Crystal Chemistry of Hydrous Calcium Silicates: I, Substitution of Aluminum in Lattice of Tobermorite

Mixtures of 0.8 moles of CaO per mole of SiO₂ plus Al₂O₃ were prepared from lime, kaolin, and tripoli (microcrystalline quartz); the amounts of SiO₂ to Al₂O₃ were varied to give from 0.2 to 20.7% Al₂O₃ by weight of dry solids. After hydrothermal treatment (170° to 175°C.), the products were examined by differential thermal analysis and by X-ray diffraction. A homogeneous solid identified as the mineral tobermorite (4CaO.5SiO₂.5H₂O) and containing up to 4 or 5% Al₂O₃ was obtained. Increasing the amount of Al₂O₃ in the raw mixture above about 5% resulted in the formation of the hydrogarnet 3CaO.Al₂O₃.SiO₂.4H₂O as a second phase. Allowing for the Al₂O₃ combined in this solid, it was indicated that slightly more Al₂O₃ was substituted in the tobermorite as the amount was increased in the raw mixture. It is suggested that the Al³⁺ ions probably assume tetrahedral coordination when substituting for the Si⁴⁺ ions.