The fate of divalent radium (Ra2+) in high ionic strength systems is an important issue with relevant aspects to environmental concerns. As a consequence, the description of the thermodynamic properties of Ra2+ in such systems is a critical matter which was not addressed yet. This can be done using the Pitzer formalism, which is regarded as the most accurate approach to describe activity coefficients of aquatic species in high ionic strength solutions. Isopiestic measurements, measurements of the electromotive force or the solubility of RaSO4,S in NaCl solutions, which are essential for the evaluation of the Pitzer ion interaction parameters, were not experimentally tested, due to the high radioactivity concentration which involves such experiments. Therefore, the present study examined the possibility to extrapolate the RaCl2 cation-anion interaction parameters (β(0), β(1) and Cφ) by linear regression of other MCl2 cation-anion interaction parameters with their respective hydrated ionic radii (M2+=Mg2+, Ca2+, Sr2+ and Ba2+).γRa2+ calculated with the estimated RaCl2 parameters revealed that the ratios of activity coefficients γMg2+/γBa2+>γCa2+/γBa2+>γSr2+/γBa2+>1>γRa2+/γBa2+ follow the opposite order of the ratios of hydrated ionic radii RMg2+/RBa2+<RCa2+/RBa2+<RSr2+/RBa2+<1<RRa2+/RBa2+.The activity coefficient of Ra2+, γRa2+, calculated with these estimated values is used to test the limitation of the common assumption that the activity coefficients ratio, γRa2+/γBa2+, is close to unity. It is found that the common assumption of γRa2+/γBa2+=1 may be considered reasonable up to high NaCl concentration. The largest deviation in the γRa2+/γBa2+ ratio from this assumption was of the order of ∼25% in the range of halite solubility (6molkg-1 of NaCl). However, experimental results of co-precipitation of Ra2+ in barite are described with more accuracy when the estimated RaCl2 Pitzer parameters are used. These results are described in a consecutive paper of this journal.
All Science Journal Classification (ASJC) codes
- Geochemistry and Petrology