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Approaching Ferrite-Based Exchange-Coupled Nanocompositesas Permanent Magnets

机译:接近基于铁氧体的交换耦合纳米复合材料作为永久磁铁

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摘要

During the past decade, CoFe2O4 (hard)/Co–Fe alloy (soft) magnetic nanocomposites have been routinely prepared by partial reduction of CoFe2O4 nanoparticles. Monoxide (i.e., FeO or CoO) has often been detected as a byproduct of the reduction, although it remains unclear whether the formation of this phase occurs during the reduction itself or at a later stage. Here, a novel reaction cell was designed to monitor the reduction in situ using synchrotron powder X-ray diffraction (PXRD). Sequential Rietveld refinements of the in situ data yielded time-resolved information on the sample composition and confirmed that the monoxide is generated as an intermediate phase. The macroscopic magnetic properties of samples at different reduction stages were measured by means of vibrating sample magnetometry (VSM), revealing a magnetic softening with increasing soft phase content, which was too pronounced to be exclusively explained by the introduction of soft material in the system. The elemental compositions of the constituent phases were obtained from joint Rietveld refinements of exsitu high-resolution PXRD and neutron powder diffraction(NPD) data. It was found that the alloy has a tendency to emerge ina Co-rich form, inducing a Co deficiency on the remaining spinel phase,which can explain the early softening of the magnetic material.
机译:在过去的十年中,通常通过部分还原CoFe2O4纳米颗粒来常规制备CoFe2O4(硬)/ Co-Fe合金(软)磁性纳米复合材料。一氧化碳(即FeO或CoO)通常被认为是还原反应的副产物,尽管目前尚不清楚该相的形成是在还原反应本身还是在随后的阶段。在这里,设计了一种新型反应池,以使用同步加速器粉末X射线衍射(PXRD)监测原位还原。现场数据的顺序Rietveld精修产生了样品成分的时间分辨信息,并确认一氧化碳是作为中间相生成的。通过振动样品磁力法(VSM)测量了不同还原阶段样品的宏观磁性能,显示出随着软相含量的增加而发生的磁软化,这一现象非常明显,无法通过在系统中引入软质材料来单独解释。组成相的元素组成是从ex的Rietveld联合精制获得的。原位高分辨率PXRD和中子粉末衍射(NPD)数据。发现该合金倾向于在富钴形式,在剩余的尖晶石相上引起钴缺乏,这可以解释磁性材料的早期软化。

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