Raman, infrared and Mossbauer spectroscopic studies of solid-state synthesized Ni-Zn ferrites

被引:29
|
作者
Palacio Gomez, Carlos Andres [1 ]
Barrero Meneses, Csar Augusto [2 ]
Antonio Jaen, Juan [3 ]
机构
[1] Univ Antonio Narino, Fac Ciencias, Grp GIFAM, Carrera 7,21-84, Tunjo 150002, Colombia
[2] Univ Antioquia UdeA, Fac Ciencias Exactas & Nat, Grp Estado Solido, Calle 70,52-21, Medellin 1226, Colombia
[3] Univ Panama, Dept Quim Fis, Fac Ciencias Nat Exactas & Tecnol, Apartado Postal 0824-001, Panama City, Panama
关键词
Ni-Zn ferrites; Solid state synthesis; Raman; Infrared; Vibrational spectroscopies; Mbssbauer; NANOCRYSTALLINE NICKEL FERRITE; X-RAY-DIFFRACTION; CATION DISTRIBUTION; MAGNETIC-PROPERTIES; ZINC FERRITE; NANOPARTICLES; TEMPERATURE; DISORDER; CO; SPECTRA;
D O I
10.1016/j.jmmm.2020.166710
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
A set of Nickel-Zinc ferrite samples (Ni1-xZnxFe2O4, x = 0.0, 0.2, 0.4, 0.6, 0.8 and 1.0) were synthesized by the low-energy ball milling method with subsequent thermal treatment. Infrared, Raman and Mossbauer spectroscopies were used to analyze the lattice dynamics and structure of the prepared samples. Infrared studies showed a dominant absorption band ranging from 548 cm(-1) to 592 cm(-1) associated with cation-oxygen stretching vibrations at tetrahedral sites. The five Raman modes, predicted by factor group analysis, were observed in all spectra. All these spectra changed in symmetry because of the incorporation of Zn into the lattice, and the reordering of Fe, Ni and Zn ions in both, tetrahedral (A) and octahedral [B] sites. It is observed that Fe3+ ions located at tetrahedral sites are gradually displaced to octahedral sites by the increase of Zn2+ ions. Mossbauer spectra were collected for all samples at 295 K and at 18 K. The spectra were properly fitted by using a model that assumes that the average hyperfine magnetic field at the octahedral sites is due to a random substitution of magnetically interacting Fe-A(3+) ions by diamagnetic Zn-A(2+) ions at the tetrahedral sites. It was found that the average supertransfered hyperfine field due to one Fe-A(3+) - O2+ - Fe-B(3+) superexchange interaction was equal to about 0.9 T at 18 K. The zinc contents at tetrahedral sites as obtained by Raman, Mossbauer and XRD techniques are compared and discussed.
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页数:9
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