Spinel ferrites MFe2O4 (M = Co, Cu, Zn) for photocatalysis: theoretical and experimental insights

被引:2
|
作者
Hall, Charlotte A. [1 ,2 ]
Ferrer, Pilar [2 ]
Grinter, David C. [2 ]
Kumar, Santosh [2 ]
da Silva, Ivan [3 ]
Rubio-Zuazo, Juan [4 ,5 ]
Bencok, Peter [2 ]
de Groot, Frank [6 ]
Held, Georg [2 ]
Grau-Crespo, Ricardo [1 ]
机构
[1] Univ Reading, Dept Chem, Reading RG6 6DX, England
[2] Diamond Light Source, Harwell Sci & Innovat Campus, Didcot OX11 0DE, England
[3] Rutherford Appleton Lab, ISIS Neutron & Muon Source, Didcot OX11 0QX, England
[4] European Synchrotron Radiat Facil, BM25 SpLine, CS40220, F-38043 Grenoble 9, France
[5] CSIC, ICMM, Sor Juana Ines de la Cruz 3, Madrid, Spain
[6] Univ Utrecht, Debye Inst Nanomat Sci, NL-3584 CA Utrecht, Netherlands
基金
英国工程与自然科学研究理事会;
关键词
ELECTRONIC-PROPERTIES; NANOPARTICLES; EVOLUTION; EFFICIENT; THERMODYNAMICS; GENERATION; REDUCTION; INVERSION; SURFACES; BEHAVIOR;
D O I
10.1039/d4ta04941a
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Spinel ferrites exhibit significant promise in photocatalysis and other applications due to their compositional diversity and favourable electronic structure, magnetism, and partially tuneable cation distribution. However, their complex properties, for example, the different behaviour of bulk and nanostructured materials, are not well understood. Here, we combine advanced computational and experimental methods with reactivity measurements to explore the inversion degrees, electronic structures, and photocatalytic activities of MFe2O4 spinels (M = Co, Cu, Zn). X-ray diffraction and anomalous X-ray scattering measurements determined bulk inversion degrees of 0.81, 0.91, and 0.26 for CoFe2O4, CuFe2O4, and ZnFe2O4, respectively. Photocatalytic tests showed that only ZnFe2O4 is active in the oxygen evolution reaction (OER), which correlates with its favourable band alignment, as determined through electronic structure simulations. Surface-sensitive X-ray Absorption Spectroscopy (XAS) measurements provided insights into the cation distributions at the surfaces, showing significant deviations from bulk properties, particularly in ZnFe2O4 in which 52% of the near-surface tetrahedral sites are occupied by Fe cations, compared to 26% in the bulk. DFT simulations of ZnFe2O4 illustrated how the surface terminations can alter the thermodynamic preference for cation distribution in comparison with the bulk. Our findings illustrate the complex interplay between surface and bulk properties in spinel ferrites.
引用
收藏
页码:29645 / 29656
页数:12
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