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large Q-band, suggesting potential application of diazachlorins
to light-harvesting materials.
The work was supported by Grants-in-Aid for Scientific Research
(No. 24350023) and Program for Leading Graduate Schools
‘‘Integrative Graduate Education and Research in Green Natural
Sciences’’, MEXT, Japan. H.S. acknowledges Yazaki Memorial
Foundation for Science and Technology for financial support.
Notes and references
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ed. K. M. Kadish, K. M. Smith and R. Guilard, World Scientific,
Singapore, 2011, vol. 11, pp. 223–290; (b) Handbook of Porphyrin
Science, ed. K. M. Kadish, K. M. Smith and R. Guilard, World
Scientific, Singapore, 2012, vol. 20.
2 M. Horie, Y. Hayashi, S. Yamaguchi and H. Shinokubo, Chem.–Eur. J.,
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3 Y. Matano, T. Shibano, H. Nakano and H. Imahori, Chem.–Eur. J.,
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Fig. 2 UV/vis absorption spectra of 3a, 4a and 5 measured in dichloromethane.
4 (a) T. Ito, Y. Hayashi, S. Shimizu, J.-Y. Shin, N. Kobayashi and
H. Shinokubo, Angew. Chem., Int. Ed., 2012, 51, 8542; (b) H. Kamiya,
T. Kondo, T. Sakida, S. Yamaguchi and H. Shinokubo, Chem.–Eur. J.,
the DFT calculation revealed the larger energy gap between
HOMO and HOMO–1 of 4a than that of 3a (Fig. S21, ESI†).
Electrochemical properties of 3a and 4a were examined
using cyclic voltammetry (ESI,† Fig. S20). One reversible oxida-
tion wave and two reversible reduction waves were observed
for diazaporphyrin 3a, while diazachlorin 4a exhibited one
reversible reduction and one reversible oxidation wave. The
electrochemical HOMO–LUMO gaps for 3a and 4a were deter-
mined to be 2.18 and 1.93 V, respectively. The narrower
HOMO–LUMO gap of 4a matches well with the optical analysis
and theoretical calculations. The saturation of the Cb–Cb bond
did not alter the reduction potential (À1.44 V for 3a vs. À1.49 V
for 4a) but induced a substantial cathodic shift in the oxidation
potential (0.74 V for 3a vs. 0.44 V for 4a).
¨
2012, 18, 16129; (c) D. Sakow, B. Boker, K. Brandhorst, O. Burghaus
¨
and M. Broring, Angew. Chem., Int. Ed., 2013, 52, 4912.
5 (a) J. C. W. Evans and C. F. H. Allen, Org. Synth., 1943, Coll. vol. II, 517;
(b) C. S. Giam and J. L. Stout, J. Chem. Soc., Chem. Commun., 1970, 478.
6 (a) J. Clayden, Organolithiums: Selectivity for Synthesis, Pergamon,
Oxford, 2002; (b) The Chemistry of Organolithium Compounds, ed.
Z. Rappoport and I. Marek, John Wiley & Sons, New York, 2004.
7 (a) M. O. Senge, W. W. Kalisch and I. Bischoff, Chem.–Eur. J., 2000,
6, 2721; (b) W. W. Kalisch and M. O. Senge, Angew. Chem., Int. Ed., 1998,
37, 1107; (c) I. Bischoff, X. Feng and M. O. Senge, Tetrahedron, 2001,
57, 5573; (d) M. O. Senge, J. Richter, I. Bischoff and A. Ryan, Tetrahedron,
2010, 66, 3508; (e) B. Krattinger and H. J. Callot, Tetrahedron Lett., 1996,
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39, 1165; (g) B. Krattinger and H. J. Callot, Eur. J. Org. Chem., 1999, 1857.
8 The starting material 1 was also recovered in ca. 30%. In addition,
trace amounts of dialkylated diazaporphyrins and diazabacterio-
chlorins were detected. Probably dialkylation is unfavorable because
of unstable dilithiated species even in the presence of an excess
amount of the alkyllithium. The present alkylation was also applic-
able for 3,5-di-tert-butyldiphenyl-substituted diazaporphyrin.
9 H. W. Whitlock, R. Hanauer, M. Y. Oester and B. K. Bower, J. Am.
Chem. Soc., 1969, 91, 7485.
In conclusion, 5,15-diazachlorins were readily prepared
by regioselective nucleophilic addition of alkyllithiums to
5,15-diazaporphyrin. Similarly to the absorption features of
typical chlorins, diazachlorins exhibited a red-shifted and relatively
c
5066 Chem. Commun., 2013, 49, 5064--5066
This journal is The Royal Society of Chemistry 2013