Thermodynamic model for the solubility of thorium dioxide in the Na+-Cl--OH--H2O system at 23°C and 90°C
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Dhanpat Rai
, Dean A. Moore , C.S. Oakes and Mikazu Yui
Data are extremely limited on the effects of temperature on crystallinity and the resulting changes in solubility products of thermally transformed thorium oxide phases. Such data are required to reliably predict thorium behavior in high-level waste repositories where higher than ambient temperatures are expected. Solubility studies were conducted as a function of pH and time and at 0.1 M NaCl for 1) ThO2(am) at 23°C, 2) ThO2 (am→c), a thermally transformed amorphous thorium hydrous oxide at 90°C, and 3) ThO2(c) at 23°C and 90°C. Results show that when ThO2(am) is heated to 90°C, it transforms to a relatively insoluble and crystalline solid [ThO2(am→c)]. At a fixed pH, the observed solubility of ThO2(am) at 23°C is more than 11 orders of magnitude greater than those for ThO2(c) at 23°C or of ThO2(am→c) and ThO2(c) at 90°C. Solubility data were interpreted using the Pitzer ion-interaction model. The log of the solubility product for the thorium dioxide dissolution reaction [ThO2(s) + 2 H2O ↔ Th4+ + 4 OH-] was determined to be -44.9 for ThO2(am) at 23°C, ≥-56.9 for ThO2(c) at 23°C, and -51.4 for ThO2(c) at 90°C. At 90°C, a relatively less crystalline phase, ThO2(am→c), showed slightly higher solubility (log Ksp = -49.2) than crystalline ThO2(c).
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Articles in the same Issue
- Investigation of 50Cr(d,n)51Mn and natCr(p,x)51Mn processes with respect to the production of the positron emitter 51Mn
- Fluoride complexation of rutherfordium (Rf, element 104)
- Continuous on-line chromatography of short lived isotopes of tungsten as homolog of seaborgium (element 106)
- Cation-cation complexes of PuO2+ and NpO2+ with Th4+ and UO22+
- The influence of dibutylphosphate on actinide extraction by 30% tributylphosphate
- Synthesis and spectroscopic properties of neptunium VI and plutonium VI oxoanion compounds
- Thermodynamic model for the solubility of thorium dioxide in the Na+-Cl--OH--H2O system at 23°C and 90°C
- Uranium and thorium isotopes in some red sea sediments