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学術論文

Insights into the structural, electronic, and magnetic properties of Fe2-xTixO3/Fe2O3 thin films with x=0.44 grown on Al2O3 (0001)

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引用

Dennenwaldt, T., Lübbe, M., Winklhofer, M., Müller, A., Döblinger, M., Nabi, H. S., Gandman, M., Cohen-Hyams, T., Kaplan, W. D., Moritz, W., Pentcheva, R., & Scheu, C. (2015). Insights into the structural, electronic, and magnetic properties of Fe2-xTixO3/Fe2O3 thin films with x=0.44 grown on Al2O3 (0001). Journal of Materials Science, 50(1), 122-137. doi:10.1007/s10853-014-8572-x.


引用: https://hdl.handle.net/11858/00-001M-0000-0024-B73D-0
要旨
The interface between hematite (alpha-(Fe2O3)-O-III) and ilmenite ((FeTiO3)-Ti-II), a weak ferrimagnet and an antiferromagnet, respectively, has been suggested to be strongly ferrimagnetic due to the formation of a mixed valence layer of Fe2+/Fe3+ (1: 1 ratio) caused by compensation of charge mismatch at the chemically abrupt boundary. Here, we report for the first time direct experimental evidence for a chemically distinct layer emerging at heterointerfaces in the hematite-Ti-doped-hematite system. Using molecular beam epitaxy, we have grown thin films (similar to 25 nm thickness) of alpha-Fe2O3 on alpha-Al2O3 (0001) substrates, which were capped with a similar to 25 nm thick Fe2-xTixO3 layer (x = 0.44). An additional 3 nm cap of alpha-Fe2O3 was deposited on top. The films were structurally characterized in situ with surface X-ray diffraction, which showed a partial low index orientation relationship between film and substrate in terms of the [0001] axis and revealed two predominant domains with (0001)(Fe2O3) vertical bar vertical bar (0001)(Al2O3,) one with [10 (1) over bar0](Fe2O3) vertical bar vertical bar [10 (1) over bar0](Al2O3), and a twin domain with [01 (1) over bar0](Fe2O3) vertical bar vertical bar [10 (1) over bar0]Al2O3. Electron energy loss spectroscopy profiles across the Fe2-xTixO3/Fe2O3 interface show that FeFe2+/Fe3+ ratios peak right at the interface. This strongly suggests the formation of a chemically distinct interface layer, which might also be magnetically distinct as indicated by the observed magnetic enhancement in the Fe2-xTixO3/alpha-Fe2O3/Al2O3 system compared to the pure alpha-Fe2O3/Al2O3 system.