Abstract
The solubility of CaSO3·1/2H2O(c) was studied under alkaline conditions (pH>8.2), in deaerated and deoxygenated Na2SO3 solutions ranging in concentration from 0.0002 to 0.4M and in CaCl2 solutions ranging in concentration from 0.0002 to 0.01M, for equilibration periods ranging from 1 to 7 days. Equilibrium was approached from both the over- and the under-saturation directions. In all cases, equilibrium was reached in <1 days. The aqueous Ca2+−SO 2−3 ion interactions can be satisfactorily modeled using either ion-association or ion-interaction aqueous thermodynamic models. In the ion-association model, the log K°=2.62±0.07 for Ca2++SO 2−3 ⇆CaSO 03 . In the Pitzer ion-interaction model, the binary parameters β(0) and β(1) for Ca2+−SO 2−4 were used, and the value of β(2) was determined from the experimental data. As expected given the strong association constant, the value of β(0) was quite small (about −134). We feel a combination of the two models is most useful. The logarithm of the thermodynamic equilibrium constant (K°) of the CaSO3·1/2H2O(c) solubility reaction (CaSO3·1/2H2O(c)⇆Ca2++SO 2+3 +0.5H2O) was found to be −6.64±0.07.
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Rai, D., Felmy, A.R., Fulton, R.W. et al. An aqueous thermodynamic model for Ca2+−SO 2−3 ion interactions and the solubility product of crystalline CaSO3·1/2H2O. J Solution Chem 20, 623–632 (1991). https://doi.org/10.1007/BF00647072
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DOI: https://doi.org/10.1007/BF00647072