We investigate the interaction between hydrothermal gases and groundwater in a major aquifer exploited for potable supply in the geothermal-volcanic area of Mt. Amiata, Central Italy. The chemical and isotope composition of more than 80 water samples from two springs emerging on the southwestern side of the volcanic edifice has been processed with geochemical modelling techniques. Best fitting conditions between analytical data and model outputs have been achieved by numerical optimization, allowing for a quantitative description of gas-water-rock interactions occurring in this aquifer.

Hydrothermal gases in a shallow aquifer at Mt. Amiata, Italy: Insights from stable isotopes and geochemical modeling.

Pierotti L;Cortecci G;Gherardi F
2015

Abstract

We investigate the interaction between hydrothermal gases and groundwater in a major aquifer exploited for potable supply in the geothermal-volcanic area of Mt. Amiata, Central Italy. The chemical and isotope composition of more than 80 water samples from two springs emerging on the southwestern side of the volcanic edifice has been processed with geochemical modelling techniques. Best fitting conditions between analytical data and model outputs have been achieved by numerical optimization, allowing for a quantitative description of gas-water-rock interactions occurring in this aquifer.
2015
Istituto di Geoscienze e Georisorse - IGG - Sede Pisa
Inglese
IAEA
3He 2H 13C 18O INTERNATIONAL SYMPOSIUM ON Revisiting Foundations and Exploring Frontiers Isotope Hydrology IAEA-CN-225
IAEA, International Symposium on Isotope Hydrology
74
77
4
Sì, ma tipo non specificato
11-15 May, 2015
Vienna
Hydrothermal gases
Mt. Amiata
stable isotopes
geochemical modelling
shallow aquifer
3
none
Pierotti, L; Cortecci, G; Gherardi, F
273
info:eu-repo/semantics/conferenceObject
04 Contributo in convegno::04.01 Contributo in Atti di convegno
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/387569
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