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Reprobing the mechanism of negative thermal expansion in siliceous faujasite

机译:在硅质化学岩石中的负热膨胀机制

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A combination of Rietveld refinement and pair distribution function analysis of total neutron scattering data are used to provide insight into the negative thermal expansion mechanism of siliceous faujasite. The negative thermal expansion mechanism of siliceous faujasite is attributed to the transverse vibrations of bridging oxygen atoms resulting in the coupled librations of the SiO _(4) tetrahedra. The constituent SiO _(4) tetrahedra are revealed to expand in size with temperature and they are also shown to undergo some distortion as temperature is increased. However, these distortions are not distinct enough in any geometric manner for the average behaviour of the SiO _(4) tetrahedra not to be considered as that of a rigid units. The work displays the benefits of using total scattering experiments to unveil the finer details of dynamic thermomechanical processes within crystalline materials.
机译:RIETVELD改进和成对分布函数分析的组合用于总中子散射数据的洞察洞察硅质化学物质的负热膨胀机理。硅质化学物质的负热膨胀机理归因于桥接氧原子的横向振动,导致SiO_(4)四边形的偶联的SiO _(4)型偶联。组分SiO_(4)Tetrahedra被揭示以在温度下扩展尺寸,并且还显示出在温度增加的情况下进行一些扭曲。然而,这些扭曲以任何几何方式不足以以任何几何方式对于SiO _(4)Tetrahedra的平均行为不被认为是刚性单元的平均行为。该作品显示使用总散射实验的好处,揭示晶体材料中的动态热机械过程的更精细细节。

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