Abstract

Geochemical study allowed to recognize four groups of groundwater for the Sibari Plain (Southern Italy): Ca-HCO3, Na-Cl, Ca-Cl and Na-HCO3. Chloride-rich waters are located close to the Crati mouth that could be a preferential path for seawater ingression. In fact, seawater and brackish waters could move inland along the stream channel and enter the nearby aquifers due to excessive pumping of wells positioned near the river. In alternative, the occurrence of processes, such as ion exchange or dissolution of halite-bearing Miocene evaporite deposits can generate aqueous solutions with similar characteristics to those produced by seawater ingression. Moreover, was calculated the infiltration average (Hi, m a.s.l.) for groundwater of the Sibari Plain by the following equations:The data showed a lower average of the infiltrations in the inner part of the Sibari Plain, with values between 550 and 870 m a.s.l., and higher values (1000/1500 m a.s.l.) moving to NW and SE.

Autore Pugliese

• Polemio Maurizio

Tutti gli autori

• Vespasiano G.; Apollaro C.; Marini L.; Dominici R.; Cianflone G.; Romanazzi A.; Polemio M.; De Rosa R.

Titolo volume/Rivista

Rendiconti online Società Geologica Italiana

Anno di pubblicazione

2016

ISSN

2035-8008

ISBN

Non Disponibile

Numero di citazioni Wos

Nessuna citazione

Ultimo Aggiornamento Citazioni

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Numero di citazioni Scopus

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Ultimo Aggiornamento Citazioni

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Settori ERC

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Codici ASJC

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