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The influence of pressure on the activity coefficients of the solutes and on the solubility of minerals in the system Na-Ca-Cl-SO sub 4 -H sub 2 O to 200 degree C and 1 kbar, and to high NaCl concentration

Journal Article · · Geochimica et Cosmochimica Acta; (USA)
 [1]
  1. Centre National de la Recherche Scientifique, Toulouse (France)
A model is presented which is used to calculate the effect of pressure on activity coefficients of aqueous solutes in the system Na-Ca-Cl-SO{sub 4}-H{sub 2}O to 200{degree}C. Literature data for the density and compressibility of aqueous binary solutions of Na{sub 2}SO{sub 4} and CaCl{sub 2} to 200{degree}C are used to calculate the first and second pressure derivatives of Pitzer's ion interaction model parameters, as well as the standard molal compressibility and volume of these two salts. Empirical correlations between the apparent molal volume and compressibility of the aqueous electrolytes are used to guide the choice of the temperature dependent expressions used for the numerical representation of the derivatives of Pitzer's parameters with respect to pressure. The volumetric properties of multicomponent solutions in the Na-Ca-Cl-SO{sub 4}-H{sub 2}O system can be predicted from the information generated here and the volumetric equations of Rogers and Pitzer (1982) for NaCl. This model is then combined with the high temperature model of Moller (1988) of the same system in order to calculate activity coefficients at high pressures to 200{degree}C. The resulting model is validated by comparing calculated and measured solubilities of anhydrite and gypsum in pure water and in NaCl solutions up to 6 M.
OSTI ID:
6054036
Journal Information:
Geochimica et Cosmochimica Acta; (USA), Journal Name: Geochimica et Cosmochimica Acta; (USA) Vol. 54:12; ISSN GCACA; ISSN 0016-7037
Country of Publication:
United States
Language:
English