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机构地区:[1]College of Chemistry Jilin University [2]Changchun Institute of Applied Chemistry Chinese Academy of Sciences
出 处:《Journal of Rare Earths》2003年第1期98-100,共3页稀土学报(英文版)
基 金:ProjectsupportedbytheNaturalScienceFoundationofJilinProvinceofChina ( 2 0 0 0 0 5 12 -2 )
摘 要:The phase-transformation in sol-gel preparation of barium hexaferrite and the formation of barium hexaferrite doped with La 3+ were studied by chemical p hase analysis, X-ray diffraction and infrared spectrometry analysis. The expe rimental results show that phase transformation reactions of FeCO 3, Fe 2O 3 and BaFe 2O 4, barium hexaferrite and γ-Fe 2O 3 take place in the heat tr eatment of gel. While the doping lanthanide ion replace barium ion, an equivalen t quantity of Fe 3+ are reduced to Fe 2+ to maintain the charge equili brium.The phase-transformation in sol-gel preparation of barium hexaferrite and the formation of barium hexaferrite doped with La 3+ were studied by chemical p hase analysis, X-ray diffraction and infrared spectrometry analysis. The expe rimental results show that phase transformation reactions of FeCO 3, Fe 2O 3 and BaFe 2O 4, barium hexaferrite and γ-Fe 2O 3 take place in the heat tr eatment of gel. While the doping lanthanide ion replace barium ion, an equivalen t quantity of Fe 3+ are reduced to Fe 2+ to maintain the charge equili brium.
关 键 词:chemical materials barium hexafettite doped rare earths sol-gel process phase transformation MECHANISM
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