凝聚态物理
反铁磁性
四方晶系
磁化
正交晶系
磁矩
物理
各向异性
材料科学
居里温度
晶格常数
结晶学
居里-维斯定律
磁化率
晶体结构
铁磁性
化学
衍射
磁场
量子力学
作者
Luis Nu�ez,Robin D. Rogers,G. W. Crabtree,U. Welp,K. G. Vandervoort,A. Umezawa,Y. Fang
出处
期刊:Physical review
[American Physical Society]
日期:1991-09-01
卷期号:44 (9): 4526-4531
被引量:24
标识
DOI:10.1103/physrevb.44.4526
摘要
Magnetization and lattice-constant measurements were done on four single crystals of ${\mathrm{YBa}}_{2}$${\mathrm{Cu}}_{3\mathrm{\ensuremath{-}}\mathit{x}}$${\mathrm{Fe}}_{\mathit{x}}$${\mathrm{O}}_{7\mathrm{\ensuremath{-}}\mathrm{\ensuremath{\delta}}}$ with Fe concentrations of x=0.06, 0.09, 0.15, and 0.24 to determine the structural and normal-state properties. Measurements of magnetization as a function of temperature were done in a temperature range between 90 and 300 K and analyzed using a Curie-Weiss law with a temperature-independent background. The effective magnetic moment obtained corresponds to a low spin state of ${\mathrm{Fe}}^{3+}$ with a magnitude of 2.18${\mathrm{\ensuremath{\mu}}}_{\mathit{B}}$. Magnetic anisotropy between the ab plane and the c direction is only present for the concentration of x=0.06 and is attributed to the various oxygen environments surrounding the iron. For concentrations larger than x=0.06, the moment on Fe is isotropic and Curie-Weiss fits predict uniform antiferromagnetic ordering. Structural measurements exhibit an orthorhombic-tetragonal transition at an Fe concentration of x=0.15, similar to that observed in the polycrystalline material.
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