新疆大学学报(自然科学版)
新疆大學學報(自然科學版)
신강대학학보(자연과학판)
XINJIANG UNIVERSITY JOURNAL(NATURAL SCIENCE EDITION)
2013年
3期
313-317,328
,共6页
阿斯叶古丽·吾布力卡丝木%拜山·沙德克%木提拉·阿曼%吾布力卡斯木·喀迪尔
阿斯葉古麗·吾佈力卡絲木%拜山·沙德剋%木提拉·阿曼%吾佈力卡斯木·喀迪爾
아사협고려·오포력잡사목%배산·사덕극%목제랍·아만%오포력잡사목·객적이
钴铁氧体%稀土元素掺杂%饱和磁化强度%矫顽力
鈷鐵氧體%稀土元素摻雜%飽和磁化彊度%矯頑力
고철양체%희토원소참잡%포화자화강도%교완력
Cobalt ferrite%rare earth element doping%saturation magnetization%coercivity
采用水热法制备了掺杂稀土元素镨(Pr)的铁氧化钴CoPrxFe2-xO4(x=0.0、0.01、0.025、0.05、0.075、0.1)纳米颗粒.实验结果表明制备出来的样品是立方体结构的纳米颗粒,当掺杂量0<x≤0.1的时候Pr3+离子成功的能掺杂到CoFe2O4晶格内,但掺杂量x >0.1(x =0.15)时出现杂峰.随着掺杂量从0增加到0.1时,样品的平均晶格尺寸从34nm 减小到15nm,饱和磁化强度(Ms)从78emu/g 单调减小至36emu/g,矫顽力从1008Oe 降低到668Oe .
採用水熱法製備瞭摻雜稀土元素鐠(Pr)的鐵氧化鈷CoPrxFe2-xO4(x=0.0、0.01、0.025、0.05、0.075、0.1)納米顆粒.實驗結果錶明製備齣來的樣品是立方體結構的納米顆粒,噹摻雜量0<x≤0.1的時候Pr3+離子成功的能摻雜到CoFe2O4晶格內,但摻雜量x >0.1(x =0.15)時齣現雜峰.隨著摻雜量從0增加到0.1時,樣品的平均晶格呎吋從34nm 減小到15nm,飽和磁化彊度(Ms)從78emu/g 單調減小至36emu/g,矯頑力從1008Oe 降低到668Oe .
채용수열법제비료참잡희토원소보(Pr)적철양화고CoPrxFe2-xO4(x=0.0、0.01、0.025、0.05、0.075、0.1)납미과립.실험결과표명제비출래적양품시립방체결구적납미과립,당참잡량0<x≤0.1적시후Pr3+리자성공적능참잡도CoFe2O4정격내,단참잡량x >0.1(x =0.15)시출현잡봉.수착참잡량종0증가도0.1시,양품적평균정격척촌종34nm 감소도15nm,포화자화강도(Ms)종78emu/g 단조감소지36emu/g,교완력종1008Oe 강저도668Oe .
Rare earth element praseodymium-doped CoPrxFe2-xO4 (x=0.0, 0.01, 0.025, 0.05, 0.075, 0.1)magnetic nanoparticles were successfully synthesized by the hydrothermal method. The results show that prepared samples are cubic structural nanoparticle, when the dopant amount in the range 0<x 6 0.1, we have not observed any trace of impurity peaks which confirms that, Pr3+ions have been incorporated into the cobalt ferrite lattice, but when its value over the 0.1, impurity peak occurs. With the increase in dopant amount from 0 to 0.1, the average crystallite size decreases from 34nm to 15nm, saturation magnetization (Ms) monotone reduces from 78emu/g to 36emu/g and coercivity decreases from 1008Oe to 668Oe.