首页> 外文会议>International Symposium on Advanced Structural and Functional Materials Design; 20041110-12; Osaka(JP) >Magnetic Phase Diagram in Layered Perovskite Manganite La_(2-2x)Sr_(1+2x)Mn_2O_7 (0.313 ≤ x ≤ 0.350)
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Magnetic Phase Diagram in Layered Perovskite Manganite La_(2-2x)Sr_(1+2x)Mn_2O_7 (0.313 ≤ x ≤ 0.350)

机译:钙钛矿层状锰La_(2-2x)Sr_(1 + 2x)Mn_2O_7(0.313≤x≤0.350)的磁相图

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摘要

We have measured the magnetization as a function of temperature and magnetic field in layered perovskite manganites of La_(2-2x)Sr_(1+2x)Mn_2O_7 single crystals (x=0.313, 0.315, 0.320, 0.350) in order to know their magnetic structures. All the present manganites exhibit magnetic transitions from ferromagnetic to paramagnetic at 76K, 107K, 120K and 125K for x=0.313, 0.315, 0.320 and 0.350, respectively. For x=0.350 and 0.320, the magnetic structure is a planar ferromagnetism whose easy axis is in the ab-plane at all temperatures below the Curie temperature. On the other hand, for x=0.315 and 0.313, the magnetic structure is an uniaxial ferromagnetism whose easy axis is along the c-axis below 85K and 66K, respectively, and a planar ferromagnetism above the temperature. From the results described above, we made the detailed magnetic phase diagram of layered perovskite manganite La_(2-2x)Sr_(1+2x)Mn_2O_7 (0.313 ≤ x ≤ 0.350).
机译:我们已经测量了La_(2-2x)Sr_(1 + 2x)Mn_2O_7单晶(x = 0.313、0.315、0.320、0.350)的钙钛矿层状锰酸盐中的磁化强度与温度和磁场的函数关系结构。对于x = 0.313、0.315、0.320和0.350,所有本发明的锰矿在76K,107K,120K和125K下均表现出从铁磁性到顺磁性的磁跃迁。对于x = 0.350和0.320,磁性结构是平面铁磁性,在居里温度以下的所有温度下,其易轴都处于ab平面。另一方面,对于x = 0.315和0.313,磁性结构是单轴铁磁性,其易轴分别沿着c轴低于85K和66K,而平面铁磁性则高于温度。根据上述结果,我们制作了层状钙钛矿锰矿La_(2-2x)Sr_(1 + 2x)Mn_2O_7(0.313≤x≤0.350)的详细磁相图。

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