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Scheme 1
and the organic ligand of complex 1 is subjected to deep oxidization.
Some active intermediates generated from the decomposition of
salen Co(II) in situ should be the true catalytic active species, which
are responsible for the oxygen evolution. Further research is under-
way in order to make clear what species and the quantity content are.
In conclusion, an efficient water oxidation system was devel-
oped using a precatalyst N, N0-bis(salicylidene)ethylenediamine-
cobalt(II). A TON of 854 and a TOF of 6.4 sꢀ1 were achieved, which
are among the highest values reported for photocatalytic water
oxidation so far.
Fig. 3 X-Ray photoelectron spectra of Co3O4 and precipitates derived
from 1 in the energy regions of Co 2p and O 1s. The binding energy of each
element was corrected by the C 1s peak (284.8 eV).
The X-ray photoelectron spectra (XPS) measurement was carried
out for the above particles, being washed several times by purified
water. Fig. 3 shows the XPS spectrum of Co 2p of the particles, with
2p3/2 and 2p1/2 appearing at 781.0 eV and 796.0 eV, respectively. No
satellite peaks of Co 2p were observed in the XPS spectrum of the
precipitate, indicating that no Co(II) species existed on the surface
of the precipitate.
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-2013-50, lzujbky-2013-ct 02).
Compared to Fukuzumi’s XPS binding energy values8 of particles
derived from [CoII(Me6tren)(OH2)]2+ (2), our compounds decom-
posed from 1 are different to them. Similarly, authentic Co3O4
shows two intense peaks at 779.8 eV for Co 2p3/2 and at 794.8 eV for
Co 2p1/2 with two satellite peaks at 790.1 eV and 805.5 eV,
respectively. Contrasted with the O1s peak of Co3O4 (530.1 eV), a
higher binding energy of 531.5 eV for the precipitate was observed,
revealing that metal hydroxide species existed in the solid.8 Based
on the ESI/MS, 1H NMR and XPS analysis, the precipitates derived
from 1 should be Co(III) inorganic species, which would be a mixture
of Co(III) containing oxide and/or Co(III) hydroxide.
The recycling of the true catalytic active species was evaluated
(Table S8, ESI†). The catalytic activity (40.9% O2 yield) of the
isolated precipitate derived from salen Co towards visible-light-
driven water oxidation was found to be considerably lower than
that of fresh salen Co (54.6% O2 yield). The sizes of most particles
in situ formed during the photocatalytic process (Fig. S15, ESI†) are
less than 100 nm. However, the sizes of isolated precipitates
derived from salen Co (Fig. S16, ESI†) are from 100 to 200 nm.
The number of active cobalt oxo sites on the surface of the active
intermediate available for O2 formation is expected to be more for
these small particles in situ formed. So, the catalytic activity of the
fresh catalyst of salen Co was better than the recovered one.
A proposed mechanism is shown in Scheme 1. The reaction
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2ꢀ
were quenched by two S2O8
through visible-light-accessible
metal-to-ligand charge-transfer, resulting in the generation of two
2ꢀ
ꢀ
[RuIII(bpy)3]3+ complexes and two SO4 and two SO4 radical
anions. The latter which is also a strong oxidant oxidizes two
another [RuII(bpy)3]2+ to give two more [RuIII(bpy)3]3+ accompanying
ꢁ
ꢀ
SO4 radical anions converting into SO42ꢀ. The light induced
ꢁ
products ꢀof [Ru(bpy)3]3+ (E[Ru(bpy)32+/3+] in our system is 1.16 V)
and SO4 [E1(SO4 ꢀ/SO42ꢀ) E 2.4 V]18 are both strong oxidants,
ꢁ
ꢁ
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Chem. Commun., 2014, 50, 2167--2169 | 2169