Abstract
The performance of a recently proposed two‐body potential model for SiO2 [van Beest et al., Phys. Rev. Lett. 6 4, 1995 (1990)] was critically evaluated through the calculation of the static and dynamical properties of several polymorphs of SiO2 using molecular dynamics methods. It was found that the calculated static structures are in excellent agreement with experiments. In particular, the pressure–volume equations of state for α‐quartz, cristobalite, and stishovite, the pressure‐induced amorphization transformation in α‐quartz and thermally induced the α→β transformation in cristobalite are well reproduced by this model. The calculated vibrational spectra are in fair agreement with experiments. The strengths and the weaknesses of the potential will be presented and discussed.