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Structural characterisation of high-temperature K-exchanged sodalite

机译:高温钾交换方钠石的结构表征

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摘要

The exchange reaction of Na-sodalite with KCl was studied by means of high-temperature X-ray powder diffraction, ex-situ and in-situ, up to 800℃. The powder data were fully refined with the Rietveld method and showed that a substantial amount of K enters the structure in the same crystallographic position of Na, causing some Cl ions to be displaced from their position. The paper shows that sodalite is a potentially good matrix for trapping alkaline metal ions from the electrorefining process of nuclear waste and proposes a method to quickly estimate the amount of K in the structure.
机译:用高温X射线粉末衍射法(最高温度为800℃)进行了异位和原位研究钠钠与KCl的交换反应。用Rietveld方法对粉末数据进行了完全精炼,结果表明大量的K以相同的Na晶体位置进入结构,从而导致一些Cl离子从其位置移位。本文表明,方钠石是一种潜在的良好基质,可用于捕集核废料电精炼过程中的碱金属离子,并提出了一种快速估算结构中K量的方法。

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