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采用溶胶-凝胶法制备 La1-xSrxMn1-yFeyO3(x=0.15,0.20,0.23;y=0.10,0.12,0.14,0.16),用HP8722型微波网络矢量分析仪测定样品在频率2~18 GHz的电磁波吸收特性. 发现Sr和Fe含量的改变都会影响体系的吸波性能,经测试得到x=0.2,y=0.14时的吸波特性最好. 对于La0.8Sr0.2Mn0.86Fe0.14O3,在涂层厚度为2 mm时,有两个吸收峰,最大峰值达到了37 dB,10 dB以上的带宽达到了6.2 GHz,在2~12.5 GHz频率段微波吸收主要以介电损耗为主,在12.5 GHz附近介电损耗和磁损耗发生突变,在12.5~18 GHz频率段微波主要以磁损耗为主,电阻率在室温时处在半导体范围内,对吸波有利.

参考文献

[1] 戴道生;熊光成;吴思诚 .Re1-xTxMnO3氧化物的结构、电磁特性和巨磁电阻[J].物理学进展,1997,17(02):201.
[2] 胡季帆,梅良模,丁志强,付刚,赵文瑾,张清泉,刘宜华.钙钛矿氧化物La0.65(Ca,Ba)0.35Mn1-xFexOy的磁电阻效应[J].稀土,2000(01):19-22.
[3] Owens F J .DC magnetic field dependent microwave absorption in CMR material La0.7Sr0.3Mn3[J].Journal of Physics and Chemistry of Solids,1997,58(09):1311.
[4] Belevtsev BI.;Cherpak NT.;Chukanova IN.;Gubin AI.;Krasovitsky VB. Lavrinovich AA. .Magnetic inhomogeneity effects in DC transport properties and microwave absorption of La0.5Sr0.5CoO3-delta film[J].Physica, E. Low-dimensional systems & nanostructures,2003(1/3):304-305.
[5] 胡国光,尹萍,吕庆荣.LaxSr1-xMnO3氧化物的导电和吸收特性[J].中国稀土学报,2002(02):179-181.
[6] Li G.;Hu GG.;Zhou HD.;Fan XJ.;Li XG. .Attractive microwave-absorbing properties of La1-xSrxMnO3 manganite powders[J].Materials Chemistry and Physics,2002(1/3):101-104.
[7] Ogale SB.;Bathe R.;Date SK.;Patil SI.;Hannoyer B.;Petit F.;Marest G.;Shreekala R. .Transport properties, magnetic ordering, and hyperfine interactions in Fe-doped La0.75Ca0.25MnO3: Localization-delocalization transition[J].Physical Review.B.Condensed Matter,1998(13):7841-7845.
[8] 李斌太,陈大明,陈钦生.铁氧体微波吸收材料的研究进展[J].硅酸盐通报,2004(05):66-69.
[9] Ahn K H;Wu X W;Liu K et al.Magnetic properties and colossal magnetoresistance of La(Ca)MnO3 materials doped with Fe[J].Physical Review,1996,B54:15299.
[10] Tkachuk A.;Brown DE.;Dabrowski B.;Fedro AJ.;Kimball CW. Pyles B.;Xiong X.;Rosenmann D.;Dunlap BD.;Rogacki K. .Dynamics of phase stability and magnetic order in magnetoresistive (La0.83Sr0.17Mn0.98Fe0.02O3)-Fe-57[J].Physical Review.B.Condensed Matter,1998(14):8509-8517.
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