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Magnetic order in hedenbergite: CaFeSi2O6
Authors:JMD Coey  Subrata Ghose
Institution:Department of Pure and Applied Physics, Trinity College, Dublin 2, Ireland;Department of Geological Sciences, University of Washington, Seattle, Washington 98195, USA
Abstract:Synthetic hedenbergite orders antiferromagnetically at 38 K although the principal interactions are ferromagnetic, between Fe2+ ions in the Ml chains of edge-sharing octahedra. The susceptibility follows a Curie-Weiss law above 100 K with θ = 35 K and peff = 4.98 μB. A fit of the 4.2 K Mossbauer spectrum yields a positive, near-axial electric field gradient and a hyperfine field of 18.8 T. The likely magnetic structure consists of ferromagnetic chains, each weakly coupled antiparallel to its four c-centred equivalents.
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