The activation of oxygen by transition metal oxides is of fundamental
importance in organic synthesis, catalysis and biochemistry.
Efficient catalysts are found in nature for the hydroxylation and oxidation
of organic molecules. Examples are cytochrome P450,
methane monooxygenase (MMO), and the antitumor drug bleomycin (BLC), all
of which have low-valent iron ions as the active centers that can be turned into
highly reactive high-valent iron-oxo, iron-peroxo or iron-hydroperoxo
complexes.
Also Fenton's reagent, a mixture of iron(II) ions and hydrogen peroxide, is
widely applied to oxidize organic substrates. Although H.J.H. Fenton himself
used the unchelated Fe/H
O
mixture in acidic aqueous solution
when he first recorded the oxidative potential of this mixture in
1876[128,155], many modifications have since then been applied in order
to alter the reactivity, to enhance the solubility in other solvents, to increase
the pH range, and to avoid precipitation of the metal catalyst.
This has led to a great variety of ligated iron(II) complexes in combination with
H
O
(or HOCl), or even with different transition metals, such as Mn(II)
or Fe(III) which are all often referred to as Fenton's reagent. To distinguish
between the iron(II) and iron(III) combinations, we will however follow the convention
of using Fenton-like reagent for the Fe
/H
O
mixture and
restrict the use of Fenton's reagent to denote the Fe
/H
O
mixture.
The Fenton-like reagent is also capable of oxidizing organic substrates, but it is
somewhat less reactive than Fenton's reagent. As iron(III) can be produced
in applications of Fenton's reagent, Fenton chemistry and Fenton-like chemistry
often occur simultaneously. Interestingly, Fenton and Fenton-like chemistry
are generally believed to proceed via similar mechanisms as oxidation reactions
with the aforementioned complex and bulky enzymes.
Until recently, Fenton chemistry was still far from being fully
understood. Numerous reaction mechanisms have been proposed based on
different active intermediates such as OH. and OOH. radicals and the
earlier mentioned high-valent iron species. Haber and Weiss' OH. radical
mechanism[156] is probably the most popular candidate for the Fenton reaction:
For the Fenton-like reagents it is believed that initially no O-O bond breaking
takes place, but instead an iron(III)hydroperoxo intermediate is formed as the
first step via hydrolysis:
In the present work, we will investigate the
active species for the Fenton-like chemistry, and we will focus on the
differences between iron(II) and iron(III) in activating hydrogen peroxide.
To simulate the generation, evolution and termination of reactive intermediates
such as hydroxyl radicals we need an accurate description of the aqueous
environment. The method of choice is ab initio (DFT)
Molecular Dynamics method (AIMD), using the Car-Parrinello technique,
which has already proven to be a very useful tool for our type of
systems.[171,144,52,184]
Density functional theory (DFT) has already proven to be very useful for the
unraveling of the activation mechanisms of
MMO[163,185,164,186,187,188]
and P450[161,159,189,190,160] and the oxidation
of methane and benzene with the bare ferryl ion
(Fe=O)[170,191,192,193,194,195,168].
The paper is organized as follows. First, we briefly summarize the computational
details in section 6.2. In section 6.3, we
present our results, starting with the static DFT calculations of the energetics
of the proposed elementary Fenton and Fenton-like reactions of the hydrated
iron hydrogen peroxide complexes in vacuo. Clearly, the different nature
of the Fe(III)/HO
reagent compared to the Fe(II)/H
O
reagent is
revealed, showing that OH. radical or ferryl ion formation via O-O lysis
as the first mechanistic step is energetically very unfavorable and instead
hydrolysis (eq 6.3) is indeed predicted to be the most likely
initial step. However, realistic modeling of the hydrolysis, i.e. simulating the donation of H
by the iron(III) complex to the aqueous solution,
requires the explicit inclusion of the solvent molecules. This is done in
subsection 6.3.2 by first presenting three illustrative AIMD simulations
of the reaction between Fe
and H
O
in water, which show
the spontaneous formation of the iron(III)hydroperoxo species, followed by the
characterization of Fe(III)OOH(aq).
We have computed the vibrational spectra for the iron(III)hydroperoxo species
in both the high-spin (
) state and the low-spin (
) state,
and have compared to experimental Raman spectra.
As the second step in the Fenton-like mechanism, the O-O homolysis of the
iron(III)hydroperoxo species, producing the ferryl ion and a hydroxyl radical,
is predicted by our static DFT calculations in vacuo. The free energy barrier
for this step was computed in aqueous solution using the method of constrained
molecular dynamics and thermodynamic integration, the results of which are presented
in subsection 6.3.3. The paper ends with conclusions in section 6.4.