Title of article :
Why the Geochemical Diversity of CO2-Bearing Groundwaters in Crystalline Massifs Occurs
Author/Authors :
Cherkasova، نويسنده , , E.V. and Ryzhenko، نويسنده , , B.N. and Limantseva، نويسنده , , O.A.، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2013
Abstract :
The diversity of geochemical types of CO2-bearing waters in crystalline massifs of similar mineralogical and petrogra- phic composition in water–rock systems is due to the influence of the following physicochemical parameters: chloride type - mainly high Rock/Water mass ratio (R/W); carbonate type - joint action of low Rock/Water mass ratio (R/W) and high CO2 partial pressure (PCO2); sulfate type - joint action of high Rock/Water mass ratio (R/W), CO2 partial pressure (PCO2), and temperature.
Keywords :
Hydrogeochemistry , MODELING , CO2-bearing waters , Water-Rock system
Journal title :
Procedia Earth and Planetary Science
Journal title :
Procedia Earth and Planetary Science
