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- W2079760129 abstract "Jamesonite, Fe2+Pb4Sb6S14, is a natural sulfide in which Fe octahedra form single chains, that would favor a quasi-one-dimensional magnetism. The susceptibility shows an antiferromagnetic behavior with a broad maximum at 30 K and an irregularity at 5 K. A neutron powder diffraction study has been undertaken between 1.4 and 44 K. In the diffractograms, below 5 K, supplementary peaks of magnetic origin and characteristic of a three-dimensional long-range magnetic ordering appear. The magnetic structure corresponds to a canted antiferromagnet with a propagation wave-vector k=[0.5,0,0] and a magnetic ordered magnetic moment on Fe atoms of 3.3(1) μB at 1.4 K. Below 30 K one-dimensional magnetic ordering or correlations are visible in the diagrams and persist down to 1.4 K." @default.
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- W2079760129 date "2004-12-01" @default.
- W2079760129 modified "2023-09-30" @default.
- W2079760129 title "Neutron diffraction study of the magnetic ordering of jamesonite (FePb4Sb6S14)" @default.
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- W2079760129 doi "https://doi.org/10.1016/j.jmmm.2004.06.031" @default.
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