Thermal behaviour of tobermorite from N'Chwaning II mine (Kalahari Manganese Field, Republic of South Africa). I. Thermo-gravimetric and X-ray diffraction studies

摘要

The minerals belonging to the tobermorite group differ essentially by their basal spacing (approximately 14, 11, and 9 A), related to their water content; additionally, the phases with an 11 A periodicity differ in their behaviour upon heating, which can be "normal" if they collapse to form a 9 A phase or "anomalous" if they preserve their original basal spacing. The "anomalous" thermal behaviour of tobermorite 11 A from N'Chwaning II mine (Kalahari Manganese Field, Republic of South Africa), which does not shrink at 300 ℃, is accurately studied by means of thermo-gravimetric and differential scanning calorimetric (TG-DSC) analysis and in situ and ex situ X-ray diffraction experiments. In situ X-ray powder diffraction shows that at ~ 420 ℃, tobermorite 11 A transforms into a phase with a basal spacing of approximately 10.1 A, namely "tobermorite 10 A". The TG-DSC study shows a twostep weight loss: the former occurs between room temperature and 300 ℃, whereas the latter is observed between 500 ℃ and 600 ℃. These two steps correspond to endothermic and exothermic processes, respectively, which are related to the dehydration of tobermorite and its transformation into tobermorite 10 A. Above 1000 ℃, tobermorite 10 A transforms into wollastonite. Finally, ex situ X-ray diffraction studies, using both powder and single-crystal techniques, show that the transformation from the 11 A to the 10 A phase passes through an intermediate clinotobermorite-like phase.