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鐵-鈀-銀合金之磁性相微結構與磁特性

Magnetic Structure and Magnetic Property of Fe-Pd-Ag Alloys

摘要


本研究論文主要利用穿透式電子顯微鏡(TEM),X-ray繞射儀,調幅式示差掃描量熱計(DSC),與超導量子干涉磁化儀(SQUID),探討鐵-30鈀-4銀磁性合金固溶處理,與固溶處理後再經400-500℃,時效於各種不同時間之磁性相微結構與磁特性關係,TEM、X-ray繞射與DSC實驗結果證實,此合金固溶與時效處理後,在fcc→L10麻田散鐵相變態間,存在一中間相,此中間相為L1(下标 m)單斜晶結構,其晶格常數為a=3.208 Å,b=3.696 Å,c=3.127 Å,及β=91.997°,此中間相可能為一種適性相麻田散鐵。 超導量子干涉磁化儀之磁性量測結果顯示,固溶處理試樣,其ZFC與FC之磁化曲線並不聚合,一直到室溫T(下標R)=300K,當試樣固溶處理,再經500℃/100小時之時效處理後,則其ZFC與FC之磁化曲線呈現鋸齒狀(serrated),此現象表示有兩種磁性相,存在時效處理之試樣內部,此兩種磁性相包括單斜晶L1(下标 m)與序化型正方晶L10微結構,這兩種磁性相具有不同之磁異向性(magnetic anisotropy)。

並列摘要


This investigation reports on TEM, X-ray diffraction, DSC, and SQUID magnetometer study of magnetic structures formed in Fe-30Pd-4Ag alloys solution treated and then thermally aged at 400-500℃ for various times. The results reveal that an intermediate structure appears between the fcc→L10 martensitic transformation. The intermediate phase, denoted L1(subscript m,) has a monoclinic structure with lattice parameters of a=3.208 Å, b=3.696 Å, c=3.127 Å, and β=91.997°, which indicates that the monoclinic structure is possibly adaptive martensite, as confirmed by TEM, X-ray diffraction, and DSC. The SQUID test shows that the ZFC and FC curves of the ST specimen do not coalesce until they reach room temperature at T(subscript R)=300 K. The serrated ZFC and FC curves of the specimen aged at 500℃ for 100 h indicate that two phases exist in the aged specimen. The two phases are comprised of monoclinic L1(subscript m) phase and tetragonal ordered L10 structure, which have differing magnetic anisotropy.

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