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Dynamically Stable Active Sites from Surface Evolution of Perovskite Materials during the Oxygen Evolution Reaction
Pietro P Lopes1, Dong Young Chung1, Xue Rui2
1Materials Science Division, Argonne National Laboratory, Lemont, Illinois 60439, United States.
Perovskite oxides show oxygen evolution reaction (OER) activity due to a surface cobalt hydr(oxy)oxide layer. This layer, interacting with iron impurities, creates stable active sites, enhancing catalyst performance and longevity.
Area of Science:
- Materials Science
- Electrochemistry
- Catalysis
Background:
- Perovskite oxides are crucial oxygen evolution reaction (OER) catalysts in alkaline environments.
- Identifying the precise active sites in these catalysts remains a significant challenge.
Purpose of the Study:
- To elucidate the origin of OER activity and active site dynamics in a La1-xSrxCoO3 (LSCO) perovskite model.
- To investigate the role of surface evolution and electrolyte interactions in catalyst performance.
Main Methods:
- Surface characterization of LSCO perovskite under OER conditions.
- Electrochemical analysis to determine activity and stability.
- In-situ studies to observe dynamic active site formation.
Main Results:
- OER activity originates from a surface cobalt hydr(oxy)oxide (CoOH) layer on LSCO.
- Trace iron species in the electrolyte interact with CoOH to form dynamically stable active sites.
- The CoOH/LSCO system exhibits a 10-fold increase in stability and a 3-fold higher activity-stability factor compared to nanoscale CoOH clusters.
Conclusions:
- Surface evolution, including A-site dissolution and O-vacancy creation, is key to forming the active CoOH layer.
- The interaction between the CoOH layer and trace Fe species is critical for stable and active OER catalysis.
- New design principles for robust perovskite oxide OER catalysts can be derived from these findings.
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