4.7 Article

Stabilisation of Fe2O3-rich Perovskite Nanophase in Epitaxial Rare-earth Doped BiFeO3 Films

Journal

SCIENTIFIC REPORTS
Volume 5, Issue -, Pages -

Publisher

NATURE PUBLISHING GROUP
DOI: 10.1038/srep13066

Keywords

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Funding

  1. Engineering and Physical Sciences Research Council [EP/I038934/1]
  2. EPSRC
  3. National Science Foundation [1005771]
  4. National Security Science and Engineering Faculty Fellowship
  5. Australian Research Council [DP110101570]
  6. National Key Basic Research Program of China [2015CB921600]
  7. National Natural Science Foundation of China (NSFC) [11274222]
  8. QiMingXing Project from the Shanghai Municipal Science and Technology Commission [14QA1402000]
  9. Eastern Scholar Program
  10. Shuguang Program from the Shanghai Municipal Education Commission [12SG34]
  11. Engineering and Physical Sciences Research Council [EP/G069069/1, EP/I038934/1] Funding Source: researchfish
  12. Direct For Mathematical & Physical Scien
  13. Division Of Materials Research [1005771] Funding Source: National Science Foundation
  14. EPSRC [EP/I038934/1, EP/G069069/1] Funding Source: UKRI

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Researchers have demonstrated that BiFeO3 exhibits ferroelectric hysteresis but none have shown a strong ferromagnetic response in either bulk or thin film without significant structural or compositional modification. When remanent magnetisations are observed in BiFeO3 based thin films, iron oxide second phases are often detected. Using aberration-corrected scanning transmission electron microscopy, atomic resolution electron energy loss spectrum-mapping and quantitative energy dispersive X-ray spectroscopy analysis, we reveal the existence of a new Fe2O3-rich perovskite nanophase, with an approximate formula (Fe0.6Bi0.25Nd0.15)(3+) Fe3+O3, formed within epitaxial Ti and Nd doped BiFeO3 perovskite films grown by pulsed laser deposition. The incorporation of Nd and Bi ions on the A-site and coherent growth with the matrix stabilise the Fe2O3-rich perovskite phase and preliminary density functional theory calculations suggest that it should have a ferrimagnetic response. Perovskite-structured Fe2O3 has been reported previously but never conclusively proven when fabricated at high-pressure high-temperature. This work suggests the incorporation of large A-site species may help stabilise perovskite-structured Fe2O3. This finding is therefore significant not only to the thin film but also to the high-pressure community.

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