Path integral Monte Carlo simulations of silicates

We investigate the thermal expansion of crystalline SiO${}_2$ in the $\beta$– cristobalite and the $\beta$-quartz structure with path integral Monte Carlo (PIMC) techniques. This simulation method allows to treat low-temperature quantum effects properly. At temperatures below the Debye temperature, thermal properties obtained with PIMC agree better with experimental results than those obtained with classical Monte Carlo methods.