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六价铬物种在粘土矿物表面 - 水界面的分布。

Distribution of hexavalent Cr species across the clay mineral surface-water interface.

作者信息

Fritzen Mauricia B, Souza Aloisio J, Silva Tiago A G, Souza Luciana, Nome Rene A, Fiedler Haidi D, Nome Faruk

机构信息

Departamento de Química, Universidade Federal de Santa Catarina, Florianópolis, SC 88040-900, Brazil.

出版信息

J Colloid Interface Sci. 2006 Apr 15;296(2):465-71. doi: 10.1016/j.jcis.2005.09.037. Epub 2005 Dec 15.

Abstract

The adsorption isotherms of Cr(VI) on kaolinite, montmorillonite, and alumina were adequately treated with Langmuir model showing behavior characteristic of single-layer adsorption. The efficiency of the adsorbents in removing Cr(VI) from water follows the order alumina > kaolinite > montmorillonite > silica. Speciation studies indicate that hydrogen chromate ions were the major adsorbed species and simultaneous adsorption of dichromate ion occurred at concentrations greater than approximately 10(-3) mol L(-1). It is most probable that the mechanism of adsorption of the hydrogen chromate ion at the surface of alumina is predominantly electrostatic adsorption, with outer sphere complex formation.

摘要

高岭土、蒙脱石和氧化铝对Cr(VI)的吸附等温线用朗缪尔模型进行了充分处理,显示出单层吸附的行为特征。吸附剂从水中去除Cr(VI)的效率顺序为:氧化铝>高岭土>蒙脱石>二氧化硅。形态研究表明,铬酸氢根离子是主要的吸附物种,当浓度大于约10(-3) mol L(-1)时,重铬酸根离子会同时被吸附。最有可能的是,铬酸氢根离子在氧化铝表面的吸附机制主要是静电吸附,并形成外层配合物。

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