Journal
JOURNAL OF APPLIED PHYSICS
Volume 93, Issue 10, Pages 6847-6849Publisher
AMER INST PHYSICS
DOI: 10.1063/1.1555986
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The pyrite Fe1-xCoxS2 (0.25less than or equal toxless than or equal to0.9) was predicted to be half metal, insensitive to Fe-Co disorder. To verify its half metallicity, we have grown single crystals of Fe1-xCoxS2 (x=0.35, 0.5, 0.75, 0.9, and 1). Crystals of up to a few mm in size by temperature gradient (923-873 K) solution growth from Te melts, which showed high crystalline quality by scanning electron microscopy, x-ray diffraction, and magnetic measurements. A half-metallic magnetization of 1+/-0.03mu(B) per Co atom was found for x=0.35-0.9. Point contact Andreev reflection measurements, however, showed spin polarization of 47%-61% with the maximum around x=0.5, well below predictions. Ferromagnetic resonance measurements give gsimilar to2.08 with large intrinsic damping, which indicates a reduced half-metallicity. Inductively coupled plasma and energy dispersive x-ray spectroscopy results confirm a sulfur deficiency of similar to1.5%-10% [(Fe,Co)S2-y,0.03less than or equal toyless than or equal to0.2] and small amounts of Te. Electronic structure calculations show the extra electron provided by Co substitution to FeS2 populates a sulfur-derived conduction band. Consequently, S deficiency and/or S site disorder are expected to affect the transport properties. This is consistent with the low polarization measurements and again indicates the importance of crystalline order in obtaining highly spin-polarized materials. (C) 2003 American Institute of Physics.
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