4.4 Article

Magnetocaloric effect in Y-doped La0.6Ca0.4MnO3 enhanced by Griffiths phase and re-entrance of first-order phase transition

期刊

CURRENT APPLIED PHYSICS
卷 42, 期 -, 页码 7-21

出版社

ELSEVIER
DOI: 10.1016/j.cap.2022.07.010

关键词

Perovskite manganites; Magnetic and magnetoocaloric behaviors; Magnetic order

资金

  1. National Research Foundation of Korea (NRF) - Korea governments Ministry of Science and ICT (MSIT) [2020R1A2B5B01002184]
  2. Materials, Components & Equipments Research Program - Gyeonggi Province [AICT-003-T1]
  3. National Key R & D Program of China [2017YFB0903700, 2017YFB0903702]
  4. Yichang Key Laboratory of Magnetic Functional Materials

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This study reveals the re-entrance of a discontinuous first-order transition in orthorhombic La0.6-xYxCa0.4MnO3 compounds, which enhances the magnetocaloric effect. The enhanced magnetocaloric effect in La0.6-xYxCa0.4MnO3 is related to a Griffiths singularity and local Jahn-Teller distortions of the perovskite structure.
It has been known that bulk La0.6Ca0.4MnO3 is an intermediate material of the first- and second-order characters with the tricritical-point exponents, and the doping of a metal ion in it usually causes a continuous second-order transition. The present work reports the re-entrance of a discontinuous first-order transition in orthorhombic La0.6-xYxCa0.4MnO3 (x = 0.03-0.09) compounds. This enhances the magnetocaloric effect. For the field H = 30 kOe, the maximum magnetic-entropy change (vertical bar Delta S-max vertical bar) and relative cooling power (RCP) have been evaluated being about 5.45-6.3 J/kg.K and 130-185 J/kg, respectively. If combining these compounds as refrigerant blocks in a rotary ring model, a magnetic cooling device can operate at temperatures T = 85-280 K, with (vertical bar Delta S-max vertical bar) approximate to 5.5 J/kg.K and RCP approximate to N 1073 J/kg. Aside from the re-entranced first-order phase transition, the magnetization and structural analyses have proved the enhanced magnetocaloric effect in La0.6-xYxCa0.4MnO3 related to a Griffiths singularity, and local Jahn-Teller distortions of the pemvskite structure (since the Mn3+/Mn4+ ratio and orthorhombic structural phase are unchanged vs. x).

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