Dioxygen activation routes in Mars-van Krevelen redox cycles catalyzed by metal oxides
[Display omitted] •O2 activation involves inner and outer sphere routes during oxidative dehydrogenation.•Inner sphere routes form bound peroxo species that insert O-atoms into alkanols/alkenes.•Outer sphere routes form H2O2(g), O-atom shuttles that oxidize non-vicinal reduced centers.•These routes...
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Published in: | Journal of catalysis Vol. 364; no. C; pp. 228 - 247 |
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Main Authors: | , , |
Format: | Journal Article |
Language: | English |
Published: |
United States
Elsevier Inc
01-08-2018
Elsevier |
Subjects: | |
Online Access: | Get full text |
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Summary: | [Display omitted]
•O2 activation involves inner and outer sphere routes during oxidative dehydrogenation.•Inner sphere routes form bound peroxo species that insert O-atoms into alkanols/alkenes.•Outer sphere routes form H2O2(g), O-atom shuttles that oxidize non-vicinal reduced centers.•These routes allow re-oxidation of two non-vicinal 2e− reduced centers by a 4e− oxidant (O2)•Kinetic, scavenging, and theoretical methods can assess the contributions of each route.
Catalytic redox cycles involve dioxygen activation via peroxo (OO∗) or H2O2 species, denoted as inner-sphere and outer-sphere routes respectively, for metal-oxo catalysts solvated by liquids. On solid oxides, O2 activation is typically more facile than the reduction part of redox cycles, making kinetic inquiries difficult at steady-state. These steps are examined here for oxidative alkanol dehydrogenation (ODH) by scavenging OO∗ species with C3H6 to form epoxides and by energies and barriers from density functional theory. Alkanols react with O-atoms (O∗) in oxides to form vicinal OH pairs that eliminate H2O to form OO∗ at O-vacancies formed or react with O2 to give H2O2. OO∗ reacts with alkanols to re-form O∗ via steps favored over OO∗ migrations, otherwise required to oxidize non-vicinal vacancies. C3H6 epoxidizes by reaction with OO∗ with rates that increase with C3H6 pressure, but reach constant values as all OO∗ species react with C3H6 at high C3H6/alkanol ratios. Asymptotic epoxidation/ODH rate ratios are smaller than unity, because outer-sphere routes that shuttle O-atoms via H2O2(g) are favored over endoergic vacancy formation required for inner-sphere routes. The relative contributions of these two routes are influenced by H2O, because vacancies, required to form OO∗, react with H2O to form OH pairs and H2O2. OO∗-mediated routes and epoxidation become favored at low coverages of reduced centers, prevalent for less reactive alkanols and lower alkanol/O2 ratios, because H2O2 then reacts preferentially with O∗ (forming OO∗), instead of vacancies (forming O∗/H2O). Such kinetic shunts between two routes compensate for lower barriers required to form H2O2 than OO∗. These re-oxidation routes prefer molecular donor (H2O2) or acceptor (alkanol) to perform stepwise two-electron oxidations by dioxygen, instead of kinetically demanding O-atom migrations. The quantitative descriptions, derived from theory and experiment on Mo-based polyoxometalate clusters with known structures, bring together the dioxygen chemistry in liquid-phase oxidations, including electro-catalysis and monooxygenase enzymes, and oxide surfaces into a common framework, while suggesting a practical process for epoxidation by kinetically coupling with ODH reaction. |
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Bibliography: | AC05-76RL0-1830; 48772 USDOE Office of Science (SC), Basic Energy Sciences (BES) |
ISSN: | 0021-9517 1090-2694 |
DOI: | 10.1016/j.jcat.2018.05.016 |