Title of article
A Multi-Isotope Study of the Castrocaro Mineral Waters (Northeastern Apennines, Italy)
Author/Authors
Pennisi، نويسنده , , M. and Cortecci، نويسنده , , G. and Magro، نويسنده , , G. and Gherardi، نويسنده , , F. and Antoniazzi، نويسنده , , Rolando A. and Bianchini، نويسنده , , G. and Sacchi، نويسنده , , E. and Adorni-Braccesi، نويسنده , , A.، نويسنده ,
Issue Information
روزنامه با شماره پیاپی سال 2013
Pages
4
From page
673
To page
676
Abstract
An applied multi-isotope approach (δ2H, δ18O, δ11B, δ13C, δ15N, δ34S), coupled with chemical evidence, allowed us to constrain a conceptual hydrogeological model for the Castrocaro sulfureous groundwater system that is composed of fresh, brackish, and saline components. In this model, the meteoric recharge enters the turbidite sequence of the Marnoso-Arenacea Fm., undergoing chemical and isotopic modifications by interaction with fine grained pelite rocks, mixing with fossil seawater, and biochemical reactions. The groundwater then rises into a biocalcarenite unit, which acts just as a reservoir from which the resource is finally exploited by wells feeding the Castrocaro Terme spa.
Keywords
Saline sulfureous groundwater , O , H , C , B , S isotopes , Castrocaro Terme , Italy , N , Hydrogeological model
Journal title
Procedia Earth and Planetary Science
Serial Year
2013
Journal title
Procedia Earth and Planetary Science
Record number
2320649
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