Magnetite (or Fe3O4) is an elaborate kind of rust - a regular lattice of oxygen and iron atoms. But this material plays an increasingly important role
as a catalyst, in electronic devices and in medical applications.
Scientists at the Vienna University of Technology have now shown that the atomic structure of the magnetite surface, which everybody had assumed to be
well-established, has in fact been wrong all along. The properties of magnetite are governed by missing iron atoms in the sub-surface layer. "It turns
out that the surface of Fe3O4 is not Fe3O4 at all, but rather Fe11O16", says Professor Ulrike Diebold, head of the metal-oxide-research group at TU
Wien (Vienna). The new findings have now been published in the journal Science.
Perhaps the most surprising property of the magnetite surface is that single atoms placed on the surface, for instance gold or palladium, stay
perfectly in place instead of balling up and forming a nanoparticle. This effect makes the surface an extremely efficient catalyst for chemical
reactions - but nobody had ever been able to tell why magnetite behaves that way.
Very often, the properties of metal oxides depend on oxygen vacancies in the topmost atomic layers. Depending on the environment, some oxygen atoms on
the surface may be missing. This can dramatically influence the electronic properties of the material. "Everyone in our community thinks about missing
oxygen atoms. That is why it took us quite a while to figure out that it is in fact missing iron atoms that do the trick", says Gareth Parkinson. [1] |