High pressure x-ray diffraction measurements on Mg2SiO4 glass

被引:25
|
作者
Benmore, C. J. [1 ,2 ]
Soignard, E. [3 ]
Guthrie, M. [1 ]
Amin, S. A. [3 ]
Weber, J. K. R. [1 ,4 ]
McKiernan, K. [2 ,3 ]
Wilding, M. C. [5 ]
Yarger, J. L. [2 ,3 ]
机构
[1] Argonne Natl Lab, Adv Photon Source, Xray Sci Div, Argonne, IL 60439 USA
[2] Arizona State Univ, Dept Phys, Tempe, AZ 85287 USA
[3] Arizona State Univ, Dept Chem & Biochem, Tempe, AZ 85287 USA
[4] Mat Dev Inc, Arlington Hts, IL 60004 USA
[5] Aberystwyth Univ, Inst Math & Phys, Aberystwyth SY23 3BZ, Dyfed, Wales
关键词
High pressure; Silicate glass; Glass structure; X-ray diffraction; Equation of state; FORSTERITE MG2SIO4; DYNAMICS; LIQUID; ATOP; MELT;
D O I
10.1016/j.jnoncrysol.2010.12.064
中图分类号
TQ174 [陶瓷工业]; TB3 [工程材料学];
学科分类号
0805 ; 080502 ;
摘要
The structure factors of Mg2SiO4 glass have been measured using high energy x-ray diffraction up to pressures of 30.2 GPa, and the equation of state measured up to 12.8 GPa. The average Mg-O coordination numbers were extracted from the experimental pair distribution functions assuming two cases (i) there is no change in Si-O coordination number with pressure and (ii) the average Si-O coordination number increases the same as for pure SiO2 glass. Both analyses give similar results and show a gradual increase in the average Mg-O coordination number from 5.0 at ambient pressure to similar to 6.6(6) at 30.2 GPa. There is good qualitative agreement between the experimental structure and equation of state data for the glass compared to several recent molecular dynamics simulations carried out on liquid Mg2SiO4. (C) 2011 Elsevier B.V. All rights reserved.
引用
收藏
页码:2632 / 2636
页数:5
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