Herein,
we investigate the oxygen-evolution reaction (OER) and
electrochemistry of a Pd foil in the presence of iron under alkaline
conditions (pH ≈ 13). As a source of iron, K2FeO4 is employed, which is soluble under alkaline conditions in
contrast to many other Fe salts. Immediately after reacting with the
Pd foil, [FeO4]2– causes a significant
increase in OER and changes in the electrochemistry of Pd. In the
absence of this Fe source and under OER, Pd(IV) is stable, and hole
accumulation occurs, while in the presence of Fe this accumulation
of stored charges can be used for OER. A Density Functional Theory
(DFT) based thermodynamic model suggests an oxygen bridge vacancy
as an active site on the surface of PdO2 and an OER overpotential
of 0.42 V. A substitution of Pd with Fe at this active site reduces
the calculated OER overpotential to 0.35 V. The 70 mV decrease in
overpotential is in good agreement with the experimentally measured
decrease of 60 mV in the onset potential. In the presence of small
amounts of Fe salt, our results point toward the Fe doping of PdO2 rather than extra framework FeO
x
(Fe(OH)3, FeO(OH), and KFeO2) species on top
of PdO2 as the active OER sites.