Investigation of amorphization effects on wollastonite and diopside crystals, indicating rapid structure changes.
The amorphization of wollastonite (CaSiO3) and diopside (CaMgSi2O6) crystals by conventional ball milling under the dry condition and the atomic-scale structures of their amorphous phases were investigated by powder X-ray diffraction (XRD) analysis and Fourier transformed infrared (FT-IR) spectroscopy. The obtained results indicate that both wollastonite and diopside crystals were almost amorphized by ball milling. Moreover, the wollastonite crystal amorphized faster than the diopside crystal. The atomic-scale structures of the amorphous phases in the milled wollastonite and diopside obtained by X-ray radial distribution analyses were approximately similar to those in the fused glasses of wollastonite and diopside, respectively. However, FT-IR data may indicate that the single chains of SiO4 tetrahedra remained as the dominant species even in the wollastonite and diopside subjected to prolonged ball milling.
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Yoshitaka et al. (2021) studied this question.
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