首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Effect of silicic acid on arsenate and arsenite retention mechanisms on 6-L ferrihydrite: A spectroscopic and batch adsorption approach
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Effect of silicic acid on arsenate and arsenite retention mechanisms on 6-L ferrihydrite: A spectroscopic and batch adsorption approach

机译:硅酸对6-L亚铁水合物中砷酸盐和亚砷酸盐保留机理的影响:分光光度法和分批吸附法

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The competitive adsorption of arsenate and arsenite with silicic acid at the ferrihydrite-water interface was investigated over a wide pH range using batch sorption experiments, attenuated total reflectance Fourier transform infrared (ATR-FTIR) spectroscopy, extended X-ray absorption fine structure (EXAFS) spectroscopy, and density functional theory (DFT) modeling. Batch sorption results indicate that the adsorption of arsenate and arsenite on the 6-L ferrihydrite surface exhibits a strong pH-dependence, and the effect of pH on arsenic sorption differs between arsenate and arsenite. Arsenate adsorption decreases consistently with increasing pH; whereas arsenite adsorption initially increases with pH to a sorption maximum at pH 7-9, where after sorption decreases with further increases in pH. Results indicate that competitive adsorption between silicic acid and arsenate is negligible under the experimental conditions; whereas strong competitive adsorption was observed between silicic acid and arsenite, particularly at low and high pH. In situ, flow-through ATR-FTIR data reveal that in the absence of silicic acid, arsenate forms inner-sphere, binuclear bidentate, complexes at the ferrihydrite surface across the entire pH range. Silicic acid also forms inner-sphere complexes at ferrihydrite surfaces throughout the entire pH range probed by this study (pH 2.8-9.0). The ATR-FTIR data also reveal that silicic acid undergoes polymerization at the ferrihydrite surface under the environmentally-relevant concentrations studied (e.g., 1.0. mM). According to ATR-FTIR data, arsenate complexation mode was not affected by the presence of silicic acid. EXAFS analyses and DFT modeling confirmed that arsenate tetrahedra were bonded to Fe metal centers via binuclear bidentate complexation with average As(V)-Fe bond distance of 3.27. ?. The EXAFS data indicate that arsenite forms both mononuclear bidentate and binuclear bidentate complexes with 6-L ferrihydrite as indicated by two As(III)-Fe bond distances of ~2.92-2.94 and 3.41-3.44. ?, respectively. The As-Fe bond distances in both arsenate and arsenite EXAFS spectra remained unchanged in the presence of Si, suggesting that whereas Si diminishes arsenite adsorption preferentially, it has a negligible effect on As-Fe bonding mechanisms.
机译:使用批处理吸附实验,衰减全反射傅立叶变换红外光谱(ATR-FTIR)光谱,扩展X射线吸收精细结构(EXAFS),研究了在宽pH范围内研究了水合物在水铁矿-水界面上砷酸和砷酸与硅酸的竞争性吸附。光谱和密度泛函理论(DFT)建模。分批吸附结果表明,砷和砷在6-L亚铁水合物表面的吸附表现出很强的pH依赖性,并且pH对砷吸附的影响在砷和砷之间有所不同。砷酸盐的吸附随着pH值的增加而持续降低;而砷的吸附最初随pH的增加而增加,在pH 7-9时达到最大吸附,此后吸附随pH的进一步增加而降低。结果表明,在实验条件下,硅酸和砷酸盐之间的竞争性吸附可以忽略不计。而在硅酸和亚砷酸盐之间观察到强烈的竞争性吸附,特别是在低pH和高pH下。原位流动的ATR-FTIR数据显示,在没有硅酸的情况下,砷酸盐会在整个pH范围内的水铁矿表面形成内球,双核双齿,络合物。硅酸还在整个这项研究探讨的整个pH范围(pH 2.8-9.0)中的水铁矿表面形成内球络合物。 ATR-FTIR数据还表明,在所研究的环境相关浓度(例如1.0mM)下,硅酸在三水铁矿表面发生聚合。根据ATR-FTIR数据,砷酸络合模式不受硅酸的存在影响。 EXAFS分析和DFT建模证实,砷化四面体通过双核双齿络合物与Fe金属中心键合,平均As(V)-Fe键距为3.27。 ? EXAFS数据表明,亚砷酸盐与6升水铁矿形成单核双齿和双核双齿复合物,这两个As(III)-Fe键距分别为〜2.92-2.94和3.41-3.44。 ?, 分别。在存在硅的情况下,砷酸盐和亚砷酸盐EXAFS光谱中的As-Fe键距离均保持不变,这表明尽管Si优先降低了砷的吸附,但对As-Fe键合机理的影响可忽略不计。

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