Se ha estudiado la influencia del humo de sílice sobre el mecanismo de hidratación del monoaluminato de calcio (CaAl 2 O 4 ) a temperatura ambiente y con una relación agua/sólidos de 0,5. La evolución de las fases hidratadas, que se forman en los primeros instantes de la reacción, se ha estudiado por difracción de rayos X de laboratorio con una resolución temporal de 36 min.
In situ X-ray difraction study of hidration of CaAl 2 O 4 -amorphous silica mixturesThe influence of the amorphous silica on the mechanism of hydration of the calcium monoaluminate (CaAl 2 O 4 ) has been studied at ambient temperature with a water/solids ratio of 0.5. The evolution of the hydrated phases, formed in the first instants of the reaction, has been studied by laboratory X ray diffraction with a time resolution of 36 min. The integration of selected diffraction peaks of the phases: Ca 2 Al 2 O 5 ·8H 2 O (Ca 2 Al 2 (OH) 10 ·3H 2 O), CaAl 2 O 4 and Ca 4 Al 2 (OH) 12 (CO 3 )·5H 2 O, has allowed to establish the kinetics of the reaction. This way, it has been shown that the amorphous silica causes a drastic decrease in the period of induction of the hydration and accelerates the formation of the metastable crystalline hydrates Ca 2 Al 2 (OH) 10 ·3H 2 O and Ca 4 Al 2 (OH) 12 (CO 3 )·5H 2 O. These results have been confirmed by Thermogravimetry, Differential Thermal Analysis and Scanning Electric Microscopy. The hydration mechanism proposed confirms previous data of Nuclear Magnetic Resonance of Solids (RMN) of 29 Si of the authors of this paper.