Effect of Crystal Grain Size and Thermal Stress on Martensitic Transformation of Phosphorus-Bearing Dicalcium Silicates

A series of P₂O₅-bearing Ca₂SiO₄ solid solutions, (Ca_{2- x /2}open square _{x /2})(Si_{1- x} P _x )O₄ with x = 0.02 and 0.06 lessthan equal to 0.11, was prepared. The alpha´_L <–> ß martensitic transformation temperatures were determined by high-temperature XRD for powder specimens with x = 0.02. With decreasing particle size, both M _s and M _f decreased, while both A _s and A _f were almost unchanged. Each transformation temperature was lower than that of pure Ca₂SiO₄. The phase composition at 25°C for the crystals with 0.075 lessthan equal to x lessthan equal to 0.10 was dependent not only on the x -value but also on the particle size and the intensity of the thermal stress upon quenching. The effect of the latter two was most clearly recognized in the phase composition of the crystals with x = 0.09. The phase composition was changed between the two extremes; one was composed of 8% alpha´_L-phase and 92%ß-phase and the other was 96% alpha´_L-phase and 4%ß-phase. For the crystals with 0.06 lessthan equal to x lessthan equal to 0.065 (ß-phase) and 0.105 lessthan equal to x lessthan equal to 0.11 (alpha´_L-phase), only the x -value governed the phase composition.