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Evidence of Hydronium Formation in Water-Chabazite Zeolite Using Inelastic Neutron Scattering Experiments and ab Initio Molecular Dynamics Simulations

机译:利用无弹性中子散射实验和AB Initio分子动力学模拟水 - 曲谱沸石中氮沸石中散水的证据

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A combined study of inelastic neutron scattering and ab initio molecular dynamics simulations has been performed in order to study the water-acid site interaction in zeolite chabazite with a ratio Si/Al = 16 that corresponds to 2 protons/uc with two different water coverages with the number of water molecules being lower and higher than that of proton sites. These results have provided a clear picture of the water-acid site interaction, and it has been demonstrated that there are two regimens of water adsorption, which depend on the water loading. (i) At low water coverage (water/acid site similar to 0.5), the main interactions between water and the zeolitic acid sites are established through hydrogen bond and there is no proton transference to water. (ii) At relatively high water loading (water/acid site similar to 3), the clustering of water molecules and hydronioum cations formed by the complete transference of the zeolitic proton to the water molecules has been observed. The formation of water-hydronium clusters interacting with oxygen atoms of the zeolite framework provides the stabilization energy needed for the protonation of water molecules confined in the cavities of chabazite. These results are the experimental evidence obtained from INS of proton transfer from the zeolitic acid site and the hydronium formation and are in agreement with a previous computational study (Phys. Chem. Chem. Phys. 2009, 11, 1702-1712) and very recent solid state NMR spectroscopy studies (J. Am. Chem. Soc. 2019, 141, 3444-3455). The inspection of the low energy bands (translational and optic modes) and librational bands of the experimental results allows obtaining information about the Hbond network of the hydronium-water cluster.
机译:已经进行了无弹性中子散射和AB初始分子动力学模拟的组合研究,以研究沸石曲谱的水酸部位相互作用,比对应于2个质子/ UC的比例,与两种不同的水覆盖物水分子的数量低于质子位点。这些结果提供了透明的水 - 酸部位相互作用的图像,并且已经证明存在两种水吸附方案,这取决于水负荷。 (i)在低水覆盖(类似于0.5)的水/酸部位),通过氢键建立水和沸石位点之间的主要相互作用,并没有对水的质子转移。 (ii)在相对高的水载荷(类似于3的水/酸部位),已经观察到通过沸石质子的完全转移到水分子形成的水分子和氢化ououm阳离子的聚类。与沸石框架的氧原子相互作用的水 - 八氢簇的形成提供了在Chabazite的腔体中被限制的水分子质量所需的稳定能量。这些结果是从沸石酸部位和氢化氢的质子转移获得的实验证据,并与先前的计算研究一致(MATH。CHEM。MATH。PHOME。7009,11,1702-1712)和最近的固态NMR光谱研究(J.IM.Chem.Soc。Soc。2019,141,3444-3455)。实验结果的低能量带(平移和光学模式)和扩展带的检测允许获得有关散水簇的Hbond网络的信息。

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