The ring-opening vibrations of the spherosilasesquioxanes of the gener
al formula (HSiO3/2)(2n), n = 2, 3, 4, etc., are normal modes in which
all Si-O stretching and/or O-Si-O bending displacements of the consid
ered ring are in phase. We have investigated the vibrational structure
of the experimentally well-known H8Si8O12 and H12Si12O15 and of I-g-H
20Si20O30 and O-h-H24Si24O36, which are not yet known as isolated mole
cules. The energy range of the 11 IR active, the 15 Raman active, and
the three inactive ring-opening modes which belong to the 4-, 5-, and
6-ring vibrations of O-h-H8Si8O12, D-5h-H10Si10O15, I-h-H20Si20O30, an
d O-h-H24Si24O36 decreases from 490-390 to 440-250 to 340-219 cm(-1).
The 4-, 5-, and 6-rings are in fact built of four, five, and six Si at
oms plus four, five, and six O atoms, respectively. The totally symmet
ric vibrations show predominantly stretching character with one except
ion, the delta(O-Si-O) line at 451 cm(-1) of H24S24O36 They occur in s
pecific regions, namely, at 460-440 cm(-1) for the 4-ring, at 340-250
cm(-1) for the 5-ring, and at 220-210 cm(-1) for the 6-ring. We show t
hat the ring-opening vibrations of the hydrosilasesquioxanes suggest a
new way to study the pore-opening vibrations of zeolites, which simpl
ifies the problem remarkably and thus leads to a better understanding
of the more complex extended structures. The vibrations of the investi
gated spherosiloxanes can be divided into six distinct regions denoted
as nu(Si-H), nu(as)(Si-O-Si), delta(O-Si-H), nu(s)(Si-O-Si), delta(O-
Si-O), and delta(Si-O-Si). This means that the concept of group freque
ncies makes sense. However 10 modes were observed which do not fit int
o this general scheme, namely, the modes at 481 and 446 cm(-1) (H8Si8O
12), at 455, 450, and 334 cm(-1) (H10Si10O15), at 336, 284, and 251 cm
(-1) (H20Si20O30), and at 219 and 214 cm(-1) (H24Si24O36). All of them
can be identified as ring-opening vibrations.