Anomalous behavior of cristobalite in helium under high pressure

• Published in: Physics and chemistry of minerals Vol. 40; no. 1; pp. 3 - 10
• Main Authors: Sato, Tomoko, Takada, Hiroto, Yagi, Takehiko, Gotou, Hirotada, Okada, Taku, Wakabayashi, Daisuke, Funamori, Nobumasa
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer-Verlag 01-01-2013
• Subjects: Crystallography and Scattering Methods; Earth and Environmental Science; Earth Sciences; Geochemistry; Mineral Resources; Mineralogy; Original Paper; Interstitial void; New phase of cristobalite; Small gas atom; Dissolution of helium; Silica
• ISSN: 0342-1791; 1432-2021
• DOI: 10.1007/s00269-012-0540-x

We have investigated the high-pressure behavior of cristobalite in helium by powder X-ray diffraction. Cristobalite transformed to a new phase at about 8 GPa. This phase is supposed to have a molar volume of about 30 % larger than cristobalite, suggesting the dissolution of helium atoms in its interstitial voids. On further compression, the new phase transformed to a different phase which showed an X-ray diffraction pattern similar to cristobalite X-I at about 21 GPa. On the other hand, when the new phase was decompressed, it transformed to another new phase at about 7 GPa, which is also supposed to have a molar volume of about 25 % larger than cristobalite. On further decompression, the second new phase transformed to cristobalite II at about 2 GPa. In contrast to cristobalite, quartz did not show anomalous behavior in helium. The behavior of cristobalite in helium was also consistent with that in other mediums up to about 8 GPa, where the volume of cristobalite became close to that of quartz. These results suggest that dissolution of helium may be controlled not only by the density (amount of voids) but also by the network structure of SiO
4
tetrahedra (topology of voids).