß, Holger-
dc.contributor.authorGrathwohl, Peter-
dc.date.accessioned2014-05-27T11:30:08Z-
dc.date.accessioned2016-10-25T18:52:32Z-
dc.date.available2014-05-27T11:30:08Z-
dc.date.available2016-10-25T18:52:32Z-
dc.date.issued2013-08-07-
dc.identifierhttp://dx.doi.org/10.1007/s12665-013-2684-5-
dc.identifier.citationEnvironmental Earth Sciences, p. 1-14.-
dc.identifier.issn1866-6280-
dc.identifier.issn1866-6299-
dc.identifier.urihttp://hdl.handle.net/11449/76231-
dc.identifier.urihttp://acervodigital.unesp.br/handle/11449/76231-
dc.description.abstractThe Guarani aquifer system (GAS) represents one of the biggest aquifers in the world and is the most relevant groundwater resource in South America. For the first time, by combining field and laboratory measurements, a high-resolution aquifer analog model of fluvial-aeolian sediments of the GAS in São Paulo State (Brazil) is constructed. Three parallel sections of frontal outcrops, 28 m × 5.8 m, and two parallel sections of lateral outcrops, 7 m × 5.8 m, are recorded during open-pit mining of sandy sediments and describe in detail the three-dimensional distribution of the local lithofacies and hydrofacies. Variations of hydraulic conductivity, K, and porosity, n, are resolved on the centimeter scale, and the most permeable units of the fluvial-aeolian facies association are identified. The constructed aquifer analog model shows moderate hydraulic heterogeneity and a mean K value of 1.36 × 10-4 m/s, which is greater than the reported range of K values for the entire GAS in São Paulo State. The results suggest that the examined sedimentary unit constitutes a relevant portion of the GAS in São Paulo State in the context of groundwater extraction and pollution. Moreover, the constructed aquifer analog is considered an ideal basis for future numerical model experiments, aiming at in-depth understanding of the groundwater flow and contaminant transport patterns at this GAS portion or at comparable fluvial-aeolian facies associations. © 2013 Springer-Verlag Berlin Heidelberg.en
dc.format.extent1-14-
dc.language.isoeng-
dc.sourceScopus-
dc.subjectFluvial-aeolian sediments-
dc.subjectGroundwater reservoir analog model-
dc.subjectGuarani aquifer-
dc.subjectPirambóia Formation-
dc.subjectReservoir characterization-
dc.titleHigh-resolution aquifer analog of fluvial-aeolian sediments of the Guarani aquifer systemen
dc.typeoutro-
dc.contributor.institutionCenter for Applied Geosciences-
dc.contributor.institutionTIMGEO GmbH-
dc.contributor.institutionETH Zurich-
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)-
dc.contributor.institutionHelmholtz Center for Environmental Research (UFZ)-
dc.description.affiliationUniversity of Tübingen Center for Applied Geosciences, Hölderlinstr. 12, Tübingen, 72074-
dc.description.affiliationTIMGEO GmbH, Hölderlinstr. 29, Tübingen, 72074-
dc.description.affiliationGeological Institute ETH Zurich, Sonneggstr. 5, Zurich, 8092-
dc.description.affiliationInstituto de Geociências e Ciências Exatas UNESP, Univ. Estadual Paulista, Av. 24-A n 1515 - B. Bela Vista, Rio Claro, 13506-900-
dc.description.affiliationHelmholtz Center for Environmental Research (UFZ), Permoserstr. 15, Leipzig, 04318-
dc.description.affiliationUnespInstituto de Geociências e Ciências Exatas UNESP, Univ. Estadual Paulista, Av. 24-A n 1515 - B. Bela Vista, Rio Claro, 13506-900-
dc.identifier.doi10.1007/s12665-013-2684-5-
dc.identifier.wosWOS:000333014500009-
dc.rights.accessRightsAcesso restrito-
dc.relation.ispartofEnvironmental Earth Sciences-
dc.identifier.scopus2-s2.0-84880937692-
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