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A Mn-54 Radiotracer Study of Mn Isotope Solid–Liquid Exchange during Reductive Transformation of Vernadite (δ-MnO2) by Aqueous Mn(II)
journal contribution
posted on 2015-04-07, 00:00 authored by Evert J. Elzinga, Adam B. KustkaWe
employed Mn-54 radiotracers to characterize the extent and dynamics
of Mn atom exchange between aqueous Mn(II) and vernadite (δ-Mn(IV)O2) at pH 7.5 under anoxic conditions. Exchange of Mn atoms
between the solid and liquid phase is rapid, reaching dynamic equilibrium
in 2–4 days. We propose that during the initial stages of reaction,
Mn atom exchange occurs through consecutive comproportionation-disproportionation
reactions where interfacial electron transfer from adsorbed Mn(II)
to lattice Mn(IV) generates labile Mn(III) cations that rapidly disproportionate
to reform aqueous Mn(II) and solid-phase Mn(IV). Following nucleation
of Mn(III)OOH phases, additional exchange likely occurs through electron
transfer from aqueous Mn(II) to solid-phase Mn(III). Our results provide
evidence for the fast and extensive production of transient Mn(III)
species at the vernadite surface upon contact of this substrate with
dissolved Mn(II). We further show that HEPES buffer is a reductant
of lattice Mn(IV) in the vernadite structure in our experiments. The
methods and results presented here introduce application of Mn-54
tracers as a facile tool to further investigate the formation kinetics
of labile Mn(III) surface species and their impacts on Mn-oxide structure
and reactivity over a range of environmentally relevant geochemical
conditions.