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RESEARCH ARTICLE

Reduction of Arsenates by Humic Materials

Noel E. Palmer A , John H. Freudenthal A and Ray von Wandruszka A B
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A Department of Chemistry, University of Idaho, Moscow, ID 83844-2343, USA.

B Corresponding author. Email: rvw@uidaho.edu

Environmental Chemistry 3(2) 131-136 https://doi.org/10.1071/EN05081
Submitted: 28 September 2005  Accepted: 1 December 2005   Published: 5 May 2006

Environmental Context. Reduction of arsenic(v) to arsenic(iii) in the environment is of interest because of the greater toxicity and mobility of the latter. It is important to know to what extent humic materials (which are ubiquitous in soils) can act as abiotic reducing agents, and what factors influence their actions.

Abstract. Inorganic arsenates were found to be reduced to arsenite by homogeneous aqueous solutions of several humic and fulvic acids. Because of the concentration dependence of the redox potentials of humics, reduction was shown to be less likely in more concentrated solutions. This was especially true in higher pH ranges, and varied with the type of material used. Ion chromatography, validated by inductively coupled plasma mass spectrometry, was used to speciate arsenic after exposure to aqueous humates and fulvates. Reduction of As(v) proceeded in the 20–60% range, depending on the humic or fulvic acid used. The fraction of arsenate that was reduced initially increased with humic concentration, but leveled off as the reduction potential decreased at higher concentrations. Re-oxidation of As(iii) in humic solutions could be achieved by extended bubbling with air. Reduction capacities of two humates tested, as measured by I2 titration, were found to be significantly different.

Keywords. : arsenate — arsenite — fulvic acid — humic substances — reduction


Acknowledgements

The authors thank the Inland North-west Research Alliance for financial support given to one of them (N.E.P.).


References


[1]   Nriagu J. O. (Ed.), Arsenic in the Environment Part I: Cycling and Characterization 1994 (John Wiley & Sons: New York).

[2]   W. Cullen, K. Reimer, Chem. Rev. 1989, 89,  713.
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