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Article Dans Une Revue Applied Geochemistry Année : 2014

A multi-tracer study of groundwater origin and transit-time in the aquifers of the Venice region (Italy)

Résumé

Located in the northeastern region of Italy, the Venetian Plain (VP) is a sedimentary basin containing an extensively exploited groundwater system. The northern part is characterised by a large undifferentiated phreatic aquifer constituted by coarse grain alluvial deposits and recharged by local rainfalls and discharges from the rivers Brenta and Piave. The southern plain is characterised by a series of aquitards and sandy aquifers forming a well-defined artesian multi-aquifer system. In order to determine origins, transit times and mixing proportions of different components in groundwater (GW), a multi tracer study (3
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Dates et versions

hal-01318686 , version 1 (19-05-2016)

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A Mayer, J Sültenfuss, Yves Travi, R Rebeix, R Purtschert, et al.. A multi-tracer study of groundwater origin and transit-time in the aquifers of the Venice region (Italy). Applied Geochemistry, 2014, 50, pp.177-198. ⟨10.1016/j.apgeochem.2013.10.009⟩. ⟨hal-01318686⟩
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