α- fe2o3中fe57的核磁共振

M. Matsuura, H. Yasuoka, A. Hirai, T. Hashi
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引用次数: 7

摘要

采用稳态法和脉冲核磁共振法对α- fe2o3中fe57的核磁共振进行了研究。该信号可以在温度范围内观察到,该温度范围内样品显示寄生铁磁性。实验结果表明,该样品的核磁共振信号是由畴壁内的核引起的。测得外加射频磁场的平均增强系数约为25000。在室温下,fe57的自旋晶格弛豫时间(t1)随激发脉冲强度的不同分布在3 ~ 100 msec之间。t1的取值可以用热畴壁波动引起的松弛机制定性地解释。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Nuclear Magnetic Resonance of Fe 57 in α-Fe 2 O 3
Nuclear magnetic resonance (NMR) of Fe 57 in α-Fe 2 O 3 was studied by using both the steady-state method and the pulsed NMR method. The signal could be observed in the temperature range, where the sample shows the parasitic ferromagnetism. From the experimental results it was concluded that the NMR signal of this sample is due to the nuclei with in the domain wall. The average enhancement factor of the applied rf magnetic field was measured to be about 25,000. The spin lattice relaxation time ( T 1 ) of Fe 57 was distributed between 3 m sec and 100 msec at room temperature, depending upon the intensity of the exciting rf pulse. The values of T 1 could be qualitatively explained by the relaxation mechanism due to the thermal domain wall fluctuation.
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