Journal
ADVANCED FUNCTIONAL MATERIALS
Volume 32, Issue 25, Pages -Publisher
WILEY-V C H VERLAG GMBH
DOI: 10.1002/adfm.202201127
Keywords
seawater splitting; lattice chloride; structural buffer; oxygen evolution reaction; long-term stability
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Funding
- National Natural Science Foundations of China [21908054, 22005098]
- Central Government Funds for Guiding Local Science and Technology Development [2021Szvup040]
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Seawater electrolysis is an attractive technique for mass production of green hydrogen. However, the presence of chloride ions in seawater can lead to deactivation of the oxygen evolution reaction (OER) catalysts. By utilizing a structural buffer engineering strategy, Co-2(OH)(3)Cl demonstrates long-term stability and a high OER selectivity in seawater electrolysis.
Seawater electrolysis is an attractive technique for massive green hydrogen production owing to the dominant advantages of seawater resources, namely low-cost and limitlessness. However, the oxygen evolution reaction (OER) catalysts will be easily deactivated for severe seawater Cl- permeation and corrosion. Herein, a structural buffer engineering strategy is reported to endow the Co-2(OH)(3)Cl with long-term operation stability and a high OER selectivity of approximate to 99.6% in seawater splitting. The lattice Cl- of Co-2(OH)(3)Cl can act as the structural buffer, whose continuous leaching during OER can leave vacancies for seawater Cl- invasion, so as to avoid catalyst deactivation. Accordingly, Co-2(OH)(3)Cl can maintain 99.9% of its initial current density after 60 000 s operation, while that of Co(OH)(2) decays by 52.7% in 7 000 s. Meanwhile, the lattice Cl- of Co-2(OH)(3)Cl can optimize the binding energy of reaction intermediates on the neighboring O-Co-O site. Thus, Co-2(OH)(3)Cl exhibits a current density of 330.5 mA cm(-2) at the potential of 1.63 V versus RHE, 45.9 times higher than that of Co(OH)(2). The structural buffer strategy may be applied to incorporate other metal oxides with suitable anions, and effectively boost their OER activity and stability in alkaline seawater.
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