Startseite In situ X-ray observation of 10 Å phase stability at high pressure
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In situ X-ray observation of 10 Å phase stability at high pressure

  • Sergey V. Rashchenko EMAIL logo , Seiji Kamada , Naohisa Hirao , Konstantin D. Litasov und Eiji Ohtani
Veröffentlicht/Copyright: 29. Oktober 2016
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Abstract

The 10 Å phase, Mg3Si4O10(OH)2·H2O, is a high-pressure hydrous phyllosilicate considered as an important link in the succession of hydrous phases transporting water into the deep mantle. In this study, in situ synchrotron X-ray diffraction combined with external heating diamond-anvil cell was used to determine limits of the 10 Å phase stability at pressures above 7 GPa. A reaction “10 Å phase + H2O→ hydroxide-perovskite (3.65 Å phase) + stishovite” at about 10 GPa was found to be a high-pressure boundary of the 10 Å phase stability field. A dehydration temperature of the 10 Å phase “10 Å phaseenstatite + stishovite + H2O” decreases with pressure from 690 °C at 7 GPa to 450 °C at 10 GPa; a nonvariant point where 10 Å phase, hydroxide-perovskite and enstatite coexist in the presence of stishovite and hydrous fluid was found near 10 GPa and 450 °C.

Acknowledgement

The research was supported by state assignment project no. 0330-2016-0004, Russian Ministry of Education and Science [grant no. 14.B25.31.0032], Russian Science Foundation [grant no. 14-13-00834], and Japan Society for the Promotion of Science [grants nos. 22000002 and 15H5748]. The research was also supported by Japan Society for the Promotion of Science and Russian Foundation for Basic Research under the Japan-Russia Research Collaboration program. The in situ synchrotron X-ray diffraction experiments were performed under SPring-8 research proposals nos. 2014B0104 and 2015B0104. We acknowledge F. Maeda, N. Suzuki, and R. Masudo for their kind assistance in preparation of this experiment.

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Received: 2016-3-12
Accepted: 2016-7-6
Published Online: 2016-10-29
Published in Print: 2016-11-1

© 2016 by Walter de Gruyter Berlin/Boston

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