CIESC Journal

• 催化、动力学与反应器 • 上一篇    下一篇

杂卤石溶解动力学

安莲英;殷辉安;唐明林;郝丽芳   

  1. 成都理工大学材料与生物工程学院,四川 成都 610059

  • 出版日期:2004-06-25 发布日期:2004-06-25

KINETICS OF LEACHING PROCESS OF POLYHALITE

AN Lianying;YIN Hui’an;TANG Minglin;HAO Lifang   

  • Online:2004-06-25 Published:2004-06-25

摘要: 杂卤石中含丰富的钾资源,由于其化学上的难溶性和埋藏较深,尚未合理开发利用.已有研究表明,杂卤石矿层具备溶浸开采的地质基本条件.矿石中钾的溶解是杂卤石资源合理利用的技术关键.利用CaCl2水溶液为溶剂,通过测定溶浸液中钾、钙离子的浓度,考察了溶浸剂浓度、矿石粒度、温度对杂卤石表观溶解动力学过程的影响.实验条件下,矿石中钾的溶解率随粒度的降低明显升高.矿石粒度在0.149~1 mm之间,钾的溶解率可达80%以上.该溶解反应为一级反应(对CaCl2而言).计算实验条件下溶浸过程表观动力学速率常数,得溶解反应表观活化能为8.34 kJ•mol-1,实验结果初步表明杂卤石溶解过程受内扩散控制,溶解动力学方程符合未反应核收缩模型,实验结论对地浸法提取钾具有理论参考意义.

Abstract: Polyhalite is a kind of resource of potassium.The key problem of extracting potassium from polyhalite is dissolution of potassium in lixiviant. This paper presents the fundamental study of a new method of exploiting-leaching potassium from polyhalite deeply underground in Sichuan Nongle using CaCl2 solution as solvent.The kinetic process of dissolving potassium from polyhalite was studied by investigating the influence of the leaching conditions such as concentrations of solvent (CaCl2), mineral particle size,and temperature on the process of lixiviation through analysing potassium concentration in the lixiviation solution.The possible lixiviation process of polyhalite was discussed.The recovery of K increased with decreasing mineral particle size and could be higher than 80% under the experimental conditions(mineral particle size:0.42—1mm,initial concentration of CaCl2:5%, solid to liquid ratio=1/10,tempreture:288—373K).The experimental results showed that the dissolution reaction order was first-order.Apparent activation energy of the reaction calculated was 8.34kJ•mol-1.The paper establishes that the process controlled the dissolution process is diffusion through the ash layer, and the leaching behaviour can be modelled as a shrinking un-reacted core. This paper introduces the fundamental theoretical and laboratory studies which shows the possibility for extracting potassium from polyhalite underground by leaching.