研究生: |
曾健家 |
---|---|
論文名稱: |
Fe/Co/Pt(111)的磁性研究 |
指導教授: | 沈青嵩 |
學位類別: |
碩士 Master |
系所名稱: |
物理學系 Department of Physics |
論文出版年: | 2005 |
畢業學年度: | 93 |
語文別: | 中文 |
論文頁數: | 77 |
中文關鍵詞: | 磁光柯爾效應 、柯爾訊號 、矯頑磁場 |
論文種類: | 學術論文 |
相關次數: | 點閱:227 下載:5 |
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摘要
我們利用表面磁光柯爾效應儀(SMOKE)探測鐵超薄膜在純白金以及鈷與白金所形成的磁性基底上磁性隨著薄膜厚度的變化。
Fe在Pt(111)上的成長,其磁性和薄膜厚度的關係受外加磁場的大小影響而有所不同,利用小磁場可以測得磁化易軸位於in plane方向,而利用大磁場測量會把磁化難軸磁化,導致在in plane與out of plane方向皆可得到磁滯訊號。在Fe薄膜的厚度為1ML時,測量不到磁滯訊號,降溫測量也是如此,有可能此樣品不具磁性,或者居禮溫度低於165K。把5ML Fe/Pt(111)經退火效應後在室溫測量磁滯訊號,發現只有在Longitudinal方向有值,當退火溫度到830K時,磁滯消失。dFe Fe/不平坦Pt用大磁場測量,會得到和dFe Fe/Pt(111)相同的結果,差別在於dFe Fe/不平坦Pt樣品Polar方向的矯頑磁場在薄膜厚度3ML時有最大值,而dFeFe/Pt(111)則是隨著厚度增加而增加。
鐵在鈷與白金所形成的磁性基底的成長,基底一開始具有Polar方向的磁性,鍍上鐵後,Polar方向的磁性消失,最後隨著層數增加,Polar與Longitudinal方向皆測的到磁滯訊號。基底若一開始具有Longitudinal方向的磁性,鍍上鐵後,Longitudinal方向的磁性仍在,隨著層數增加,Polar方向的磁性也顯現出來,最後兩個方向皆有訊號。
經由以上鐵薄膜在不同基底的磁性探討,和實驗室之前的研究統整,希望將來能夠把鐵磁性物質在白金上的磁性與結構變化做個完整的探究。
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