New Journal of Physics (Jan 2016)

Charge and spin coupling in magnetoresistive oxygen-vacancy strontium ferrate SrFeO3–δ

  • S H Lee,
  • T W Frawley,
  • C H Yao,
  • Y C Lai,
  • Chao-Hung Du,
  • P D Hatton,
  • M J Wang,
  • F C Chou,
  • D J Huang

DOI
https://doi.org/10.1088/1367-2630/18/9/093033
Journal volume & issue
Vol. 18, no. 9
p. 093033

Abstract

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Using magnetization, conductivity and x-ray scattering measurements, we demonstrate that the giant magnetoresistance of the oxygen-deficient ferrite SrFeO _2.875±0.02 is a consequence of the coupling between the charge and spin order parameters and the tetragonal to monoclinic structural distortion. Upon cooling the sample at T ≃ 120 K we find a shoulder in both field-cool and zero field cool magnetization data and the simultaneous appearance of incommensurate structural satellites observed using x-ray diffraction. These satellites are shown to be due to incommensurate charge ordering with the high temperature delocalized Fe ${}^{3.5+}$ ions becoming localized with a charge disproportion forming an incommensurate charge-ordered phase. Strong resonant enhancement of these satellites at the Fe L _III absorption edge confirms that this charge ordering is occurring at the Fe(2) sites. Further cooling increases the charge order correlation until T ≃ 62 K where there is a full structural transition from the tetragonal phase to a mononclinic phase. This causes a jump in the charge order wavevector from an incommensurate value of 0.610 to a commensurate ground state position of 5/8. This first-order structural transition displays considerable hysteresis as well as dramatic reductions in the magnetization, resistivity and magnetoresistance. The transition also causes an antiferromagnetic spin-ordering with a doubled unit cell along the c -axis. Well as observing new commensurate magnetic reflections at the Fe _III edge we also observed resonant enhancement at the oxygen K -edge showing considerable hybridization between the Fe 3d and oxygen 2p states at low temperatures. Our results show that the formation of a magnetic long-rage ordered ground state drives the charge ordering from an incommensurate ordering to a commensurate ground state. This is evidence of a strong coupling between the magnetic and charge order parameters which is the basis for the unusual magnetoresistive effects observed at the transition.

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