Impact of high temperature and pressure on the structure and phase transition of Mg2SiO4 oxide via molecular dynamics simulation

This article investigates the effects of high temperature and high pressure (P) on the structure and phase transition process of Mg 2 SiO 4 oxide using molecular dynamics simulations with Oganov's pair interaction potential. The study reveals that as the temperature increases from 300 K to 6000 K, Mg 2 SiO 4 transitions from an amorphous state to a liquid state. This transition is accompanied by an increase in lengths of the links (Mg-Mg, Mg-Si, Mg-O, Si-Si, Si-O, O-O) and changes in the numbers of structural units (SiO 4 , SiO 5 , SiO 6 , MgO 3 , MgO 4 , MgO 5 , MgO 6 ). While the total system size and total energy of systems increase, the bond angles of Si-O-Si and Mg-O-Mg remain relatively stable under 0 GPa. The phase transition temperature (T m ) of Mg 2 SiO 4 is determined to be 2168 K. Furthermore, varying P from 0 to 200 GPa at temperatures of 300, 1000, 2000, 4000, and 6000 K reveals a relationship between temperature and pressure. At 300 K, the system can withstand a maximum pressure of 200 GPa, while at 6000 K, the minimum pressure is 0 GPa. These findings provide valuable insights for future experimental research and contribute to the development of high-performance materials for applications in the communications industry. • The Oganov pair interaction force field effectively models the structural and thermodynamic properties of Mg 2 SiO 4 under varying temperature and pressure. • Temperature increase from 300 K to 6000 K induces structural changes, expansion of the material, and a phase transition at T g = 2168 K. • Pressure increase at different temperatures reduces system size and total energy, • Higher pressures lead to the formation of high-coordination Mg-O units (MgO 7 – MgO 10 ), • The observed trends suggest lower compressibility of Mg 2 SiO 4 at high temperatures,

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Publication Details

Journal
Physica B Condensed Matter
Published
2025-09-08
DOI
https://doi.org/10.1016/j.physb.2025.417784
Citations
1
Primary Topic
High-pressure geophysics and materials
Type
article
Field-Weighted Citation Impact
1.87
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article

Impact of high temperature and pressure on the structure and phase transition of Mg2SiO4 oxide via molecular dynamics simulation

Tuan Tran Quoc, Ştefan Ţălu, Dũng Nguyễn Trọng
1 citations
Physica B Condensed Matter
High-pressure geophysics and materials
1.87
article

Impact of high temperature and pressure on the structure and phase transition of Mg2SiO4 oxide via molecular dynamics simulation

Tuan Tran Quoc, Ştefan Ţălu, Dũng Nguyễn Trọng
article en
1 citations

Abstract

This article investigates the effects of high temperature and high pressure (P) on the structure and phase transition process of Mg 2 SiO 4 oxide using molecular dynamics simulations with Oganov's pair interaction potential. The study reveals that as the temperature increases from 300 K to 6000 K, Mg 2 SiO 4 transitions from an amorphous state to a liquid state. This transition is accompanied by an increase in lengths of the links (Mg-Mg, Mg-Si, Mg-O, Si-Si, Si-O, O-O) and changes in the numbers of structural units (SiO 4 , SiO 5 , SiO 6 , MgO 3 , MgO 4 , MgO 5 , MgO 6 ). While the total system size and total energy of systems increase, the bond angles of Si-O-Si and Mg-O-Mg remain relatively stable under 0 GPa. The phase transition temperature (T m ) of Mg 2 SiO 4 is determined to be 2168 K. Furthermore, varying P from 0 to 200 GPa at temperatures of 300, 1000, 2000, 4000, and 6000 K reveals a relationship between temperature and pressure. At 300 K, the system can withstand a maximum pressure of 200 GPa, while at 6000 K, the minimum pressure is 0 GPa. These findings provide valuable insights for future experimental research and contribute to the development of high-performance materials for applications in the communications industry. • The Oganov pair interaction force field effectively models the structural and thermodynamic properties of Mg 2 SiO 4 under varying temperature and pressure. • Temperature increase from 300 K to 6000 K induces structural changes, expansion of the material, and a phase transition at T g = 2168 K. • Pressure increase at different temperatures reduces system size and total energy, • Higher pressures lead to the formation of high-coordination Mg-O units (MgO 7 – MgO 10 ), • The observed trends suggest lower compressibility of Mg 2 SiO 4 at high temperatures,

Physica B Condensed MatterVol. 717
Technical University of Cluj-Napoca (RO), University Of Transport Technology (VN)
Openalex Percentile: Top 14%
High-pressure geophysics and materials
1.87
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