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dc.contributor.authorBinda, Gilberto
dc.contributor.authorFrascoli, Francesca
dc.contributor.authorSpanu, Davide
dc.contributor.authorFerrario, Maria F.
dc.contributor.authorTerrana, Silvia
dc.contributor.authorGambillara, Roberto
dc.contributor.authorTrotta, Sara
dc.contributor.authorNoble, Paula J.
dc.contributor.authorLivio, Franz A.
dc.contributor.authorPozzi, Andrea
dc.contributor.authorMichetti, Alessandro M.
dc.date.accessioned2022-03-24T12:05:10Z
dc.date.available2022-03-24T12:05:10Z
dc.date.created2022-03-09T10:26:56Z
dc.date.issued2022
dc.identifier.citationWater. 2022, 14 (1), 124.en_US
dc.identifier.issn2073-4441
dc.identifier.urihttps://hdl.handle.net/11250/2987342
dc.description.abstractThe analysis of geochemical markers is a known valid tool to explore the water sources and understand the main factors affecting natural water quality, which are known issues of interest in environmental science. This study reports the application of geochemical markers to characterize and understand the recharge areas of the multi-layer urban aquifer of Como city (northern Italy). This area presents a perfect case study to test geochemical markers: The hydrogeological setting is affected by a layered karst and fractured aquifer in bedrock, a phreatic aquifer hosted in Holocene sediments and connected with a large freshwater body (Lake Como); the aquifers recharge areas and the water geochemistry are unknown; the possible effect of the tectonic setting on water flow was overlooked. In total, 37 water samples were collected including water from two stacked aquifers and surface water to characterize hydrochemical features. Moreover, six sediment samples in the recent palustrine deposits of the Como subsurface were collected from cores and analyzed to understand the main geochemistry and mineralogy of the hosting material. The chemical analyses of water allow to observe a remarkable difference between the shallow and deep aquifers of the study area, highlighting different recharge areas, as well as a different permanence time in the aquifers. The sediment geochemistry, moreover, confirms the differences in trace elements derived from sediment-water interaction in the aquifers. Finally, an anomalous concentration of As in the Como deep aquifer was observed, suggesting the need of more detailed analyses to understand the origin of this element in water. This study confirms the potentials of geochemical markers to characterize main factors affecting natural water quality, as well as a tool for the reconstruction of recharge areas.en_US
dc.language.isoengen_US
dc.publisherMDPIen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleGeochemical Markers as a Tool for the Characterization of a Multi-Layer Urban Aquifer: The Case Study of Como (Northern Italy)en_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.rights.holder© 2022 by the authorsen_US
dc.source.pagenumber21en_US
dc.source.volume14en_US
dc.source.journalWateren_US
dc.source.issue1en_US
dc.identifier.doi10.3390/w14010124
dc.identifier.cristin2008427
dc.source.articlenumber124en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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