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Non-isothermal Kinetic Analysis of Processes Occurring During Thermal Treatment of Kaolinite

机译:高岭土热处理过程中发生的过程的非等温动力学分析

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A non-isothermal kinetic analysis of processes occurring during thermal treatment of kaolinite is carried out using differential thermal analysis on powder samples with heating rates from 1 to 10°C min~(-1) in static air atmosphere. For the parameterization of dehydroxylation process and crystallization of Al-Si spinel phase from metakaolinite the Kissinger method is used. The determined values of apparent activation energy for the dehydroxylation of kaolinite and formation of Al-Si spinel phase are (163 ± 11) kJ mol~(-1) and (826 ± 16) kJ mol~(-1), respectively. For the dehydroxylation of kaolinite the diffusion controlled growth of a new phase with a decreasing nucleation rate is determined as a mechanism of the process. The results also show that the formation of Al-Si spinel phase from metakaolinite is controlled by grain edge nucleation after saturation.
机译:在高岭石热处理期间发生的过程的非等温动力学分析在静态空气气氛中使用从1至10℃min〜(-1)的粉末样品上的粉末样品进行差动热分析。对于脱羟基化工艺的参数化和来自Metakaolinite的Al-Si尖晶石相结晶,使用吻指针方法。对于高岭土的脱羟基化的明显活化能量和Al-Si尖晶石相的形成的确定值分别分别为(163±11)kJ mol〜(-1)和(826±16)kJ mol〜(-1)。对于高岭土的脱羟基化,通过降低成核速率的新相的扩散控制生长被确定为该方法的机制。结果还表明,饱和后的颗粒边缘成颗成颗成颗核来控制来自Metakaolinite的Al-Si尖晶石相。

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