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Paper No. 5
Presentation Time: 9:15 AM

A FIRST PRINCIPLES STUDY OF THE OXIDATION ENERGETICS AND KINETICS OF REALGAR


RENOCK, Devon, Dept. Earth Sciences, Dartmouth College, Hanover, NH 03755 and BECKER, Udo, Department of Earth and Environmental Sciences, Univ of Michigan, 1100 North University Avenue, C.C.Little Building, Ann Arbor, MI 48109-1063, drenock@umich.edu

Quantum-mechanical calculations allow resolving and quantifying important aspects of reaction mechanisms such as spin transitions and oxygen dissociation that can be the major rate-limiting steps in redox processes on sulfide and oxide surfaces. The interaction of As4S4 clusters with oxygen and co-adsorbed ions provides a model system for understanding the molecular-scale processes that underpin empirically-derived rate expressions, and provides clues to the oxidation mechanisms of other sulfides and oxides. Two activated processes are shown to dominate the kinetics of oxidation by molecular oxygen: i) a paramagnetic (3O2) to diamagnetic (1O2) spin transition and ii) oxygen dissociation on the surface, in that order. The activation energies for the spin transition and O2 dissociation step were determined to be 106 kJ/mol and 87 kJ/mol, respectively, for dry oxidation. 3O2 transfers its spin to As4S4 and forms a low-spin, peroxo intermediate on the surface before dissociating. The adsorption of a hydroxide ion on the surface proximate to the 3O2 adsorption site changes the adsorption mechanism by lowering the activation energy barriers for both the spin transition (29 kJ/mol) and the O2 dissociation step (69 kJ/mol). Thus, while spin transition is rate limiting for oxidation with O2 alone, dissociation becomes the rate-limiting step for oxidation with co-adsorption of OH-. Thus, assuming that an As4S4 cluster with an adsorbed hydroxyl group is a reasonable approximation of the surface of As4S4 at high pH, the theoretically calculated oxidation rate (~10-10 mol·m-2·s-1) is of the same order as empirically-derived rates from experiments at pH = 8. In addition, the co-adsorption of other anions found in alkaline waters (carbonate, bicarbonate, sulfate, and sulfite) are shown to energetically promote the oxidation of As4S4.

Activation-energy barriers due to spin transitions are rarely discussed in the literature as key factors for controlling oxidation rates of mineral surfaces, even though the magnitude of these barriers is enough to alter the kinetics significantly. Lowering the activation energy by co-adsorbed anions suggests the possibility of pH- or p(co-adsorbate)-dependent activation energies that can be used to refine oxidation rate laws for semiconducting minerals, such as sulfides and oxides.

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