Synthesis, structural, optical, electrical and Mossbauer spectroscopic studies of Co substituted Li0.5Fe2.5O4

被引:26
|
作者
Sharma, Parul [1 ]
Thakur, Preeti [1 ]
Mattei, Jean Luc [2 ]
Queffelec, Patrick [2 ]
Thakur, Atul [1 ,3 ]
机构
[1] Shoolini Univ, Sch Phys & Mat Sci, Solan, HP, India
[2] CNRS, Lab Sci & Tech Informat Commun & Connaissance, UMR 6285, CS 93837, 6 Av Le Gorgeu, F-29238 Brest 3, France
[3] Innovat Sci Res Soc, Nanotechnol Wing, Shimla 171001, Himachal Prades, India
关键词
Metal oxides; Wet chemical method; Spinel phase; DOPED LITHIUM FERRITE; MAGNETIC-PROPERTIES; DIELECTRIC-PROPERTIES; NANOPARTICLES; NANOFERRITES; MANGANESE; BEHAVIOR; NUCLEI;
D O I
10.1016/j.jmmm.2016.01.023
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
A series of cobalt substituted lithium ferrite Li0.5CoxFe2.5-xO4 with x=0, 0.2, 0.4 was prepared by a chemical technique called citrate precursor method. In this technique citric acid was used as a reducing agent. Structural, morphological, topographical, optical, electrical, and magnetic properties were studied by using X -Ray Diffractometer (XRD), Scanning Electron Microscopy (SEM), Transmission Electron Microscopy (TEM), Fourier Transform Infrared Spectroscopy (FTIR), Raman Spectroscopy, DC resistivity, Mossbauer Spectroscopy. XRD patterns showed characteristic (2 2 0), (3 1 1), (4 0 0), (4 2 2), (5 1 1), (4 4 0) peaks which confirmed the inverse spinel phase. SEM and TEM support the formation of cubic nanoparticles. FTIR studies reported the ferrite peaks between 400 cm(-1) and 800 cm(-1) confirming the inverse spinel structure. Five optical Raman modes (A(1g)+E-g+3F(2g)), characteristics of the cubic spinel structure with (P4332) space group are also observed. Electrical DC resistivity studied from room temperature to 300 degrees C showed the semiconducting behavior of lithium ferrite. Porosity, transition temperature and activation energy are found to decrease with cobalt ion concentration. The room temperature Mossbauer spectra of all the samples showed normal Zeeman Splitting sextets supporting the formation of ferromagnetic phase. With increase in cobalt content, the value of hyperfine field at A site is found to vary from 53.15 to 54.96 T whereas at B site it vary from 54.79 to 52.82 T. The obtained results have been explained based on possible mechanisms, models and theories. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:17 / 23
页数:7
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