Intermediate states of GeO2 glass under pressures up to 35 GPa

被引:61
作者
Hong, Xinguo [1 ]
Shen, Guoyin
Prakapenka, Vitali B.
Newville, Matt
Rivers, Mark L.
Sutton, Stephen R.
机构
[1] Univ Chicago, Consortium Adv Radiat Sources, Chicago, IL 60637 USA
[2] Carnegie Inst Washington, HP CAT, Argonne, IL 60439 USA
[3] Univ Chicago, Dept Geophys Sci, Chicago, IL 60637 USA
来源
PHYSICAL REVIEW B | 2007年 / 75卷 / 10期
关键词
D O I
10.1103/PhysRevB.75.104201
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Density-driven polyamorphism of GeO2 glass under high pressure has been studied by density, x-ray scattering, and optical Raman measurements. Density data obtained by an x-ray absorption method display distinct compression behavior in different pressure regions, with rapid density increases at 5 and 10 GPa and a plateau at 6-9 GPa. Simultaneous x-ray diffraction reveals that the position of the first sharp diffraction peak (FSDP) increases nearly linearly towards higher scattering vector with pressure up to 10 GPa. Both the width of the FSDP and the Raman stretching band of Ge-O-Ge (419 cm(-1)) increase with pressure but exhibit changes in behavior at 2.5 and 7.5 GPa, indicating intermediate states exist in the glass before the collapse of local tetrahedral and pentahedral structural units, respectively. At pressures above 15 GPa, post-octahedral compression with progressive enhancement in network correlation is observed. The results indicate not only the discrete but also rotating intermediate states exist in GeO2 glass under pressures up to 35 GPa.
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页数:5
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