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Local coordination geometry within cobalt spinel oxides mediates photoinduced polaron formation
Erica P Craddock1, Jacob L Shelton1, Michael T Ruggiero1
1Department of Chemistry, University of Rochester Rochester NY 14627 USA kknowles@ur.rochester.edu.
None:
Understanding the photophysics of transition metal oxides is crucial for these materials to realize their considerable potential in applications such as photocatalysis and optoelectronics. Recent studies suggest that formation of localized excited states consisting of polarons (quasi-particles comprising a charge carrier strongly coupled to a proximal lattice distortion) plays a crucial role in the photophysics of these materials. Cobalt-containing spinel oxides (Co3O4 and ZnCo2O4) offer a unique opportunity to investigate the influence of local geometry, and cation inversion on photoinduced polaron formation. Here, we use Hubbard-corrected density functional theory (DFT + U) paired with resonance Raman and temperature-dependent optical spectroscopies to demonstrate that low-energy transitions observed in Co3O4 are associated with d-d transitions involving cobalt ions occupying tetrahedral sites within the spinel lattice. These low-energy optical transitions exhibit strong coupling to phonon modes associated with tetrahedral sites. Replacing most tetrahedral cobalt ions with zinc produces the slightly inverted ternary spinel material, ZnCo2O4, in which we observe a phonon-coupled optical transition that occurs at the same energy as observed in Co3O4. We propose that these phonon-coupled optical transitions enable direct access to a polaronic state upon photoexcitation; however, the intensity of this optical transition depends on temperature in Co3O4, whereas no significant temperature dependence is observed in ZnCo2O4. We therefore hypothesize that in Co3O4 the mechanism of polaron formation is coupling of the optical transition to dynamic, thermally-gated lattice distortions, whereas, in ZnCo2O4, the transition couples to static lattice defects that arise from the presence of a small population of tetrahedrally-coordinated cobalt ions.
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