摘要
本文对一定粒级分布的高岭石的脱水反应进行了研究,研究表明高岭石的脱水反应级数与加热速度有关,并首次发现不同温度有不同的脱水量,说明了高岭石的脱水过程是跳跃式的,且其脱水是由水的层间扩散和水的形成共同控制的。
This paper studied the dehydration of kaolinite with a certain size distribution. It was discovered that order of the dehydration of kaolinite varys with heating rates. It is first found out that there is a certain amount of loss in water at a certain point of temperature,which shows that the dehydration of kaolinite is jumpy.
