Published October 25, 2017 | Version v1
Journal article

Phase equilibria of CaO-SiO2-5wt.%MgO-30 wt.%Al2O3-TiO2 system at 1400 °C and 1450 °C relevant to high Al2O3 Ti-bearing blast furnace slag system

  • 1. School of Metallurgy, Northeastern University, Shenyang, 110819 (China)
  • 2. Key Laboratory for Ecological Metallurgy of Multimetallic Ores (Ministry of Education), Shenyang, 110819 (China)

Description

Due to the important effect of Al2O3 addition to the phase change in Ti-bearing slag system, the phase equilibrium relationships were investigated for the CaO-SiO2-5wt.%MgO-30 wt.%Al2O3-TiO2 phase diagram system with high Al2O3 content. The equilibrium phases were experimentally determined at 1400 °C and 1450 °C using the high temperature equilibrium technique followed by X-Ray Fluoroscopy (XRF), X-Ray Diffraction (XRD), Scanning Electron Microscope (SEM) and Energy Dispersive X-ray spectroscope (EDX) analysis. The gehlenite phase (2CaO·Al2O3·SiO2), perovskite phase (CaO·TiO2), spinel phase (MgO·Al2O3), Ti-rich diopside solid solution phase and anosovite solid solution phase were found. Based on the experimental results, the 1400 °C and 1450 °C isotherms and phase relations were obtained for CaO-SiO2-5wt.%MgO-30 wt.%Al2O3-TiO2 system relevant to high Al2O3 Ti-bearing slag system. - Highlights: • Phase diagram of CaO-SiO2-5wt.%MgO-30 wt. %Al2O3-TiO2 system is established. • The equilibria phase of 2CaO·Al2O3·SiO2, CaO·TiO2, MgO·Al2O3, Ti-rich diopside and anosovite are found at 1400 °C. • The equilibria phase of 2CaO·Al2O3·SiO2 and MgO·Al2O3 are found at 1450 °C. • Liquidus lines were constructed at 1400 °C and 1450 °C, respectively.

Availability note (English)

Available from http://dx.doi.org/10.1016/j.jallcom.2017.06.058

Additional details

Identifiers

DOI
10.1016/j.jallcom.2017.06.058;
PII
S0925-8388(17)32045-5;

Publishing Information

Journal Title
Journal of Alloys and Compounds
Journal Volume
722
Journal Page Range
p. 25-32
ISSN
0925-8388
CODEN
JALCEU

Optional Information

Copyright
Copyright (c) 2017 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.