X-ray absorption and photoemission spectroscopies, high-resolution electron energy loss spectroscopy, spot profile analysis low energy electron diffraction, and density functional theory calculations are employed to study the growth of (001) oriented ${\mathrm{Mn}}_3{\mathrm{O}}_4$ surfaces on a Pd(100)-supported MnO(001) substrate, with the Hausmannite planar lattice constants aligned along the [110] direction of the underlying MnO(001) support. We show that despite the rather large lattice mismatch, abrupt interfaces may exist between rocksalt MnO and Hausmannite. We argue that this process is facilitated by the relatively low computed strain energy and we propose realistic models for the interface. An atop site registry between the Mn(O) atoms of the oxygen rich ${\mathrm{Mn}}_3{\mathrm{O}}_4$ termination and the MnO(001) O(Mn) atoms underneath is found to be the energetically most favorable configuration. The significant planar expansion is accompanied by a large compression of the ${\mathrm{Mn}}_3{\mathrm{O}}_4$ vertical lattice constant, yielding structural distortion of the O-Mn-O octahedral axis. Spot profile analysis low energy electron diffraction experiments show that the conversion reaction proceeds easily in both directions, thus indicating the reversible redox character of the transition.

• Received 29 June 2007

DOI:https://doi.org/10.1103/PhysRevB.76.165428