Abstract

Iron(IV) oxides are strongly correlated materials with negative charge-transfer energy (negative \ensuremath{\Delta}), and exhibit peculiar electronic and magnetic properties such as topological helical spin structures in the metallic cubic perovskite ${\mathrm{SrFeO}}_{3}$. Here, the spin structure of the layered negative-\ensuremath{\Delta} insulator ${\mathrm{Sr}}_{2}{\mathrm{FeO}}_{4}$ was studied by powder neutron diffraction in zero field and magnetic fields up to 6.5 T. Below ${T}_{\mathrm{N}}=56\phantom{\rule{0.16em}{0ex}}\mathrm{K}$, ${\mathrm{Sr}}_{2}{\mathrm{FeO}}_{4}$ adopts an elliptical cycloidal spin structure with modulated magnetic moments between 1.9 and 3.5 ${\ensuremath{\mu}}_{\mathrm{B}}$ and a propagation vector $\mathbit{k}=(\ensuremath{\tau},\ensuremath{\tau},0)$ with $\ensuremath{\tau}=0.137$. With increasing magnetic field the spin structure undergoes a spin-flop transition near 5 T. Synchrotron $^{57}\mathrm{Fe}$-M\"ossbauer spectroscopy reveals that the spin spiral transforms to a ferromagnetic structure at pressures between 5 and 8 GPa, just in the pressure range where a Raman-active phonon nonintrinsic to the ${\mathrm{K}}_{2}{\mathrm{NiF}}_{4}$-type crystal structure vanishes. These results indicate an insulating ground state which is stabilized by a hidden structural distortion and differs from the charge disproportionation in other Fe(IV) oxides.

Highlights

  • The interplay between charge, orbital, spin, and lattice degrees of freedom in compounds with strong electron correlations leads to a large, complex array of structural and physical properties [1]

  • Synchrotron 57Fe-Mössbauer spectroscopy reveals that the spin spiral transforms to a ferromagnetic structure at pressures between 5 and 8 GPa, just in the pressure range where a Raman-active phonon nonintrinsic to the K2NiF4-type crystal structure vanishes. These results indicate an insulating ground state which is stabilized by a hidden structural distortion and differs from the charge disproportionation in other Fe(IV) oxides

  • In this work we report a powder neutron diffraction study which reveals that Sr2FeO4 forms an elliptical cycloidal spin spiral undergoing a spin-flop transition in a magnetic field of about 5 T

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Summary

INTRODUCTION

The interplay between charge, orbital, spin, and lattice degrees of freedom in compounds with strong electron correlations leads to a large, complex array of structural and physical properties [1]. Examples of negative- oxides include NaCuO2 [4] and several rare-earth nickelates LnNiO3 the insulating ground states of which feature a charge disproportion (CD) transition of the nominal Ni3+ ions accompanied by a breathing-type structural distortion [5,6]. CaFeO3 [14,15] or Sr3Fe2O7 [16,17,18,19] are known to exhibit a comparable CD, whereas metallic SrFeO3 [20,21] as well as the cubic phase of BaFeO3 [22] do not show any CD These ferrates were shown to be negativematerials [23] and the CD state was formulated as 2d5L−1 (t2g3eg1 ) → d5 (t2g3eg2 ) + d5L−2(t2g3eg0 ), where, similar to the nickelates, singly occupied σ -type eg∗ orbitals occur, being coupled to more-localized π -type t2g. Our results shed new light on the nature of insulating states and emerging spin structures in negative- materials which may be of relevance for understanding topological spin textures in this class of compounds

EXPERIMENTAL DETAILS
Magnetic properties
Magnetic structure
Spin-flop transition
Synchrotron powder x-ray diffraction
Mössbauer spectra at ambient pressure
Change of spin structure at high pressure
CONCLUSIONS
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