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Toward Increasing Micropore Volume between Hybrid Layered Perovskites with Silsesquioxane Interlayers

机译:跨越杂交层状钙酸盐与Silsesquioxane中间层之间的微孔体积增加

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Hybrid organic–inorganic layered perovskites are typically nonporous solids. However, the incorporation of silsesquioxanes with a cubic cage structure as interlayer materials creates micropores between the perovskite layers. In this study, we increase in the micropore volume in layered perovskites by replacing a portion of the silsesquioxane interlayers with organic amines. In the proposed method, approximately 20% of the silsesquioxane interlayers can be replaced without changing the layer distance owing to the size of the silsesquioxane. When small amines (e.g., ethylamine) are used in this manner, the micropore volume of the obtained hybrid layered perovskites increases by as much as 44%; when large amines (e.g., phenethylamine) are used, their micropore volume decreases by as much as 43%. Through the variation of amine fraction, the micropore volume can be adjusted in the range. Finally, the magnetic moment measurements reveal that the layered perovskites with mixed interlayers exhibit ferromagnetic ordering at temperature below 20 K, thus indicating that the obtained perovskites maintain their functions as layered perovskites.
机译:杂种有机无机层状钙钛矿通常是无孔固体。然而,作为层间材料的立方笼结构结合Silsesquioxanes,在钙钛矿层之间产生微孔。在这项研究中,通过用有机胺取代一部分Silsesquio烷夹层,我们在层状钙锌矿中增加微孔体积。在所提出的方法中,可以在不改变由于Silsesquioxane的尺寸而改变层距离的情况下更换大约20%的倍半硅氧烷中间层。当以这种方式使用小胺(例如,乙胺)时,所得杂合层状钙酸盐的微孔体积增加高达44%;当使用大胺(例如,苯甲胺)时,它们的微孔体积减少多达43%。通过胺馏分的变化,可以在范围内调节微孔体积。最后,磁矩测量表明,具有混合中间层的层状钙酸盐在低于20k的温度下表现出铁磁性排序,从而表明所获得的钙酸盐保持其作为层状钙锌矿的功能。

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