Published April 2021 | Version v1
Journal article

Synthesis, structure and magnetic properties of La1-x Ln xCr0.5Co0.5O3 (x = 0 and 0.2 & Ln = Pr, Sm and Gd) perovskites

  • 1. Department of Chemistry, Jadavpur University, Kolkata 700032 (India)
  • 2. Department of Chemistry, Visva-Bharati, Santiniketan 731235, West Bengal (India)
  • 3. Discipline of Physics, Indian Institute of Information Technology, Design & Manufacturing Jabalpur, Dumna Airport Road, Madhya Pradesh 482005 (India)

Description

We report the sol–gel synthesis of La1-xLnxCr0.5Co0.5O3 (x = 0 and 0.2 & Ln = Pr, Sm and Gd) perovskites. The samples were characterized using powder X-ray diffraction (PXRD), field emission scanning electron microscopy (FE-SEM), energy dispersive X-ray (EDX) and magnetization measurements. It is worth mentioning that all the samples in this study are found to be monophasic as attested from the PXRD patterns in sharp comparison with the previously reported work on LaCr0.5Co0.5O3 [Solanki et al. J. Magn. Magn. Mater. 469 (2019) 95–99.]. This could be related to the slight modifications in synthesis condition like the metal to citric acid ratio, drying as well decomposition temperature of gel, final calcination temperature and time. The parent phase (x = 0) crystallizes in rhombohedral, R-3c, structure whereas the Ln-doped samples are orthorhombic, Pbnm. FE-SEM imaging revealed the irregular shape and large variation in particle size. The particles are highly agglomerated but show faceted surface irrespective of shape and size. The EDX analysis confirms the nominal cationic composition of the samples. The magnetic measurements suggest the onset of antiferromagnetic ordering in all the samples with TN ranging from 130 K to 124 K depending on the size of the Ln-dopant ion. The high temperature effective paramagnetic moments obtained from Curie-Weiss law for all the samples suggest that the most likely spin-state of cobalt is intermediate-spin state. The low temperature magnetic behaviour of the substituted samples could be related to the rare earth-transition metal interaction. The magnetic ground states can be attributed to the Cr3+–O–Co3+, Cr3+–O–Cr3+ and Co3+–O–Co3+ antiferromagnetic superexchange interactions between the randomly distributed Cr3+ and Co3+ ions.

Availability note (English)

Available from http://dx.doi.org/10.1016/j.jmmm.2020.167621

Additional details

Identifiers

DOI
10.1016/j.jmmm.2020.167621;
PII
S0304885320325889;

Publishing Information

Journal Title
Journal of Magnetism and Magnetic Materials
Journal Volume
523
Journal Page Range
vp.
ISSN
0304-8853
CODEN
JMMMDC

Optional Information

Copyright
Copyright (c) 2020 Elsevier B.V. All rights reserved.