
Abstract
Using ab initio thermodynamics we compile a phase diagram for the surface of Fe3O4(001) as a function of temperature and oxygen pressures. A hitherto ignored polar termination with octahedral iron and oxygen forming a wavelike structure along the direction is identified as the lowest energy configuration over a broad range of oxygen gas-phase conditions. This novel geometry is confirmed via x-ray diffraction analysis. The stabilization of the Fe3O4(001) surface goes together with dramatic changes in the electronic and magnetic properties, e.g., a half metal to metal transition.
Item Type: | Journal article |
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Faculties: | Geosciences > Department of Earth and Environmental Sciences > Crystallography and Materials Science |
Subjects: | 500 Science > 530 Physics 500 Science > 540 Chemistry 500 Science > 550 Earth sciences and geology |
URN: | urn:nbn:de:bvb:19-epub-18543-1 |
Language: | English |
Item ID: | 18543 |
Date Deposited: | 10. Mar 2014, 14:10 |
Last Modified: | 04. Nov 2020, 13:00 |