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Updated: Feb 18, 2026

Methods of Ex Situ and In Situ Investigations of Structural Transformations: The Case of Crystallization of Metallic Glasses
Published on: June 7, 2018
Multiple pathways in pressure-induced phase transition of coesite
Wei Liu1, Xuebang Wu1, Yunfeng Liang2,3
1Key Laboratory of Materials Physics, Institute of Solid State Physics, Chinese Academy of Sciences, Hefei 230031, People's Republic of China.
High-pressure experiments reveal coesite transforms into a novel octahedral phase (HPO) and amorphous states. Molecular dynamics simulations explain these diverse transformation pathways under hydrostatic pressure.
Area of Science:
- Geophysics and materials science
- Mineral physics under extreme conditions
Background:
- Coesite, a dense silica phase, is known for pressure-induced amorphization.
- Previous studies observed different transformation pathways under hydrostatic pressure, leading to ambiguity.
Purpose of the Study:
- To elucidate the transformation mechanisms of coesite under high-pressure hydrostatic conditions.
- To explain the formation of the high-pressure octahedral (HPO) phase and amorphous silica.
Main Methods:
- High-pressure single-crystal X-ray diffraction with precise hydrostatic control (He or Ne).
- Ab initio parameterized potential molecular dynamics simulations.
Main Results:
- Reproduced experimental observations, including transformation to an HPO phase with a defective hcp oxygen sublattice.
- The HPO phase transforms into the α-PbO2 phase upon further compression.
- High-pressure amorphous silica phases are characterized by a mixture of fcc and hcp sublattices.
Conclusions:
- The HPO phase forms via continuous oxygen sublattice rearrangement towards an hcp arrangement.
- Molecular dynamics simulations successfully model diverse coesite transformation pathways under pressure.
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