Polycrystalline samples ofX‐type Ba2Me2Fe28O46(Me2‐X, Me=Fe, Co, and Mn) hexagonal ferrite have been prepared by the classic ceramic method. Low‐temperature magnetic properties, Curie temperatures, and distribution of divalent cations were studied. The substitution of Fe2+ions with Co2+and Mn2+ions causes a decrease of the spontaneous moment mgr; and the Curie temperatureTcofX‐type hexaferrites. The lower mgr; andTcof Co2‐Xhexaferrite originate from the smaller magnetic moment of Co2+ions. In the case of Mn2‐X, the lower mgr; may be due to the valence state of Mn and the lowerTcmay be caused by the fact that the space distribution of 3d electrons of Mn is different from that of Fe. In the Co2‐Xand Fe2‐Xcompounds the Co2+and Fe2+ions enter the octahedral sites of spinelSblocks.
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机译:采用经典陶瓷法制备了X&连字符;Ba2Me2Fe28O46(Me2‐X, Me=Fe, Co, and Mn)六方铁氧体的多晶样品.研究了低温磁性、居里温度和二价阳离子的分布。Fe2+离子被Co2+和Mn2+离子取代导致自发矩&mgr;和居里温度TcofX‐型六铁氧体的降低。较低的&mgr;和Tcof Co2‐Xhexaferrite起源于较小的Co2+离子磁矩。在 Mn2&连字符;X 的情况下,较低的 &mgr; 可能是由于 Mn 的价态,而较低的 Tc 可能是由于 Mn 的 3d 电子的空间分布与 Fe 的空间分布不同。在 Co2&连字符;X和 Fe2&连字符;X化合物中,Co2+ 和 Fe2+ 离子进入尖晶石块的八面体位点。
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