Abstract:
FeI2 is an insulating antiferromagnet with an unusual magnetic structure at ambient pressure. Recently, hyperfine field, electric field gradient, and other local quantities at the Fe site were measured over a wide range of pressures indicating a collapse of the orbital magnetic moment below the insulator-to-metal transition. In the present work we apply local density approximation ~LDA! and LDA1U approaches to calculate the electronic structure and to investigate the Fe on-site quantities. We propose that the vanishing of the orbital moment is connected to the change of orbital order as reflected in the symmetry of the occupied minority-spin orbital. We find good agreement between the calculated and measured hyperfine fields and quadrupolar shifts, and make predictions which can serve to validate the proposed mechanism of orbital moment collapse experimentally.
The magnetic behavior of the compound FeI2 presents a conundrum. The iron dihalide structure type is simple, consisting of a hexagonal layered CdI2 structure (P¯3m1 space group, No. 164 in the International Tables! characteristic of many transition-metal dihalides (NiI2 , FeCl2, etc.!
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