双钙钛矿氧化物Pr_(2-x)Tb_xCoMnO_6(x=0.00,0.05,0.10)的磁性研究
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  • 英文篇名:Magnetic study of double perovskite oxide Pr_(2-x)Tb_xCoMnO_6 (x=0.00,0.05,0.10)
  • 作者:李晓欣 ; 刘娇 ; 王婷 ; 田野 ; 云慧琴 ; 邢茹 ; 赵建军
  • 英文作者:LI Xiaoxin;LIU Jiao;WANG Ting;TIAN Ye;YUN Huiqin;XING Ru;ZHAO Jianjun;School of Physics Science and Technology, Baotou Teachers' College;Key Laboratory for Magnetism and Magnetic Material of Inner Mongolia Autonomous Region, Baotou Teachers' College;
  • 关键词:双钙钛矿 ; 磁性 ; 类Griffiths相
  • 英文关键词:double perovskite;;magnetic;;Griffiths-like phase
  • 中文刊名:GNCL
  • 英文刊名:Journal of Functional Materials
  • 机构:包头师范学院物理科学与技术学院;包头师范学院内蒙古自治区磁学与磁性材料重点实验室;
  • 出版日期:2019-03-31
  • 出版单位:功能材料
  • 年:2019
  • 期:v.50;No.426
  • 基金:国家自然科学基金资助项目(11164019,51562032,61565013);; 内蒙古自治区科学基金资助项目(2015MS0109);; 内蒙高校科学研究基金资助项目(NJZZ11166,NJZY12202);; 包头市科学技术局产学研合作资助项目(2014X1014-01,2015Z2011);; 内蒙古自治区研究生科研创新资助项目(S201710127(S01)
  • 语种:中文;
  • 页:GNCL201903024
  • 页数:5
  • CN:03
  • ISSN:50-1099/TH
  • 分类号:148-152
摘要
利用传统高温固相反应法制备了钙钛矿钴氧化物Pr_(2-x)Tb_xCoMnO_6(x=0.00,0.05,0.10)系列多晶样品,通过样品的XRD谱线、磁化强度随温度、外加磁场的变化曲线(M-T、M-H)等对样品的晶体结构和磁性进行了研究.结果表明:系列样品Pr_(2-x)Tb_xCoMnO_6(x=0.00,0.05,0.10)呈现良好的单相性,空间点群为P2_1/n;由于Co~(2+)与Mn~(4+)之间的铁磁超交换相互作用和少量无序的Co~(3+)与Mn~(3+)之间的铁磁超交换相互作用,3个样品均出现两个铁磁转变点(T_(C1)和T_(C2)),观察到系列样品存在类Griffiths相,温度T>T_G则为纯顺磁态;在T_(C2)-T_G之间属于顺磁-铁磁共存状态;在低温区(T        A series of polycrystalline samples of perovskite cobalt oxide Pr_(2-x)Tb_xCoMnO_6(x=0.00,0.05,0.10) were prepared by traditional high-temperature solid-state reaction. The XRD spectra, magnetization curves and variation curve of applied magnetic field(M-T, M-H) with temperature were measured to study the crystal structure and magnetic properties of the sample. The results show that the series of samples Pr_(2-x)Tb_xCoMnO_6(x=0.00,0.05,0.10) exhibited good single phase. The spatial point group was P2_1/n. Due to the ferromagnetic super-exchange interaction between Co~(2+) and Mn~(4+) and a small amount of disordered ferromagnetic super-exchange interaction between Co~(3+) and Mn~(3+), two ferromagnetic transition points appeared in all the three samples. It is observed that there is a Griffiths-like phase in the series of samples. When temperature T was higher than T_G, it showed pure paramagnetic state. When temperature was between T_(C2)-T_G, it showed paramagnetic-ferromagnetic coexistence state. At low temperature(T
引文
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