研究成果 - 林敏聰 博士
尖端材料與表面科學組

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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最後更新於 2025-04-30 14:15:19
地址: 106319 台北市羅斯福路四段一號 或 106923 臺北臺大郵局 第23-166號信箱
電話:886-2-2362-0212 傳真:886-2-2362-0200 電子郵件:iamspublic@gate.sinica.edu.tw
最後更新於 2025-04-30 14:15:19