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Reduction Kinetics of Polymeric (Soluble) Manganese (IV) Oxide (MnO2) by Ferrous Iron (Fe2+)

In numerous freshwater and marine environments, ferrous iron (Fe²⁺) can react with manganese oxides in a redox reaction. However, there are few quantitative data describing reaction rates. A “soluble” (colloidal and nanoparticulate) phase manganese dioxide (MnO₂) was used to obtain kinetic data on M...

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Bibliographic Details
Published in:Aquatic geochemistry 2015-07, Vol.21 (2-4), p.143-158
Main Authors: Siebecker, Matthew, Madison, Andrew S, Luther, George W., III
Format: Article
Language:English
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Summary:In numerous freshwater and marine environments, ferrous iron (Fe²⁺) can react with manganese oxides in a redox reaction. However, there are few quantitative data describing reaction rates. A “soluble” (colloidal and nanoparticulate) phase manganese dioxide (MnO₂) was used to obtain kinetic data on MnO₂ reduction by Fe²⁺ with a stopped flow UV–Vis method. Stopped flow experiments were carried out in unbuffered solutions between pH 4.9 and 5.36 and also at pH 7. The reaction was determined to be first order with respect to MnO₂ and Fe²⁺ and second order overall. It is important to subtract absorbance of Fe(III) products from the UV–Vis data and to acquire data from the first milliseconds of the reaction. After subtracting Fe(III) product absorbance, the average second-order rate constant was determined to be 4338 ± 249 M⁻¹ s⁻¹ at 25 °C and pH 5. Reactions of 5 μM MnO₂ with 50 and 100 μM Fe²⁺ were more than 50 % complete in 1.77 and 0.7 s, respectively. The reaction is an inner sphere electron transfer process as an outer sphere process is symmetry-forbidden. Studies show that Mn(III) intermediates are produced during the reaction. The fast kinetics makes this reaction significant to consider when modeling manganese oxide and reduced iron in environmental redox systems.
ISSN:1380-6165
1573-1421
DOI:10.1007/s10498-015-9257-z