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Triggering the Dual-Metal-Site Lattice Oxygen Mechanism with In Situ-Generated Mn3+ Sites for Enhanced Acidic Oxygen Evolution

  • Jianyun Liu
  • , Tanyuan Wang*
  • , Mingzi Sun
  • , Mengyi Liao
  • , Shiyu Wang
  • , Shuxia Liu
  • , Hao Shi
  • , Yang Liu
  • , Yue Shen
  • , Ruiguo Cao
  • , Yunhui Huang
  • , Bolong Huang*
  • , Qing Li*
  • *Corresponding author for this work

Research output: Journal Publications and ReviewsRGC 21 - Publication in refereed journalpeer-review

Abstract

The development of high-performance non-Ir/Ru catalysts for the oxygen evolution reaction (OER) in acid is critical for the applications of proton exchange membrane water electrolyzers (PEMWEs). Here, we report a new kind of heterostructure catalyst by loading 5.8% Ag nanoparticles on MnO nanorods (Ag/MnO) for acidic OER. The as-prepared Ag/MnO requires only an overpotential of 196 mV for the OER at a current density of 10 mA cm-2 in 0.5 M H2SO4 and operates in a PEMWE for over 300 h at a current density of 200 mA cm-2, representing one of the best non-Ir/Ru OER catalysts. Operando X-ray absorption spectroscopy confirms that the introduction of trace Ag can promote the generation of highly active Mn3+-O sites with oxygen vacancies at a low voltage, leading to a dual-metal-site lattice oxygen-mediated pathway with faster kinetics than the adsorbate evolution mechanism. Theoretical calculations indicate that the trace Ag promotes the overlap between the d orbitals of Mn and the s, p orbitals of O, thereby activating the lattice oxygen and reducing the OER energy barrier. The dissolution of Mn is also suppressed by Ag due to the increased energy for vacancy formation of Mn, where the stability number reaches a high value of 3058, supporting improved structural stability. © 2024 American Chemical Society.
Original languageEnglish
Pages (from-to)33276-33287
JournalJournal of the American Chemical Society
Volume146
Issue number48
Online published21 Nov 2024
DOIs
Publication statusPublished - 4 Dec 2024
Externally publishedYes

Funding

This work was financially supported by the National Natural Science Foundation of China (22122202, 22072051, 22379048, and 22479056), the National Key Research and Development Program of China (2021YFA1600800 and 2021YFA1501101), the Fundamental Research Funds for the Central Universities (5003110132), Research Grant Council of Hong Kong (15304023), National Natural Science Foundation of China/Research Grant Council of Hong Kong Joint Research Scheme (N_PolyU502/21), National Natural Science Foundation of China/Research Grants Council of Hong Kong Collaborative Research Scheme (CRS_PolyU504/22), Shenzhen Fundamental Research Scheme-General Program (JCYJ20220531090807017), and Natural Science Foundation of Guangdong Province (2023A1515012219). The authors thank the Analytical and Testing Center of Huazhong University of Science and Technology (HUST) for carrying out the XPS, XRF, and TEM measurements. The authors thank BL11B beamline in Shanghai Synchrotron Radiation Facility (SSRF) for providing the beam time. B.H. also thanks the support from Research Centre for Carbon-Strategic Catalysis (RC-CSC), Research Institute for Smart Energy (RISE), and Research Institute for Intelligent Wearable Systems (RI-IWEAR) of the Hong Kong Polytechnic University.

RGC Funding Information

  • RGC-funded

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