Possible observation of Griffith phase over large temperature range in plasma sintered La0.67Ca0.33MnO3

被引:9
作者
Mishra, D. K. [1 ]
Roul, B. K. [2 ]
Singh, S. K. [3 ]
Srinivasu, V. V. [4 ]
机构
[1] Siksha O Anusandhan Univ, Fac Engn & Technol ITER, Dept Phys, Khandagiri Sq, Bhubaneswar 751030, Odisha, India
[2] Inst Mat Sci Agh, Planetarium Bldg, Bhubaneswar 751013, Odisha, India
[3] CSIR, Inst Minerals & Mat Technol, Adv Mat Technol Dept, Bhubaneswar 751013, Odisha, India
[4] Univ South Africa, Coll Sci Engn & Technol, Dept Phys, ZA-1710 Johannesburg, South Africa
关键词
Griffith phase; Curie temperature; Plasma sintering; ESR; EPMA; LCMO; ROOM-TEMPERATURE; MANGANITES; TRANSITION; RESONANCE; MAGNETORESISTANCE; FIELD; EPR;
D O I
10.1016/j.jmmm.2017.06.075
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
We report on the possible observation of Griffith phase in a wide range of temperature (> 272-378 K) in the 2.5 min plasma sintered La0.67Ca0.33MnO3 (LCMO) as deduced from careful electron spin resonance studies. This is 106 K higher than the paramagnetic to ferromagnetic transition (Curie transition similar to 272 K) temperature. The indication of Griffith phase in such a wide range is not reported earlier by any group. We purposefully prepared LCMO samples by plasma sintering technique so as to create a disordered structure by rapid quenching which we believe, is the prime reason for the observation of Griffith Phase above the Curie transition temperature. The inverse susceptibility curve represents the existence of ferromagnetic cluster in paramagnetic region. The large resonance peak width (40-60 mT) within the temperature range 330-378 K confirms the sample magnetically inhomogeneity which is also established from our electron probe microstructure analysis (EPMA). EPMA establishes the presence of higher percentage of Mn3+ cluster in comparison to Mn4+. This is the reason for which Griffith state is enhanced largely to a higher range of temperature. (C) 2017 Elsevier B.V. All rights reserved.
引用
收藏
页码:287 / 291
页数:5
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