An experimental and computational investigation of structure and magnetism in pyrite CoFeS: Chemical bonding and half-metallicity
arXiv:cond-mat/0404660 · doi:10.1103/PhysRevB.70.214409
Abstract
Bulk samples of the pyrite chalcogenide solid solutions CoFeS 0 <= x <= 0.5, have been prepared and their crystal structures and magnetic properties studied by X-ray diffraction and SQUID magnetization measurements. Across the solution series, the distance between sulfur atoms in the persulfide (S) unit remains nearly constant. First principles electronic structure calculations using experimental crystal structures as inputs point to the importance of this constant S-S distance, in helping antibonding S-S levels pin the Fermi energy. In contrast hypothetical rock-salt CoS is not a good half metal, despite being nearly isostructural and isoelectronic. We use our understanding of the CoFeS system to make some prescriptions for new ferromagnetic half-metals.
8 pages including 9 figures
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