| Literature DB >> 32309955 |
Martina Fracchia1, Paolo Ghigna1,2, Tommaso Pozzi1, Umberto Anselmi Tamburini1,2, Valentina Colombo2,3, Luca Braglia4, Piero Torelli4.
Abstract
The mechanisms of CO oxidation on the Mg0.2Co0.2Ni0.2Cu0.2Zn0.2O high-entropy oxide were studied by means of operando soft X-ray absorption spectroscopy. We found that Cu is the active metal and that Cu(II) can be rapidly reduced to Cu(I) by CO when the temperature is higher than 130 °C. Co and Ni do not have any role in this respect. The Cu(II) oxidation state can be easily but slowly recovered by treatment of the sample with O2 at ca. 250 °C. However, it should be noted that CuO is readily and irreversibly reduced to Cu(I) when it is treated with CO at T > 100 °C. Thus, the main conclusion of this work is that the high configurational entropy of Mg0.2Co0.2Ni0.2Cu0.2Zn0.2O stabilizes the rock-salt structure and permits the oxidation/reduction of Cu to be reversible, thus permitting the catalytic cycle to take place.Entities:
Year: 2020 PMID: 32309955 PMCID: PMC8007101 DOI: 10.1021/acs.jpclett.0c00602
Source DB: PubMed Journal: J Phys Chem Lett ISSN: 1948-7185 Impact factor: 6.475
Figure 1(A) Cu L2,3-edge XAS spectra of the Mg0.2Co0.2Ni0.2Cu0.2Zn0.2O HEO material under different conditions. The inset shows on an enlarged scale the Cu(I) peak at ca. 934.8 eV. (B) Cu L2,3-edge XAS spectra of CuO under different conditions and Cu2O at room temperature. In this panel, non-normalized spectra are shown.
Figure 2(A) Co and (B) Ni L2,3-edge XAS spectra of the Mg0.2Co0.2Ni0.2Cu0.2Zn0.2O HEO material under different conditions.
Figure 3(A) Cu L2,3-edge XAS spectra of the Mg0.2Co0.2Ni0.2Cu0.2Zn0.2O HEO material for different time periods in CO at 235 °C (red to blue lines; numbers 0 → 60 are the dwell times under these conditions expressed in minutes) and then in O2 at the same temperature (black line). (B) Comparison of the PXRD patterns of the raw HEO material (red line) and the same material after all of the thermal treatments described in this work (black line). The patterns are indexed according to the rock-salt structure (Fm3̅m, a = 4.2366(5) Å).