Abstract

The infrared (IR) spectroscopic data for a series of 15 rare earth double-deckers M[Pc(MeOPhO) 8] 2 [M = Y, La, …, Lu, except Pm; H 2Pc = 2, 3, 9, 10, 16, 17, 23, 24-octakis(4-methoxyphenoxy)phthalocyanine] with tervalent rare earths M III[Pc(MeOPhO) 8] 2 (M = Y, La, …, Lu except Ce and Pm) and intermediate-valent cerium Ce[Pc(MeOPhO) 8] 2 have been collected with resolution of 2 cm −1. For M III[Pc(MeOPhO) 8] 2, typical IR marker band of the monoradical anion Pc(MeOPhO) 8 − shows characteristic absorption band whose frequency linearly varies in the range from 1313 cm −1 as a weak band for La[Pc(MeOPhO) 8] 2 to 1324 cm −1 as a medium band for Lu[Pc(MeOPhO) 8] 2 along with the decrease of rare earth ionic size. For Ce[Pc(MeOPhO) 8] 2, a weak band at 1324 cm −1 with contribution from pyrrole stretching was the marker IR band of phthalocyanine dianion Pc 2−. In conclusion, all the metal size-dependent IR absorptions should be contributed primarily from the vibrations of pyrrole, isoindole stretching, breathing or deformation or aza stretching of the Pc ring.

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