Study on the magnetic properties and critical behavior of CoFe2−x Al x O4 (x = 1.0 and 1.2) spinel ferrite

Zonghao Song, Ruiyang Cao, C. Ruan, Xian Zhang, Shou-Yang Wang, Meiling Wang, Yongqing Ma, Ganhong Zheng
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Abstract

We have examined the behavior of CoFe2−x Al x O4 (x = 1.0 and 1.2) ferrite close to the transition from ferromagnetic to paramagnetic phases (T C). The findings indicate that at a temperature of T C = 314 K (x = 1.0) and T C = 224 K (x = 1.2), there is a second order magnetic phase transition. We used various methods, including modified Arrott plot, Kouvel–Fisher method, and critical isotherm analysis, to determine the critical exponents which were found to be similar to those expected for the Tricritical Mean-field model (β = 0.288, γ = 1.057, and δ = 4.665) for the x = 1.0 sample. The critical exponents for the x = 1.2 sample (β = 0.771, γ = 1.081, and δ = 2.403) belonged to a different universality class. These results suggest that the replacement of Fe ions with non-magnetic Al ions decreases the Co–Fe, Fe–Fe, Co–Co interaction sites in the CoFe2O4 spinel ferrite, increasing magnetic disorder.
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CoFe2-x Al x O4(x = 1.0 和 1.2)尖晶石铁氧体的磁性能和临界行为研究
我们研究了 CoFe2-x Al x O4(x = 1.0 和 1.2)铁氧体在从铁磁相过渡到顺磁相 (T C) 附近的行为。研究结果表明,在 T C = 314 K (x = 1.0) 和 T C = 224 K (x = 1.2) 的温度下,存在二阶磁性相变。我们使用各种方法,包括改良阿罗特图、库维尔-费舍法和临界等温线分析,确定了 x = 1.0 样品的临界指数,发现这些指数与三临界平均场模型的预期指数(β = 0.288、γ = 1.057 和 δ = 4.665)相似。x = 1.2 样本的临界指数(β = 0.771、γ = 1.081 和 δ = 2.403)属于不同的普遍性类别。这些结果表明,用非磁性 Al 离子取代 Fe 离子会减少 CoFe2O4 尖晶石铁氧体中的 Co-Fe、Fe-Fe、Co-Co 相互作用位点,从而增加磁性无序性。
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