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首页> 外文期刊>Journal of Colloid and Interface Science >Tungstate sorption mechanisms on boehmite: Systematic uptake studies and X-ray absorption spectroscopy analysis
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Tungstate sorption mechanisms on boehmite: Systematic uptake studies and X-ray absorption spectroscopy analysis

机译:勃姆石上钨酸盐的吸附机理:系统吸收研究和X射线吸收光谱分析

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Mechanisms of tungstate sorption on the mineral boehmite (gamma-AlOOH) were studied using batch uptake experiments and X-ray absorption spectroscopy. Batch uptake experiments over the pH range 4-8 and [W] = 50-2000 mu M show typical oxyanion behavior, and isotherm experiments reveal continued uptake with increasing tungstate concentration without any clear uptake maximum. Desorption experiments showed that sorption is irreversible at pH 4 and partly reversible at pH 8. Tungsten L-1- and L-3-edge XANES spectroscopy indicates that all sorbed tungstates are octahedrally coordinated, even though the dominant solution species at pH 8 is a tetrahedral monotungstate. Tungsten L-3-edge EXAFS analysis shows that sorbed tungstate occurs as polymeric form(s), as indicated by the presence of corner- and edge-sharing of distorted tungstate octahedra. The occurrence of polymeric tungstate on the surface at pH 8 indicates that sorption is accompanied by polymerization and a coordination change from tetrahedral (in solution) to distorted octahedral (on the surface). The strong tendency for tungstate polymerization on boehmite can explain the continued uptake without an apparent maximum in sorption, and the limited desorption behavior. Our results provide the basis for a predictive model of tungstate uptake by boehmite, which can be important for understanding tungstate mobility, toxicity, and bioavailability. (C) 2015 Elsevier Inc. All rights reserved.
机译:利用分批吸收实验和X射线吸收光谱研究了钨酸盐在矿物勃姆石(γ-AlOOH)上的吸附机理。在4-8的pH范围和[W] = 50-2000μM的范围内的分批吸收实验显示出典型的氧阴离子行为,等温线实验表明,随着钨酸盐浓度的增加,持续的吸收没有任何明显的最大吸收。解吸实验表明,在pH 4时吸附是不可逆的,在pH 8时部分吸附是可逆的。钨的L-1-和L-3-edge XANES光谱表明,所有吸附的钨酸盐都是八面体配位的,即使在pH 8时占主导地位的溶液是四面体钨酸钨。钨L-3-边缘EXAFS分析表明,吸附的钨酸盐以聚合物形式出现,这是扭曲的钨酸盐八面体的边角和边角共享所表明的。在pH值为8的表面上出现聚合钨酸,表明吸附伴随着聚合反应,以及从四面体(溶液中)到扭曲的八面体(表面上)的配位变化。勃姆石上钨酸盐聚合的强烈趋势可以解释在没有明显的最大吸附和有限的解吸行为的情况下持续吸收。我们的结果为勃姆石吸收钨酸盐的预测模型提供了基础,这对于理解钨酸盐的迁移率,毒性和生物利用度可能非常重要。 (C)2015 Elsevier Inc.保留所有权利。

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