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Structural Characterization of Mullite Formed from Heated Kaolin of Tamazert deposit (Algeria)

机译:由塔玛泽特矿床(阿尔及利亚)加热的高岭土形成的莫来石的结构表征

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A quantitative analysis of the mullite phase obtained after sintering of the kaolin has been performed by treatment of X ray diagrams Kaolin is treated in the range of 950-1400 °C. The oxide NiO is added as internal standard after cooling to sintered sample kaolin. Bragg Brentano diffractometer, scanning electron microscopy and differential thermal analysis were used. Analyses of selected directions profile of mullite were carried out by using the adjustment of program, available in the software Highscore of Pan Analytical. The mullite phase that formed from kaolin appears at 1000 °C, observed by XRD and tallies with DTA. The primary mullite crystal showed a plate-like morphology. Two kinds of morphology corresponding to primary (elongated grains) and secondary (equiaxed grains) mullite were observed. A bimodal crystallite size distribution was detected through XRD microstructural analysis from 1300 °C. The apparent sizes obtained of crystallites are determined for mullite with directions-dependent (anisotropy).
机译:通过X射线图的处理,对高岭土烧结后获得的莫来石相进行了定量分析。高岭土在950-1400℃的温度范围内进行处理。冷却后,将氧化物NiO作为内标添加到烧结的样品高岭土中。使用了Bragg Brentano衍射仪,扫描电子显微镜和差热分析。通过使用程序的调整对莫来石的所选方向轮廓进行分析,该程序可在软件Pan Analytical的Highscore中获得。 XRD观察到由高岭土形成的莫来石相出现在1000°C,DTA记录。初级莫来石晶体显示出板状形态。观察到了两种形态,分别对应于一次(细长晶粒)和二次(等晶粒)莫来石。通过XRD微观结构分析从1300°C检测到双峰微晶尺寸分布。确定具有方向依赖性(各向异性)的莫来石的微晶获得的表观尺寸。

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