Abstract
The crystal structure, magnetic and local ferroelectric properties of polycrystalline Bi1-xGdxFeO3 (x = 0.1, 0.2, 0.3) samples were investigated at room temperature. Gadolinium substitution was found to induce a polar-to-polar R3c → Pn21a structural phase transition at x ≈ 0.1. Increasing the content of the substituting element suppressed the spontaneous polarization in Bi1-xGdxFeO3, resulting in a ferroelectric-paraelectric Pn21a → Pnma phase transition at 0.2 < x < 0.3. The substitution caused the appearance of a weak ferromagnetic moment. The data presented are consistent with the hypothesis that the most effective way to induce spontaneous magnetization in antiferromagnetic BiFeO3 seems to be related to A-site substitution by rare-earth ions with a large difference in ionic radius with respect to Bi3+. The effect of the magnetically active Gd3+ substitution on the low-temperature magnetic properties of Bi1-xGdxFeO3 samples is also discussed.
| Original language | English |
|---|---|
| Pages (from-to) | 5137-5145 |
| Number of pages | 9 |
| Journal | Acta Materialia |
| Volume | 57 |
| Issue number | 17 |
| DOIs | |
| Publication status | Published - Oct 2009 |
| Externally published | Yes |
Keywords
- Ferroelectricity
- Magnetic properties
- Multiferroics
- Perovskites
- X-ray diffraction
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