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以硝酸锂、硝酸铝和碳酸氢铵为原料,采用溶胶-凝胶法制备了Li-β-Al2O3纳米粉体.研究了pH值、热处理温度和锂铝物质的量比[n(Li)/n(Al)]对制备Li-β-Al2O3纳米粉体的影响.用X射线衍射仪(XRD)、场发射扫描电镜(FE-SEM)和自动电位粒度仪对制备的粉体进行了表征.结果表明,当n(Li)/n(Al) =1∶ 5(为化学计量比时),pH值在3.6左右时,可得到稳定透明的凝胶,经1000℃热处理后,产物为纯相的Li-β-Al2O3,FE-SEM结果表明粉体的粒度在100nm以内.

参考文献

[1] Sartori S;Martucci A;Muffato A et al.Sol-gel synthesis of Na+ beta-Al2O3 power[J].Journal of the European Ceramic Society,2004,24:911-914.
[2] 金从进,洪彦若.Laβ-Al2O3固体电解质的导电性能[J].硅酸盐学报,1998(02):217-225.
[3] Arnoud P;Kroon D;Gstrein F et al.Ionic conductivity of dense K-β-alumina ceramics:microstructural dependence and the influence of phase transformations[J].Solid-State Ionicis,2000,133:107-120.
[4] V. Jayaraman;G. Periaswami;T. R. N. Kutty .Preparation and characterization of rubidium-β-alumina by the gel-to-crystallite conversion method[J].Materials Research Bulletin: An International Journal Reporting Research on Crystal Growth and Materials Preparation and Characterization,2000(8):1213-1225.
[5] Miroslaw M. Bucko;Maria Cichocinska .Preparation of Ca-β″-Al_2O_3 from Alumina Gel[J].Journal of the European Ceramic Society,1996(1):79-84.
[6] Zhang AY.;Akashi T.;Goto T. .Electrical conductivity of non-stoichometric Sr beta-alumina single crystals prepared by a floating zone method[J].Solid state ionics,2003(3):425-431.
[7] Zhang AY;Akashi T;Goto T .Electrical conductivity of nonstoichiometric Ba beta-alumina single crystals prepared by a floating zone method[J].Solid state ionics,2004(1/2):77-82.
[8] 王常珍.固体电解质和化学传感器[M].北京:冶金工业出版社,2000:519-522.
[9] H.C. PARK;Y.B. LEE;S.G. LEE .Synthesis of beta-alumina powders by microwave heating from solution-derived precipitates[J].Ceramics International,2005(2):293-296.
[10] Li Q;Zhang C;Komeya K et al.Nano powers of β-Sialon carbothermally produced via a sol-gel process[J].Journal of Materials Science Letters,2003,22(12):885-887.
[11] 杨南如;余桂郁 .溶胶-凝胶法的基本原理与过程[J].硅酸盐通报,1992,11(02):561-563.
[12] 黄剑锋.溶胶凝胶原理与技术[M].北京:化学工业出版社,2005:159-160.
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