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been reported as 3.7 × 10−3[26] and 2 × 10−3[23] with values for
HOOH ~3.2 × 10−2 M−1 and for K2HOOH ~6.6 × 10−4 M−1[23].
In 1999, Pignatello et al. reported the reactions of a photo activated
K
Fenton-like reagent (0.2 mM Fe(III)aq/2.0 mM H2O2/I = 0.1 M, NaClO4/
HClO4, pH 1–3) with cyclohexane, cyclohexene, 1,1,2-trichloroethane,
trichloroethene and tetrachloroethene in a stirred two-phase system
at 25 °C [27]. KOOH Eq. (4) was determined spectrophotometrically
at 450 nm to be (9.0
1.5) × 10−3 at pH 2.8 shifting to (1.4
0.5) ×
10−2 at pH 1.45. This latter value is similar to that reported by Lewis et
al. [23] for KHOOH and is presumed here to refer to reaction (3). Interest-
ingly the reactions with the chlorinated hydrocarbons; trichloroethene
and tetrachloroethene studied at pH 2.8 gave a distribution of carboxylic
acid products (particularly high yields of dichloroethanoic acid from
trichloroethene) not consistent with solely radical processes initiated
by H atom abstraction, e.g. by OH radicals, but rather from the decompo-
sition of an intermediate epoxide [27]. Subsequent investigations with
cyclohexene at pH 2.8 led to the detection of significant amounts
of epoxide accompanying formation of the expected allylic oxidation
products; 2-cyclohexen-1-ol and 2-cyclohexen-1-one [27]. However a
surprising observation was the slow appearance of reaction products
over several hours. Substitution of water on [Fe(OH2)5OH]2+, the likely
Fig. 1. GC trace following sampling of the cyclohexene layer after 2 min at 25 °C.
The labeled products are A; cyclohexene epoxide, B; 2-cyclohexen-1-ol/cyclohexanol,
C; 2-cyclohexen-1-one. The peak at Rf 6.91 min is from cyclooctane added as reference
prior to running the GC. Aqueous layer: [H2O2]init = 10 mM; [Fe(III)]init = 0.2 mM, pH 2.7.
aqua iron(III) species present under the stated conditions [28,29], is fast
298
(k
ex
= 1.4 × 105 s−1) [30] suggesting that assembly of the active cata-
lyst from complexes such as [Fe(OH2)4(HOOH)OH]2+ Eq. (6) or more
likely, given the higher acidity of coordinated H2O2[25], its tautomeric
form [Fe(OH2)5OOH]2+ Eq. (7) occurs on the submillisecond timescale.
a slow but steady decrease over the first hour. The addition of further
aliquots of stock H2O2 solution after 10 and 20-minute reaction,
Figure S1, indeed failed to restore the catalytic activity of the solution.
However, the addition of aliquots of fresh iron(III) solution did re-
store some activity over the first 30 min, Figure S2, when amounts
of H2O2 were still present, Fig. 2. A gradual darkening of the aqueous
phase followed by a brown turbidity after 1 h suggested that the
loss of catalytic oxygenation activity is due to gradual depletion of
soluble mononuclear aqua iron(III) via hydrolytic polymerization to
inactive colloidal forms and finally precipitation of insoluble iron(III)
oxy-hydroxides [28]. A closer inspection of the H2O2 decay profile,
Fig. 2, reveals an induction period within the first 2 min correlating
with the maximum rate of H2O2 activation towards oxygenation.
Thereafter, efficient catalysis of H2O2 decomposition dominates.
A further insight into the nature of the putative iron(III) oxygenation
catalyst came from monitoring the pH dependence of the yields of oxi-
dation products following the initial sampling after 2-minute reaction,
Fig. 3. The yields of all products increase sharply in the pH range 2.7–
3.2 before decreasing at higher pHs. Interestingly there is a small but
noticeable increase in the relative yield of epoxide compared to the
allylic oxidation products; the epoxide yield increasing between pH
2.7 and 3.2 to reach ~13% of the total oxidation products seen. Above
pH 3.2 the total product yield decreases but the relative yield of epoxide
remains steady at ~11%. The speciation profiles of aqua iron(III) at
below mM concentrations (data from [29a] shown in Fig. 3 for com-
parison) indicate a correlation of oxygenation catalytic activity with
amounts of the hydroxopentaaqua ion; [Fe(OH2)5OH]2+ (pK11 = 2.54
at I = 0.1 M, NaClO4) [29a]. With oxo-aquairon(IV) not proven as an
effective epoxidation catalyst [31c], we tentatively propose the follow-
ing mechanism for alkene epoxidation, Fig. 4. Firstly, an activated com-
plex forms between [Fe(OH2)5OOH]2+ and cyclohexene which then
undergoes intramolecular iron-bound oxygen atom transfer (most
electrophilic) to the cyclohexene double bond accompanying (H3O+)-
assisted O\O heterolysis. Formation of the allylic oxidation products;
2-cyclohexen-1-ol and 2-cyclohexen-1-one will arise via the generally
accepted radical autoxidation mechanism (8)
½FeðOH2Þ OHꢀ2þ þ H2O2→½FeðOH2Þ ðHOOHÞOHꢀ2þ þ H2O
ð6Þ
5
4
ð7Þ
Furthermore, the formation of epoxide, which is only observed in
the presence of iron(III), is not consistent with reactions involving OH
radicals e.g. via Eq. (1) and suggests another source for the oxidation.
It was speculated [27] that [Fe(OH2)5OOH]2+ could homolytically
cleave at the O\O group to generate the oxo-aquairon(IV) complex;
[Fe(_O)(OH2)5]2+ which actually transfers oxygen to the cyclohexene.
However extensive studies by Bakac and co-workers on the chemistry
of oxo-aquairon(IV), generated via reaction of ozone with [Fe(OH2)6]2+
,
show that it tends to rather promote H atom or hydride abstraction and
only transfers oxygen to highly oxophilic substrates such as sulfoxides
or phosphines [31,32].
We have re-investigated Pignatello's reaction of aqueous iron(III)
(added as a freshly made up acidified solution of [Fe(OH2)6](ClO4)3
adjusted to pH 2–4) and H2O2 with neat cyclohexene in a stirred
two-phase system [33]. A typical GC trace for the reaction products
isolated from the cyclohexene layer at pH 2.7, Fig. 1, confirms the
presence of cyclohexene epoxide A (Rf = 5.78 min) accompanying
the formation of 2-cyclohexen-1-ol/cyclohexanol B (not resolved)
(Rf = 6.23) and 2-cyclohexen-1-one C (Rf = 6.68). The peak at
Rf = 6.91 is from cyclooctane added as an internal reference. Fig. 2
shows a typical plot (25 °C) at pH 3.0 representing integration of
the GC peaks A–C as a function of sampling time after the initial injec-
tion of H2O2. The product yields were calculated relative to the
amount of the internal reference added to each sample. Clearly appar-
ent from Fig. 2 is the rapid formation of products within the first
2-minute sampling time with little or no change thereafter over a
1-hour period. It was initially thought that the loss of activity after
the initial 2-minute sampling was due to rapid depletion of H2O2
from the reaction solution. However subsequent monitoring of the
[H2O2] concentration via permanganate titration of aliquots of the
aqueous phase in a separate run (shown also in Fig. 2) showed only
ð8Þ