In the exploration
of the optimal material for achieving the photoelectrochemical
dissociation of water into hydrogen, hematite (α-Fe
2
O
3
) emerges as a highly promising candidate for proof-of-concept
demonstrations. Recent studies suggest that the concurrent application
of external electric fields could enhance the photoelectrochemical
(PEC) process. To delve into this, we conducted nonequilibrium
ab initio
molecular dynamics (NE-AIMD) simulations in this
study, focusing on hematite–water interfaces at room temperature
under progressively stronger electric fields. Our findings reveal
intriguing evidence of water molecule adsorption and dissociation,
as evidenced by an analysis of the structural properties of the hydrated
layered surface of the hematite–water interface. Additionally,
we scrutinized intermolecular structures using radial distribution
functions (RDFs) to explore the interaction between the hematite slab
and water. Notably, the presence of a Grotthuss hopping mechanism
became apparent as the electric field strength increased. A comprehensive
discussion based on intramolecular geometry highlighted aspects such
as hydrogen-bond lengths, H-bond angles, average H-bond numbers, and
the observed correlation existing among the hydrogen-bond strength,
bond-dissociation energy, and H-bond lifetime. Furthermore, we assessed
the impact of electric fields on the librational, bending, and stretching
modes of hydrogen atoms in water by calculating the vibrational density
of states (VDOS). This analysis revealed distinct field effects for
the three characteristic band modes, both in the bulk region and at
the hematite–water interface. We also evaluated the charge
density of active elements at the aqueous hematite surface, delving
into field-induced electronic charge-density variations through the
Hirshfeld charge density analysis of atomic elements. Throughout this
work, we drew clear distinctions between parallel and antiparallel
field alignments at the hematite–water interface, aiming to
elucidate crucial differences in local behavior for each surface direction
of the hematite–water interface.