吸附
氟化物
浸出(土壤学)
沉积(地质)
图层(电子)
金属
材料科学
溶解
无机化学
化学工程
化学
冶金
环境科学
地质学
纳米技术
物理化学
土壤科学
工程类
古生物学
沉积物
土壤水分
作者
Pengfei Shen,Xiaolin Zhang,Hui Xu,Bingcai Pan
标识
DOI:10.1021/acs.est.4c11768
摘要
Surface complexation has long been recognized as the basic mode involved in fluoride adsorption onto metal oxides. However, such general recognition is challenged by the unusual pH dependence observed in fluoride adsorption. Here, we selected hydrated zirconium oxide (HZO) as a representative metal oxide to revisit the fluoride adsorption mechanism. Multiple in situ microscopic analyses and thermodynamic simulations suggest that, unlike the adsorption of other anions that proceed exclusively via substituting protonated terminal hydroxyl (η-OH2+) groups of metal oxides, fluoride can displace both η-OH2+ and protonated bridging hydroxyl (μ-OH+) groups of HZO (i.e., Substitution). This distinctive displacement drives the leaching of Zr from HZO, generating aqueous polyfluorozirconium complexes (i.e., Leaching) which subsequently deposit onto HZO via outer-sphere complexation (i.e., Deposition). The adsorbed polyfluorozirconium gradually converts into a fluorozirconate (Na5Zr2F13) coating, resulting in a surface layer reconstruction of up to 100 nm in depth. The atypical pH dependency of fluoride adsorption can be explained by the processes of Substitution, Leaching, and Deposition (i.e., SLD processes). More attractively, the SLD-driven surface layer reconstruction is reversible in nature, ensuring the constant defluoridation capability of HZO during cyclic adsorption-desorption assays. This study advances our understanding of fluoride adsorption at water-metal oxide interfaces.
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