T. Chaplin et al., COMPUTER-SIMULATION OF THE INFRARED AND RAMAN ACTIVITY OF PYROPE GARNET, AND ASSIGNMENT OF CALCULATED MODES TO SPECIFIC ATOMIC MOTIONS, The American mineralogist, 83(7-8), 1998, pp. 841-847
The lattice dynamics computer code PARAPOCS was successfully used to c
alculate the 240 vibrational frequencies of pyrope garnet, Mg3Al2Si3O1
2, at ambient conditions. The atomic displacement vectors (eigenvector
s) for each frequency were also calculated and their symmetry relation
s analyzed with the aid of factor group analysis (FCA), to determine t
he symmetry species of each vibrational mode. Comparison with the expe
rimental IR and Raman data shows excellent agreement, but no LO-TO rev
ersals were identified. Calculation of the frequency shifts due to the
isotopic substitution of Mg-26 and Si-30, together with a more detail
ed analysis of the calculated eigenvectors, enabled identification of
the dominant site or cation motion contributing to each vibrational mo
de. Previous assignments of the high-frequency vibrations to pure SiO4
internal modes and the lower-frequency vibrations to mixed cation mod
es are supported. We conclude that the specific number of site/atom mo
tions predicted by site group analysis (SGA) is not adhered to due to
substantial mode mixing, and that FCA and SCA, in which the SiO4 tetra
hedra are treated as isolated units, are only applicable at high frequ
encies. The agreement observed between the calculated and experimental
data leads us to conclude that the method of computer modeling used a
nd the interatomic potentials employed in the simulations provide a go
od description of the lattice dynamical behavior of pyrope garnet.