
Abstract
Recently Tobin et al (2007 J. Phys.: Condens. Matter 19 315218) reported on the spin-resolved photoemission study of Fe3O4(001) films, claiming magnetite being a case against half-metallicity. In the present communication we re-examine recent spin-resolved photoemission experiments on Fe3O4 and explain why their criticism is unfounded.
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-18961-8 |
Language: | English |
Item ID: | 18961 |
Date Deposited: | 10. Mar 2014, 14:17 |
Last Modified: | 04. Nov 2020, 13:00 |