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Updated: Jan 19, 2026
Phase Transitions and Effect of Intermolecular Forces
Phase transitions beyond post-perovskite in NaMgF3 to 160 GPa
Rajkrishna Dutta1, Eran Greenberg2, Vitali B Prakapenka2
1Department of Geosciences, Princeton University, Princeton, NJ 08544; rd7@princeton.edu.
Neighborite (NaMgF3) undergoes a series of phase transitions under high pressure, revealing a novel post-post-perovskite structure. This provides a model for understanding transitions in similar Earth and planetary materials.
Area of Science:
- Mineral Physics
- High-Pressure Geophysics
- Materials Science
Background:
- Neighborite (NaMgF3) serves as a model for ABX3 systems, crucial for understanding Earth's mantle and exoplanet interiors.
- Phase transitions in ABX3 compounds at high pressures are key to interpreting geophysical data.
Purpose of the Study:
- To experimentally investigate the high-pressure phase transitions of NaMgF3 up to 162 GPa.
- To identify novel high-pressure phases and transition pathways in ABX3 systems.
- To provide experimental validation for theoretical predictions of high-pressure mineral behavior.
Main Methods:
- Diamond anvil cell experiments were used to subject NaMgF3 to extreme pressures.
- X-ray diffraction was employed to analyze the structural changes and identify resulting phases.
Main Results:
- A sequence of phase transitions was observed: perovskite → post-perovskite → Sb2S3-type (post-post-perovskite) → NaF (B2) + NaMg2F5 (P2/c) → NaF (B2) + MgF2 (cotunnite-type).
- The study experimentally confirms the existence of an Sb2S3-type post-post-perovskite phase.
- The formation of the P2/c AB2X5 phase, previously only theorized, was experimentally demonstrated.
Conclusions:
- Neighborite exhibits a complete sequence of phase transitions from perovskite to breakdown into binary compounds under compression.
- The findings validate theoretical models and highlight the potential for similar transitions in geologically significant materials like MgSiO3.
- This research has implications for understanding the mineralogy and dynamics within the deep interiors of large, rocky extrasolar planets.
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