Investigation of cation distribution and magnetocrystalline anisotropy of Ni x Cu 0.1 Zn 0.9−x Fe 2 O 4 nanoferrites: Role of constant mole percent of Cu 2+ dopant in place of Zn 2+
| Autor: | D.L. Sastry, Ch. Srinivas, D.M. Potukuchi, Sher Singh Meena, S. M. Yusuf, C.L. Prajapat, K.S. Ramakrishna, Pramod Bhatt, B. V. Tirupanyam |
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| Rok vydání: | 2017 |
| Předmět: |
010302 applied physics
Materials science Rietveld refinement Process Chemistry and Technology Analytical chemistry 02 engineering and technology 021001 nanoscience & nanotechnology Magnetocrystalline anisotropy 01 natural sciences Surfaces Coatings and Films Electronic Optical and Magnetic Materials Crystallography Magnetization Lattice constant Differential scanning calorimetry 0103 physical sciences Materials Chemistry Ceramics and Composites Ferrite (magnet) 0210 nano-technology Diffractometer Superparamagnetism |
| Zdroj: | Ceramics International. 43:7984-7991 |
| ISSN: | 0272-8842 |
| Popis: | Co-precipitated and 800 °C heat treated Ni-Cu-Zn nanoferrites with chemical formula Ni x Cu 0.1 Zn 0.9- x Fe 2 O 4 ( x =0.5, 0.6, 0.7) were prepared because of their potential use as multilayer chip inductors in electromagnetic applications. Their structural, magnetic properties and phase formation were studied using X-ray diffractometer (XRD), field emission scanning electron microscope (FE–SEM), vibrating sample magnetometer (VSM), Mossbauer spectrometer, thermogravimetric analyzer (TGA) and differential scanning calorimeter (DSC). The XRD patterns confirm the cubic spinel structure of the ferrite phase belonging to Fd3m space group. Lattice parameters and cation distributions were obtained by Rietveld refinement of the XRD patterns. The lattice parameter decreases with increase in Ni 2+ ion concentration. Rietveld analysis indicates that Cu 2+ ions predominantly occupy the B -sites and Ni 2+ ions partly going into B -sites but predominantly into A -sites. An excellent agreement is observed between the experimental lattice parameters and lattice parameters theoretically calculated using this cation redistribution. The inversion parameter (λ) observed for Fe 3+ ions by Mossbauer spectroscopy is different from that of Rietveld analysis. Magnetization and Mossbauer spectroscopic measurements indicate that the ferrite nanoparticles are mostly superparamagnetic. The cation redistribution is supposed to alter the magnetocrystalline anisotropy which in turn affects the magnetic parameters of the present ferrite samples. The reduced magnetization is attributed to core-shell interactions and possible canting of A - and B -shell magnetizations. TGA-DSC studies indicate that ferrite formation in the 800 °C heat treated samples is completed but grain growth increases as the particles are subject to the increased temperature. |
| Databáze: | OpenAIRE |
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