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为了研究形核剂氟化物、氧化铬及其复合作用对SiO2-Al2O3-MgO-K2O系玻璃陶瓷形核和析晶的影响,采用高温熔融法制备了不同氟化物和氧化铬含量的基础玻璃,并对该基础玻璃进行了差热分析、显微分析和X射线衍射分析.结果表明:在所研究的玻璃体系中,氟化物或氧化铬的加入,都不同程度地削弱了玻璃体的结构,降低了玻璃的转变温度;当基础玻璃只含有氟化物时,玻璃在表面析出云母晶体,内部发生分相现象,而玻璃中仅含有氧化铬时,玻璃中发生整体析晶;没有氟化物的存在,不能析出云母晶体;当同时加入两种元素的物质后,对玻璃体析晶的影响不是简单的加合,复合的作用更为突出,进一步降低了玻璃的转变温度和析晶温度,整体均匀析出云母晶体.

参考文献

[1] 乔冠军;金志浩 .微晶玻璃的发展--组成、性能及应用[J].硅酸盐通报,1994,85(04):52-56.
[2] L. ARNAULT;M. GERLAND;A. RIVIERE .Microstructural study of two LAS-type glass-ceramics and their parent glass[J].Journal of Materials Science,2000(9):2331-2345.
[3] Wange P.;Hoche T.;Russel C.;Schnapp ED. .Micro structure-property relationship in high-strength MgO-Al2O3-SiO2-TiO2 glass-ceramics[J].Journal of Non-Crystalline Solids: A Journal Devoted to Oxide, Halide, Chalcogenide and Metallic Glasses, Amorphous Semiconductors, Non-Crystalline Films, Glass-Ceramics and Glassy Composites,2002(2/3):137-145.
[4] DESIKARJC;SOWEMIMO O S .Effect of zirconia addition on crystallinity,hardness,and microstructure of gel-derived barium alumnosilicate,BaAl2 Si2 O8[J].Journal of Materials Science,1992,27:5320-5324.
[5] Muller R. .Coarsening of needle-shaped apatite crystals in SiO2·Al2O3·Na2O·K2O·CaO·P2O5·F glass[J].Journal of Materials Science,1999(1):65-69.
[6] CliffordA;HILL R G;TOWLER M R.ThecrystallizationofglassesfromtheternaryCaF2-CaAl2Si2O8-P2O5system[J].Journal of Materials Science,2001(36):3955-3961.
[7] STANTONK;HILL R .TheroleoffluorineinthedevitrificationofSiO2Al2O3CaOCaFglasses[J].Journal of Materials Science,2000,35:1911-1916.
[8] ARIERIL;LEONELLI C;MANFREDINI T.Solubility,reactivityandnucleationeffectofCr2O3intheCaO-MgO-Al2O3-SiO2glassysystem[J].Journal of Materials Science,1994(29):6273-6280.
[9] 田清波 .SiO<,2>-Al<,2>O<,3>-MgO-F系可加工玻璃陶瓷制备工艺,相变机理及性能研究[D].东北大学,2002.
[10] HAMASAKIT;EGUCHI K;KOYONAGI Y et al.Preparation and characterization of machinable mica glass-ceramics by the sol-gel process[J].Journal of the American Ceramic Society,1988,71(12):1120-24.
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