Thaumasite Ca6[Si(OH)6]2(CO3) 2(SO4)2·24H2O is a product of low temperature sulphate attack under conditions favourable for its formation. It is a complex calcium carbonate silicate sulphate hydroxide hydrate, which has no binding capacity. There are actually two reactions for thaumasite formation, both of which arise below ca. 15°C. They are very slow and usually occur simultaneously in
... [Show full abstract] Portland-based cementitious systems. One reaction involves C-S-H reacting directly with carbonates and sulphates in the presence of calcium ions and excess water. The other reaction takes place once ettringite is formed, by engulfing the latter with C-S-H, sulphate and carbonate in the presence of calcium ions. This first of all converts ettringite into woodfordite (a solid solution whose end members are ettringite and thaumasite) and thence into thaumasite. Both thaumasite-forming reactions are also interdependent, since they are effectively competing for the same mass of C-S-H, carbonate and sulphate in many instances within each hydrating Portland-based cement system. There are no thermodynamic data yet available for these reactions. The formation of thaumasite at low temperatures and ordinary pressures can be explained by the need to stabilise the transition state intermediate sufficiently long to allow for [Si(OH)6]2- groups to form in a stable configuration, which is assisted by delocalisation of charge on to the planar CO2-3 groups. The lack of binding power for thaumasite causes its destructive sulphate attack. Once formed thaumasite is actually more stable than ettringite and decomposes at ca. 110°C to form a disordered structure ("thaumasite glass") that contains SiO2-4 tetrahedra.