吸附
化学
离子强度
金属
镉
吸收(声学)
傅里叶变换红外光谱
壤土
有机质
光谱学
红外光谱学
无机化学
朗缪尔
水溶液中的金属离子
土壤水分
化学工程
材料科学
物理化学
有机化学
水溶液
地质学
复合材料
土壤科学
工程类
物理
量子力学
作者
Xueyan Guo,Shuzhen Zhang,Xiao‐Quan Shan,Lei Luo,Zhiguo Pei,Yong‐Guan Zhu,Tao Liu,Yaning Xie,Andrew G. Gault
摘要
Abstract Evidence exists for significant metal enrichment in particulate organic matter (POM) compared to other soil constituents, but the relevant mechanisms are poorly understood. In the present study, adsorption of the heavy metals Pb, Cu, and Cd on a loamy soil and on POM separated from this soil was investigated. The adsorption kinetic data can be well described with a pseudo–second order model, whereas the equilibrium data are well fitted by a Langmuir model. Adsorption isotherms and kinetics data, in addition to the influence of pH on metal adsorption, showed that POM had a much higher adsorption capacity for Pb, Cu, and Cd compared to the whole soil. Ionic strength effects on metal adsorption, Fourier transform infrared spectroscopy, x‐ray absorption spectroscopy x‐ray absorption spectroscopy including x‐ray absorption near‐edge structure and extended x‐ray absorption fine‐structure spectroscopy were employed to elucidate the adsorption mechanisms. The results suggested that Pb and Cu adsorption on POM was mainly through inner‐sphere complexes with carboxyl and hydroxyl groups. Cadmium was possibly adsorbed via outer‐sphere complexation, indicated by the influence of ionic strength on Cd adsorption.
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