The accuracy of published inorganic tin thermodynamic data was evaluated to
obtain a reliable basis for modeling Sn migration in a deep repository of
radioactive waste. Hydrolysis, complexation with halide ions or other inorg
anic compounds, and precipitation reactions of Sn(II) and Sn(IV) were studi
ed. The Guggenheim-Scatchard Specific Interaction Theory was used to correc
t equilibrium constant to zero ionic strength.
Tin(II) can be hydrolysed into SnOH+, Sn(OH)(2)(0) and Sn(OH)(3)(-) at low
concentration. For higher tin levels, the Sn-2(OH)(2)(2+) and Sn(OH)(4)(2+)
polynuclear species are predominant. Stability constants of these equilibr
ia at the standard state were evaluated from data available in the literatu
re and recommended values are proposed. Complexation reactions between tin(
II) and halide ions are well known, but the complex species formed are only
present in solution when halide concentration is >10(-3) mol L-1 and at pH
values <4. In the presence of sulphides, selenides, or tellurides, the sta
nnous ions form very stable solid phases. Because of the very low solubilit
y of SnO2(s), little information is available in the literature about Sn(IV
) hydrolysis, complexation, or precipitation reactions. Copyright (C) 2001
Elsevier Science Ltd.