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Crystal Structure and Spontaneous Magnetism of BiFeO_3 Powder Synthesized by Hydrothermal Method

机译:水热法合成BiFeO_3粉末的晶体结构和自发磁性

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Single-phase BiFeO_3 powder was successively synthesized by a low-temperature hydrothermal method. Scanning electron microscopy and transmission electron microscopy results showed that BiFeO_3 powder had several hundred nanometers to micrometer-sized particles with a broad size distribution. BiFeO_3 powder showed weak-ferromagnetic behavior with a small magnetization value (M_s ~20 memu/g) at room temperature. Rietveld refinement results for the crystal structure show the displacive disorder of the Fe-site(6a); the Fe-site(6a) splits into two pairs, Fe(1) and Fe(2) displaced by 0.9 A from each other and these sites are partially occupied. Hence the O-site(18b) also splits into the two partially occupied sites forming a distorted FeO_6 octahedras. The weak ferromagnetism observed in the hydrothermal BFO powder is ascribed to the displacive disorder of FeO_6 octahedras resulting in an incomplete counterbalance between the antiferromagnetic sublattices of the Fe-ions.
机译:采用低温水热法连续合成了单相BiFeO_3粉末。扫描电子显微镜和透射电子显微镜结果表明,BiFeO_3粉末具有数百纳米至微米大小的颗粒,且粒径分布较宽。 BiFeO_3粉末在室温下表现出弱铁磁行为,磁化值较小(M_s〜20 memu / g)。晶体结构的Rietveld细化结果表明,Fe-位错位错(6a)。 Fe位点(6a)分成两对,彼此错开0.9 A的Fe(1)和Fe(2),这些位点被部分占据。因此,O-位点(18b)也分成两个部分占据的位点,形成扭曲的FeO_6八面体。在水热BFO粉末中观察到的弱铁磁性归因于FeO_6八面体的置换性紊乱,从而导致Fe离子的反铁磁亚晶格之间的平衡不完全。

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