Raman spectra of low-temperature polymorphic forms of AlPO4 (berlinite, pho
sphocristobalite and phosphotridymite) are presented. The interpretation of
the spectra has been carried out using the model of [PO4](3-) tetrahedron
isolated by Al3+ cations. The theoretical number of Raman active modes has
been determined using the factor group analysis. Raman and IR spectra have
been compared regarding adequate selection rules. The crystalline field spl
itting and Davydov effects have been discussed. It has been shown that AlPO
4 polymorphs, usually classified as a framework structure, because of the s
imilarity to SiO2, should be rather treated as an orthophosphate structure.
Thus the model of the oxygen bridge, commonly used for interpretation of f
ramework structures, should not be used in the case of AlPO4. (C) 2000 Else
vier Science B.V. All rights reserved.