Unified Spin Model for Magnetic Excitations in Iron Chalcogenides
arXiv:1607.05295 · doi:10.1103/PhysRevB.96.174403
Abstract
Recent inelastic neutron scattering (INS) measurements on FeSe and Fe(TeSe), have sparked intense debate over the nature of the ground state in these materials. Here we propose an effective bilinear-biquadratic spin model which is shown to consistently describe the evolution of low-energy spin excitations in FeSe, both under applied pressure and upon Se/Te substitution. The phase diagram, studied using a combination of variational mean-field, flavor-wave calculations, and density-matrix renormalization group (DMRG), exhibits a sequence of transitions between the columnar antiferromagnet common to the iron pnictides, the non-magnetic ferroquadrupolar phase attributed to FeSe, and the double-stripe antiferromagnetic order known to exist in FeTe. The calculated spin structure factor in these phases mimics closely that observed with INS in the Fe(TeSe), series. In addition to the experimentally established phases, the possibility of incommensurate magnetic order is also predicted.
9 pages, 10 figures in the main text; plus 5 pages of supplementary materials
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