Abstract

The crystal and local structures of ${\mathrm{La}}_{1\ensuremath{-}x}{\mathrm{Sr}}_{x}\mathrm{Fe}{\mathrm{O}}_{3\ensuremath{-}\ensuremath{\delta}}$ $(0\ensuremath{\leqslant}x\ensuremath{\leqslant}1)$ samples have been studied by x-ray diffraction and x-ray absorption spectroscopy techniques. The Fe-O bond length decreases with increasing $x$. Accordingly, the x-ray absorption near edge spectroscopy (XANES) spectra reveal a chemical shift of the iron $K$ edge to higher energies. Both results agree with an Fe valence increase as La is substituted with Sr. Extended x-ray absorption fine structure spectroscopy and XANES show that the chemical state of Fe atoms in intermediate compositions can be described either by a bimodal distribution of formal ${\mathrm{Fe}}^{3+}$ and ${\mathrm{Fe}}^{4+}$ ions or by an ${\mathrm{Fe}}^{3.\mathrm{x}+}$ intermediate valence. The large value of the Debye-Waller factors obtained for intermediate compositions indicates that hole doping produces local disorder around the Fe ions. These factors show unusually large values below the metal-insulator (MI) transition for $x=2∕3$ or $3∕4$. We show that a significant charge disproportionation of the type $2{\mathrm{Fe}}^{4+}\ensuremath{\rightarrow}{\mathrm{Fe}}^{3+}+{\mathrm{Fe}}^{5+}$ cannot account for the local structure observed below the MI transition temperature of these samples. We suggest that an electronic localization arises from an order-disorder transition between dynamic and static distortions, resulting in the opening of a gap at the Fermi level.

Highlights

  • The perovskite series La1−xSrxFeO3 ͑0 ഛ x ഛ 1͒ shows interesting changes in their physical properties as a function of composition.[1,2] LaFeO3 is an antiferromagnetic insulator with a high Néel temperatureTNof approximately 750 K.3 The substitution of La3+ with Sr2+ produces a formal change in the valence state of Fe ion from +3 ͑x = 0͒ to +4 ͑x = 1͒.This leads to the decrease of TN and the increase of electronic conductivity.[4]

  • La1/3Sr2/3FeO3 samples undergoes a metal-insulatorMItransition at ϳ200 K, evidenced by a jump in the resistivity of more than 1 order of magnitude with decreasing temperature. This MI transition is accompanied by an antiferromagnetic ordering

  • A pioneering work on La1−xSrxFeO3, reporting Mössbauer spectroscopy results at low temperature, has revealed two kinds of Fe ions with different hyperfine fields,[6] which have been attributed to different charge states

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Summary

Introduction

A pioneering work on La1−xSrxFeO3, reporting Mössbauer spectroscopy results at low temperature, has revealed two kinds of Fe ions with different hyperfine fields,[6] which have been attributed to different charge states. In view of these results, the MI transition has been interpreted as a charge disproportionation from an average-valence stateFe+3.67͒ in the paramagnetic phase above 200 K into a mixture of 2Fe3+ and 1Fe5+ in the antiferromagnetic charge orderingCOstate below 200 K.7. The magnetic moments found for the two nonequivalent Fe ions seem to depend on the synthetic route.[8,11] the occurrence of this type of CO transitions depends on the rare-earth size.[12,13]

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