蒙脱石
吸附
水溶液中的金属离子
纳米孔
吸附
金属
分子动力学
扩散
镉
离子
锌
化学
化学物理
化学工程
材料科学
无机化学
纳米技术
物理化学
计算化学
有机化学
热力学
物理
工程类
作者
Libin Liu,Chi Zhang,Wenjun Jiang,Xiong Li,Yunchao Dai,Hanzhong Jia
标识
DOI:10.1016/j.jhazmat.2021.125976
摘要
The molecular-scale adsorption mechanism of heavy metal ions in the interlayer and nanopore regions of montmorillonite (MMT) were investigated by molecular dynamics simulations. Three typical heavy metals (zinc, cadmium, and lead) were selected as the model ions, and two types of MMT (Arizona and Wyoming) were considered. The results showed that Cd2+ and Pb2+ can form both inner- and outer-sphere complexes on Wyoming MMT, while Zn2+ only formed outer-sphere complex due to the stronger hydration interaction of Zn2+ than Cd2+ and Pb2+. For Arizona MMT, all of the three ions only formed outer-sphere complexes on its interlayer and external basal surface in which the cations remained a fully hydrated state. The calculated diffusion coefficients of three cations in interlayer and nanopore indicated that their diffusion abilities were significantly impaired, implying that MMT adsorbents have a strong ability to fix and retard heavy metal ions. The derived results and mechanisms are instrumental to a profound understanding of the transport and retention of heavy metal elements in subsurface environments, and provide guidance for the management of heavy metal pollution.
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