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Direct Observations of a Dynamically Driven Phase Transition with in situ X-Ray Diffraction in a Simple Ionic Crystal
Patricia Kalita1, Paul Specht1, Seth Root1
1Sandia National Laboratories, Albuquerque, New Mexico 87125, USA.
We observed the fluorite to cotunnite phase transition in calcium fluoride (CaF2) under high pressure. This study reveals the transition kinetics on nanosecond and minute timescales using synchrotron X-ray diffraction.
Area of Science:
- High-pressure physics
- Materials science
- Solid-state chemistry
Background:
- Calcium fluoride (CaF2) serves as a model AB2 structure for studying phase transitions.
- Understanding phase transitions in ionic solids is crucial for materials science and geophysics.
Purpose of the Study:
- To investigate the real-time kinetics and hysteresis of the fluorite to cotunnite structural phase transition in CaF2.
- To provide insights into the transition mechanisms under dynamic and static compression.
Main Methods:
- In situ synchrotron X-ray diffraction.
- Dynamic loading up to 27.7 GPa.
- Static compression.
- Rietveld refinement techniques.
Main Results:
- Real-time observations of the fluorite to cotunnite phase transition were achieved.
- The kinetics and hysteresis of the transition were examined on nanosecond and minute timescales.
- Data provides insight into the kinetic time scale of the transition under shock compression.
Conclusions:
- The study elucidates the dynamic behavior of the CaF2 phase transition.
- Findings are relevant to isomorphic compounds and high-pressure physics applications.
- Real-time diffraction offers a powerful tool for studying rapid material transformations.
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