【摘要】 本文在较宽温度范围内系统地研究了Y_3-xGd_xFe₅O₁₂单晶体的饱和磁矩、铁磁共振和穆斯堡尔效应谱随成分和温度的变化,用亚铁磁理论解释了不同成分的热磁曲线及抵消点的变化,理论计算和实验结果符合较好.比较了几种铁磁共振线宽理论的计算结果,发现以亚铁磁共振理论加以适当条件后与实验结果较符合;发现Y³⁺和Gd³⁺在十二面体晶位中的代换,对四面体和八面体晶位中的Fe³⁺的穆斯堡尔谱参量无明显影响;观测到代表四面体和八面体晶位中Fe³⁺的谱线在磁有序区又再分成两组亚谱.更多还原

【Abstract】 The dependence of the saturation magnetic moment, ferromagnetic resonance (FMR) and Mossbauer effect on the composition and temperature for the Y3-xGdxFe5O12 single crystal system with x=0, 0.5, 1.0, 1.5, 2.0, 2.5, and 3.0 have been studied at a wide range of temperature. The variations of thermo-magnetic curves and compansation points with composition are explained by the theory of ferrimagnetism. The theoretically calculated results agree well with those of experiments. The line-widths of FMR for several theories are evaluated. It is found that the experimental results can be well explained by the phenome-nological theory of ferrimagnetic resonance with some reasonable assumptions. It is also tcund that the substitution of Gd3+ for Y3+ ions in the dodecahedral site has hardly any significant influence on the Mossbouer parameters of Fe3+ ions in the tetrahedral and octahedral sites, whose spectra can be resolved into two subspectra again.更多还原