4.5 Article

Surface oxygen dynamics and H2 oxidation on cobalt spinel surface probed by 18O/16O isotopic exchange and accounted for by DFT molecular modeling: facile interfacial oxygen atoms flipping through transient peroxy intermediate

Journal

RESEARCH ON CHEMICAL INTERMEDIATES
Volume 43, Issue 5, Pages 2865-2880

Publisher

SPRINGER
DOI: 10.1007/s11164-016-2798-y

Keywords

Reactive oxygen species; Co3O4; Nanocrystal; Isotopic studies; DFT calculations

Funding

  1. Polish National Science Center [DEC-2011/03/B/ST5/01564]

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Surface dynamics of reactive oxygen species (ROS) and hydrogen oxidation on cobalt spinel nanocatalyst, faceted predominantly with (100), were investigated by means of pulsed O-16(2)/O-18(2) isotopic exchange and thermoprogrammed surface reaction investigations, corroborated by periodic spin-unrestricted DFT-PW91+U modelling of the principal surface reaction molecular events. Three temperature windows [T < 350 A degrees C (i), 350 A degrees C < T < 700 A degrees C (ii), and T > 700 A degrees C (iii)] where identified and associated with diatomic oxygen species of superoxo (Co-O-(O-2)(-)-Co-O, peroxo (Co-T-(O-2)(2-)-Co-O) (i), and monoatomic metaloxo (Co-T-O, Co-O-O) nature (ii), and with oxygen vacancies V-O (iii). A new oxygen isotopic exchange pathway was proposed that involves peroxy transient intermediates produced during ROS oxygen surface diffusion. Flipping of the supra- (RSO) and intra-facial (lattice) oxygen moieties within the [O-18(sup)-O-16(int)](2-) peroxy unit requires 0.39 eV only, opening an easy pathway for rapid isotopic exchange without explicit formation of energetically more costly oxygen vacancies. The latter may occur effectively at T > 700 A degrees C. The catalytic activity of ROS species was probed by H-2 oxidation reaction. The diatomic ROS reactivity (below 160 A degrees C) is characterized by E (a) = 16 kcal/mol, and for monoatomic species (between 160 A degrees C and 300 A degrees C) it falls to E (a) = 9.2 kcal/mol. It was shown that suprafacial dehydroxylation of ROS generated water is energetically less costly (E (a) = 1.15 eV) than intrafacial dehydroxylation (E (a) = 1.71 eV) entailing removal of water associated with the lattice oxygen. Thus, the former may operate even at relatively low temperatures (below 300-350 A degrees C). The appearance of significant amount of H (2) (16) O in the reaction products is related to easy isotopic O-18/O-16 scrambling via transient peroxo intermediates, and is not diagnostic of direct involvement of the Mars van Krevelen mechanism.

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