摘要

The crystallization behavior of mineral wool was investigated by means of differential thermal analysis (DTA) and X-ray diffraction (XRD). DTA curves reveal the presence of two overlap exothermic peaks and XRD results shows that two crystalline phases are separated out: one is akermanite-gehlenite (AlCa2Mg0.5O7Si1.5), which was crystallized between 850°C and 920°C; the other is anorthite (CaAl2Si2O8), which was crystallized between 880°C and 1 010°C. The Ozawa method and the modified Kissinger method were used to analyze the crystallization mechanism and the activation energy of crystallization. For the crystalline of akermanite-gehlenite, the activation energy of crystallization and the Avrami exponent are 248 kJ&middotmol-1 and 0.682 respectively, indicating surface crystallization; whereas for anorthite, the activation energy of crystallization is 347 kJ&middotmol-1, revealing three-dimensionality of crystal growth according to the results of scanning electron microscopy (SEM).

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