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    Adsorption of Cd by the Different Soil Solid–Phase Components Kaolinite, Mica, and Goethite

    Source: Journal of Environmental Engineering:;2023:;Volume ( 149 ):;issue: 011::page 04023072-1
    Author:
    Junming Gong
    ,
    Shunhong Huang
    ,
    Liang Chen
    ,
    Mengfei Li
    ,
    Xianzheng Xu
    ,
    Mengya Xu
    ,
    Qiang Chen
    ,
    Xiaoxue Yu
    DOI: 10.1061/JOEEDU.EEENG-7393
    Publisher: ASCE
    Abstract: Pollution caused by the heavy metal cadmium (Cd) in smelting site soil has become an environmental problem that cannot be ignored. The process of Cd ion adsorption, migration, and diffusion in soil is influenced by various factors, including soil solid–phase composition and soil environment conditions. In order to investigate the adsorption behavior of Cd in smelting site soil, this study collected uncontaminated soil samples from the vicinity of a smelter, with kaolinite, mica, and goethite identified as abundant components of the soil solid phase. We conducted batch adsorption experiments, zeta-potential analysis, scanning electron microscopy (SEM), X-ray diffraction (XRD), and X-ray photoelectron spectroscopy (XPS) to investigate the mechanism of adsorption of Cd ions by kaolinite, mica, and goethite. Our results showed that the pH of the solution significantly influenced the adsorption of Cd ions by these minerals, with increased adsorption observed as the pH increased. Furthermore, the adsorption of Cd ions on kaolinite, mica, and goethite exhibited the best fit with the Freundlich model. SEM and XRD analyses indicated that the crystal structures of the minerals remained unchanged after Cd ion adsorption, suggesting that the Cd ions were primarily bound to the mineral surfaces. XPS measurements of the binding energy changes in the O1s and Cd3d orbitals before and after adsorption were compared with standard binding energy spectra. This comparison confirmed that heavy metal Cd primarily existed on mineral surfaces in the form of outer-sphere and inner-sphere complexes. This study examined the impact of pH on the adsorption of Cd by three types of mineral; fit the data using the isotherm adsorption model equation; and analyzed the mechanisms of binding Cd on different mineral surfaces through characterization techniques. The study’s findings should contribute to a better understanding of Cd adsorption mechanisms and provide valuable insights into the behavior of cadmium in soil at smelting sites.
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      Adsorption of Cd by the Different Soil Solid–Phase Components Kaolinite, Mica, and Goethite

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4294025
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    • Journal of Environmental Engineering

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    contributor authorJunming Gong
    contributor authorShunhong Huang
    contributor authorLiang Chen
    contributor authorMengfei Li
    contributor authorXianzheng Xu
    contributor authorMengya Xu
    contributor authorQiang Chen
    contributor authorXiaoxue Yu
    date accessioned2023-11-28T00:02:43Z
    date available2023-11-28T00:02:43Z
    date issued8/30/2023 12:00:00 AM
    date issued2023-08-30
    identifier otherJOEEDU.EEENG-7393.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4294025
    description abstractPollution caused by the heavy metal cadmium (Cd) in smelting site soil has become an environmental problem that cannot be ignored. The process of Cd ion adsorption, migration, and diffusion in soil is influenced by various factors, including soil solid–phase composition and soil environment conditions. In order to investigate the adsorption behavior of Cd in smelting site soil, this study collected uncontaminated soil samples from the vicinity of a smelter, with kaolinite, mica, and goethite identified as abundant components of the soil solid phase. We conducted batch adsorption experiments, zeta-potential analysis, scanning electron microscopy (SEM), X-ray diffraction (XRD), and X-ray photoelectron spectroscopy (XPS) to investigate the mechanism of adsorption of Cd ions by kaolinite, mica, and goethite. Our results showed that the pH of the solution significantly influenced the adsorption of Cd ions by these minerals, with increased adsorption observed as the pH increased. Furthermore, the adsorption of Cd ions on kaolinite, mica, and goethite exhibited the best fit with the Freundlich model. SEM and XRD analyses indicated that the crystal structures of the minerals remained unchanged after Cd ion adsorption, suggesting that the Cd ions were primarily bound to the mineral surfaces. XPS measurements of the binding energy changes in the O1s and Cd3d orbitals before and after adsorption were compared with standard binding energy spectra. This comparison confirmed that heavy metal Cd primarily existed on mineral surfaces in the form of outer-sphere and inner-sphere complexes. This study examined the impact of pH on the adsorption of Cd by three types of mineral; fit the data using the isotherm adsorption model equation; and analyzed the mechanisms of binding Cd on different mineral surfaces through characterization techniques. The study’s findings should contribute to a better understanding of Cd adsorption mechanisms and provide valuable insights into the behavior of cadmium in soil at smelting sites.
    publisherASCE
    titleAdsorption of Cd by the Different Soil Solid–Phase Components Kaolinite, Mica, and Goethite
    typeJournal Article
    journal volume149
    journal issue11
    journal titleJournal of Environmental Engineering
    identifier doi10.1061/JOEEDU.EEENG-7393
    journal fristpage04023072-1
    journal lastpage04023072-14
    page14
    treeJournal of Environmental Engineering:;2023:;Volume ( 149 ):;issue: 011
    contenttypeFulltext
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