TY - JOUR
T1 - Volcano-shaped correlation dictated superior activity for ultralow Al-doped iron oxide toward high-temperature water-gas shift reaction
AU - Qian, Binbin
AU - Yan, Xue
AU - Yang, Sasha
AU - Zhang, Jianghao
AU - Liu, Cheng
AU - Liu, Zongtang
AU - Fei, Zhenghao
AU - Dai, Baiqian
AU - Liu, Jefferson Zhe
AU - Wang, Yong
AU - Zhang, Lian
N1 - Funding Information:
The authors gratefully acknowledge financial support from the National Natural Science Foundation of China (52300175), the Natural Science Foundation of Jiangsu Province of China (BK20220701), the Australian Research Council Linkage Project (LP220100365), the Opening Project of Jiangxi Province Key Laboratory of Polymer Micro/Nano Manufacturing and Devices (PMND202210), the Yancheng Key Research and Development Program (Social Development, YCBE202244), and the start-up grant (204060037) from Yancheng Teachers University. Australian synchrotron is acknowledged for the XAS characterization under the projects PA20278, M19329, and M16167. All the DFT calculations were undertaken with the assistance of resources and services from the National Computational Infrastructure (NCI), which is supported by the Australian Government. The authors also acknowledge the use of facilities within the analysis testing center in Yancheng Teachers University.
Publisher Copyright:
© 2024 American Chemical Society.
PY - 2024/5/17
Y1 - 2024/5/17
N2 - Earth-abundant iron oxide is an important catalyst for the production of hydrogen via a broad range of catalytic reactions, including the high-temperature water-gas shift reaction (HT-WGSR). For iron oxide catalysts, the aluminum (Al) dopant, with a relatively large concentration of ∼5 wt %, is commonly considered as a textural promoter to stabilize the active phase magnetite. However, the role of Al and its underlying mechanisms are yet to be fully understood. Here, we report the discovery of a volcano-shaped correlation between the Al doping amount and catalyst activity and, potentially, an extremely low yet optimum content of ∼0.85 wt % for Al. Such a low-content Al is initially highly dispersed within iron oxide, exerting a negligible effect on the catalyst structure. However, it can undertake in situ transformation into a Fe3O4@Fe(Fe1-x,Alx)2O4 core-shell structure during H2 reduction. The resultant catalyst outperforms pure magnetite (Al-free) and those with larger Al contents, enabling the achievement of the thermodynamic limit of 76-80% CO conversion at 425-450 °C and a low apparent activation energy of ∼41 kJ/mol compared to its high-Al counterparts. Advanced in situ and ex situ characterizations, along with density functional theory (DFT) calculations, confirmed a preferential diffusion of Al on the catalyst surface/shell, occupying the octahedral Fe sites of magnetite which are in turn highly activated in moderating the adsorption of CO and simultaneously alleviating the hydrogen-binding energy for a spontaneous H2O dissociation. In contrast, for the high-Al content such as 1.72 wt %, phase segregation for the formation of discrete alumina occurs on the surface, exerting strong adsorption of CO but weak adsorption of H2O at temperatures >400 °C. This in turn poisons and deactivates the catalyst quickly. By precisely controlling the amount of a dopant such as Al on the atomic level, the activity of the iron oxide-based catalysts can be unlocked in achieving maximal performance.
AB - Earth-abundant iron oxide is an important catalyst for the production of hydrogen via a broad range of catalytic reactions, including the high-temperature water-gas shift reaction (HT-WGSR). For iron oxide catalysts, the aluminum (Al) dopant, with a relatively large concentration of ∼5 wt %, is commonly considered as a textural promoter to stabilize the active phase magnetite. However, the role of Al and its underlying mechanisms are yet to be fully understood. Here, we report the discovery of a volcano-shaped correlation between the Al doping amount and catalyst activity and, potentially, an extremely low yet optimum content of ∼0.85 wt % for Al. Such a low-content Al is initially highly dispersed within iron oxide, exerting a negligible effect on the catalyst structure. However, it can undertake in situ transformation into a Fe3O4@Fe(Fe1-x,Alx)2O4 core-shell structure during H2 reduction. The resultant catalyst outperforms pure magnetite (Al-free) and those with larger Al contents, enabling the achievement of the thermodynamic limit of 76-80% CO conversion at 425-450 °C and a low apparent activation energy of ∼41 kJ/mol compared to its high-Al counterparts. Advanced in situ and ex situ characterizations, along with density functional theory (DFT) calculations, confirmed a preferential diffusion of Al on the catalyst surface/shell, occupying the octahedral Fe sites of magnetite which are in turn highly activated in moderating the adsorption of CO and simultaneously alleviating the hydrogen-binding energy for a spontaneous H2O dissociation. In contrast, for the high-Al content such as 1.72 wt %, phase segregation for the formation of discrete alumina occurs on the surface, exerting strong adsorption of CO but weak adsorption of H2O at temperatures >400 °C. This in turn poisons and deactivates the catalyst quickly. By precisely controlling the amount of a dopant such as Al on the atomic level, the activity of the iron oxide-based catalysts can be unlocked in achieving maximal performance.
KW - Al promoter
KW - core−shell structure
KW - HO dissociation
KW - volcano-shaped correlation
KW - water−gas shift reaction
UR - http://www.scopus.com/inward/record.url?scp=85192151711&partnerID=8YFLogxK
U2 - 10.1021/acscatal.4c01403
DO - 10.1021/acscatal.4c01403
M3 - Article
AN - SCOPUS:85192151711
SN - 2155-5435
VL - 14
SP - 7402
EP - 7415
JO - ACS Catalysis
JF - ACS Catalysis
IS - 10
ER -