Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4675195 | Procedia Earth and Planetary Science | 2013 | 4 Pages |
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.
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