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:	SCOPUS: 2-s2.0-77951973296; DOI: 10.1088/1742-6596/215/1/012099;
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.
Ключевые слова:	Andersons; Compression data; Ferropericlase; High pressure; In-situ; Over-pressures; Pressure standards; Sintered diamond; Spin transition; SPring-8; Sintering; Spin dynamics; X ray diffraction; Data compression;
Издано:	2010
Физ. характеристика:	012099