Water splitting for large-scale hydrogen production is
a method
for storing sustainable but intermittent energy sources. Oxygen evolution
reaction (OER) through the water oxidation reaction provides low-cost
electrons for the formation of hydrogen. OER is a complicated, sluggish
reaction and a bottleneck for water splitting. Herein, first, a tetranuclear
Ni complex with di(2-pyridyl) ketone (compound 1) has
been synthesized. In the next step, OERs in the presence of compound 1 at pHs 3.0 and 7.0 have been investigated. The study attempts
to answer the following questions for the metal complex during OER:
(i) what is the true catalyst for OER in the presence of a Ni complex
under neutral or acidic conditions? (ii) Why is low OER observed in
the presence of a Ni complex under neutral or acidic conditions? The
experiments show that the Ni-oxo cluster of γ-NiO(OH) is formed
during OER in the presence of compound 1 at pHs 3.0 and
7.0. In addition, compound 1 is reduced on the counter
electrode surface at pH 3.0 during OER. The reduced complex is characterized
by Raman spectroscopy and electron paramagnetic resonance as a Ni(I)
complex, which is unstable and decomposed after a few hours. Thus,
a metal complex must be stable on the working electrode surface and
the counter electrode surface for OER in a single-cell setup.