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In situ Raman spectroscopic study of transient polyhedral distortions during cesium ion exchange into sitinakite

机译:铯离子交换到硅铁矿中的瞬时多面体畸变的原位拉曼光谱研究

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The Na-form of the synthetic counterpart of the mineral sitinakite (sitinakite-Na) was studied in situ for the ion exchange systems of Na→Cs and Na→H→Cs using time-resolved Raman spectroscopy. Raman spectral mode analysis was performed based on a comparative study of previous titanium silicate Raman spectroscopy, as well as time-resolved X-ray diffraction studies. The Raman spectrum of sitinakite can be broken down to three main groups of bending and stretching modes, respectively: Ti-O-Ti, Si-O-Ti, and O-Ti-O bends between 200 and 400 cm~(-1); and Ti-O stretch between 400 and 625 cm~(-1). During Na-form to H-form ion exchange, rapid red shifts were observed in absolute peak positions, as well as relative changes between peak positions, indicating a symmetry change. TiO_6 polyhedral groups distort as hydroxyl groups form on the TiO6 octahedra. Upon Cs exchange into the H-form, a rapid, two-step blue shift was observed for all peak positions, which indicated that the eight membered-ring becomes more circular. Upon Cs exchange into the Na-form, slow changes of peaks in the Raman spectrum indicated up to four discrete polyhedral distortions during ion exchange. The advantage of Raman spectroscopy in this study was the observation of transient polyhedral distortions for the initial swelling of sitinakite while immersed in deionized H_2O and during H and Cs ion exchange in the crystal structure. Previous X-ray diffraction studies were not of sufficient resolution to model H_2O swelling effects and framework polyhedral distortions during ion exchange, thus Raman spectroscopy offers a complementary tool to measure changes in framework geometry in situ during ion exchange. The results presented here are directly relevant to other ion exchange research on titanium silicates, zirconium silicates, aluminum silicates, and aluminum phosphates. Additionally this work shows the usefulness of in operando experiments, conducted in deliberately variable environments, which can monitor the molecular dynamics of a system, collect information concerning structure-response mechanisms, and capture the catalytic parameters for the reaction/process.
机译:使用时间分辨拉曼光谱法,就Na→Cs和Na→H→Cs的离子交换系统原位研究了矿物西铁in石(sitinakite-Na)的合成对应物的Na型。拉曼光谱模式分析是基于对先前硅酸钛拉曼光谱的比较研究以及时间分辨X射线衍射研究而进行的。硅铁矿的拉曼光谱可分为三个主要的弯曲和拉伸模式组:200-400 cm〜(-1)的Ti-O-Ti,Si-O-Ti和O-Ti-O弯曲; Ti-O在400至625 cm〜(-1)之间拉伸。在从Na型到H型的离子交换过程中,在绝对峰位置以及峰位置之间的相对变化中观察到快速的红移,表明对称性变化。 TiO_6多面体基团随着TiO6八面体上形成的羟基而变形。当Cs交换为H型时,对于所有峰位置均观察到快速的两步蓝移,这表明八个成员环变得更圆。当Cs交换成Na形式时,拉曼光谱中峰的缓慢变化表明在离子交换过程中多达四个离散的多面体畸变。拉曼光谱法在这项研究中的优势是可以观察到瞬态多面体畸变,可用于浸泡在去离子水H_2O中以及在晶体结构中进行H和Cs离子交换时,锡铁矿的初始溶胀。以前的X射线衍射研究尚不足以模拟离子交换过程中H_2O的溶胀效应和骨架多面体变形,因此拉曼光谱法提供了一种补充工具,可在离子交换过程中现场测量骨架几何形状的变化。本文介绍的结果与其他有关硅酸钛,硅酸锆,硅酸铝和磷酸铝的离子交换研究直接相关。此外,这项工作还展示了在有意变化的环境中进行操作实验的有用性,该实验可以监控系统的分子动力学,收集有关结构响应机制的信息,并捕获反应/过程的催化参数。

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