In situ x-ray diffraction study of dynamically compressed α-cristobalite using a dynamic diamond anvil cell

In this study we present results of the dynamic compression of alpha-cristobalite up to a pressure of 106 GPa with the use of the dynamic diamond anvil cell. X-ray diffraction images were recorded at different ramp compression and decompression rates to investigate in situ the high-pressure phase transitions of alpha-cristobalite. Our results suggest that the pressure onset of the phase transformation of alpha-cristobalite to cristobalite II, cristobalite XI, and ultimately to seifertite (alpha-PbO2 type SiO2) is dependent on the applied compression rates and stress conditions of the experiment. Increasing compression rates in general shift the studied phase transitions to higher pressures. Furthermore, our results indicate for single crystals under hydrostatic conditions a suppression of a phase transition from cristobalite X-I to seifertite at pressures of up to 82 GPa.

Automated summary

In this study, the dynamic compression of alpha-cristobalite was performed using a dynamic diamond anvil cell, and the in situ high-pressure phase transitions were investigated. The results show that the pressure onset of the phase transformation depends on the compression rates and stress conditions, and increasing compression rates shift the phase transitions to higher pressures. Additionally, under hydrostatic conditions, a phase transition from cristobalite X-I to seifertite is suppressed at pressures up to 82 GPa.