Nikmanesh Hossein, Jaberolansar Elnaz, Kameli Parviz, Varzaneh Ali Ghotbi
Department of Physics, Persian Gulf University, Bushehr 75169, Iran.
Department of Physics, Isfahan University of Technology, Isfahan 84156-83111, Iran.
Nanotechnology. 2022 Apr 20;33(27). doi: 10.1088/1361-6528/ac5ee4.
This work reports cation distribution, magnetic, structural, and morphological studies of rare-earth Pr doped cobalt ferrite nanoparticles CoFePrO(= 0, 0.02, 0.04, 0.06 at%) fabricated by sol-gel auto-combustion method. X-ray diffraction analysis, field emission scanning electron microscopy (FESEM), high resolution transmission electron microscopy (HRTEM), selected area electron diffraction (SAED), and Fourier-transform infrared (FTIR) microscopy were utilized to study the structural and morphological characteristics of the prepared samples. Rietveld refinement by the Material Analyses Using Diffraction (MAUD) software showed the formation of mono-phase cubic spinel structure with Fd-3m space group; however, there was a trace of impure PrFeOphase for the sample CoFePrO(= 0.06). Cation distribution was inferred from the XRD patterns using MAUD program. FESEM analysis revealed the spherical-shaped particles with dimensions close to the data extracted from XRD analysis and HRTEM images confirmed it. FTIR measurements revealed the presence of two prominent stretching vibrational modes confirming the successful formation of ferrite spinel structure. Magnetic properties of the nanoparticles were measured at two different temperatures 300 K and 10 K. For the low temperature of 10 K a high sensitive measurement method as Superconducting Quantum Interference Device (SQUID) magnetometry was used and Vibrating Sample Magnetometer (VSM) recorded the magnetic data at 300 K. Comparison of the magnetic results exhibited a significant enhancement with temperature drop due to the reduction in thermal fluctuations. Paramagnetic nature of rare-earth ions may be the main reason fordecrement from 76 emu g(= 0.0) to 60 emu g(= 0.02) at 300 K. At 10 K, the estimated cation distribution played a vital role in justification of obtained magnetic results. All the obtained data showed that the synthesized magnetic nanoparticles can be implemented in permanent magnet industry and information storage fields, especially when it comes to lower temperatures.
本研究报告了采用溶胶-凝胶自燃烧法制备的稀土Pr掺杂钴铁氧体纳米颗粒CoFePrO(= 0、0.02、0.04、0.06原子百分比)的阳离子分布、磁性、结构和形态学研究。利用X射线衍射分析、场发射扫描电子显微镜(FESEM)、高分辨率透射电子显微镜(HRTEM)、选区电子衍射(SAED)和傅里叶变换红外(FTIR)显微镜来研究制备样品的结构和形态特征。使用材料分析衍射(MAUD)软件进行的Rietveld精修显示形成了具有Fd-3m空间群的单相立方尖晶石结构;然而,对于样品CoFePrO(= 0.06)存在微量的不纯PrFeO相。使用MAUD程序从XRD图谱推断阳离子分布。FESEM分析揭示了尺寸接近于从XRD分析和HRTEM图像提取数据的球形颗粒,HRTEM图像证实了这一点。FTIR测量揭示了存在两种突出的拉伸振动模式,证实了铁氧体尖晶石结构的成功形成。在300 K和10 K这两个不同温度下测量了纳米颗粒的磁性。对于10 K的低温,使用了超导量子干涉装置(SQUID)磁力测量这种高灵敏度测量方法,振动样品磁强计(VSM)记录了300 K时的磁性数据。磁性结果的比较表明,由于热涨落的减少,随着温度下降有显著增强。稀土离子的顺磁性质可能是300 K时从76 emu g(= 0.0)降至60 emu g(= 0.02)的主要原因。在10 K时,估计的阳离子分布在解释所获得的磁性结果中起着至关重要的作用。所有获得的数据表明,合成的磁性纳米颗粒可应用于永磁工业和信息存储领域,特别是在较低温度的情况下。