Raman spectra of glassy PbO-GeO
2 and PbO-B
2O
3 systems were measured and analyzed. For pure glassy GeO
2, several bands were observed at 300-600 (peak position: 410), 760, 860 and 970cm
-1. The bands at 410, 760 and 860cm
-1 were assigned respectively to ν
4, ν
1 and ν
3 mode of the vibration of the tetrahedral GeO
4 which has
Td symmetry. For PbO-GeO
2 system a new band appeared at 750-850cm
-1 and it could be separated into two bands by the polarization. analysis. One of these new bands, the band of higher energy, corresponding to the band at 860cm
-1 of glassy GeO
2, was found to shift toward a lower wavenumber with increasing PbO content. The wavenumber of this band showed a nearly constant value in the neighbourhood of PbO⋅GeO
2 composition. The similar shift of another band of lower energy was also found. The fact might be related to the 6-folded coordination of Ge in tetragonal GeO
2 (rutile type). Such a trend of band shifting found in Raman spectra is similar to that of the infrared absorption spectra previously reported by the authors.
For pure glassy B
2O
3, several bands were also observed at 450, 650, 806, 1260 and 1470cm
-1. The bands at 650, 806, 1260 and 1470cm
-1 were assigned respectively to ν
4′, ν
1′, ν
3′, and ν
3′ mode of the vibration of the triangular BO
3 which is
D3h symmetry. For PbO-B
2O
3 system, the bands at 1260 and 1470cm
-1 were united into a broad band and showed the shift toward a lower wavenumber with increasing PbO content, e.g. 1350cm
-1 for PbO 30mol% and 1245cm
-1 for PbO 70mol%, suggesting the effect of the interaction between Pb
2+ ion and BO
3 group. A new band appeared at 1000-1150cm
-1, and could be assigned to ν
3 mode of BO
4 tetrahedral structure (
Td symmetry). The intensity of this band increased up to about PbO 50mol%, and then decreased with further increase of PbO. The fact might be related to the number of BO
4 structural units which are found in the system.
Based on the above assignments, we estimated the force constants in GeO
4 and BO
3 structural units by
GF matrix method. The values of
fr,
fφ and
frφ for GeO
4 were 5.45, 0.55 and 0.13 (mdyn/Å) and for BO
3 were 6.13, 0.80 and 0.76 (mdyn/Å), respectively.
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