The hydration of CA2 (CaAl4O7) is usually a slow process. However, we found that CA2 is easily grindable and that the BET surface area and the amount of X-ray amorphous phase highly influence the hydration kinetics. Tempering of ground samples significantly decreased the BET surface area and the amount of X-ray amorphous phase. The hydration of tempered CA2 started later and proceeded much more slowly. A different degree of crystallinity of CA2 explains the wide range of different hydration kinetics and especially the occurrence of the often observed exothermic heat flow peak prior to the CA2 main reaction. By different grinding procedures and tempering we were able to prepare samples that were completely hydrated within 24h and such samples which did not react within 24h. Using heat flow calorimetry, in-situ XRD and in-situ ¹H-TD-NMR we show that X-ray amorphous CA2 reacts prior to crystalline CA2.

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grinding heat flow calorimetry insitu xrd insitu sup locpre1suphtdnmr cainf locpost2inf caalinf locpost4infoinf bet surface area hydration kinetics

J. Neubauer,F. Hueller, D. Ectors, F. Goetz-Neunhoeffer,.Influence of crystallinity and surface area on the hydration kinetics of CA2. 89 (0),136-144.

J. Neubauer, et al."Influence of crystallinity and surface area on the hydration kinetics of CA2" 89

J. Neubauer,F. Hueller, D. Ectors, F. Goetz-Neunhoeffer,"Influence of crystallinity and surface area on the hydration kinetics of CA2"