Structure of Molten CaSiO3: Neutron Diffraction Isotope Substitution with Aerodynamic Levitation and Molecular Dynamics Study

被引:48
作者
Skinner, L. B. [1 ,2 ]
Benmore, C. J. [3 ]
Weber, J. K. R. [3 ,4 ]
Tumber, S. [4 ]
Lazareva, L. [1 ,2 ]
Neuefeind, J. [5 ]
Santodonato, L. [5 ]
Du, J. [6 ]
Parise, J. B. [1 ,2 ,7 ]
机构
[1] SUNY Stony Brook, Inst Mineral Phys, Stony Brook, NY 11794 USA
[2] SUNY Stony Brook, Dept Geosci, Stony Brook, NY 11794 USA
[3] Argonne Natl Lab, Xray Sci Div, Adv Photon Source, Argonne, IL 60439 USA
[4] Mat Dev Inc, Arlington Hts, IL 60004 USA
[5] Oak Ridge Natl Lab, Spallat Neutron Source, Oak Ridge, TN USA
[6] Univ N Texas, Dept Mat Sci & Engn, Denton, TX 76203 USA
[7] Brookhaven Natl Lab, Light Source Div, Upton, NY 11973 USA
关键词
ORDERED MATERIALS DIFFRACTOMETER; CALCIUM SILICATE GLASS; HIGH-TEMPERATURE; LIQUIDS; MELTS; COORDINATION; DETECTOR; SNS;
D O I
10.1021/jp3066019
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
We have performed neutron diffraction isotopic substitution experiments on aerodynamically levitated droplets of CaSiO3, to directly, extract intermediate and local structural information on the Ca environment The results show a substantial broadening of the first Ca-O peak in the pair distribution function of the melt compared to the glass, which comprises primarily of 6 and 7-fold coordinated Ca-polyhedra. The broadening can be explained by a redistribution of Ca-O bond lengths, :especially toward longer distances in the liquid. The first order neutron difference function provides a test of recent molecular dynamics simulations and supports the MD model which contains short chains or channels of edge shared Ca octahedra in the liquid state. It is suggested that the polymerization of Ca polyhedra is responsible for the fragile viscosity behavior of the melt and the glass forming ability in CaSiO3.
引用
收藏
页码:13439 / 13447
页数:9
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