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sites of diiron 2 and gives the dibridged complex with two cis
free coordination sites which could represent a key structural
aspect of the process of oxygen evolution. However, the replace-
ment of the carboxylate with other anionic conjugate bases and
the protonation of the oxo bridge engender the expected changes
in the (m-oxo)(m-carboxylato)diiron mode (Fig. S8, ESI†).
The catalytic activity of FeTPA in Britton–Robinson buffer
solution was evaluated, and a monomer species existed as stated
above in the system. As is listed in Table S2 (ESI†), the activity
of monomeric FeTPA in Britton–Robinson buffer solution was
an order of magnitude lower than that of the dimeric species
in acetate buffer. All these results mentioned above clearly
indicate that the (m-oxo)(m-acetato)diiron formed and func-
tioned as the active species.
A number of parameters must be considered when an
oxygen-evolving reaction is conducted, and among them, pH is
always a key factor that influences the performance of an OEC. As
is depicted in Fig. S9 (ESI†), titration of FeTPA was conducted in
acetate buffer between pH 3.5 and 5.5 with 4 M solution of NaOH.
The absorbance of the characteristic peaks of the Fe–O–Fe dimer
in acetate buffer increased as more NaOH solution was added
from pH 3.5 to 4.5. This demonstrates that more iron dimers
existed in pH 4.5 acetate buffer solution since the monomeric
species shows no obvious response to visible light (Fig. 3). We
speculated that this was because the oxo bridges of the as-formed
Fe–O–Fe dimer were susceptible to protons and more H+ resulted
in more monomeric species in the solution.
Based on the discussion mentioned above, the catalytic
activity of FeTPA should be dependent on pH values. In order
to confirm this speculation, oxygen evolution reactions were
carried out in acetate buffer solutions with different pH values
(pH = 3.5; 4.5; 5.5) in parallel. As depicted in Fig. S10 (ESI†),
reaction at pH 4.5 gave the highest O2 yield and TON. Combining
the results of titration measurements with the results of oxygen
evolution experiments gives the conclusion that the optimum
pH value is 4.5 and further supports the above statement that
the Fe–O–Fe dimer is the actual catalyst for oxygen evolution.
Under other pH conditions, the oxygen evolution is poorer.
Therefore, subsequent experiments involving catalytic O2
evolving processes were carried out in acetate buffered (0.23 M,
pH = 4.5) aqueous solution.
The catalytic activity of the title complex was also compared
with catalysts 3, 4, 5 and 6 (Fig. 2). As is revealed in Fig. 2, the
fastest O2 liberation was observed with complex 3 and oxygen
evolution reached a plateau for only a few minutes; however,
the turnover number was quite low compared with catalyst 2.
The relatively low TON obtained over catalyst 3 might be due to
its inferior stability. The trigonal bipyramidal geometry ligand
with a particularity of phenolate oxygen in compound 3 is
labile and prone to oxygenolysis in its high oxidation states
(Fig. S11 and S12, ESI†). A small amount of oxygen was released
when catalyzed by complex 5, which dissociates under the test
conditions (Fig. S13, ESI†). No oxygen evolution was observed
when catalysts 4 and 6 were tested. These results show that
the m-oxo-bridged diiron units are necessary and capable of
homogenous catalytic oxygen-evolution.
Fig. 4 UV-vis spectral evolution of 2 (0.5 mM) before (black) and after
(color) addition of 20 equiv. of Oxone in acetate buffer at room
temperature.
To investigate what species are involved in the oxygen evolution
processes, further experiments were carried out. Fig. 4 depicts the
UV-vis spectral evolution of diiron in acetate buffer when 20 equiv.
of Oxone was added. An isosbestic point is observed and the peak
at 700 nm red shifted gradually to 726 nm with the addition of
Oxone, indicating the formation of a new species with a higher
molar absorptivity. Analogous spectra of [Fe(O)(TPA)(ClO4)]+ are
reported through the reaction of [Fe(TPA)(NCCH3)2]2+ with 1 equiv.
CH3CO3H.16 Therefore, a highly oxidizing Fe(IV)QO intermediate
was supposed to be formed on the basis of the experimental
evidence discussed above.
In summary, a series of coordination complexes based on earth-
abundant, environmentally benign iron metal were designed and
examined for oxygen evolution. Several lines of evidence suggested
that complexes 1 and 2 convert to (m-O)(m-OAc)diiron(III) in
acetate buffer, which is responsible for the O–O bond formation.
A quite high TON (2380) and TOF (2.2 sÀ1) were obtained over
[(TPA)2Fe2(m-O)(m-OAc)]3+ under the optimum conditions. To the
best of our knowledge, this TON represents the highest value for
any first-row transition metal–organic complex based homo-
geneous WOCs reported to date. The key m-oxo structure is
useful for the conceptual design of iron-based homogeneous
oxygen evolving complexes. A high-valent iron oxo species
observed in UV-vis spectra maybe an intermediate in the catalytic
cycle of O2 evolution with Oxone. Compared with the heteroge-
neous Fe based WOCs, taking the Fe2O3–NA/RGO/BiV1ÀxMoxO4
heterojunction20 for example, the diiron unit exhibits a quite high
efficiency. However, its stability is inferior to that of the hetero-
geneous ones due to dimer splitting.
This work was financially supported by the National Natural
Science Foundation of China (Grant No. 21173105 and 21172098)
and the Fundamental Research Funds for the Central Universities
(lzujbky-2014-67).
Notes and references
1 V. Artero and M. Fontecave, Chem. Soc. Rev., 2013, 42, 2338–2356.
2 F. Y. Song, Y. Ding, B. C. Ma, C. M. Wang, Q. Wang, X. Q. Du, S. Fu
and J. Song, Energy Environ. Sci., 2013, 6, 1170.
3 R. Cao, W. Lai and P. Du, Energy Environ. Sci., 2012, 5, 8134.
4 S. W. Gersten, G. J. Samuels and T. J. Meyer, J. Am. Chem. Soc., 1982,
104, 4029–4030.
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5 X. Sala, S. Maji, R. Bofill, J. Garcıa-Anton, L. Escriche and A. Llobet,
Acc. Chem. Res., 2013, 47, 504–516.
6 T. Kikuchi and K. Tanaka, Eur. J. Inorg. Chem., 2014, 2014, 607–618.
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