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通过吸附在中国第四纪黄土上从水溶液中去除Cu(II):动力学和平衡研究

Removal of Cu(II) from aqueous solution by adsorption on Chinese Quaternary loess: kinetics and equilibrium studies.

作者信息

Tang Xiao W, Li Zhen Z, Chen Yun M, Wang Yan

机构信息

Key Laboratory of Soft Soils and Geoenvironmental Engineering, Zhejiang University, Hangzhou, PR China.

出版信息

J Environ Sci Health A Tox Hazard Subst Environ Eng. 2008 Jun;43(7):779-91. doi: 10.1080/10934520801960144.

DOI:10.1080/10934520801960144
PMID:18444081
Abstract

This paper dealt with the characteristics of Cu(II) adsorption on Chinese Quaternary loess. The Cu(II) adsorption isotherm and kinetics fit the Langmuir model and pseudo-second order kinetics well, respectively, with a predicted adsorption capacity of 109 mg g(-1). The adsorption is ion exchange adsorption due to D-R model. Factors that are positively correlated with the adsorption capacity of loess include equilibrating time, pH, temperature, and solid-solution ratio. The adsorption of Cu(II) on loess involves 2-3 sequential diffusing steps into the micropores, and an endothermic and spontaneous process with predicted enthalpy, entropy, and Gibb's free energy changes of 7.64 kJ mol(-1), 81.21 J mol(-1)K(-1) and -14.94-17.37 kJ mol(-1), respectively. Moreover, the applicability of loess on industrial wastewater treatment was investigated and satisfactorily proved. Finally, FT-IR spectra shows the precipitation of copper carbonate and the complexation of Cu(II) with clay minerals at pH > 5.0 and pH > 2.67, respectively.

摘要

本文研究了Cu(II)在中国第四纪黄土上的吸附特性。Cu(II)吸附等温线和动力学分别很好地拟合了Langmuir模型和准二级动力学,预测吸附容量为109 mg g(-1)。根据D-R模型,吸附为离子交换吸附。与黄土吸附容量呈正相关的因素包括平衡时间、pH值、温度和固液比。Cu(II)在黄土上的吸附涉及2 - 3个连续的向微孔扩散步骤,是一个吸热且自发的过程,预测的焓变、熵变和吉布斯自由能变化分别为7.64 kJ mol(-1)、81.21 J mol(-1)K(-1)和 -14.94 - 17.37 kJ mol(-1)。此外,研究了黄土在工业废水处理中的适用性并得到了满意的证明。最后,傅里叶变换红外光谱表明,分别在pH > 5.0和pH > 2.67时,有碳酸铜沉淀以及Cu(II)与粘土矿物发生络合作用。

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