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Methods of Ex Situ and In Situ Investigations of Structural Transformations: The Case of Crystallization of Metallic Glasses
Published on: June 7, 2018
Heterogeneous grain-scale response in ferroic polycrystals under electric field
John E Daniels1, Marta Majkut2, Qingua Cao1
1School of Materials Science and Engineering, UNSW Australia, Sydney NSW 2052, Australia.
Researchers used 3D X-ray diffraction (3D-XRD) to study ferroelectric domain switching in polycrystalline ceramics. Individual grain behavior deviates from averages due to local heterogeneities, but these effects average out across multiple grains.
Area of Science:
- Materials Science
- Condensed Matter Physics
- Crystallography
Background:
- Understanding ferroic properties in polycrystalline materials is challenging due to limitations in probing individual grain behavior.
- Grain boundaries and clusters significantly influence ferroic property coupling.
Purpose of the Study:
- To investigate ferroelectric domain switching at the individual grain scale within bulk polycrystalline electro-ceramics.
- To identify factors influencing domain switching behavior and deviations from average properties.
Main Methods:
- Utilized a variant of three-dimensional X-ray diffraction (3D-XRD) to resolve non-180° ferroelectric domain switching strain components.
- Analyzed data from 191 individual grains in a polycrystalline electro-ceramic undergoing electric-field-induced phase transformation.
Main Results:
- Grain orientation significantly impacts phase and domain texture, but substantial deviations from average behavior were observed at the grain scale.
- Local strain and electric field heterogeneities within the polycrystal contribute to these deviations.
- Deviations at the grain scale were found to average out over approximately 10-20 grains.
Conclusions:
- Individual grain behavior in ferroic polycrystalline materials is highly heterogeneous.
- Local microstructural environments significantly influence ferroic property coupling.
- Results offer crucial insights for modeling ferroic materials at the grain scale.
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