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研究成果 - 林敏聰 博士

尖端材料與表面科學組
林敏聰 博士
奈米磁學實驗室
主持人:林敏聰 博士
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辦公室:10617台北市羅斯福路四段一號台大物理系 625室
辦公室電話:+886-2-3366-5173
實驗室:台大物理系 619, 620
實驗室電話:+886-2-3366-5168
透過鐵磁反鐵磁交換耦合產生垂直磁性

B. Y. Wang,N. Y. Jih,W. C. Lin,C. H. Chuang,P. J. Hsu,C. W. Peng,Y. C. Yeh,Y. L. Chan,D. H. Wei, W. C. Chiang, and Minn-Tsong Lin*
 

透過鐵磁反鐵磁交換耦合產生垂直磁性
Using x-ray photoemission electron microscopy and the magneto-optical Kerr effect, we have demonstrated a perpendicular magnetic anisotropy that could be due to exchange coupling between the ferromagnetic and antiferromagnetic layers. The results of magnetic imaging and hysteresis loops show that the magnetization of Fe and permalloy (Py) films orients from the in-plane to perpendicular direction, as an Mn underlayer is above a threshold value that depends on the Fe or Py layer thickness. Their thickness-dependent behaviors can be quantitatively described by a phenomenological model that takes into account the finite-size effect of the antiferromagnet on exchange coupling. The anisotropy energy extracted from the model and the thermal stability of perpendicular magnetization enhanced with the increase of the Mn underlayer further demonstrate the exchange coupling nature.FIG 1. (a)-(c) Magnetic domain images of a 6 ML Fe/wedged-Mn bilayer measured with different relative orientations between the polarization of incoming x-ray and samples at 220 K. The magnetization direction of the Fe domains switches from in-plane to perpendicular direction while the thickness of Mn layer is increased.FIG 2.Magnetic easy axis phase diagram for (a) Fe/Mn biayers and (b) Py/Mn bilayes, measured by MOKE at 220 K. The solid lines are the SRT boundaries fitted with theoretical model







 
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