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煅烧膨润土对水溶液中镍离子的吸附动力学和平衡研究。

Sorption kinetics and equilibrium for the removal of nickel ions from aqueous phase on calcined Bofe bentonite clay.

机构信息

UNICAMP/FEQ/DTF, Campinas/SP, Brazil.

出版信息

J Hazard Mater. 2010 May 15;177(1-3):362-71. doi: 10.1016/j.jhazmat.2009.12.040. Epub 2009 Dec 16.

Abstract

In this paper the kinetics and dynamics of nickel adsorption on calcined Bofe bentonite clay were studied. The clay was characterized through EDX, surface area (BET) and XRD analysis. The influence of parameters (pH, amount of adsorbent, adsorbate concentration and temperature) was investigated. Kinetic models were evaluated in order to identify potential adsorption process mechanisms. The Langmuir and Freundlich models were utilized for the analysis of adsorption equilibrium. Thermodynamic parameters were assessed as a function of the process temperature. The kinetics data were better represented by the second-order model. The process was found to be strongly influenced by the factors studied. The Bofe clay removed nickel with maximum adsorption capacity of 1.91 mg metal/g of clay (20 degrees C; pH 5.3) and that the thermodynamic data indicated that the adsorption reaction is spontaneous and of an exothermal nature. The Langmuir model provided the best fit for sorption isotherms.

摘要

本文研究了镍在煅烧后的伯斐膨润土上的吸附动力学和动力学。通过 EDX、比表面积(BET)和 XRD 分析对粘土进行了表征。考察了参数(pH 值、吸附剂用量、吸附质浓度和温度)的影响。为了确定潜在的吸附过程机制,对动力学模型进行了评估。利用 Langmuir 和 Freundlich 模型对吸附平衡进行了分析。评估了热力学参数作为过程温度的函数。动力学数据由二级模型更好地表示。发现该过程受研究因素的强烈影响。伯斐粘土以最大吸附容量 1.91mg 金属/g 粘土(20°C;pH5.3)去除镍,热力学数据表明吸附反应是自发的和放热的。Langmuir 模型为吸附等温线提供了最佳拟合。

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