Pregled bibliografske jedinice broj: 1068497
Upwelling time of thermal waters inferred using radionuclides: the case study of the Euganean Geothermal Field (Veneto - NE Italy)
Upwelling time of thermal waters inferred using radionuclides: the case study of the Euganean Geothermal Field (Veneto - NE Italy) // Flowpath 2014, National Meeting on Hydrogeology - Abstract Volume / Baiocchi, Antonella ; Lotti, Francesca ; Onofri, Silvano ; Piscopo, Vincenzo (ur.).
Vetralla: Leograph.it, 2014. str. 116-117 (predavanje, međunarodna recenzija, prošireni sažetak, znanstveni)
CROSBI ID: 1068497 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Upwelling time of thermal waters inferred using radionuclides: the case study of the Euganean Geothermal Field (Veneto - NE Italy)
Autori
Pola, Marco ; Mayer, Adriano ; Fabbri, Paolo ; Piccinini, Leonardo ; Zampieri, Dario
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, prošireni sažetak, znanstveni
Izvornik
Flowpath 2014, National Meeting on Hydrogeology - Abstract Volume
/ Baiocchi, Antonella ; Lotti, Francesca ; Onofri, Silvano ; Piscopo, Vincenzo - Vetralla : Leograph.it, 2014, 116-117
ISBN
978-88-907553-4-7
Skup
Flowpath 2014 - National Meeting on Hydrogeology
Mjesto i datum
Viterbo, Italija, 18.06.2014. - 20.06.2014
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
radium isotope ; groundwater age ; thermal water ; Euganean Geothermal Field
Sažetak
The Euganean thermal waters (65-86°C) constituting the homonymous thermal field (Euganean Geothermal Field ; Veneto region ; NE Italy) are investigated in this work to constraint the time scales of their upwelling based on Ra and Rn isotopes. Two groups of samples can be distinguished on the base of the 223Ra/226Ra and goethite saturation index. The thermal waters in the northern part of the thermal field are characterized are characterized by goethite S.I. <1.6 and 223Ra/226Ra<0.046 that were interpreted as the result of quick rise to the surface (maximum 3 days) through large fractures. The thermal waters in the central and southern parts of the thermal field are clearly saturated in goethite (S.I.>1.6) and in general characterized by 223Ra/226Ragreater than equilibrium value (0.046). This result was interpreted as connected to a slower rising path through a finely fractured aquifer yielding an enhanced water/rock interactions.
Izvorni jezik
Engleski
Znanstvena područja
Rudarstvo, nafta i geološko inženjerstvo
