Nanocrystalline
MnFe2O4 has shown promise
as a catalyst for the oxygen reduction reaction (ORR) in alkaline
solutions, but the material has been sparingly studied as highly ordered
thin-film catalysts. To examine the role of surface termination and
Mn and Fe site occupancy, epitaxial MnFe2O4 and
Fe3O4 spinel oxide films were grown on (001)-
and (111)-oriented Nb:SrTiO3 perovskite substrates using
molecular beam epitaxy and studied as electrocatalysts for the oxygen
reduction reaction (ORR). High-resolution X-ray diffraction (HRXRD)
and X-ray photoelectron spectroscopy (XPS) show the synthesis of pure
phase materials, while scanning transmission electron microscopy (STEM)
and reflection high-energy electron diffraction (RHEED) analysis demonstrate
island-like growth of (111) surface-terminated pyramids on both (001)-
and (111)-oriented substrates, consistent with the literature and
attributed to the lattice mismatch between the spinel films and the
perovskite substrate. Cyclic voltammograms under a N2 atmosphere
revealed distinct redox features for Mn and Fe surface termination
based on comparison of MnFe2O4 and Fe3O4. Under an O2 atmosphere, electrocatalytic
reduction of oxygen was observed at both Mn and Fe redox features;
however, a diffusion-limited current was only achieved at potentials
consistent with Fe reduction. This result contrasts with that of nanocrystalline
MnFe2O4 reported in the literature where the
diffusion-limited current is achieved with Mn-based catalysis. This
difference is attributed to a low density of Mn surface termination,
as determined by the integration of current from CVs collected under
N2, in addition to low conductivity through the MnFe2O4 film due to the degree of inversion. Such low
densities are attributed to the synthetic method and island-like growth
pattern and highlight challenges in studying ORR catalysis with single-crystal
spinel materials.