Abstract
Magnetic contrast at the atomic level has been observed for the first time in scanning tunneling microscopy experiments on a magnetite (Fe3O4(001)) surface using in-situ prepared ferromagnetic Fe tips. A periodic corrugation with a 12 Å periodicity is clearly observed along the rows of FeB-sites which corresponds to the repeat period of Fe2+ and Fe3+ along these rows. This periodicity is not observed by using non-magneticW tips although the rows of FeB-sites can be resolved as well. The magnetic contrast observed with Fe tips is attributed to the different spin configurations of the magnetic ions Fe2+ and Fe3+ in Fe3O4.
References
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Wiesendanger, R., Shvets, I.V., Bürgler, D. et al. Magnetic imaging at the atomic level. Z. Physik B - Condensed Matter 86, 1–2 (1992). https://doi.org/10.1007/BF01323538
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DOI: https://doi.org/10.1007/BF01323538