Rare-Earth Doped Gd3−xRExFe5O12 (RE = Y, Nd, Sm, and Dy) Garnet: Structural, Magnetic, Magnetocaloric, and DFT Study

IF 2.7 Q1 MATERIALS SCIENCE, CERAMICS
Dipesh Neupane, Noah Kramer, Romakanta Bhattarai, Christopher Hanley, Arjun K. Pathak, Xiao Shen, Sunil Karna, Sanjay R. Mishra
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Abstract

The study reports the influence of rare-earth ion doping on the structural, magnetic, and magnetocaloric properties of ferrimagnetic Gd3−xRExFe5O12 (RE = Y, Nd, Sm, and Dy, x = 0.0, 0.25, 0.50, and 0.75) garnet compound prepared via facile autocombustion method followed by annealing in air. X-Ray diffraction (XRD) data analysis confirmed the presence of a single-phase garnet. The compound’s lattice parameters and cell volume varied according to differences in ionic radii of the doped rare-earth ions. The RE3+ substitution changed the site-to-site bond lengths and bond angles, affecting the magnetic interaction between site ions. Magnetization measurements for all RE3+-doped samples demonstrated paramagnetic behavior at room temperature and soft-ferrimagnetic behavior at 5 K. The isothermal magnetic entropy changes (−ΔSM) were derived from the magnetic isotherm curves, M vs. T, in a field up to 3 T in the Gd3−xRExFe5O12 sample. The maximum magnetic entropy change (−∆SMmax) increased with Dy3+ and Sm3+substitution and decreased for Nd3+ and Y3+ substitution with x content. The Dy3+-doped Gd2.25Dy0.75Fe5O12 sample showed −∆SMmax~2.03 Jkg−1K−1, which is ~7% higher than that of Gd3Fe5O12 (1.91 Jkg−1K−1). A first-principal density function theory (DFT) technique was used to shed light on observed properties. The study shows that the magnetic moments of the doped rare-earths ions play a vital role in tuning the magnetocaloric properties of the garnet compound.
稀土掺杂Gd3−xRExFe5O12 (RE = Y, Nd, Sm, and Dy)石榴石:结构、磁性、磁热学和DFT研究
本研究报道了稀土离子掺杂对铁磁性Gd3−xrexfe50o12 (RE = Y, Nd, Sm, and Dy, x = 0.0, 0.25, 0.50, 0.75)石榴石化合物的结构、磁性和磁热学性能的影响。x射线衍射(XRD)数据分析证实了单相石榴石的存在。化合物的晶格参数和胞体体积随掺杂稀土离子的离子半径的不同而变化。RE3+取代改变了位点间的键长和键角,影响了位点离子间的磁相互作用。所有掺RE3+样品的磁化测量结果显示室温下的顺磁性和5k下的软铁磁性。等温磁熵变化(−ΔSM)由Gd3−xRExFe5O12样品在高达3t的磁场下的磁等温曲线M vs. T得到。最大磁熵变化(−∆SMmax)随Dy3+和Sm3+取代量的增加而增大,随Nd3+和Y3+取代量的增加而减小。Dy3+掺杂的Gd2.25Dy0.75Fe5O12样品显示出−∆SMmax~2.03 Jkg−1K−1,比Gd3Fe5O12 (1.91 Jkg−1K−1)提高了~7%。一主密度函数理论(DFT)技术被用来阐明观察到的性质。研究表明,稀土离子的磁矩对石榴石化合物的磁热学性质起着至关重要的调节作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
3.00
自引率
7.10%
发文量
66
审稿时长
10 weeks
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