磁硬石-聚丙烯腈插层化合物碳热还原过程中Si/ 3N/ 4的形成。

Y. Sugahara, Yasuyuki Nomizu, K. Kuroda, C. Kato
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引用次数: 9

摘要

采用碳热还原法制备了磁硬石(层状聚硅酸盐)-聚丙烯腈(PAN)插层化合物。在1400℃以上,镁辉石中的SiO2被还原,没有形成任何结晶氧化物。在1400℃以上加热时,α和β-Si3N4均被检测到,而在1600℃加热时则观察到α和β-SiC的额外生成。另一方面,由磁石-碳混合物合成的反应涉及方石英、α和β-Si3N4以及β-SiC的形成。此外,还表明该混合物对Si3N4的形成反应性较弱。这些结果表明,磁硬石- pan络合物的反应过程与磁硬石-碳混合物的反应过程不同,插层化合物的使用有利于Si3N4的生成。
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Si//3N//4 FORMATION IN THE CARBOTHERMAL REDUCTION PROCESS OF A MAGADIITE-POLYACRYLONITRILE INTERCALATION COMPOUND.
Silicon nitride was formed from a magadiite (layered polysilicate)-polyacrylonitrile (PAN) intercalation compound through a novel process of carbothermal reduction. SiO2 from magadiite was reduced above 1400°C without the formation of any crystalline oxides. On heating above 1400°C, both α-and β-Si3N4 were detected, and the additional formation of α-and β-SiC was observed by heating at 1600°C. On the other hand, the reactions for the synthesis from a magadiite-carbon mixture involved the formation of cristobalite as well as α-and β-Si3N4, and β-SiC. In addition, it was also indicated that the mixture was less reactive for the formation of Si3N4. These observations suggest that the reaction process of the magadiite-PAN complex was different from that of the magadiite-carbon mixture, and that the use of the intercalation compound was favorable for Si3N4 production.
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