Structural changes of quartz-type crystalline and vitreous GeO2 under pressure

Using a large volume high pressure apparatus, quartz‐type crystalline GeO2 and Li2O‐4GeO2 glass have been compressed up to 14 GPa at room temperature and their local structural changes have been investigated by an in‐situ XAFS method. In quartz‐type crystalline GeO2, the change of the coordination n...

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Published inJournal of synchrotron radiation Vol. 8; no. 2; pp. 791 - 793
Main Authors Ohtaka, Osamu, Yoshiasa, Akira, Fukui, Hiroshi, Murai, Kei-ichiro, Okube, Maki, Katayama, Yoshinori, Utsumi, Wataru, Nishihata, Yasuo
Format Journal Article
LanguageEnglish
Published 5 Abbey Square, Chester, Cheshire CH1 2HU, England Munksgaard International Publishers 01.03.2001
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Summary:Using a large volume high pressure apparatus, quartz‐type crystalline GeO2 and Li2O‐4GeO2 glass have been compressed up to 14 GPa at room temperature and their local structural changes have been investigated by an in‐situ XAFS method. In quartz‐type crystalline GeO2, the change of the coordination number from 4 to 6 begins above 8 GPa and finishes below 12 GPa. On decompression, reversal transition begins below 8 GPa and there is a large hysteresis. Almost no sixfold coordination of Ge is preserved after releasing pressure. Change of coordination number in vitreous Li2O‐4GeO2 begins above 6 GPa and is completed below 10 GPa. Reversal transition begins below 10 GPa and the hysteresis is smaller than that of quartz‐type GeO2. Change of coordination number in vitreous Li2O‐4GeO2 is also reversal.
Bibliography:ark:/67375/WNG-XX3ZCM4T-X
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ArticleID:JSYTG5385
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ISSN:1600-5775
0909-0495
1600-5775
DOI:10.1107/S0909049500018306