Karst systems usually host a thermal basin, especially when in contact with volcanic masses. For hydro-geological purposes, the main goal lies in understanding circulation paths and defining water fluxes; on the other hand, it is important to define the heat transfer, in order to exploit the geothermal potentiality of a site. To permit subsequent thermodynamic considerations, a preliminary study on Suio spring site has been led, focusing on the hydrogeological features of the area. Taking into account geologic, structural, geomorphologic, geochemical and hydrological data, this work intends to give support to a first numericalmodeling of Suio spring.
Study on the hydrothermal Suio-Castelforte basin (LT, Italy)
SAROLI, Michele;CASALE, Anna;LANCIA, Michele;GIOVINCO, Gaspare;DELL'ISOLA, Marco;
2014-01-01
Abstract
Karst systems usually host a thermal basin, especially when in contact with volcanic masses. For hydro-geological purposes, the main goal lies in understanding circulation paths and defining water fluxes; on the other hand, it is important to define the heat transfer, in order to exploit the geothermal potentiality of a site. To permit subsequent thermodynamic considerations, a preliminary study on Suio spring site has been led, focusing on the hydrogeological features of the area. Taking into account geologic, structural, geomorphologic, geochemical and hydrological data, this work intends to give support to a first numericalmodeling of Suio spring.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
