356
H. OGAWA, T. FUJIGAKI AND T. CHIHARA
amount required for complete surface coverage could be
estimated as 2.7 Â 10 3 mol g 1 on the basis of the cross-
1
sectional area of Gly (ca 0.23 nm2 molecule
by
molecular modelling) and the specific surface area of
silica gel (371 m2 g 1) by BET measurement. These data
imply that a decrease in the amount of Gly on silica gel
allows easier dispersion of Gly molecules on the silica gel
surface, thus suppressing intermolecular interactions
between Gly molecules. This resulted in Gly being
adsorbed predominantly as neutral species having C=O
and NH2 groups. This species is considered to promote
the dehydration of Gly readily, and the selective
formation of intermediate GlyGly is believed to be
achieved with the suppression of intermolecular inter-
actions between GlyGly molecules.
REFERENCES
1. J. H. Clark, A. P. Kybett and D. J. Macquarrie, Supported
Reagents: Preparation, Analysis, and Applications. VCH, New
York (1992); K. Smith (Ed.), Solid Supports and Catalysis in
Organic Synthesis. Prentice Hall, Englewood Chiffs, NJ (1992); P.
Laszlo (Ed.), Preparative Chemistry Using Supported Reagents.
Academic Press, San Diego (1987); A. McKillop and D. W.
Young, Synthesis 401 (1979); G. H. Posner, Angew. Chem., Int. Ed.
Engl. 17, 487 (1978); A. Cornelis and P. Laszlo, Synthesis 909;
(1985); H. Ogawa, M. Kodomari and T. Chihara, PETROTECH
19, 404 (1996).
Figure 2. IR absorption of Gly at various loadings
2. Z. Cohen, E. Keinan, Y. Mazur and T. H. Varkony, J. Org. Chem.
40, 2141 (1975); E. Keinan and Y. Mazur, J. Org. Chem. 42, 844
(1977), and references cited therein.
3. G. Bram and T. Fillebeen-Khan, J. Chem. Soc., Chem. Commun.
522 (1979).
4. E. Keinan and Y. Mazur, J. Am. Chem. Soc. 99, 3861 (1977); J.
Muzard, Synthesis 60 (1982).
5. T. Chihara, S. Teratani and H. Ogawa, J. Chem. Soc., Chem.
Commun. 1120 (1981); T. Chihara, Y. Takagi, S. Teratani and H.
Ogawa, Chem. Lett. 1451 (1982).
6. T. Nishiguchi, K. Kawamine and T. Ohtsuka, J. Chem. Soc., Perkin
Trans. 1 153; (1992) T. Nishiguchi and K. Kawamine, J. Chem.
Soc., Chem. Commun. 1766. (1990)
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(1985); H. Ogawa, J. Phys. Org. Chem. 4, 346 (1991); H. Ogawa,
T. Chihara, S. Teratani and K. Taya, J. Chem. Soc., Chem.
Commun. 1337 (1986).
1
ences existed, including new bands at 1700–1630 cm
due to the ꢁC O stretching vibration together with the
=
disappearance of the characteristic CO2 absorption as
seen with Gly in the solid state. Slight differences also
existed in the absorption intensities of the bands at ca
3400–3200 and ca 2900–2500 cm due to ꢁNH2 and
ꢁNH3 , respectively, i.e. an increase in intensity of ꢁNH2
1
was observed with a decrease in that of ꢁNH3
.
IR spectra of Gly on various loadings are illustrated in
Fig. 2. Changes in the spectra were observed with a
decrease in the amount of Gly, where the intensity of the
absorption of ꢁC=O increased with a simultaneous
decrease in that of ꢁasCO2 (spectra d–a, Fig. 2). This
8. H. Ogawa, K. Nozawa and P. Ahn, J. Chem. Soc., Chem. Commun.
1393 (1993).
indicates that Gly at lower loadings is adsorbed mainly as
9. N. Yoshino and T. Yoshino, Bull. Chem. Soc. Jpn. 46, 2899 (1973).
10. R. M. Silverstein, G. C. Bassler and T. C. Morrill, Spectrometric
Identification of Organic Compounds, 4th ed., p. 126. J Wiley,
New York (1981); S. Sternhell and J. R. Kalman, Organic
Structures from Spectra, p. 13. J Wiley, New York (1987).
species having a C=O group. At fairly high loadings
3
1
(more than 2.7 Â 10
mol g
SiO2, ꢀ > 1.0), the
spectra were similar to that of Gly in the solid state. The
Copyright 1999 John Wiley & Sons, Ltd.
J. Phys. Org. Chem. 12, 354–356 (1999)