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Magnetic anomalies and canting effects in nanocrystalline spinel copper ferrites CuxFe3-xO4

机译:纳米晶晶石铜铁氧体CuxFe3-xO4的磁异常和倾斜效应

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摘要

The magnetic behavior of nanocrystalline copper spinel ferrites CuxFe3-xO4 (0.42 <= x <= 1) exhibiting different degrees of crystallinity, have been investigated by means of in-field Mossbauer and dc magnetic measurements. The samples were obtained by a coprecipitation method and were subsequently high-energy ball milled for different times, which induced a progressive improvement of the ferrite crystallinity and cation redistribution. Their magnetism shows some peculiar features; at 5 K, the virgin magnetization curves remain outside the main hysteresis loop for applied fields of approximate to 1 T and display an S-shaped form. Below 60 K, the field-cooled hysteresis loops are shifted toward the negative field direction. In addition, in the same temperature range, the field-cooled magnetization of the samples with poorest crystallinity decreases sharply due to the spin freezing at the surface. The in-field Mossbauer spectra at 4.2 K show that the magnetic moments of the Fe3+ ions are in a canted spin state for both the tetrahedral and octahedral sites of the spinel structure, and evidence a decrease of the average spin canting with the degree of crystallinity. After calcination at 950 degrees C, the coprecipitated sample no longer displays the magnetic anomalous and canting features. We explain our results as due to the partially disordered surface within the frame of the core-shell model rather than to the effect of cation redistribution. (C) 2005 American Institute of Physics.
机译:通过现场莫斯鲍尔和直流磁测量研究了表现出不同结晶度的纳米晶铜尖晶石铁氧体CuxFe3-xO4(0.42 <= x <= 1)的磁性行为。通过共沉淀法获得样品,随后进行不同时间的高能球磨,导致铁素体结晶度和阳离子再分布逐渐提高。它们的磁性显示出一些奇特的特征;在 5 K 时,对于近似 1 T 的外加磁场,原始磁化曲线保持在主磁滞回路之外,并显示 S 形。低于 60 K,场冷磁滞回路向负场方向移动。此外,在相同的温度范围内,结晶度最差的样品的场冷磁化强度由于表面的自旋冻结而急剧降低。4.2 K的场内Mossbauer光谱表明,尖晶石结构的四面体和八面体位点的Fe3+离子的磁矩都处于倾斜自旋状态,并证明平均自旋倾斜度随着结晶度的增加而降低。在950°C煅烧后,共沉淀样品不再显示磁异常和倾斜特征。我们将我们的结果解释为由于核壳模型框架内的部分无序表面,而不是阳离子重新分布的影响。(C) 2005年美国物理研究所。

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