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The structure of low-temperature tridymite in silica refractories

机译:硅质耐火材料中低温鳞石英的结构

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The paper presents results of investigations aimed at determining the structure of lowtemperature tridymite in refractory silica materials.In the initial phase of works, the literature and Internet databases containing structural data of crystalline compounds were reviewed in search of a model of tridymite structure which best fits the one forming in silica materials. The results of reviewing the models of polymorphous tridymite forms which are available in the world literature have been verified by Rietveld method, using a sample of silica material that contained tridymite without Cristobalite and residual quartz. On the basis of analyses it was found that tridymite in refractory silica materials occurs in a form of two low-temperature polymorphous forms C1 and F1, instead of one form - Cc, as it was assumed before.The developed model has been used in a quantitative analysis (Rietvield method) of phase composition of several silica refractories.
机译:本文介绍了旨在确定耐火硅材料中低温鳞石英的结构的研究结果。在工作的初期,回顾了包含结晶化合物结构数据的文献和Internet数据库,以寻找最适合的鳞石英结构模型一种在二氧化硅材料中形成的。 Rietveld方法已验证了审查世界文献中可得的多晶形硅藻土形式的模型的结果,使用的样品中含有无鳞石英和残余石英的硅藻土的二氧化硅材料样品。在分析的基础上发现,耐火硅材料中的鳞闪石以两种低温多晶形式C1和F1的形式出现,而不是以前假定的一种Cc形式出现。几种耐火材料的相组成的定量分析(Rietvield方法)。

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