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Oxygen evolution from water is one of the key reactions for solar fuel production. Here, two nanostructured K‐containing δ‐MnO 2 are synthesized: K‐δ‐MnO 2 nanosheets and K‐δ‐MnO 2 nanoparticles, both of which exhibit high catalytic activity in visible‐light‐driven water oxidation. The role of alkaline cations in oxygen evolution is first explored by replacing the K + ions in the δ‐MnO 2 structure with H + ions through proton ion exchange. H‐δ‐MnO 2 catalysts with a similar morphology and crystal structure exhibit activities per surface site approximately one order of magnitude lower than that of K‐δ‐MnO 2 , although both nanostructured H‐δ‐MnO 2 catalysts have much larger Brunauer–Emmett–Teller (BET) surface areas. Such a low turnover frequency (TOF) per surface Mn atom might be due to the fact that the Ru 2+ (bpy) 3 sensitizer is too large to access the additional surface area created during proton exchange. Also, a prepared Na‐containing δ‐MnO 2 material with an identical crystal structure exhibits a TOF similar to that of the K‐containing δ‐MnO 2 , suggesting that the alkaline cations are not directly involved in catalytic water oxidation, but instead stabilize the layered structure of the δ‐MnO 2 .
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Boppana et al. (2012) studied this question.
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