This work deals with the identification and kinetics of crystallisation of
the wollastonite polytypes which form in the system CaO-SiO2 in the tempera
ture range 700-1000 degrees C. The kinetics of phase transformations in the
system have been determined from analysis of in situ synchrotron X-ray pow
der diffraction data. Two different systems with the same compositions were
investigated: one is more reactive, having grains with a larger surface ar
ea per unit volume, the other is less reactive, being composed of grains wi
th a smaller surface area per unit volume. 1T-wollastonite forms first and
progressively transforms in an intermediate 1Td-wollastonite disordered for
m. Both phases in turn transform into 2M-wollastonite polytype. Differences
in the polytypes forming and reaction kinetics were observed for the two s
ystems. In the more reactive system, the conversion 1T to 1Td polytypes is
the dominant process. The kinetic parameters calculated using the Avrami mo
dels fully describe the reaction process of formation of both polytypes and
transformation of one polytype into the other.