Communication
Catalysis Science & Technology
FMN in competition with the four-electron reduction of O
2
1
9c
and the reduced FMN reacts with O to produce H O .
2
2 2
In conclusion, a water-soluble iridium(III) complex (1) can
efficiently catalyse the oxidation of HCOOH by O to mainly
2
generate water with evolution of a little amount of H2
under acidic conditions at 298 K. This reaction occurred in
both water and water-containing ethylene glycol. The rate-
determining step of the catalytic cycle is the β-hydrogen
elimination of the formate complex (2) to form the hydride
complex (3) in the same manner as the hydrogen evolution
from HCOOH catalysed by 1. This study provides an efficient
way to remove undesired formic acid in water as well as in
water-containing ethylene glycol.
Fig. 2 Time courses of oxidation of HCOOH (2.0 mM; black circle)
and DCOOH (2.0 mM; blue square) by O
under an O atmosphere in water (1.0 mL) at pH 2.8 at 298 K. R
.99 and 0.98 for the linear correlations (black and blue, respectively).
2
in the presence of 1 (10 μM)
2
2
=
0
Acknowledgements
value (4.0) reported for the hydrogen evolution reaction
under an N atmosphere under otherwise the same experimental
2
1
This work was supported by the Advanced Low Carbon
Technology Research and Development (ALCA) program of
Japan Science Technology Agency (JST) (to S.F.) and Grants-in-
Aid (no. 24550077 to T.S.) from MEXT, Japan.
9
conditions. This indicates that the rate-determining step in
the overall catalytic cycle for oxidation of HCOOH by O is the
2
β-hydrogen elimination of the formate complex (2) to form the
hydride complex (3).
The catalytic oxidation of HCOOH by O2 also occurred
in a mixed solution (3.0 mL) of ethylene glycol and water
Notes and references
[
2
4 : 1 (v/v)] and the yield of H was decreased as compared
with that under an N2 atmosphere (Fig. 3). In the same
manner, various concentrations of HCOOH were oxidised by
O under an O atmosphere by using 1 in water-containing
2 2
1 (a) D. L. Royer, R. A. Berner and J. Park, Nature, 2007, 446,
530; (b) R. Masel, Nature, 2006, 442, 521; (c) S. Y. Reece,
J. A. Hamel, K. Sung, T. D. Jarvi, A. J. Esswein, J. J. H. Pijpers
and D. G. Nocera, Science, 2011, 334, 645.
ethylene glycol at various pH values (Fig. S2 and S3 in the
ESI†). The amount of the remaining HCOOH was quantified
by H NMR, in which no oxidized product of ethylene glycol
2 W. Reutemann and H. Kieczka, Formic acid in Ullmann's
Encyclopedia of Industrial Chemistry, online edition, Wiley
VCH, Weinheim, 7th edn, 2011, DOI: 10.1002/14356007.
a12_013.pub2.
3 (a) S. Enthaler, J. von Langermann and T. Schmidt, Energy
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1
was detected. The amount of H O produced was analysed
2
2
by spectral titration using the oxo[5,10,15,20-tetra(4-pyridyl)
2
0
porphyrinato]titanium(IV) complex in water. Neither H
2
O
2
nor H was formed in the absence of HCOOH. The amount
2
of H
3 μM at 5 h, which is also negligible as in the case of the
reaction in water. The TON reached 1300 at 22 h (Fig. 3). The
amount of H was significantly increased by adding flavin
2 2
O generated in the reaction of 2.0 mM HCOOH was
1
2
O
2
mononucleotide (FMN), as shown in Fig. S4 in the ESI.† In
the presence of FMN, the hydride complex (3) reacts with
4
(a) M. Grasemann and G. Laurenczy, Energy Environ. Sci.,
2
1
4
012, 5, 8171; (b) S. Fukuzumi, Eur. J. Inorg. Chem., 2008,
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2, 18.
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Fig. 3 Time courses of H
ethylene glycol and water [4 : 1 (v/v)] mixed solution (3.0 mL) in the
presence of 1 (18 μM) under N and O atmosphere (red circle and
green triangle, respectively) at pH 5.9 at 298 K.
2
evolution from formic acid (0.50 M) in an
2
2
3638 | Catal. Sci. Technol., 2014, 4, 3636–3639
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