Using a large-volume high-pressure apparatus, Li 2 O–4GeO 2 glass and pure GeO 2 gel have been compressed to 14 GPa at room temperature and their local structural changes have been investigated by an in situ XAFS (x-ray absorption fine-structure) method. On compression of Li 2 O–4GeO 2 glass, the Ge–O distance gradually becomes short below 7 GPa, showing the conventional compression of the GeO 4 tetrahedron. Abrupt increase in the Ge–O distance occurs between 8 and 10 GPa, which corresponds to the coordination number (CN) changing from 4 to 6. The CN change is completed at 10 GPa. On decompression, the reverse transition occurs gradually below 10 GPa. In contrast to the case for Li 2 O–4GeO 2 glass, the Ge–O distance in GeO 2 gel gradually increases over a pressure range from 2 to 12 GPa, indicating that continuous change in CN occurs. The Ge–O distance at 12 GPa is shorter than that of Li–4GeO 2 indicating that the change in CN is not completed even at this pressure. On complete release of pressure, the Ge–O distance reverts to that of the starting gel.
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Ohtaka et al. (2002) studied this question.
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