2019年10月1日
Solid Solution and Compression Behavior of Hydroxides in the Lower Mantle
Journal of Geophysical Research: Solid Earth
- ,
- ,
- ,
- ,
- ,
- ,
- ,
- 巻
- 124
- 号
- 10
- 開始ページ
- 10231
- 終了ページ
- 10239
- 記述言語
- 英語
- 掲載種別
- 研究論文(学術雑誌)
- DOI
- 10.1029/2019JB018146
- 出版者・発行元
- American Geophysical Union ({AGU})
The high-pressure solid solution and compression behavior of hydroxides in the ternary MgSiO H -AlOOH-FeOOH system were studied at pressures of 16–60 GPa and temperatures of 300–1513 K. We applied in situ X-ray measurements in conjunction with a multianvil apparatus using sintered diamond anvils to achieve homogeneous temperature distributions within large sample volumes. Our results show that CaCl -type hydroxides form solid solutions over a wide composition range. We also observed the volume reductions in the solid solutions accompanied by a spin transition of iron at ~50 GPa, and the wide compositional ranges are maintained through this process. Consequently, water may be transported into the deep lower mantle by the hydrous CaCl -type solid solution with changing its composition depending on the chemical and thermal environments. 4 2 2 2
- リンク情報
- ID情報
-
- DOI : 10.1029/2019JB018146
- ISSN : 2169-9313
- eISSN : 2169-9356
- ORCIDのPut Code : 71513870
- SCOPUS ID : 85074597927