1. Phase equilibria relationship in the FetO-TiO2-CaO-SiO2 system with CaO/SiO2 weight ratio of 1.2 at 1673K.
- Author
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Li, Youyu and Yan, Baijun
- Subjects
- *
PHASE equilibrium , *ELECTRON probe microanalysis , *LIQUID crystal states , *PHASE separation , *X-ray diffraction - Abstract
Phase equilibria relationship in the Fe t O-TiO 2 -CaO-SiO 2 system with CaO/SiO 2 weight ratio of 1.2 under argon atmosphere were identified experimentally at 1673K by employing high-temperature equilibration method followed by electron probe X-ray microanalysis (EPMA) and X-Ray Diffraction (XRD) measurements. It was found that there exist 7 crystal phases and 1 liquid phase in the system, and 19 different kinds of phase equilibria relationship exist among these 8 phases. The 7 crystal phases are as follows: kilchoanite (Ca 3 Si 2 O 7), ulvöspinel (Fe 3-x Ti x O 4), pseudobrookite (FeO·2TiO 2), ilmenite (FeTiO 3), perovskite (CaTiO 3), rutile (TiO 2) and wüstite (Fe t O). By using L as the symbol for liquid phase, K for kilchoanite, U for ulvöspinel, B for pseudobrookite, I for ilmenite, P for perovskite, R for rutile and W for wüstite, the 19 phase equilibria relationships formed by these phases can be summarized as follows: 1) single L, 2) L + U, 3) L + R, 4) L + W, 5) L + K, 6) L + I, 7) L + B, 8) L + P, 9) L + R + P, 10) L + I + P, 11) L + B + I, 12) L + R + B, 13) L + U + W, 14) L + U + I, 15) L + U + P, 16) L + P + B, 17) L + U + I + P, 18) L + R + B + P, and 19) L + B + I + P. Finally, based on the above-determined phase equilibria relationship, a section phase diagram of the system at 1673K was constructed. From the constructed phase diagram, the evolution of phases caused by composition change can be seen graphically. [ABSTRACT FROM AUTHOR]
- Published
- 2024
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