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机构地区:[1]College of Applied Science, Beijing University of Technology, Beijing 100022, China [2]School of Physics Science and Information Engineering, Liaocheng University,Liaocheng 252059, China
出 处:《Journal of Rare Earths》2007年第1期27-30,共4页稀土学报(英文版)
基 金:Project supported by the National Natural Science Foundation of China (69977005)
摘 要:CdGd2 (WO4)4 -δ single crystal was grown using the Czochralski's method. The crystal structure was tetragonal seheelite with lattice parameters a = b = 0.5203 nm and c = 1. 1359 nm. There were vacancies of (WO4)^2- , therefore, there were some Gd^2+ ions. Langevin paramagnetism and anisotropy were observed from the δ-T curves at room temperature. The susceptibility X//was 3.5018×10^-3, and X⊥ was 3.4403× 10^-2. The anisotropy was also observed in the electron spin resonance (ESR) experiments. The anisotropic Land6 factors were g//= 2. 1333 and g~ = 2. 8411. The direction of easy magnetization was in the α-b plane. Anisotropic paramagnetic Curie constants C//and C⊥ were not only related to macroscopic a that was observed through the experiment, but were also related to J⊥ and J//, which were the microscopic quantum numbers of the Gd^2+ and Gd^3| ions. Based on the detailed analyses, the proportion of 36.8% of Gd^3+ ions to 63.2% of Gd^2+ ions in the Gd ions of the CdGd2(WO4)4-δ crystal was calculated, and δ was 0.638 in the single crystal.CdGd2 (WO4)4 -δ single crystal was grown using the Czochralski's method. The crystal structure was tetragonal seheelite with lattice parameters a = b = 0.5203 nm and c = 1. 1359 nm. There were vacancies of (WO4)^2- , therefore, there were some Gd^2+ ions. Langevin paramagnetism and anisotropy were observed from the δ-T curves at room temperature. The susceptibility X//was 3.5018×10^-3, and X⊥ was 3.4403× 10^-2. The anisotropy was also observed in the electron spin resonance (ESR) experiments. The anisotropic Land6 factors were g//= 2. 1333 and g~ = 2. 8411. The direction of easy magnetization was in the α-b plane. Anisotropic paramagnetic Curie constants C//and C⊥ were not only related to macroscopic a that was observed through the experiment, but were also related to J⊥ and J//, which were the microscopic quantum numbers of the Gd^2+ and Gd^3| ions. Based on the detailed analyses, the proportion of 36.8% of Gd^3+ ions to 63.2% of Gd^2+ ions in the Gd ions of the CdGd2(WO4)4-δ crystal was calculated, and δ was 0.638 in the single crystal.
关 键 词:CdGd(WO4)4-δ single crystal ANISOTROPY Langevin paramagnetism rare earths
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