Abstract
The objective of this study was to replace some of the metal ions in the n-type zinc ferrite spinel lattice with Ni2+ ions to evaluate its catalytic behavior during water splitting. XPS and Raman spectroscopy revealed that the substituted Ni2+ ions were preferentially located at the octahedral (Oh) sites in the zinc ferrite spinel lattice, rather than the tetrahedral (Td) sites. When the amount of substituted Ni2+ was >0.6 mol, the crystal structure was converted to an inverse spinel structure. Ni2+ substitution resulted in the formation of oxygen vacancies in the spinel lattice. With Ni2+ substitution, the bandgap state changes from direct to indirect. The TRPL, IMVS, and IMPS analyses revealed the carrier diffusion length, e−/h+ recombination time, and charge transport rate for the Zn1-xNixFe2O4 inverse spinel. The electrons excited from the valence bands (VBs) to the CBs (O 2p → Fe3+ 3d) moved to Ni2+ 3d (Fe3+ 3d → Ni2+ 3d) and, subsequently, the longer carrier diffusion length suppressed e−/h+ recombination. Eventually, an optimum hydrogen production of 19.2 μmol g−1 was achieved using the Zn0.4Ni0.6Fe2.0O4 catalyst for a 10 h-hydrogen evolution reaction in neutral water splitting, without any sacrificial agent under visible light; Zn0.4Ni0.6Fe2.0O4 exhibited a four-fold improvement compared to ZnFe2O4. The material did not significantly deteriorate the catalytic performance, even after six regeneration experiments, and the catalyst material was separated using a magnet after the reaction. Thus, the goal of this study was to develop a simple, eco-friendly, and efficient catalyst via partial cation substitution in the spinel structure.
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