Инд. авторы: | Ito E., Yoshino T., Yamazaki D., Shatskiy A.S., Shan S., Guo X., Katsura T., Higo Y., Funakoshi K. |
Заглавие: | High pressure generation and investigation of the spin transition of ferropericlase (Mg0.83Fe0.17)O |
Библ. ссылка: | Ito E., Yoshino T., Yamazaki D., Shatskiy A.S., Shan S., Guo X., Katsura T., Higo Y., Funakoshi K. High pressure generation and investigation of the spin transition of ferropericlase (Mg0.83Fe0.17)O // Journal of Physics: Conference Series. - 2010. - Vol.215. - Art.012099. - ISSN 1742-6588. - EISSN 1742-6596. |
Внешние системы: | DOI: 10.1088/1742-6596/215/1/012099; SCOPUS: 2-s2.0-77951973296; |
Реферат: | eng: High pressure generation has been tried by using the Kawai-cell equipped with sintered diamond cubes in conjunction with investigation of the spin transition in Fe2+ of (Mg0.83Fe0.17)O (ferropericlase, Fp). The Kawai-cell was squeezed in the DIA type press SPEED mkII installed at SPring-8. The volumes of the Fp and Au pressure standard were simultaneously determined by in situ X-ray diffraction using the synchrotron radiation. The maximum attainable pressure has reached 90 GPa at 300 K based on Anderson et al.'s Au scale [4]. The P-V data of (Mg0.83Fe 0.17)O were acquired at 300 K and 700 K up to 90 GPa. From detailed analysis of the compression data, it is suggested that the spin transition proceeds over pressure ranges from 50 to 70 GPa at 300 K and from 50 to 75 GPa at 700 K. © 2010 IOP Publishing Ltd.
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Ключевые слова: | X ray diffraction; Spin dynamics; Sintering; SPring-8; Spin transition; Sintered diamond; Data compression; Over-pressures; In-situ; High pressure; Ferropericlase; Compression data; Andersons; Pressure standards; |
Издано: | 2010 |
Физ. характеристика: | 012099 |