The Finer Details of Rust

Magnetite (Fe₃O₄) is one of the Earths' oldest known, most naturally abundant and cost affective materials. In the bulk it exhibits interesting phenomena such as ferrimagnetism, half-metallicity, and the Verwey transition, in which almost all the properties change drastically on cooling through 123 K. Fe₃O₄ plays an important role in many natural and man made processes. For example, magnetite nanoparticles are present in the beaks of homing pigeons (thought to be related to the sensing of the Earths magnetic field). Fe₃O₄ particles can be dragged around the body using magnets to deliver drugs in a highly localized way. However, while the bulk properties are much studied, much less work has gone into studying the surfaces, which turn out to be critical to the function performed in the majority of applications.

Our group has been interested in Fe₃O₄ surfaces since we published the first atomically resolved image of the Fe₃O₄(001) in 2000 [1]. In the last two years we have come back to this surface and begun to study the surface chemistry in detail. By systematically varying the preparation conditions, we found that several highly ordered metastable Fe terminated surfaces can be created [2]. The ability to tailor the surface structure in this way presents an unrivalled opportunity to investigate the effect of cation concentration and co-ordination on the surface reactivity [2].

So far, our investigations have produced very interesting results. We have found that a small lattice distortion (which is responsible for the opening of a surface band gap) plays a huge role in the adsorption of small molecules. Covering the surface in atomic H re-metallizes the surface [3], while water undergoes a highly unusual adsorption process in which only H atoms are deposited at room temperature [4]. This mechanism is linked to the adsorption geometry in the distorted surface, which isolates adsorbed H and OH.

Many applications of Fe₃O₄ contain Fe₃O₄-organic interfaces, yet there have been almost no studies of how organics adsorb at Fe₃O₄ surfaces. We are currently investigating interfaces important for biomedical and spintronic applications, which is required to understand how their properties affect the performance.

1. B. Stanka, W. Hebenstreit, U. Diebold, S. A. Chambers
   Surface Reconstructions of Fe3O4(001)
   Surf. Sci. 448 (2000) 49-63 ⋅ full text*
2. G. S. Parkinson, Z. Novotný, P. Jacobson, M. Schmid, U. Diebold
   A metastable Fe(A) termination at the Fe3O4(001) surface
   Surf. Sci. 605 (2011) L42-L45 ⋅ full text*
3. G. S. Parkinson, N. Mulakaluri, Y. Losovyj, P. Jacobson, R. Pentcheva, U. Diebold
   Semiconductor-half metal transition at the Fe3O4(001) surface upon hydrogen adsorption
   Phys. Rev. B 82 (2010) 125413 ⋅ full text
4. G. S. Parkinson, Z. Novotný, P. Jacobson, M. Schmid, U. Diebold
   Room Temperature Water Splitting at the Surface of Magnetite
   J. Am. Chem. Soc. 133 (2011) 12650-12655 ⋅ full text*

* Please note: access to full text (PDF files) of some articles is restricted due to copyright reasons.