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Origin of room temperature weak-ferromagnetism in antiferromagnetic Pb(Fe2/3W1/3)O3 ceramic

机译:反铁磁pb(Fe 2/3 W 1/3 )O 3 陶瓷的室温弱铁磁性的起源

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摘要

We report the origin of room temperature weak ferromagnetic behavior of polycrystalline Pb(FeW)O (PFW) powder. The structure and magnetic properties of the ceramic powder prepared by a Columbite method were characterized by X-ray and neutron diffraction, Mössbauer spectroscopy and magnetization measurements. Rietveld analysis of diffraction data confirm the formation of single phase PFW, without traces of any parasitic pyrochlore phase. PFW was found to crystallize in the cubic structure at room temperature. The Rietveld refinement of neutron diffraction data measured at room temperature confirmed the G-type antiferromagnetic structure of PFW in our sample. However, along with the antiferromagnetic (AFM) ordering of the Fe spins, we have observed the existence of weak ferromagnetism at room temperature through: (i) a clear opening of hysteresis (M-H) loop, (ii) bifurcation of the field cooled and zero-field cooled susceptibility; supported by Mössbauer spectroscopy results. The P-E loop measurements showed a non-linear slim hysteresis loop at room temperature due to the electronic conduction through the local inhomogeneities in the PFW crystallites and the inter-particle regions. By corroborating all the magnetic measurements, especially the spin glass nature of the sample, with the conduction behavior of the sample, we report here that the observed ferromagnetism originates at these local inhomogeneous regions in the sample, where the Fe-spins are not perfectly aligned antiferromagnetically due to the compositional disordering. © 2015 Elsevier Ltd and Techna Group S.r.l.
机译:我们报告了室温下多晶Pb(FeW)O(PFW)粉末的弱铁磁行为的起源。通过X射线和中子衍射,穆斯堡尔光谱法和磁化强度测量,表征了通过哥伦比方法制备的陶瓷粉末的结构和磁性。衍射数据的Rietveld分析证实了单相PFW的形成,没有任何寄生烧绿石相的痕迹。发现PFW在室温下以立方结构结晶。在室温下测量的中子衍射数据的Rietveld改进证实了我们样品中PFW的G型反铁磁结构。但是,随着铁自旋的反铁磁(AFM)排序,我们通过以下方法观察到了室温下弱铁磁的存在:(i)磁滞(MH)回路的清晰开放,(ii)冷却磁场的分叉和零场冷却磁化率;由Méssbauer光谱学结果支持。 P-E回路测量结果显示,由于通过PFW晶粒和粒子间区域中的局部不均匀性进行电子传导,因此在室温下出现非线性细长的磁滞回线。通过证实所有的磁测量值,尤其是样品的自旋玻璃性质,以及样品的导电性能,我们在此报告,观察到的铁磁性起源于样品中的这些局部不均匀区域,在这些区域中,Fe纺丝未完全对准由于成分紊乱而产生反铁磁性。 ©2015 Elsevier Ltd和Techna Group S.r.l.

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