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M?ssbauer spectroscopy study of aluminium substituted nickel-ferrites

机译:铝取代镍铁氧体的Msssbauer光谱研究

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Powders of Al substituted Ni-ferrites (NiAl x Fe2 ? x O4 x = 0, 0.5, 1.0 and 1.5) were prepared using the calcination method. M?ssbauer spectroscopy results of all samples show two well defined magnetic sextets corresponding to Fe3 + ions in the A (tetrahedral) and B (octahedral) sites of the spinel structure. In addition, a quadrupole doublet with quadrupole splitting of (~0.53 mm/s) starts evolving upon Al substitution. This doublet is associated with a new Fe–Al-oxide phase. The X-ray diffraction patterns show, in addition to the original peaks, new peaks evolve and increase in intensity as the Al concentration increases, confirming the evolution of this new phase.
机译:使用煅烧方法制备了Al取代的镍铁氧体粉末(NiAl x 2 Fe xαxO4 x = 0、0.5、1.0和1.5)。所有样品的Msssbauer光谱结果表明,尖晶石结构的A(四面体)和B(八面体)位点对应于Fe3 +离子的两个定义明确的磁性六边形。此外,四极双峰(四极分裂为(〜0.53 mm / s))在Al取代后开始发展。该双峰与新的Fe-Al-氧化物相相关。 X射线衍射图谱显示,除了原始峰外,随着Al浓度的增加,新的峰也逐渐演化并强度增加,从而证实了这一新相的演化。

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