Effect of composition on structural and magnetic properties of nanocrystalline Ni0. 8− xZn0. 2MgxFe2O4 ferrite
MA Gabal, WA Bayoumy - Polyhedron, 2010 - Elsevier
MA Gabal, WA Bayoumy
Polyhedron, 2010•ElsevierNanocrystalline magnetic particles of Ni0. 8− xZn0. 2MgxFe2O4 ferrites with x lying between
0.0 and 0.8 were synthesized using metal nitrates and freshly extracted egg-white. The
synthesized powders were characterized using X-ray diffraction (XRD), Fourier transform
infrared (FT-IR) and transmission electron microscopy (TEM). With increasing magnesium
concentration, the lattice constant increases while X-ray density decreases. The average
crystallite size determined from XRD data using Scherrer formula lie in the range of 35 …
0.0 and 0.8 were synthesized using metal nitrates and freshly extracted egg-white. The
synthesized powders were characterized using X-ray diffraction (XRD), Fourier transform
infrared (FT-IR) and transmission electron microscopy (TEM). With increasing magnesium
concentration, the lattice constant increases while X-ray density decreases. The average
crystallite size determined from XRD data using Scherrer formula lie in the range of 35 …
Nanocrystalline magnetic particles of Ni0.8−xZn0.2MgxFe2O4 ferrites with x lying between 0.0 and 0.8 were synthesized using metal nitrates and freshly extracted egg-white. The synthesized powders were characterized using X-ray diffraction (XRD), Fourier transform infrared (FT-IR) and transmission electron microscopy (TEM). With increasing magnesium concentration, the lattice constant increases while X-ray density decreases. The average crystallite size determined from XRD data using Scherrer formula lie in the range of 35–59nm. TEM image shows spherically agglomerated particles with average crystallite size agreed well with that obtained from XRD. Magnetic properties measured at room temperature by vibrating sample magnetometer (VSM) reveal a decrease in saturation magnetization up to Mg content of 0.6. In agreement with FT-IR results, the unexpected increase in the magnetization at Mg content of 0.8 can be attributed to the tendency of Mg2+ ions to occupy the tetrahedral site. The decrease in the value of coercivity with increasing magnesium content can be explained based on the magneto-crystalline anisotropy.
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