摘要
采用平衡吸附法,进行了连云港近海沉积物对水溶液中铜离子的等温吸附研究,考察了溶液pH、时间、温度对吸附性能的影响。结果表明,在pH=5.0,7 h后反应基本达到平衡。该沉积物对水中铜离子的吸附等温线为台阶形的二级交换等温线,这与该沉积物由伊利石、蒙脱石等矿物组成有关。利用分级离子交换反应模型求出了平衡常数K1和K2。温度升高,K1和K2增大,表明升高温度有利于吸附反应的进行。
Isotherm adsorption of copper ions by marine sediment from Lianyungang was studied by batch test with the effect of pH, contact time and temperature on the adsorption clarified. Re- suits showed that the best pH value for the adsorption was 5. 0 and after 7 h the adsorption reached equilibrium. The isothermal curve belonged to second order exchange isotherm, and the sediment that mainly consists of iolite and montmorillonite accounted for the results. The ex- change equilibrium constants K1 and K2 were calculated by using the isothermal equation of surface stepwise ion exchange, which showed that high temperature favored the adsorption.
出处
《淮海工学院学报(自然科学版)》
CAS
2008年第4期49-52,共4页
Journal of Huaihai Institute of Technology:Natural Sciences Edition
基金
江苏省海洋生物技术重点建设实验室开放课题(2006HS020)
淮海工学院自然科学基金资助项目(Z2006008)
关键词
沉积物
铜离子
二级离子交换
连云港
sediments
copper ions
second order exchange
Lianyungang