Abstract
We present a first-principles investigation of the structural, electronic, and magnetic properties of ultrathin FeO(0001) films on a polar MgO(111) substrate. The results imply that the heterointerface is atomically abrupt with oxidelike stacking for film thicknesses between 1.5 and 8.5 Å. The Fe-Fe bilayer (nominal separation of 0.59 Å in FeO) at the interface collapses into an “Fe” monolayer. Both electronic polarization and structural relaxations effectively screen the dipole field of the polar interface system. The structural relaxations—consisting of interpenetration, separation, and merger of Fe and oxygen planes—are particularly drastic in the three- and four-bilayers-thick films, giving rise to barrierless movement of oxygen towards the surface and the formation of an “FeFeO” layer structure not seen in hematite. Comparisons to calculations of unsupported polar FeO(0001) slabs demonstrate that these unusual changes in stacking sequence and electronic structure are associated with the polar nature of this oxide heterointerface.
- Received 3 June 2012
DOI:https://doi.org/10.1103/PhysRevB.86.035431
©2012 American Physical Society