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Surface-directed corner-sharing MnO 6 octahedra within numerous manganese oxide compounds containing Mn 3+ or Mn 4+ oxidation states show strikingly different catalytic activities for water oxidation, paradoxically poorest for Mn 4+ oxides, regardless of oxidation assay (photochemical and electrochemical). This is demonstrated herein by comparing crystalline oxides consisting of Mn 3+ (manganite, γ-MnOOH; bixbyite, Mn 2 O 3 ), Mn 4+ (pyrolusite, β-MnO 2 ) and multiple monophasic mixed-valence manganese oxides. Like all Mn 4+ oxides, pure β-MnO 2 has no detectable catalytic activity, while γ-MnOOH (tetragonally distorted Mn 3+ O 6, D 4 h symmetry) is significantly more active and Mn 2 O 3 (trigonal antiprismatic Mn 3+ O 6, D 3 d symmetry) is the most active. γ-MnOOH deactivates during catalytic turnover simultaneous with the disappearance of crystallographically defined corner-sharing Mn 3+ O 6 and the appearance of Mn 4+ . In a comparison of 2D-layered crystalline birnessites (δ-MnO 2 ), the monovalent Mn 4+ form is catalytically inert, while the hexagonal polymorph, containing few out-of-layer corner-sharing Mn 3+ O 6, has ∼10-fold higher catalytic activity than the triclinic polymorph, containing in-plane edge-sharing Mn 3+ O 6 . These electronic and structural correlations point toward the more flexible (corner-shared) Mn 3+ O 6 sites, over more rigid (edge-shared) sites as substantially more active catalytic centers. Electrochemical measurements show and ligand field theory predicts that, among corner-shared Mn 3+ O 6 sites, those possessing D 3 d ligand field symmetry have stronger covalent Mn–O bonding to the six equivalent oxygen ligands, which we ascribe as responsible for more efficient and faster electrolytic water oxidation. In contrast, D 4 h Mn 3+ O 6 sites have weaker Mn–O bonding to the two axial oxygen ligands, have separated electrochemical oxidation waves for Mn and O, and are catalytically less efficient and exhibit slower catalytic turnover. By controlling the ligand field geometry and strength to oxygen ligands, we have identified the key variables for tuning water oxidation activity by manganese oxides. We apply these findings to propose a mechanism for water oxidation by the CaMn 4 O 5 catalytic site of natural photosynthesis.
Smith et al. (Tue,) studied this question.
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