Effects of Fulvic and Humic Acids on Arsenate Adsorption to Goethite: Experiments and Modeling

Data for interactions between arsenate (AsO4 3−) and fulvic acids (FA) or humic acids (HA) at the surface of goethite are presented (pH 3−7, ionic strength 2 mM and 10 mM). Adsorption of FA and HA leads to desorption of arsenate and a correspondingly strong increase of arsenic concentration in solut...

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Bibliographic Details
Published in:Environmental science & technology 2009-10, Vol.43 (19), p.7198-7204
Main Authors: Weng, Liping, Van Riemsdijk, Willem H, Hiemstra, Tjisse
Format: Article
Language:English
Subjects:
Adsorption
Applied sciences
Arsenates - chemistry
Benzopyrans - chemistry
binding
charge-distribution
Chemistry Techniques, Analytical
competition
Environmental Monitoring
Exact sciences and technology
Humic Substances
ion adsorption
Iron Compounds - chemistry
iron-oxides
Minerals
Models, Chemical
natural organic-matter
Pollution
speciation
surface structural approach
water interface
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Summary:Data for interactions between arsenate (AsO4 3−) and fulvic acids (FA) or humic acids (HA) at the surface of goethite are presented (pH 3−7, ionic strength 2 mM and 10 mM). Adsorption of FA and HA leads to desorption of arsenate and a correspondingly strong increase of arsenic concentration in solution. Adsorption of both FA and HA is mutually decreased by the competition with arsenate. The competition between FA and arsenate is much stronger than that between HA and arsenate. Using an advanced model, the LCD model (Ligand and Charge Distribution), arsenate adsorption to goethite in the presence of both adsorbed FA and HA can be predicted reasonably well. The stronger effects of FA on arsenate adsorption are caused, according to the model, by its spatial location which is closer to the oxide surface, and as a consequence, the electrostatic interactions between adsorbed FA particles and arsenate ions are much stronger than those for HA particles. The results show that site and electrostatic competition are the major mechanisms explaining the effects of natural organic matter on the arsenic speciation, whereas other possible mechanisms, such as a chemical reduction of arsenate to arsenite and formation of ternary organic arsenic complexes, are of minor significance.
ISSN:0013-936X
1520-5851
DOI:10.1021/es9000196