Catalytic role of bridging oxygens in TiO2 liquid phase photocatalytic reactions: Analysis of H216O photooxidation on labeled Ti18O2

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  • J.F. Montoya
  • D.W. Bahnemann
  • P. Salvador
  • J. Peral

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Original languageEnglish
Pages (from-to)902-910
Number of pages9
JournalCatalysis Science and Technology
Volume7
Issue number4
Publication statusPublished - 21 Feb 2017

Abstract

Experiments of photocatalytic oxidation of H 2 16O with a suspended oxygen-isotope labelled Ti 18O 2 photocatalyst are presented here for the first time. The photo-induced evolution of 18O 16O demonstrates that bridging surface oxygens (> 18O br 2-) behave as real catalytic species of the global water splitting photocatalytic reaction (2H 2O + 4h + → O 2(g)↑ + 4H +). The experimental results are interpreted according to a previously developed water redox photooxidation (WRP) mechanism (Salvador, P. Prog. Surf. Sci. 2011, 86, 41-58), opening a new mechanistic pathway that involves the participation of terminal >O br 2- bridging oxygens as real photocatalytic species. In the primary step, one-fold coordinated - 18O br - radicals are generated from the direct photooxidation of > 18O br 2- oxygens with valence band holes (> 18O br 2- + h + → - 18O br -). In the second step, a couple of adjacent - 18O br - radicals chemically react, giving rise to peroxo species (2 18O br -18O 2 2-), which are further photooxidized with photogenerated valence band holes, initially leading to 18O 2(g) evolution according to the global photoreaction 18O 2 2- + 4h + → 2V[> 18O br 2-] + 18O 2(g)↑. Terminal oxygen vacancies (V[> 18O br 2-]) become further healed via dissociative adsorption of H 2 16O water molecules (2V[> 18O br 2-] + 2H 2 16O → 2(> 16O br 2-) + 2H +), in such a way that > 18O br 2- bridging ions are progressively substituted by > 16O br 2- and the initially evolved 18O 2(g) is further replaced by 16,18O 2(g) and finally by 16O 2(g).

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Catalytic role of bridging oxygens in TiO2 liquid phase photocatalytic reactions: Analysis of H216O photooxidation on labeled Ti18O2. / Montoya, J.F.; Bahnemann, D.W.; Salvador, P. et al.
In: Catalysis Science and Technology, Vol. 7, No. 4, 21.02.2017, p. 902-910.

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title = "Catalytic role of bridging oxygens in TiO2 liquid phase photocatalytic reactions: Analysis of H216O photooxidation on labeled Ti18O2",
abstract = "Experiments of photocatalytic oxidation of H 2 16O with a suspended oxygen-isotope labelled Ti 18O 2 photocatalyst are presented here for the first time. The photo-induced evolution of 18O 16O demonstrates that bridging surface oxygens (> 18O br 2-) behave as real catalytic species of the global water splitting photocatalytic reaction (2H 2O + 4h + → O 2(g)↑ + 4H +). The experimental results are interpreted according to a previously developed water redox photooxidation (WRP) mechanism (Salvador, P. Prog. Surf. Sci. 2011, 86, 41-58), opening a new mechanistic pathway that involves the participation of terminal >O br 2- bridging oxygens as real photocatalytic species. In the primary step, one-fold coordinated - 18O br - radicals are generated from the direct photooxidation of > 18O br 2- oxygens with valence band holes (> 18O br 2- + h + → - 18O br -). In the second step, a couple of adjacent - 18O br - radicals chemically react, giving rise to peroxo species (2 18O br - → 18O 2 2-), which are further photooxidized with photogenerated valence band holes, initially leading to 18O 2(g) evolution according to the global photoreaction 18O 2 2- + 4h + → 2V[> 18O br 2-] + 18O 2(g)↑. Terminal oxygen vacancies (V[> 18O br 2-]) become further healed via dissociative adsorption of H 2 16O water molecules (2V[> 18O br 2-] + 2H 2 16O → 2(> 16O br 2-) + 2H +), in such a way that > 18O br 2- bridging ions are progressively substituted by > 16O br 2- and the initially evolved 18O 2(g) is further replaced by 16,18O 2(g) and finally by 16O 2(g). ",
author = "J.F. Montoya and D.W. Bahnemann and P. Salvador and J. Peral",
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T1 - Catalytic role of bridging oxygens in TiO2 liquid phase photocatalytic reactions

T2 - Analysis of H216O photooxidation on labeled Ti18O2

AU - Montoya, J.F.

AU - Bahnemann, D.W.

AU - Salvador, P.

AU - Peral, J.

N1 - Publisher Copyright: © 2017 The Royal Society of Chemistry. Copyright: Copyright 2017 Elsevier B.V., All rights reserved.

PY - 2017/2/21

Y1 - 2017/2/21

N2 - Experiments of photocatalytic oxidation of H 2 16O with a suspended oxygen-isotope labelled Ti 18O 2 photocatalyst are presented here for the first time. The photo-induced evolution of 18O 16O demonstrates that bridging surface oxygens (> 18O br 2-) behave as real catalytic species of the global water splitting photocatalytic reaction (2H 2O + 4h + → O 2(g)↑ + 4H +). The experimental results are interpreted according to a previously developed water redox photooxidation (WRP) mechanism (Salvador, P. Prog. Surf. Sci. 2011, 86, 41-58), opening a new mechanistic pathway that involves the participation of terminal >O br 2- bridging oxygens as real photocatalytic species. In the primary step, one-fold coordinated - 18O br - radicals are generated from the direct photooxidation of > 18O br 2- oxygens with valence band holes (> 18O br 2- + h + → - 18O br -). In the second step, a couple of adjacent - 18O br - radicals chemically react, giving rise to peroxo species (2 18O br - → 18O 2 2-), which are further photooxidized with photogenerated valence band holes, initially leading to 18O 2(g) evolution according to the global photoreaction 18O 2 2- + 4h + → 2V[> 18O br 2-] + 18O 2(g)↑. Terminal oxygen vacancies (V[> 18O br 2-]) become further healed via dissociative adsorption of H 2 16O water molecules (2V[> 18O br 2-] + 2H 2 16O → 2(> 16O br 2-) + 2H +), in such a way that > 18O br 2- bridging ions are progressively substituted by > 16O br 2- and the initially evolved 18O 2(g) is further replaced by 16,18O 2(g) and finally by 16O 2(g).

AB - Experiments of photocatalytic oxidation of H 2 16O with a suspended oxygen-isotope labelled Ti 18O 2 photocatalyst are presented here for the first time. The photo-induced evolution of 18O 16O demonstrates that bridging surface oxygens (> 18O br 2-) behave as real catalytic species of the global water splitting photocatalytic reaction (2H 2O + 4h + → O 2(g)↑ + 4H +). The experimental results are interpreted according to a previously developed water redox photooxidation (WRP) mechanism (Salvador, P. Prog. Surf. Sci. 2011, 86, 41-58), opening a new mechanistic pathway that involves the participation of terminal >O br 2- bridging oxygens as real photocatalytic species. In the primary step, one-fold coordinated - 18O br - radicals are generated from the direct photooxidation of > 18O br 2- oxygens with valence band holes (> 18O br 2- + h + → - 18O br -). In the second step, a couple of adjacent - 18O br - radicals chemically react, giving rise to peroxo species (2 18O br - → 18O 2 2-), which are further photooxidized with photogenerated valence band holes, initially leading to 18O 2(g) evolution according to the global photoreaction 18O 2 2- + 4h + → 2V[> 18O br 2-] + 18O 2(g)↑. Terminal oxygen vacancies (V[> 18O br 2-]) become further healed via dissociative adsorption of H 2 16O water molecules (2V[> 18O br 2-] + 2H 2 16O → 2(> 16O br 2-) + 2H +), in such a way that > 18O br 2- bridging ions are progressively substituted by > 16O br 2- and the initially evolved 18O 2(g) is further replaced by 16,18O 2(g) and finally by 16O 2(g).

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