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Initial structure memory of pressure-induced changes in the phase-change memory alloy Ge2Sb2Te5
M Krbal1, A V Kolobov, J Haines
1Institut Charles Gerhardt, UMR 5253 CNRS-UM2-ENSCM-UM1, PMDP/PMOF, Université Montpellier II, Place Eugène Bataillon, Montpellier Cedex 5, France.
Physical Review Letters
|October 2, 2009
Summary
Ge2Sb2Te5
Area of Science:
- Materials Science
- Solid-state Chemistry
- Geochemistry
Background:
- Ge2Sb2Te5 is a phase-change material with potential applications in data storage.
- Understanding its structural behavior under pressure is crucial for optimizing its performance.
- The material exists in different crystalline phases, including face-centered cubic (fcc) and trigonal.
Purpose of the Study:
- To investigate the structural response of Ge2Sb2Te5 to hydrostatic compression.
- To compare the behavior of the metastable fcc phase and the stable trigonal phase.
- To elucidate the mechanisms behind structural changes and phase transitions.
Main Methods:
- Hydrostatic compression experiments using a diamond anvil cell.
- In-situ X-ray diffraction (XRD) to monitor structural changes.
- Analysis of phase transitions and structural recovery upon decompression.
Main Results:
- The metastable fcc phase of Ge2Sb2Te5 amorphizes around 15 GPa.
- The stable trigonal phase remains crystalline under similar compression.
- Both phases transform to a body-centered cubic (bcc) phase around 30 GPa.
- Upon decompression, the amorphous phase is retained from the initial fcc phase, while the trigonal phase recovers its initial structure.
Conclusions:
- The presence of vacancies and atomic displacements in the fcc phase leads to nanoscale phase separation.
- This phase separation results in a loss of structural memory in the amorphous Ge2Sb2Te5.
- The trigonal phase's structural integrity is maintained due to its crystalline nature and fewer vacancies.
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