Phase boundary between rutile-type and CaCl2-type germanium dioxide determined by in situ X-ray observations

Shigeaki Ono, Kei Hirose, Norimasa Nishiyama, Maiko Isshiki

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Abstract

In situ synchrotron X-ray experiments of the GeO2 system were made at pressures of 28-45 GPa and temperatures of 300-2300 K, using a diamond anvil cell combined with a laser heating and a 6-8 type multianvil high-pressure apparatus. We observed a second-order phase transition between tetragonal rutile-type (P42/mnm) and orthorhombic CaCl2-type (Pnnm) phases under high pressure and temperature. The transition kinetics seem to have little effect on the second-order phase transition because the cell constants exhibit no discontinuities between the phases. Therefore, the phase transitions could be observed at low temperature conditions in this study. The phase boundary was determined to be P (GPa) = (34.9 ± 1.2) + (0.0086 ± 0.0024) × (T - 1300) (K).

Original languageEnglish
Pages (from-to)99-102
Number of pages4
JournalAmerican Mineralogist
Volume87
Issue number1
DOIs
Publication statusPublished - Jan 1 2002
Externally publishedYes

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All Science Journal Classification (ASJC) codes

  • Geophysics
  • Geochemistry and Petrology

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