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    煤系高岭石流态化煅烧脱碳活化实验研究

    Experimental study on the decarburization and activation of coal-Series kaolin by fluidized calcination

    • 摘要: 替代熟料技术对水泥工业的降碳优势显而易见。煅烧煤系高岭石作为一种高活性低碳材料,可以用作混合材替代部分熟料。为明确流态化煅烧参数对产物活性的影响规律及其流态化煅烧活化机理,采用自主设计的流态化煅烧设备开展煤系高岭石煅烧实验,探究了煅烧温度、煅烧时间和原料粒径等因素对煅烧产物活性的影响规律,并借助XRD和FT−IR手段表征煅烧产物的微观结构,揭示煤系高岭石流态化煅烧活化机理。结果表明:煤系高岭石最佳流态化活化温度在750 ℃左右,此时煅烧产物的Al3+、Si4+浓度最高,火山灰活性最好。在一定范围内延长保温时间有利于产物活性的激发,当煅烧时间达到30 min时,产物活性提高78%,继续增大保温时间对活性影响不大。细粒径原料对火山灰活性的激发有积极作用,但极细的原料不利于实际生产使用。通过煅烧产物的XRD和FT−IR图谱,发现流态化煅烧能有效脱除高岭石的内、外羟基,其稳定的晶体结构被破坏,变为亚结晶态的偏高岭石,同时Al转变为Al。从煅烧产物活性和结构变化之间的关系可知,煅烧煤系高岭石的活性来源是高岭石矿物因脱羟基引起的结晶态和铝配位形式的改变。

       

      Abstract: The carbon reduction advantages of substitute clinker technology for cement industry are obvious. Calcined coal-series kaolin, as a high activity and low carbon material, can be used as a mixture to replace some clinker. In order to clarify the law of influence of fluidized calcination conditions on product activity and the activation mechanism of fluidized calcination, this paper carried out the calcination experiment of calcined coal-series kaolin with self-designed fluidized calcination equipment, and explored the law of influence of factors such as calcination temperature, calcination time and particle size of raw materials on product activity. The microstructure of calcined products was characterized by XRD and FTIR, and the activation mechanism of calcined coal-series kaolin was revealed. The results show that the optimum fluidization activation temperature of calcined coal-series kaolin is about 750 ℃, at which the concentration of Al3+ and Si4+ of calcined products is the highest, and the activity of volcanic ash is the best. Prolonging the holding time in a certain range is conducive to the activation of product activity. When the calcination time reaches 30min, the product activity increases by 78%, and further increasing the holding time has little effect on the activity. Fine particle size raw material has a positive effect on the activation of volcanic ash activity, but very fine raw material is not conducive to practical production and use. Through XRD and FTIR spectra of calcined products, it is found that the internal and external hydroxyl groups of kaolinite can be effectively removed by fluidized calcination, and its stable crystal structure is destroyed and transformed into subcrystalline metakaolinite, and Al is transformed into Al. From the relationship between calcined product activity and structure change, it can be seen that the activity source of calcined coal-series kaolin is the change of crystallinity and aluminum coordination form caused by dehydroxylation of kaolinite minerals.

       

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