High-pressure phase transformation of the silicon clathrate Si136

被引:59
作者
Ramachandran, GK [1 ]
McMillan, PF
Deb, SK
Somayazulu, M
Gryko, J
Dong, JJ
Sankey, OF
机构
[1] Arizona State Univ, Dept Chem & Biochem, Tempe, AZ 85287 USA
[2] Arizona State Univ, Ctr Solid State Sci, Tempe, AZ 85287 USA
[3] Arizona State Univ, Dept Phys & Astron, Tempe, AZ 85287 USA
[4] Carnegie Inst Washington, Geophys Lab, Washington, DC 20005 USA
关键词
D O I
10.1088/0953-8984/12/17/308
中图分类号
O469 [凝聚态物理学];
学科分类号
070205 ;
摘要
The compressional behaviour of a new expanded form of silicon, the cubic Si-136 clathrate, is studied by energy dispersive x-ray diffraction in a diamond anvil cell experiment. The ambient temperature bulk modulus and its pressure derivative are determined to be K-0 = 90(3) GPa and K-0' = 5.2(8), in agreement with LDA theoretical calculations. At pressures between 8 and 10 GPa, the structure transforms into the thermodynamically stable beta-Sn phase. This behaviour is analogous to that of diamond-structured silicon. However, the metastable transition from Si-136 to the beta-Sn structure should occur at a much lower pressure (3-4 GPa), from consideration of free energy-pressure relations. The observation can be related to the absence of a convenient low-energy pathway for the IV- to VI-fold coordination change involved in the transition from Si-136 to beta-Sn.
引用
收藏
页码:4013 / 4020
页数:8
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