Magnetocaloric study and estimation of the spontaneous magnetization by a magnetic entropy analysis in Pr0.6Ca0.1Sr0.3Mn0.975Fe0.025O3

被引:25
|
作者
Mahjoub, Saoussen [1 ]
Baazaoui, Mohamed [1 ]
M'nassri, Rafik [1 ,2 ]
Hlil, E. K. [3 ]
Oumezzine, Mohamed [1 ]
机构
[1] Univ Monastir, Fac Sci Monastir, Dept Phys, Lab Physicochim Mat, Monastir 5019, Tunisia
[2] Kairouan Univ, Higher Inst Appl Sci & Technol Kasserine, BP 471, Kasserine 1200, Tunisia
[3] Univ Grenoble 1, CNRS, Inst Neel, BP166, F-38042 Grenoble, France
关键词
Perovskite; Landau theory; Magnetic entropy change; Spontaneous magnetization; TEMPERATURE; SUBSTITUTION; COMPOUND; BEHAVIOR; CR;
D O I
10.1016/j.jallcom.2016.04.113
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
A systematic study on the magnetic and magnetocaloric properties of a polycrystalline sample of Pr0.6Ca0.1Sr0.3Mn0.975Fe0.025O3 prepared by solid-state reaction has been studied. Structural study shows that our sample is of a single phase and crystallizes in the distorted orthorhombic system with Pbnm space group. The measurements of the temperature and field dependences of the magnetization clearly show that the Pr0.6Ca0.1Sr0.3Mn0.975Fe0.025O3 ceramic exhibit a paramagnetic-ferromagnetic transition with decreasing temperature. The magnetic entropy change (-Delta S-M) is determined from isothermal magnetization curves. The field dependence of magnetic entropy change is analyzed and showing the power law dependence, Delta S-max(T,H) = a(T)(mu H-0)(n(T,H)) at the Curie temperature (T-C). It has been noted that the value of n obeys to the Curie-Weiss law above T-C. The Landau theory (LT) for phase transitions framework is applied to describe the magnetocaloric effect (MCE) in Pr0.6Ca0.1Sr0.3Mn0.975Fe0.025O3 manganite. The analysis of the MCE using the LT shows good agreement with the experimental data, indicating the importance of magneto-elastic coupling and electron interaction in the MCE properties of manganite. Based on the obtained magnetic entropy change (-Delta S-M) under different magnetic fields, we determined the spontaneous magnetization (M-Sp). For comparison, the M-Sp has been also deduced from the classical extrapolation from the Arrott plot. An excellent agreement is found between the spontaneous magnetization determined from the entropy change (Delta S-M vs. M-2) and the Arrot curves (H/M vs. M-2), confirming that the use of magnetic entropy change to get the spontaneous magnetization is valid. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:381 / 387
页数:7
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