Abstract
Vitreous GeO2 has been compressed at high temperature to investigate the effect of thermal activation on the structural reorganization during compression. The measurements were performed in-situ using micro Raman spectroscopy under pressure up to 6 GPa and temperature up to 400 °C. The evolution of the Raman shift of the main band (400–500 cm−1) with temperature during compression evidences a pressure window around 3 GPa within which temperature has a remarkable influence on the structure, in particular, the intermediate range order. We find that this change is well correlated with previous ex-situ density measurements from high pressure-high temperature densifications. Moreover, coordination changes from tetrahedrally (GeO4) to octahedrally (GeO6) coordinated GeO2 are accelerated with the heating during the compression.
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