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Phase equilibria in TiO2-rich part of the MgO–CaO–TiO2 system at 1500–1600 °C

  • Min Chen
  • , Xingbang Wan*
  • , Pekka Taskinen
  • , Dmitry Sukhomlinov
  • , Junjie Shi
  • , Radoslaw Michallik
  • , Ari Jokilaakso
  • *Tämän työn vastaava kirjoittaja
  • Central South University
  • Northeastern University China
  • Geological Survey of Finland

Tutkimustuotos: LehtiartikkeliArticleScientificvertaisarvioitu

13 Viittaukset (Web of Science)
114 Lataukset (Pure)

Abstrakti

The equilibrium phase relations of the MgO–CaO–TiO2 system were investigated at 1500–1600 °C in air using the high-temperature isothermal equilibration of samples in platinum crucibles followed by the rapid quenching technique. The phase compositions were analyzed using an electron probe X-ray microanalyzer (EPMA). The isothermal sections at 1500 °C and 1600 °C were constructed based on the experimentally determined liquid phase compositions. The present results deviate significantly from previous observations as well as the predictions by MTDATA and FactSage using their oxide databases, in particular in the perovskite primary phase field.

AlkuperäiskieliEnglanti
Sivut20116-20125
Sivumäärä10
JulkaisuCeramics International
Vuosikerta48
Numero14
Varhainen verkossa julkaisun päivämäärähuhtik. 2022
DOI - pysyväislinkit
TilaJulkaistu - 15 heinäk. 2022
OKM-julkaisutyyppiA1 Alkuperäisartikkeli tieteellisessä aikakauslehdessä

Rahoitus

The use of the Academy of Finland's RawMatTERS Finland Infrastructure (RAMI), housed jointly at Aalto University, GTK, and VTT in Espoo, is greatly acknowledged. Min Chen is grateful for the financial support from the China Scholarship Council (#201806370217). This work is partly financed by Aalto University, School of Chemical Engineering as well as the Natural Science Foundation of Liaoning Province (2021-MS-083). The authors would like to thank Ms. Fabiola Lasar and Mr. Kezhou Song for the assistance in experiments. Dr. Lassi Klemettinen is greatly acknowledged for his valuable discussion. The use of the Academy of Finland's RawMatTERS Finland Infrastructure (RAMI), housed jointly at Aalto University, GTK, and VTT in Espoo, is greatly acknowledged. Min Chen is grateful for the financial support from the China Scholarship Council (# 201806370217 ). This work is partly financed by Aalto University, School of Chemical Engineering as well as the Natural Science Foundation of Liaoning Province (2021-MS-083). The authors would like to thank Ms. Fabiola Lasar and Mr. Kezhou Song for the assistance in experiments. Dr. Lassi Klemettinen is greatly acknowledged for his valuable discussion.

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