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钾长石矿热分解过程的研究
Studies on the Thermal Dissociative Process of Microcline
【摘要】 研究了钾长石矿热分解过程的反应行为和动力学.对6种钾长石体系进行了热力学分析,计算了各反应在800~1600K的ΔG0T,并以此指导实验.研究了焙烧温度、停留时间和助剂配比对钾长石体系热分解为水溶性钾的影响,得出最佳操作条件.添加0.9%添加剂I能使适宜焙烧温度由1323K降至1223K,钾分解率可达84%.不加与加入添加剂I的2种钾长石体系热分解过程皆符合克-金-布动力学方程,均受固膜扩散控制,表观活化能分别为184.84kJ/mol和158.9kJ/mol,并给出相应的动力学方程.
【Abstract】 The microcline CaSO 4 CaO system was determined to be used to obtain K 2SO 4 by thermodynamical analysing and computing lots of possible reactions of 6 microcline systems. The effects of roasting temperature, time and ratios of reactants on the potassium recovery of the microcline CaSO 4 CaCO 3 were studied and the favorable conditions were determined as follow: 1 323 K, 3.0 h, m (microcline)∶ m (CaSO 4\52H 2O)∶ m (CaCO 3)=1∶1∶3. In the presence of 0.9% additive I, the roasting temperature decreased from 1 323 K to 1 223 K and the potassium recovery was 84%. Kinetic experimental data of the two systems with or without additive I both fitted a diffusion through product layer reaction control model, and their kinetic equations were presented with apparent activation energies 184.4 kJ\5mol -1 and 158.9 kJ\5mol -1 respectively.
- 【文献出处】 高等学校化学学报 ,CHEMICAL RESEARCH IN CHINESE UNIVERSITIES , 编辑部邮箱 ,1998年03期
- 【分类号】TQ443.5
- 【被引频次】50
- 【下载频次】549