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海泡石对铵离子的吸附特性:用多种等温线分析平衡数据

Nature of ammonium ion adsorption by sepiolite: analysis of equilibrium data with several isotherms.

作者信息

Balci Suna

机构信息

Faculty of Engineering and Architecture, Department of Chemical Engineering, Gazi University, 06570 Maltepe, Ankara, Turkey.

出版信息

Water Res. 2004 Mar;38(5):1129-38. doi: 10.1016/j.watres.2003.12.005.

Abstract

Adsorption isotherms for an ammonium ion-sepiolite system have been established for initial ammonium ion solution concentrations in the range of 8.32-388.06 mmol NH(4)(+)/L (150-7000 ppm). The change of the "g sepiolite/mL solution" ratios from 1/10 to 1/70 caused an increase in the adsorption from 1.82 to 3.70 mmol NH(4)(+)/g for the average particle size of 2.8mm. The equilibrium data were fitted to "general-purpose isotherms" and "first-order adsorption model", and the adjustable parameters of the isotherms were estimated by nonlinear least-squares analysis. Langmuir and Freundlich models were found insufficient to explain the adsorption equilibrium, while Langmuir-Freundlich and Tooth isotherms explained the data well. Goodness of fit increased with the increased sepiolite quantity in the treated suspension.

摘要

已建立了铵离子-海泡石体系的吸附等温线,初始铵离子溶液浓度范围为8.32 - 388.06 mmol NH₄⁺/L(150 - 7000 ppm)。对于平均粒径为2.8mm的情况,“海泡石克数/毫升溶液”的比例从1/10变为1/70,导致吸附量从1.82 mmol NH₄⁺/g增加到3.70 mmol NH₄⁺/g。将平衡数据拟合到“通用等温线”和“一级吸附模型”,并通过非线性最小二乘法分析估计等温线的可调参数。发现朗缪尔和弗伦德利希模型不足以解释吸附平衡,而朗缪尔-弗伦德利希等温线和图思等温线能很好地解释数据。拟合优度随处理悬浮液中海泡石量的增加而提高。

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