We have theoretically investigated several polymeric (nonmolecular) CO2 sol
ids analogous to various phases of SiO2. Our calculations reveal that CO2 d
iffers dramatically from SiO2 because of its rigid intertetrahedron angular
interaction. Because of this, we find that a beta-cristobalitelike phase i
s energetically the favored polymeric CO2 phase rather than quartz, which i
s preferred in SiO2. The calculated Raman spectrum of beta-cristobalite CO2
shows a dominant A, peak at about 780 cm(-1) at 40 GPa which shifts down t
o about 640 cm(-1) at 1 GPa. This is consistent with the recent high-pressu
re experiments of Iota et al.