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RESEARCH ARTICLE

Geochemistry of Cu, Zn and Fe in the Tambo River, Australia I. Oxidation of Fe(II)-rich water entering the river

Barry T. Hart A B and Tina Hines A
+ Author Affiliations
- Author Affiliations

A Water Studies Centre and School of Chemistry, Monash University, Victoria 3800, Australia.

B Corresponding author. Email: barry.hart@waterscience.com.au

Marine and Freshwater Research 59(1) 72-79 https://doi.org/10.1071/MF07056
Submitted: 15 March 2007  Accepted: 7 September 2007   Published: 25 January 2008

Abstract

The behaviour of Fe, Cu and Zn was studied during the laboratory oxidation of an acidic (pH 5.8) sample of naturally contaminated water from the Tambo River (Victoria, Australia). Changes in the concentrations of the dissolved, colloidal and particulate fractions of these metals were followed over 288 h. The initial concentrations of dissolved Cu (18.5 mg L–1) and Zn (22.6 mg L–1) were ~15-fold greater than that of the dissolved Fe (1.13 mg L–1). Dissolved Fe was completely removed from solution in 60 h, with removal following the well established first order oxidation kinetics for Fe(II). A relatively small amount of the dissolved Cu (18%) and dissolved Zn (14%) was removed from the solution, although the removal mechanisms appear to be different. A ‘co-precipitation-surface precipitation’ mechanism is proposed to explain the behaviour of the Cu and Zn, with Cu(II), Zn(II) and Fe(III) co-precipitating to form colloidal Fe(OH)3-Cu(OH)2-Zn(OH)2 particles following the initial oxidation of Fe(II) to Fe(III).

Additional keywords: contamination, co-precipitation-surface precipitation, heavy metals, hydrous iron oxide, kinetics.


Acknowledgements

Macquarie Resources Ltd funded the present study and also provided a scholarship for TH. We are grateful to Jovo Basic, Paul Dowd, Craig Jeffs and Hugh Stein of Macquarie Resources Ltd for their support and assistance, and to Steven Hines for his assistance particularly with the fieldwork. BTH thanks the University of Western Australia for awarding him a Senior Gledden Fellowship and to the Centre for Water Research at UWA for providing him facilities during which time this paper was completed.


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