Low temperature transport anomaly in Cr substituted (La0.67Sr0.33) MnO3 manganites

被引:15
作者
Tank, Tejas M. [1 ]
Shelke, Vilas
Das, Sarmistha [1 ,2 ]
Rana, D. S. [2 ]
Thaker, C. M. [3 ]
Samatham, S. S. [4 ]
Ganesan, V. [4 ]
Sanyal, S. P. [1 ]
机构
[1] Barkatullah Univ, Dept Phys, Solid State Phys Lab, Bhopal 462026, MP, India
[2] Indian Inst Sci Educ & Res, Dept Phys, Bhopal 462023, India
[3] MVM Sci & Home Sci Coll, Rajkot 360005, Gujarat, India
[4] UGC DAE Consortium Sci Res, Khandwa Rd, Indore 452001, Madhya Pradesh, India
关键词
Manganite; Colossal magnetoresistance; Ferromagnetic; VRH model; COLOSSAL MAGNETORESISTANCE RESPONSE; INSULATOR-METAL TRANSITION; RESISTIVITY; X=0;
D O I
10.1016/j.jmmm.2017.02.037
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The structural, electrical, and magnetic properties of La0.67Sr0.33Mn1 xCrxO3 ( 0 <= x <= 0.10) manganites have been studied by substitution of antiferromagnetic trivalent Cr ion at Mn-site. Systematic efforts have been carried out to understand the electrical resistivity behavior in the ferromagnetic metallic and paramagnetic semi-conducting phases of Cr substituted La(0.67)Sr(0.33)Mn(1 x)CrxO(3) manganites. Polycrystalline samples show a resistivity minimum at a temperature (T-min) of < 40 K in the ferromagnetic metallic phase. T-min shifts to higher temperatures on application of magnetic fields. The appearance of this resistivity minimum was analyzed by fittings the data according to the model that considers e-e scattering caused by enhanced Coulombic interactions. The electrical resistivity data has been best fitted in the metallic and semiconducting regime using various models. Present results suggest that intrinsic magnetic inhomogeneity like Cr3+ ions in these strongly electron-correlated manganite systems is originating due to the existence of the ferromagnetic interactions. (C) 2017 Elsevier B.V. All rights reserved.
引用
收藏
页码:581 / 590
页数:10
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