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首页> 外文期刊>Inorganic Chemistry: A Research Journal that Includes Bioinorganic, Catalytic, Organometallic, Solid-State, and Synthetic Chemistry and Reaction Dynamics >Structure Determination and Time-Resolved Raman Spectroscopy of Yttrium Ion Exchange into Microporous Titanosilicate ETS-4
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Structure Determination and Time-Resolved Raman Spectroscopy of Yttrium Ion Exchange into Microporous Titanosilicate ETS-4

机译:钇离子交换进入微孔钛硅酸盐ETS-4的结构测定和时间分辨拉曼光谱

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The ion exchange of yttrium, one of the five most critical rare-earth elements as, outlined by the U.S. Department of Energy, into ETS-4 is a dynamic, multistep ion exchange process. The ion exchange process was followed using in situ time-resolved Raman spectroscopy, and the crystal structures of the pre-exchange and post-exchange forms were determined by single-crystal X-ray diffraction. In situ Raman spectroscopy is an ideal tool for this type of study, as it measures the spectral changes that are a result of molecular geometry changes at fast time intervals, even where symmetry and unit volume changes are minimally detected by X-ray diffraction. By tracking the stepwise changes in the peak positions and intensities in the spectra, where we focused primarily on the strong spectral features corresponding to titania quantum wires and three-membered-ring bending and breathing modes, we constructed molecular models to explain the changes in the Raman spectrum during ion exchange. The multistep ion exchange process started with rapid absorption of Y into the Na2 site, causing titania quantum wires to kink. After this initial uptake, the exchange process slowed, likely caused by hydration coordination changes within the channels. Next, Y exchange accelerated again, during which time the Y site moved closer to the framework O-2(-). Crystal structures of the maximal Y exchanged ETS-4 material were determined and confirmed the splitting of the Y site. Inductively coupled plasma optical emission spectroscopy was also used to quantify the extent of Y exchange and to measure if there were indications of titania leaching from the framework.
机译:由美国能源部概述,钇是五个最关键的稀土元素之一的离子交换到ETS-4的过程是动态的,多步的离子交换过程。使用原位时间分辨拉曼光谱仪跟踪离子交换过程,并通过单晶X射线衍射确定交换前和交换后形式的晶体结构。原位拉曼光谱法是进行此类研究的理想工具,因为它可以测量由于分子几何学在快速的时间间隔内变化而导致的光谱变化,即使在对称性和单位体积变化很少被X射线衍射检测到的情况下。通过跟踪光谱中峰值位置和强度的逐步变化,我们主要关注对应于二氧化钛量子线和三元环弯曲和呼吸模式的强光谱特征,我们构建了分子模型来解释离子交换过程中的拉曼光谱。多步离子交换过程开始于将Y快速吸收到Na2位置,导致二氧化钛量子线扭结。在最初吸收之后,交换过程变慢了,这很可能是由于通道内的水合作用变化引起的。接下来,Y交换再次加速,在此期间Y位置移近框架O-2(-)。确定了最大的Y交换ETS-4材料的晶体结构,并确认了Y位点的分裂。电感耦合等离子体发射光谱也用于量化Y交换的程度,并测量是否有迹象表明二氧化钛从框架中浸出。

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