Key points are not available for this paper at this time.
Investigations of tricalcium silicate (C 3 S) suspensions using different techniques have shown the initial hydration kinetics of C 3 S are strongly dependent on the water/C 3 S ratio. In order to provide new experimental data on the hydration, we have adapted a Tian‐Calvet heat flow isothermal microcalorimeter to study thermal flow variation released by C 3 S stirred suspensions in water and saturated lime water. We observed three exothemic peaks and one endothermic peak. Their relative magnitude and duration depend on the W/C ration and the lime solution concentration. The protective layer theory appears to be consistent with our results for high W/C ratio. Moreover, portlandite precipitation seems to be a consequence and not the cause of the acceleratory period.
Damidot et al. (Thu,) studied this question.