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oxoironIV

Oxoiron(IV) refers to an iron center in the +4 oxidation state bearing an oxo ligand, typically written as FeIV=O. It is a high-valent iron–oxo species that plays a central role in both biological oxidation reactions and synthetic oxidation chemistry.

Structure and properties

FeIV=O species can adopt various coordination geometries depending on surrounding ligands, often described as octahedral or

Formation and occurrence

In biology, oxoiron(IV) intermediates arise in several enzymatic systems. In heme enzymes such as cytochrome P450,

Reactivity

Oxoiron(IV) species are potent oxidants capable of hydrogen-atom abstraction and oxygen-atom transfer reactions, enabling substrates such

square-pyramidal.
The
Fe=O
unit
is
short
and
highly
reactive.
The
electronic
state
is
commonly
S
=
1
or
S
=
2,
with
the
exact
spin
depending
on
ligand
field
and
coordination
environment.
Spectroscopic
methods
such
as
Mössbauer
spectroscopy,
EPR
(sometimes
silent
or
weak,
depending
on
spin),
resonance
Raman
(notably
the
characteristic
Fe=O
stretch
around
the
800–900
cm−1
region)
and
UV–visible
spectroscopy
are
used
to
identify
and
characterize
oxoiron(IV)
complexes.
X-ray
crystallography
can
provide
precise
Fe–O
bond
lengths
and
geometry.
ferryl
species
appear
during
the
catalytic
cycle,
with
Compound
II
often
identified
as
an
FeIV=O
species.
In
non-heme
iron
enzymes,
FeIV=O
intermediates
form
during
oxygen
activation
by
2-oxoglutarate–dependent
dioxygenases.
In
synthetic
chemistry,
oxoiron(IV)
complexes
are
generated
by
oxidizing
FeII
precursors
with
oxidants
such
as
iodosylbenzene,
peracids,
or
hydrogen
peroxide,
often
in
the
presence
of
supporting
ligands
that
stabilize
the
high-valent
state.
as
alkanes,
alkenes,
and
sulfides
to
be
oxidized.
They
serve
as
key
models
for
understanding
high-valent
iron
chemistry
and
are
studied
for
applications
in
selective
oxidation
catalysis
and
mechanistic
enzymology.