Adsorption of As (V) on iron oxide nanoparticle films studied by in situ ATR-FTIR spectroscopy

被引:88
作者
Carabante, Ivan [1 ]
Grahn, Mattias [1 ]
Holmgren, Allan [1 ]
Kumpiene, Jurate [2 ]
Hedlund, Jonas [1 ]
机构
[1] Lulea Univ Technol, Div Chem Engn, SE-97187 Lulea, Sweden
[2] Lulea Univ Technol, Div Waste Sci & Technol, SE-97187 Lulea, Sweden
基金
瑞典研究理事会;
关键词
Ferrihydrite; Iron oxide film; In situ; ATR-FTIR; Arsenic (V); Adsorption; CHROMATE RETENTION MECHANISMS; HEPTYL XANTHATE; ION ADSORPTION; ARSENATE; GOETHITE; SURFACE; CARBONATE; KINETICS; MINE; STABILIZATION;
D O I
10.1016/j.colsurfa.2009.05.032
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070305 [高分子化学与物理];
摘要
Stabilization of arsenic contaminated soils by iron oxides has been proposed as a remediation technique to prevent leaching of arsenate into the environment. Fundamental studies are needed to establish under which conditions the complexes formed are stable. In the present work, a powerful technique, viz. ATR-FTIR spectroscopy, is adapted to the studies of adsorption of arsenate species on iron oxides. This technique facilitates acquisition of both quantitative and qualitative in situ adsorption data. In the present work, about 800 nm thick films of 6-lineferrihydrite were deposited on ZnSe ATR crystals. Arsenate adsorption on the ferrihydrite film was studied at pD values ranging from 4 to 12 and at an arsenate concentration of 0.03 mM in D2O solution. The amount of adsorbed arsenate decreased with increasing pD as a result of the more negatively charged iron oxide surface at higher pD values. The adsorption and desorption kinetics were also studied. Arsenate showed a higher adsorption rate within the first 70 min and a much lower adsorption rate from 70 to 300 min. The low adsorption rate at longer reaction times was partly due to a low desorption rate of already adsorbed carbonate species adsorbed at the surface. The desorption of carbonate species was evidenced by the appearance of negative absorption bands. The desorption of adsorbed arsenate complexes was examined by flushing with D2O at pD 4 and 8.5 and it was found that the complexes were very stable at pD 4 suggesting formation of mostly inner-sphere complexes whereas a fraction of the complexes at pD 8.5 were less stable than at pD 4, possibly due to the formation of outer-sphere complexes. In summary, the ATR technique was shown to provide in situ information about the adsorption rate, desorption rate and the speciation of the complexes formed within a single experiment, which is very difficult to obtain using other techniques. (C) 2009 Elsevier B.V. All rights reserved.
引用
收藏
页码:106 / 113
页数:8
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