Direct and inverse magnetocaloric effects in magnetostrictive GdMn2Ge2 with field-induced metamagnetic transition

Author:

Li Canglong1ORCID,Li Zhaohu2,Yang Wenqian1ORCID,Tian Zhaoming2ORCID,Qiu Yang1ORCID,Hua Junfan3ORCID,Huang Shuai34ORCID

Affiliation:

1. Key Laboratory of Microelectronics and Energy of Henan Province, College of Physics and Electronic Engineering, Xinyang Normal University 1 , Xinyang 464000, People's Republic of China

2. Wuhan National High Magnetic Field Center and School of Physics, Huazhong University of Science and Technology 2 , Wuhan 430074, People's Republic of China

3. Key Laboratory of Novel Materials for Sensor of Zhejiang Province, Hangzhou Dianzi University 3 , Hangzhou 310018, People's Republic of China

4. Guangxi Key Laboratory of Nuclear Physics and Nuclear Technology, Guangxi Normal University 4 , Guilin 541001, People's Republic of China

Abstract

Heavy rare-earth-based ternary intermetallic compounds with the formula RT2X2 have drawn great interest because of their multiple magnetic transitions and various magnetic structures. Here, anisotropic magnetic behaviors, magnetocaloric effects (MCEs), and magnetostriction effects in single-crystalline GdMn2Ge2 are studied in two different directions. Experiments show a magnetic transition characterized by a sudden decrease in magnetization for μ0H//a and a sharp increase for μ0H//c at Tt. The transition is driven by lower temperatures for μ0H//a, contrasting that for μ0H//c with an increase in the magnetic field. An inverse MCE is observed for μ0H//a with a maximum magnetic entropy change (−ΔSMmax) of −7.4 J kg−1 K−1 (μ0ΔH = 6 T), while a direct MCE is obtained for μ0H//c with an −ΔSMmax of 8.0 J kg−1 K−1 under the same magnetic field change. Moreover, a remarkable field-induced metamagnetic transition and a magnetostriction effect are observed simultaneously at Tt, indicating strong magneto-lattice coupling. The T-μ0H phase diagrams are constructed based on the magnetic properties. The coexistence of direct and inverse MCEs is discussed and is due to the spin-flop of Mn and anisotropic magnetic properties under magnetic fields in different directions.

Funder

Natural Science Foundation of Henan Province

National Natural Science Foundation of China

the Fundamental Research Funds of Guangdong Province

The Open Project of Guangxi Key Laboratory of Nuclear Physics and Nuclear Technology

Publisher

AIP Publishing

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