Abstract

The effect of a small thiol-containing organic molecule on the adsorption of Mo to pyrite was investigated through the use of equilibration experiments with molybdate (MoO42−), tetrathiomolybdate (MoS42−), and 2-mercaptopropionic acid (2MPA). MoO42−, MoS42−, and 2MPA individually adsorb to pyrite through the formation of specific interactions with the mineral surface. In select combination experiments, 2MPA effectively out-competes MoO42− for pyrite surface sites, which is indicative of the relatively weaker MoO42−-pyrite interactions. Results suggest that the presence of 2MPA on the pyrite surface would inhibit MoO42− access to catalytic mineral surface sites for the transformation of MoO42− to MoS42−. In contrast, thiols are not expected to be an obstacle to Mo uptake once the “switch point”, or the critical H2S concentration required for the formation of MoS42−, has been surpassed. This is due to the stronger adsorption of MoS42− to the pyrite surface. EXAFS results support weak specific interactions with little change to the MoO42− environment upon adsorption to pyrite. In contrast, larger changes to the Mo–S internuclear distances during MoS42− adsorption to pyrite support a more substantial structural change upon adsorption. MoS42− is able to bind to both the pyrite surface and a thiol-containing organic molecule to form a ternary structure on the pyrite surface, and may provide for a molecular-level connection between Mo and thiol-containing organic molecules. Mo(VI) is reduced to Mo(IV) during MoS42− adsorption to pyrite as a result of ligand-induced reduction, thereby confirming that the thiolated form of Mo is necessary for Mo reduction.

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