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Probing the Redox Reactivity of a Reduced Nontronite: A Quick XAS Operando Study.
Léo Chevrier1, Sylvain Grangeon2, Anthony Beauvois3
1ISTO, UMR 7327, Univ Orléans, CNRS, BRGM, OSUC, 45071 Orléans, France.
Structural iron in clay minerals drives redox reactions. This study shows both fast and slow reaction rates in chromium reduction, influenced by iron location and redox equilibrium, impacting contaminant fate.
Area of Science:
- Environmental Geochemistry
- Mineralogy
- Environmental Science
Background:
- Fe-bearing clay minerals possess redox-active structural iron crucial for electron transfer reactions with aqueous species.
- Understanding the interplay of kinetic and thermodynamic controls on clay structural iron's redox activity is vital for environmental applications.
- Previous research extensively studied clay redox properties, yet precise mechanisms governing steady-state conditions remain debated.
Purpose of the Study:
- To investigate the reduction kinetics of aqueous Cr(VI) to Cr(III) mediated by structural Fe(II) in ferruginous clay (Nontronite NAu-1).
- To elucidate the roles of kinetic and thermodynamic constraints in establishing redox steady-state conditions.
- To determine the contribution of different iron locations within clay structures to redox reactivity.
Main Methods:
- Utilized quick X-ray absorption spectroscopy (XAS) to monitor the reduction kinetics of Cr(VI) by Fe(II) in Nontronite NAu-1.
- Performed mass and electron balance calculations to assess the contribution of different iron pools.
- Analyzed the Fe(II)/Fe(III) ratio evolution to understand steady-state attainment.
Main Results:
- Observed at least two distinct reaction processes with contrasting fast and slow kinetic rates during Cr(VI) reduction.
- Calculations indicated that edge Fe(II) alone could not explain the observed fast reactivity, suggesting electron transfer from inner clay structures.
- The Fe(II)/Fe(III) ratio rapidly reached steady state, consistent with either Cr(VI) depletion or thermodynamic equilibrium between Fe and Cr redox couples.
Conclusions:
- Clay structural iron exhibits complex redox behavior involving both fast and slow kinetic pathways.
- Electron transfer from the clay mineral's interior significantly contributes to the overall reaction rate.
- Both kinetic limitations and thermodynamic equilibrium govern the redox state of structural iron and influence contaminant transformation.
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