Crystal structure and compressibility of magnesium chloride heptahydrate found under high pressure

被引:0
|
作者
Yamashita, Keishiro [1 ,2 ,3 ]
Komatsu, Kazuki [1 ]
Hattori, Takanori
Machida, Shinichi [4 ]
Kagi, Hiroyuki [1 ]
机构
[1] Univ Tokyo, Geochem Res Ctr, Grad Sch Sci, Hongo 7-3-1,Bunkyo ku, Tokyo 1130033, Japan
[2] Univ Innsbruck, Inst Phys Chem, Innrain 52c, A-6020 Innsbruck, Austria
[3] J PARC Ctr, Japan Atom Energy Agcy, 2-4 Shirakata, Tokai, Ibaraki 3191195, Japan
[4] Neutron Sci & Technol Ctr, Comprehens Res Org Sci & Soc CROSS, IQBRC Bldg,162-1 Shirakata, Tokai, Ibaraki 3191106, Japan
基金
日本学术振兴会;
关键词
salt hydrate; high pressure; hydrogen bond; orientational disorder; isothermal compressibility; POWDER DIFFRACTION; PHASE-TRANSITIONS; ICE-VIII; X-RAY; WATER; PERFORMANCE; CALIBRATION; APPARATUS; BROMIDE; STATE;
D O I
10.1107/S205252062400903X
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
The odd hydration number has so far been missing in the water-rich magnesium chloride hydrate series (MgCl2 center dot nH(2)O). In this study, magnesium chloride heptahydrate, MgCl2 center dot 7H(2)O (or MgCl2 center dot 7D(2)O), which forms at high pressures above 2 GPa and high temperatures above 300 K, has been identified. Its structure has been determined by a combination of in-situ single-crystal X-ray diffraction at 2.5 GPa and 298 K and powder neutron diffraction at 3.1 GPa and 300 K. The single-crystal specimen was grown by mixing alcohols to prevent nucleation of undesired crystalline phases. The results show orientational disorder of water molecules, which was also examined using density functional theory calculations. The disorder involves the reconnection of hydrogen bonds, which differs from those in water ice phases and known disordered salt hydrates. Shrinkage by compression occurs mainly in one direction. In the plane perpendicular to this most compressible direction, oxygen and chlorine atoms are in a hexagonal-like arrangement.
引用
收藏
页码:695 / 705
页数:11
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