Evolution of Griffiths phase and spin reorientation in perovskite manganites

  • Xu Zheng
  • , Tian Gao*
  • , Wei Jing
  • , Xingyu Wang
  • , Yongsheng Liu
  • , Bin Chen
  • , Hongliang Dong
  • , Zhiqiang Chen
  • , Shixun Cao
  • , Chuanbing Cai
  • , Vyacheslav V. Marchenkov
  • *Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

Abstract

Magnetic properties of polycrystalline La1- xCaxMn0.9Cu0.1O3 (0.02 ≤ x ≤ 0.4) have been investigated in detail. All samples show a clear ferromagnetic-paramagnetic transition. The Curie temperature TC decreases with increasing Ca-dopant. Inverse susceptibility of all the samples deviates from Curie-Weiss law above TC, indicating the presence of a short range ferromagnetic and/or antiferromagnetic ordering state in the paramagnetic background. For 0.02 ≤ x ≤ 0.2, the upward deviation is attributed to antiferromagnetic interactions, while the downward for x ≥ 0.3 samples is caused by a Griffiths-like behavior, which is suppressed by an applied field. A charge ordering transition associated with an antiferromagnetic phase is detected in x ≥ 0.3 samples, the melting of which results in a spin reorientation transition and a new FM phase. Finally, the phase diagrams of this manganite system have been established.

Original languageEnglish
Article number165611
JournalJournal of Magnetism and Magnetic Materials
Volume491
DOIs
StatePublished - 1 Dec 2019
Externally publishedYes

Keywords

  • Griffiths phase
  • Magnetic phase transitions
  • Manganites
  • Phase separation
  • Short range ferromagnetic order

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