Comparison of isotherms for the ion exchange of Pb(II) from aqueous solution onto homoionic clinoptilolite

被引:71
作者
Berber-Mendoza, M. S.
Leyva-Ramos, R. [1 ]
Alonso-Davila, P.
Fuentes-Rubio, L.
Guerrero-Coronado, R. M.
机构
[1] UASLP, Fac Ciencias Quim, Ctr Invest & Estudios Posgrado, San Luis Potosi 78260, SLP, Mexico
[2] Inst Potosino Invest Cientif & Tecnol, DMASC, San Luis Potosi 78260, SLP, Mexico
关键词
clinoptilolite; ion exchange; isotherm; lead zeolite;
D O I
10.1016/j.jcis.2006.04.037
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The ion exchange equilibrium of Pb(II) on clinoptilolite modified with NH4Cl and NaCl can be represented by two types of isotherms. The first one is the ion exchange isotherm based upon the constant of thermodynamic equilibrium for the ion exchange reaction; however, the fitting procedure for this isotherm can be very tedious due to all the calculations involved and additional thermodynamic data. The second one is the Langmuir isotherm. The use of the Langmuir isotherm to represent ion exchange equilibrium has increased in recent last years since it adequately fits the equilibrium data and, furthermore, its calculation is much simpler. A comparison between the two isotherms showed that they fitted the experimental data reasonably well, but the Langmuir isotherm is much simpler and easier to use. (c) 2006 Elsevier Inc. All rights reserved.
引用
收藏
页码:40 / 45
页数:6
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