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Preparation and Magnetic Properties of Low Temperature Sintering Bi-Substituted Yttrium Iron Garnet

机译:低温烧结双取代钇铁石榴石的制备及磁性能

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摘要

The low temperature sinterability and magnetic properties of Bi-substituted yttrium iron garnet (YIG) polycrystalline samples were studied in this paper. The results showed that Bi-substitution can lower garnet phase formation temperature from about 1200℃ to 900℃ and ceramic sintering temperature from over 1300℃ to about 1050℃ respectively. The Bi-substitution leads to a decrease in initial permeability and an increase in ferromagnetic resonance linewidth (ΔH) of sintered specimens. Saturation magnetization decreases and coercive force increases a few with an increase of Bi content. The mechanism of Bi-substitution on initial permeability and ΔH is discussed. The change in initial permeability of Bi-substituted specimens relative to unsubstituted YIG results from Bismuth volatilization and weakening of superexchange interaction. The lattice dilatation in Bi-substituted YIG gives cause for a decrease of saturation magnetization and an increase of coactivity force.
机译:本文研究了双取代钇铁石榴石(YIG)多晶样品的低温烧结性和磁性。结果表明,Bi取代可分别将石榴石的相形成温度从1200℃降低至900℃,并将陶瓷烧结温度从1300℃以上降低至1050℃。 Bi替代导致烧结样品的初始磁导率降低和铁磁共振线宽(ΔH)增大。随着Bi含量的增加,饱和磁化强度降低,矫顽力增加一些。讨论了双取代对初始渗透率和ΔH的作用机理。 Bi取代的样品相对于未取代的YIG的初始磁导率的变化是由于铋的挥发和超交换作用的减弱而引起的。 Bi-取代的YIG中的晶格膨胀导致饱和磁化强度降低和协同作用力增大。

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