Naveed-Ul-Haq M, Hussain Shahzad, Webers Samira, Salamon Soma, Ahmad Ibtisam, Bibi Tayyaba, Hameed Amna, Wende Heiko
Department of Physics, COMSATS University Islamabad, Lahore Campus 54000, Pakistan.
Phys Chem Chem Phys. 2021 Sep 7;23(33):18112-18124. doi: 10.1039/d1cp02625a. Epub 2021 Aug 16.
We report a combined experimental and theoretical study of pure and doped cobalt ferrite where 25% of Fe ions were replaced by Al, Ga, and In ions, respectively, i.e., CoFeXO (X = Al, Ga, and In). The ferrite compositions were successfully synthesized using the solid-state reaction method. The X-ray powder diffraction method established that all ferrite samples had a spinel unit cell structure with the Fd3[combining macron]m (No. 227) space group. The lattice constants of ferrites increased from 8.382 Å (for undoped CoFeO) to 8.520 Å (for In-doped cobalt ferrite) in direct relation to the dopant ion size. The magnetic properties were obtained at 4.3 K and 300 K. At 4.3 K, the In-doped CoFeO showed the highest saturation magnetic moment of 4.68 μ f.u., while Al-doped CoFeO showed the smallest value of 2.72 μ f.u.. The Fe distribution among the spinel tetrahedral and octahedral sites was determined from the Mössbauer spectra. From ultraviolet-visible diffuse reflectance spectroscopy the direct optical bandgaps were determined, which have values between 1.20 eV and 1.28 eV for these ferrites. The ferrite compositions were also studied theoretically using plane-wave density functional theory using the CASTEP code where it was revealed that arrangements of the non-magnetic cations at the tetrahedral and octahedral sites strongly influence the electronic structure, the bandgap value, and the net magnetic moment per formula unit. Light Al ions at the octahedral site give a low value of the net magnetic moment while the heavier Ga and In ions at the tetrahedral sites of the spinel give an enhanced magnetic moment. The magnetic moment values obtained from theoretical calculations match very well with the experimental values. Moreover, the theoretical calculations reveal that there exists a strong p-d hybridization among the oxygen and magnetic ions, which is affected by the non-magnetic dopant ions. The change in hybridization with the non-magnetic ion doping is responsible for the altered magnetic moments of the doped ferrites. Thus, our study provides a comprehensive investigation covering the synthesis and characterization of ferrites along with a good understanding of the phenomenon of how non-magnetic ion doping into spinel ferrites provides a method to tune the electronic and magnetic properties of the spinel ferrite.
我们报告了一项关于纯钴铁氧体和掺杂钴铁氧体的实验与理论相结合的研究,其中分别用铝、镓和铟离子取代了25%的铁离子,即CoFeXO(X = Al、Ga和In)。采用固态反应法成功合成了铁氧体组合物。X射线粉末衍射法确定所有铁氧体样品均具有Fd3[combining macron]m(编号227)空间群的尖晶石晶胞结构。铁氧体的晶格常数从8.382 Å(未掺杂的CoFeO)增加到8.520 Å(铟掺杂的钴铁氧体),与掺杂离子尺寸直接相关。在4.3 K和300 K下获得了磁性。在4.3 K时,铟掺杂的CoFeO显示出最高的饱和磁矩,为4.68 μ f.u.,而铝掺杂的CoFeO显示出最小值,为2.72 μ f.u.。通过穆斯堡尔谱确定了铁在尖晶石四面体和八面体位点之间的分布。通过紫外 - 可见漫反射光谱法确定了直接光学带隙,这些铁氧体的带隙值在1.20 eV至1.28 eV之间。还使用CASTEP代码通过平面波密度泛函理论对铁氧体组合物进行了理论研究,结果表明非磁性阳离子在四面体和八面体位点的排列强烈影响电子结构、带隙值和每个化学式单元的净磁矩。八面体位点的轻铝离子给出较低的净磁矩值,而尖晶石四面体位置较重的镓和铟离子给出增强的磁矩。理论计算得到的磁矩值与实验值非常吻合。此外,理论计算表明氧和磁性离子之间存在强烈的p - d杂化,这受到非磁性掺杂离子的影响。非磁性离子掺杂引起的杂化变化是掺杂铁氧体磁矩改变的原因。因此,我们的研究对铁氧体的合成与表征进行了全面的研究,并很好地理解了向尖晶石铁氧体中掺杂非磁性离子如何提供一种调节尖晶石铁氧体电子和磁性性质的方法这一现象。