Khlifi M, Bejar M, Dhahri E, Lachkar P, Hlil E K
J Appl Phys. 2012 May 15;111(10):103909-1039096. doi: 10.1063/1.4718450. Epub 2012 May 21.
La(0.8)Ca(0.2 - x)□(x)MnO(3) (x = 0.00, 0.10, and 0.20) perovskite was prepared by the conventional solid-state reaction and annealed at 1473 K. X-ray diffraction and scanning electron microscopy shown the existence of a secondary phase attributed to the unreacted Mn(3)O(4) oxide. The magneto transport properties have been investigated based on the temperature dependence of the resistivity ρ(T) measurements under several applied magnetic fields. We note that the La(0.8)Ca(0.2)MnO(3) (x = 0.00) sample has a classical metal-insulator transition at T(ρ). But we have observed that the lacunars samples (x = 0.10 and 0.20) include a metallic and insulator behavior simultaneously below T(ρ) and the resistivity is dominated by tunneling through the barriers associated with the insulating phase. In other words, the calcium deficiency favors the enhancement of the insulator behavior. The electrical resistivity is fitted with the phenomenological percolation model, which is based on the phase segregation of ferromagnetic metallic clusters and paramagnetic insulating regions. Furthermore, we found that the estimated results are in good agreement with experimental data. Above all, the resistivity dependence on the temperature and magnetic field data is used to deduce the magnetic entropy change. We have found that these magnetic entropy change values are similar to those calculated in our previous work from the magnetic measurements. Finally, we have found an excellent estimation of the magnetic entropy change based on the Landau theory.
通过传统固态反应制备了La(0.8)Ca(0.2 - x)□(x)MnO₃(x = 0.00、0.10和0.20)钙钛矿,并在1473 K下进行退火。X射线衍射和扫描电子显微镜显示存在归因于未反应的Mn₃O₄氧化物的第二相。基于在几个外加磁场下电阻率ρ(T)测量的温度依赖性研究了磁输运性质。我们注意到La(0.8)Ca(0.2)MnO₃(x = 0.00)样品在T(ρ)处有经典的金属-绝缘体转变。但我们观察到,缺位样品(x = 0.10和0.20)在T(ρ)以下同时表现出金属和绝缘体行为,并且电阻率主要由通过与绝缘相相关的势垒的隧穿主导。换句话说,钙缺乏有利于增强绝缘体行为。电阻率符合基于铁磁金属团簇和顺磁绝缘区域相分离的唯象渗流模型。此外,我们发现估计结果与实验数据吻合良好。最重要的是,利用电阻率对温度和磁场数据的依赖性来推导磁熵变。我们发现这些磁熵变值与我们之前工作中通过磁测量计算得到的值相似。最后,基于朗道理论我们对磁熵变有了很好的估计。