Structural and Magnetocaloric Properties of Classical Rare-Earth Manganite Ceramics

Zhiwei Gong, N. Liedienov, A. Pashchenko, Ziyu Wei, Wei Xu
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Abstract

Structure, microstructure, chemical and phase composition, as well as magnetic state and magnetocaloric effect of the $\text{La}_{0.9}\text{Mn}_{1.1}\mathrm{O}_{3}$ manganite have been investigated by X-ray diffraction, energy-dispersive X-ray spectroscopy, scanning electron microscopy, and magnetic methods. The $\text{La}_{0.9}\text{Mn}_{1.1}\mathrm{O}_{3}$ ceramics have been synthesized using a two-step solid-state reaction method at an annealing temperature of $1150^{\circ}\mathrm{C}$ (22 h). Based on the X-ray diffraction results, a crystal structure of the $\text{La}_{0.9}\text{Mn}_{1.1}\mathrm{O}_{3}$ ceramic has a rhombohedral $R-3c$ (No. 167) type of symmetry. Chemical and phase composition of the $\text{La}_{0.9}\text{Mn}_{1.1}\mathrm{O}_{3}$ sample has been confirmed by energy-dispersive X-ray spectroscopy. The average grain size has been determined by means of Nano Measure 1.2.5 software and is 1.6 $\mu \mathrm{m}$. Based on the magnetic data, $\text{La}_{0.9}\text{Mn}_{1.1}\mathrm{O}_{3}$ ceramic displays a ferromagnetic to paramagnetic phase transition at the Curie temperature $T_{\mathrm{C}}=227\mathrm{K}$ with a high magnetic entropy change $\Delta S_{\mathrm{M}}{}^{\max}=-3.50\mathrm{J}/(\text{kg}\cdot \mathrm{K})$ at the field of 2 T. Moreover, the magnetic parameters in the paramagnetic state have been defined using the Curie- Weiss law.
经典稀土锰酸盐陶瓷的结构和磁热性能
利用x射线衍射、能量色散x射线能谱、扫描电镜和磁学方法研究了$\text{La}_{0.9}\text{Mn}_{1.1}\mathrm{O}_{3}$锰矿石的结构、微观结构、化学和物相组成、磁态和磁热效应。在$1150^{\circ}\mathrm{C}$ (22 h)的退火温度下,采用两步固相反应法合成了$\text{La}_{0.9}\text{Mn}_{1.1}\mathrm{O}_{3}$陶瓷。根据x射线衍射结果,$\text{La}_{0.9}\text{Mn}_{1.1}\mathrm{O}_{3}$陶瓷的晶体结构具有菱形$R-3c$ (No. 167)型对称性。通过能量色散x射线光谱法确定了$\text{La}_{0.9}\text{Mn}_{1.1}\mathrm{O}_{3}$样品的化学和物相组成。通过Nano Measure 1.2.5软件测定平均晶粒尺寸为1.6 $\mu \mathrm{m}$。根据磁性数据,$\text{La}_{0.9}\text{Mn}_{1.1}\mathrm{O}_{3}$陶瓷在居里温度$T_{\mathrm{C}}=227\mathrm{K}$处呈现铁磁向顺磁相变,在2 t的磁场下具有较高的磁熵变化$\Delta S_{\mathrm{M}}{}^{\max}=-3.50\mathrm{J}/(\text{kg}\cdot \mathrm{K})$,并利用居里-魏斯定律定义了顺磁状态下的磁性参数。
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