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铝、硅、碳还原剂对合成矾土基Sialon的作用及机理探讨
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摘要
本论文采用我国丰富的高铝矾土,分别以碳黑、Si粉和Al粉为还原剂利用综合差热分析(TG-DTA)、热天平、X-ray衍射(XRD)和扫描电子显微镜(SEM)来探讨铝、硅、碳三种还原剂对合成矾土基Sialon的作用及其合成机理;同时简单探讨了矾土原料中结晶水对合成Sialon的影响和三种还原剂对合成矾土基Sialon的过程的对比。
     论文较全面地探讨了铝、硅、碳三种还原剂合成矾土基Sialon的反应过程,实验数据表明:铝热还原氮化合成矾土基Sialon的过程可分为以下5个阶段:(1)AlN的形成(600-800℃);(2)SiO_2被还原并形成Si_3N_4(900-1200℃);(3)β-Sialon开始形成(1300-1350℃);(4)形成Si_2N_2O和过渡态Sialon(1400℃左右);(5)最终形成z=3的β-Sialon(1450-1500℃)。得到的β-Sialon相大部分为短柱状,尺寸为10um左右。
     硅热还原氮化合成矾土基Sialon的过程如下:(1)Si粉的氮化(900-1200℃);(2)Si_3N_4从1200℃左右与SiO_2反应生成Si_2N_2O,从1300℃左右开始Si_2N_2O与Al_2O_3反应生成O′-Sialon;(3)1300℃左右开始,Si还原原料中的SiO_2生成SiO,在N_2下SiO与N_2反应生成Si_2N_2O,从而从1400℃开始β-Sialon生成;(4)在1450-1500℃,还原氮化反应完成,最终主要产物为β-Sialon和O′-Sialon。得到的Sialon相主要为晶须状。
     碳热还原氮化合成矾土基Sialon的过程如下:(1)碳还原原料中SiO_2和莫来石生成SiO,SiO与N_2反应生成Si_2N_2O,Si_2N_2O与Al_2O_3反应生成X相(1300-1350℃);(2)β-Sialon开始生成,X相为中间产物(1400-1450℃);(3)一部分β-Sialon分解生成15R,最终物相为z=3的β-Sialon和少量的15R(1500-1550℃)。得到的β-Sialon相大多为长柱状,尺寸为10um左右。
This paper studies the process of synthesizing Sialon based on bauxite by aluminum thermal reduction-nitridation, silicon thermal reduction-nitridation and carbonthermal reduction-nitridation methods, using DTA-TG, thermal balance, XRD analysis and SEM with ED AX. The effect of crystal water on synthesization of Sialon and the influnces of the three reduction agents on the reaction processes are also compared.
    The aluminum thermal reduction-nitridation reactions involved are found to proceed in five stages as follows: (1) Formation of A1N(600-800); (2) Reduction of SiO2 and formation of Si3N4(900-1200癈); (3) Initial formation of P -Sialon(1300-1350癈); (4) Formation of Si2N2O and transitory Sialon phase(1400or so); (5) Ultimate formation of P -Sialon(Z=3) (1450-1500 癈).The ultimate microstructure of P -Sialon crystals are regular short and long column with crystal size about 1 Oum.
    The silicon thermal reduction-nitridation reactions involved are found to proceed in four
    stages as follows: (1) Formation of Si3N4 (900-1200 );(2)Initial formation of Si2N2O and
    further formation of O'-Sialon (1200-1300);(3) Reduction of SiO2 and initial formation of
    P-Sialon(l 300-1400 );(4) Ultimate formation of 逽ialon and O'-Sialon (1450-1500
    ).Most of the Sialon crystals formed are whiskers.
    The carbonthermal reduction-nitridation reactions involved are found to proceed in three stages as follows: (1) Reduction of mullite and cristobalite(1300-1350);(2) Formation of P -Sialon from X-phase as the intermediate product(1400-1450癈);(3) Partially formation of 15R from P -Sialon(1500-1550).The ultimate microstructure of P -Sialon crystals are long column with crystal size about lOum.
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