Defect
engineering in nickel ferrite has been performed to enhance
the power output of the hydroelectric cell (HEC). Oxygen vacancies
can be tuned in the ferrite using different valence element substitutions
to enhance water dissociation by hydroelectric cells. In this work,
Li+, Mg2+, and Al3+ substituted at
the nickel site in nickel ferrite (NiFe2O4)
are synthesized and studied for hydroelectric cell devices. Introducing
these Li+, Mg2+, and Al3+ substituents
(of a different atomic radius and valence charge state) in nickel
ferrite leads to the generation of oxygen vacancy differently, which
is discussed thoroughly in this work. In comparison to Mg and Al,
lithium substitution lowers the overall cationic charge in nickel
ferrite, leading to formation of a high number of oxygen vacancies
for overall ionic charge compensation. Lithium-substituted nickel
ferrite (NLFO) has a high number of defects (oxygen vacancies, etc.)
compared to Mg-substituted (NMFO) and Al-substituted (NAFO) nickel
ferrite, confirmed by X-ray photoelectron spectroscopy (XPS) and photoluminescence
(PL) spectroscopy. The highest peak area of oxygen vacancies in the
O 1s core-level spectra has been obtained for the case of NLFO among
NLFO, NMFO, and NAFO. These vacancy sites provide a large number of
adsorption sites for water molecule adsorption and dissociation. A
high lattice strain (9.83 × 10–4) is induced
in NLFO calculated by the Williamson–Hall plot. The porous
nature of all samples has been confirmed from FESEM and BET analysis.
The charge transfer processes in dry and wet HECs have been analyzed
by fitting an equivalent RC circuit in the Nyquist spectra. The lithium-substituted
nickel ferrite HEC with rich oxygen vacancies generates a high short-circuit
current of ∼58.7 mA, which is ∼2 times higher than that
of NMFO HEC and ∼3 times higher than that of NAFO HEC.