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水溶液中Pb(II)在土耳其高岭土上吸附的平衡、动力学及热力学研究

Equilibrium, kinetic and thermodynamic studies of adsorption of Pb(II) from aqueous solution onto Turkish kaolinite clay.

作者信息

Sari Ahmet, Tuzen Mustafa, Citak Demirhan, Soylak Mustafa

机构信息

Department of Chemistry, Gaziosmanpasa University, 60250 Tokat, Turkey.

出版信息

J Hazard Mater. 2007 Oct 22;149(2):283-91. doi: 10.1016/j.jhazmat.2007.03.078. Epub 2007 Mar 30.

Abstract

The adsorption of Pb(II) onto Turkish (Bandirma region) kaolinite clay was examined in aqueous solution with respect to the pH, adsorbent dosage, contact time, and temperature. The linear Langmuir and Freundlich models were applied to describe equilibrium isotherms and both models fitted well. The monolayer adsorption capacity was found as 31.75 mg/g at pH 5 and 20 degrees C. Dubinin-Radushkevich (D-R) isotherm model was also applied to the equilibrium data. The mean free energy of adsorption (13.78 kJ/mol) indicated that the adsorption of Pb(II) onto kaolinite clay may be carried out via chemical ion-exchange mechanism. Thermodynamic parameters, free energy (deltaG degrees ), enthalpy (deltaH degrees ) and entropy (deltaS degrees ) of adsorption were also calculated. These parameters showed that the adsorption of Pb(II) onto kaolinite clay was feasible, spontaneous and exothermic process in nature. Furthermore, the Lagergren-first-order, pseudo-second-order and the intraparticle diffusion models were used to describe the kinetic data. The experimental data fitted well the pseudo-second-order kinetics.

摘要

研究了土耳其(班德尔马地区)高岭土对水溶液中Pb(II)的吸附作用,考察了pH值、吸附剂用量、接触时间和温度的影响。应用线性朗缪尔模型和弗伦德利希模型描述平衡等温线,两个模型拟合效果均良好。在pH值为5、温度为20℃时,单层吸附容量为31.75 mg/g。还将杜宾宁-拉杜舍维奇(D-R)等温线模型应用于平衡数据。吸附平均自由能(13.78 kJ/mol)表明,Pb(II)在高岭土上的吸附可能通过化学离子交换机制进行。还计算了吸附的热力学参数,即自由能(ΔG°)、焓(ΔH°)和熵(ΔS°)。这些参数表明,Pb(II)在高岭土上的吸附在本质上是可行的、自发的和放热过程。此外,用 Lagergren 一级、伪二级和颗粒内扩散模型描述动力学数据。实验数据与伪二级动力学拟合良好。

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