首页> 外文期刊>Journal of Applied Physics >Magnetic anomalies and canting effects in nanocrystalline spinel copper ferrites Cu_(x)Fe_(3-x)O_(4)
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Magnetic anomalies and canting effects in nanocrystalline spinel copper ferrites Cu_(x)Fe_(3-x)O_(4)

机译:纳米晶晶石铜铁氧体的磁异常和倾斜效应Cu_(x)Fe_(3-x)O_(4)

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摘要

The magnetic behavior of nanocrystalline copper spinel ferrites Cu_(x)Fe_(3-x)O_(4) (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 ≈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 Fe~(3+) 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℃, 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.
机译:通过现场莫斯鲍尔和直流磁测量研究了纳米晶铜尖晶石铁氧体Cu_(x)Fe_(3-x)O_(4)(0.42≤x≤1)表现出不同结晶度的磁性行为。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 ≈1 T 的外加场,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Fe~(3+)离子的磁矩均处于倾斜自旋状态,并证明平均自旋倾斜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。

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