Crystallisation of BaFe12O19 hexagonal ferrite with an aid of B2O3 and the effects on microstructure and magnetic properties useful for permanent magnets and magnetic recording devices

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Abstract

Polycrystalline Ba-ferrite (BaFe12O19) using B2O3 (up to 1 mol) as a sintering aid has been prepared by the usual solid state reaction of BaCO3 and Fe2O3. The B2O3, which exists in molten form during the reaction (operated at 1000–1400°C), dissolves the reactants in intimate contact. The dissolved solid and molten B2O3 both diffuse into the system to facilitate the reaction, BaCO3+6Fe2O3BaFe12O19+CO2, of ferrite formation. The reaction is very sensitive to B2O3 addition and temperature (Ts) employed for the sintering. The distortion of Ba-ferrite lattice, that usually appeared due to sintering at higher temperature, Ts⩾1300°C, is considerably reduced by the use of B2O3(x) ⩽0.3 mol addition. The distortion however appears for the intermediate B2O3 content of 0.3 molx<0.7 mol. A model for the reaction based on the experimental results of X-ray diffractometry and microstructure of the samples is proposed. It accounts successfully for the crystallisation of magnetic particles and variation in the magnetic anisotropies. The effect of B2O3 additions to Ba-ferrite is reflected by the increase of magnetisation Ms (by ≈13%) and the decrease of coercivity Hc (to as small as 5 Oe), subjected to the sintering especially at higher Ts. The materials obtained with Ms as large as 79 emu/gandHc=4−3 kOe (at 25°C) are suitable for the use as permanent magnets, whereas those comprising small Hc of ≈1 kOe can be useful for magnetic recording applications. The increase of Ms is explained by invoking the fact that B2O3(B3+) substitutes on Fe3+ (tetrahedral) sites according to BaFe12−yByO19, with y up to 0.4 (equivalent to x ≈ 0.2 mol). The substitution (B3+→Fe3+) causes distortion in the tetrahedral sites within the crystal unit cell as evidenced by the EPR spectroscopy. We also developed an empirical relation describing the EPR linewidth (ΔH) in Fe3+ ferrimagnetic resonance at g ≈ 2.5 and the various magnetic anisotropy factors. This enables us to analyse for the anisotropy factors by using the observed values for ΔH, Hc and Ms.

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