Crystal data for [2]PF6ꢁNH4PF6: C22H24F12N6O2OsP2S, M = 916.67,
monoclinic, space group P21/c, a = 15.9170(3), b = 9.4043(2), c =
20.2031(5) A, b = 100.5150(10)1, V = 2973.38(11) A3, Z = 4, T = 200 K,
28 325 reflections collected, 6779 independent reflections, 6065 observed
reflections (I > 2s(I)), R1 (I > 2s(I)) = 0.026, wR2 (all data) = 0.064. H
atoms of amine and imine groups were found in difference Fourier maps
and were refined with [Uiso = 1.2Ueq(N)].
1 (a) D. C. Jicha and D. H. Busch, Inorg. Chem., 1962, 1, 872;
(b) D. Gibson and S. J. Lippard, Inorg. Chem., 1986, 25, 219;
(c) R. V. Parish, Z. Salehi and R. G. Pritchard, Angew. Chem., Int. Ed.
Engl., 1997, 36, 251; (d) H. Fleischer, Coord. Chem. Rev., 2005, 249, 799.
2 (a) T. Konno, Bull. Chem. Soc. Jpn., 2004, 77, 627; (b) Z. N. Chen,
N. Zhao, Y. Fan and J. Ni, Coord. Chem. Rev., 2009, 253, 1.
3 (a) S. G. Murray and F. R. Hartley, Chem. Rev., 1981, 81, 365;
(b) L. Roecker, M. H. Dickman, D. L. Nosco, R. J. Doedens and
E. Deutsch, Inorg. Chem., 1983, 22, 2022; (c) N. Yoshinari and
T. Konno, Inorg. Chem., 2008, 47, 7450.
4 (a) B. A. Lange, K. Libson, E. Deutsch and R. C. Elder, Inorg.
Chem., 1976, 15, 2985; (b) I. K. Adzamli, K. Libson, J. D. Lydon,
R. C. Elder and E. Deutsch, Inorg. Chem., 1979, 18, 303;
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275; (d) M. Kita, K. Yamanari and Y. Shimura, Bull. Chem. Soc.
Jpn., 1983, 56, 3272.
Fig. 4 Cyclic voltammograms of [1]PF6 (left) and [2]PF6 (right) in
H2O/NaNO3 (0.1 M) at 25 1C with a scan rate of 100 mV sꢀ1
.
As shown in Fig. 4, the cyclic voltammogram (CV) of [1]PF6
in water under a nitrogen atmosphere is characterized by two
irreversible oxidation waves at Epa = +0.55 and +0.70 V
(vs. Ag/AgCl). On the other hand, the CV of [2]PF6 displays
only one irreversible oxidation wave at Epa = +0.70 V, the
potential of which is the same as the second oxidation wave for
[1]+ (Fig. 4). The spectroelectrochemical experiments were
carried out for [1]PF6 using an optically transparent thin-layer
electrode cell. When the potential was increased from 0 V, the
absorption spectrum of [1]PF6 gradually changed with several
isosbestic points, and the absorption spectrum recorded at
+0.45 V was almost the same as that of [2]+ (Fig. S8, ESIw).
From these results, it is considered that the first oxidation at
5 M. Tamura, K. Tsuge, A. Igashira-Kamiyama and T. Konno,
Inorg. Chem., 2011, 50, 4764.
6 (a) S. Decurtins, F. Felix, J. Ferguson, H. U. Gudel and A. Ludi,
J. Am. Chem. Soc., 1980, 102, 4102; (b) P. A. Lay, R. H. Magnuson
and H. Taube, Inorg. Chem., 1988, 27, 2848; (c) J.-P. Sauvage,
J.-P. Collin, J.-C. Chambron, S. Guillerez and C. Coudret, Chem.
Rev., 1994, 94, 993; (d) R. T. F. Jukes, B. Bozic, P. Belser, L. D. Cola
and F. Hartl, Inorg. Chem., 2009, 48, 1711; (e) S. Verma, P. Kar,
A. Das, D. K. Palit and H. N. Ghosh, Chem.–Eur. J., 2010, 16, 611.
7 E. M. Kober, J. V. Caspar, B. P. Sullivan and T. J. Meyer, Inorg.
Chem., 1988, 27, 4587.
E
pa = +0.55 V observed for [1]+ is due to the amine-to-imine
conversion. On the other hand, the CV of [Ru(aesi)(bpy)2]+ in
water under the same conditions showed only one irreversible
oxidation wave at Epa = +1.00 V (Fig. S9, ESIw), which is
0.45 V more positive than the first oxidation wave for [1]+.15
Thus, the facile conversion of [1]+ to [2]+ by the photo-
induced air oxidation or by the AgI oxidation is ascribed to
the relatively low oxidation potential of [1]+.
8 M. Tamura, M. Yamagishi, T. Kawamoto, A. Igashira-Kamiyama,
K. Tsuge and T. Konno, Inorg. Chem., 2009, 48, 8998.
9 G. Vitzthum and E. Lindner, Angew. Chem., Int. Ed. Engl., 1971, 10, 315.
10 To date, only one sulfinato osmium complex, which contains an
O-bonded sulfinato group, has been structurally characterized.
W. R. Roper, J. M. Waters and A. H. Wright, J. Organomet.
Chem., 1984, 276, c13.
In summary, we showed that 2-aminoethanethiolate (aet) is
easily air oxidized to 2-aminoethanesulfinate (aesi) on binding
with an [OsII(bpy)2]2+ core to form [Os(aesi-N,S)(bpy)2]+ ([1]+).
Remarkably, the aesi in [1]+ was found to be further air oxidized
to 2-iminoethanesulfinate (iesi) on irradiating light to form
[Os(iesi-N,S)(bpy)2]+ ([2]+).16,17 Although a similar amine-to-
imine conversion by air oxidation has been recognized in several
coordination systems,14b the photoinduced conversion found in
this work is unprecedented.18 Note that [1]+ is also readily
converted to [2]+ with use of Ag+, and furthermore, [2]+ is
reverted back to [1]+ with use of BH4ꢀ in aqueous media. Thus,
the present system represents a clean, reversible amine-to-imine
conversion, which is most likely due to the presence of a redox-
active OsII center whose +III state is more accessible than that of
RuII, together with the presence of an inert sulfinato donor.
This work was partly supported by a Grant-in-Aid for JSPS
Fellows from the Japan Society for the Promotion of Science (JSPS).
11 This assignment was confirmed by the 1H–1H COSY spectrum
(Fig. S5, ESIw).
12 E. Jandrasics, B. Kolp, J. A. Wolny and A. von Zelewsky, Inorg.
Chim. Acta, 1998, 272, 153.
13 (a) K. Sakai, Y. Yamada and T. Tsubomura, Inorg. Chem., 1996,
35, 3163; (b) L. Bendahl, A. Hammershøi, D. K. Jensen, S. Larsen,
A. Riisager, A. M. Sargeson and H. O. Sørensen, J. Chem. Soc.,
Dalton Trans., 2002, 3054.
14 (a) F. R. Keene, M. J. Ridd and M. R. Snow, J. Am. Chem. Soc.,
1983, 105, 7075; (b) F. R. Keene, Coord. Chem. Rev., 1999, 187, 121.
15 Meyer and co-workers have reported a similar electrochemical
oxidation of primary-amine complexes. They proposed that the
deprotonation of a primary amine group is induced by the one-
electron oxidation of RuII to RuIII, followed by the additional one-
electron oxidation to give an imine group with retention of the
Ru–N bond. G. M. Brown, T. R. Weaver, F. R. Keene and
T. J. Meyer, Inorg. Chem., 1976, 15, 190.
1
16 The appearance of sharp proton signals in the H NMR spectra of
[1]PF6 and [2]PF6 clearly indicates that the octahedral osmium center
in each compound exists in a diamagnetic +II oxidation state.
17 A plausible mechanism of this reaction involves the initial genera-
tion of a metal-to-ligand charge-transfer excited species of [1]+
,
.
Notes and references
which is readily oxidized by air to produce [OsIII(aesi)(bpy)2]2+
This OsIII species would be converted to [2]+via the pathways that
are proposed for the electrochemical oxidation.15
z Crystal data for [1]ClO4ꢁNaClO4: C22H22Cl2N5NaO10OsS, M =
832.60, monoclinic, space group C2/c,
a = 9.5421(3), b =
16.8001(7), c = 34.0526(10) A, b = 96.6130(10)1, V = 5422.6(3) A3,
Z = 8, T = 200 K, 26 730 reflections collected, 6220 independent
reflections, 5150 observed reflections (I > 2s(I)), R1 (I > 2s(I)) =
0.046, wR2 (all data) = 0.125. H atoms of amine and imine groups
18 Photoinduced conversions by dioxygen have been reported for
organic compounds, but the resulting amine species are not an end
product and have not been isolated. Y. Mitsumoto and M. Nitta,
J. Org. Chem., 2004, 69, 1256; F. Su, S. C. Mathew, L. Mohlmann,
M. Antonietti, X. Wang and S. Blechrt, Angew. Chem., Int. Ed.,
2011, 50, 657.
were found in difference Fourier maps and were refined with [Uiso
1.2Ueq(N)].
=
c
12466 Chem. Commun., 2011, 47, 12464–12466
This journal is The Royal Society of Chemistry 2011