Abstract

Synthetic Mg2TiO4 qandilite was investigated to 50 and 40.4 GPa at room temperature using Raman spectroscopy and X-ray diffraction, respectively. The Raman measurements showed that cubic Mg2TiO4 spinel transforms to a high pressure tetragonal (I41/amd, No.141) phase at 14.7 GPa. Owing to sluggish kinetics at room temperature, the spinel phase coexists with the tetragonal phase between 14.7 and 24.3 GPa. In the X-ray diffraction experiment, transformation of the cubic Mg2TiO4 to the tetragonal structure was complete by 29.2 GPa, ~5 GPa higher than the transition pressure obtained by Raman measurements, owing to slow kinetics. The obtained isothermal bulk modulus of Mg2TiO4 spinel is KT0 = 148(3) GPa when KT0’ = 6.6, or KT0 = 166(1) GPa when KT0’ is fixed at 4. The isothermal bulk modulus of the high-pressure tetragonal phase is calculated to be 209(2) GPa and V0 = 270(2) Å3 when KT0’ is fixed at 4, and the volume reduction on change from cubic to tetragonal phase is about 9%. The calculated thermal Grüneisen parameters (γth) of cubic and tetragonal Mg2TiO4 phases are 1.01 and 0.63. Based on the radii ratio of spinel cations, a simple model is proposed to predict post-spinel structures.

Highlights

  • Synthetic Mg2TiO4 qandilite was investigated to 50 and 40.4 GPa at room temperature using Raman spectroscopy and X-ray diffraction, respectively

  • In situ high- pressure Raman measurements and equations of states of both spinel and post-spinel structures of synthetic Mg2TiO4 qandilite were investigated at room temperature

  • The cubic Mg2TiO4 spinel fully transformed to a tetragonal phase above 24.3 GPa and the new phase persisted to 50 GPa

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Summary

Introduction

Synthetic Mg2TiO4 qandilite was investigated to 50 and 40.4 GPa at room temperature using Raman spectroscopy and X-ray diffraction, respectively. The isothermal bulk modulus of the high-pressure tetragonal phase is calculated to be 209(2) GPa and V0 = 270(2) Å3 when KT0’ is fixed at 4, and the volume reduction on change from cubic to tetragonal phase is about 9%. In addition to the orthorhombic structures, a tetragonal structure (space group I41/amd) was reported for post-spinel phases at high pressure conditions as an intermediate phase[20,21,22,23,24,25]. In situ high- pressure Raman measurements and equations of states of both spinel and post-spinel structures of synthetic Mg2TiO4 qandilite were investigated at room temperature. The post-spinel phase was identified and a model for prediction of post-spinel structure is reported

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