The solubility of Sn(IV) in cementitious systems is directly related to the presence of dissolved Ca. In the presence of typical Ca concentrations, solid Ca[Sn(OH)6](s) is precipitated, resulting in dissolved tin(IV) concentrations that are about four to six orders of magnitude lower than observed in alkaline, Ca-free systems. From different experiments carried out in initially oversaturated and undersaturated solutions, solubility products have been evaluated.
A constant of 109.85 at I=0 has been derived for the formation of fresh Ca[Sn(OH)6](precip) according to the reaction Ca2++{Sn(OH)62- ↔ Ca[Sn(OH)6](s). A constant of 1010.93 has been derived in undersaturation experiments for the equilibrium with crystalline Ca[Sn(OH)6](cr).
Print ISSN: 0033-8230
Volume: 88, 09/2000
Pages: 521