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由氢氧化物前驱体合成钙铝石:结构形成及其表面活性位点

Mayenite Synthesis from Hydroxide Precursors: Structure Formation and Active Sites on Its Surface.

作者信息

Kapishnikov Aleksandr V, Kenzhin Roman M, Koskin Anton P, Volodin Alexander M, Geydt Pavel V

机构信息

Laboratory of Functional Diagnostics of Low-Dimensional Structures for Nanoelectronics, Department of Physics, Novosibirsk State University, Pirogova Str., 2, 630090 Novosibirsk, Russia.

Federal Research Center Boreskov Institute of Catalysis, Siberian Branch of the Russian Academy of Sciences, Prospekt Lavrentieva, 5, 630090 Novosibirsk, Russia.

出版信息

Materials (Basel). 2022 Jan 20;15(3):778. doi: 10.3390/ma15030778.

Abstract

We studied the formation process of a mayenite structure from hydroxide precursors in different gas media. According to X-ray diffraction data, this method allows a well-crystallized mayenite (CaAlO or C12A7) phase to be obtained at low (500-900 °C) temperatures with an insignificant impurity of CaO. It was shown that the lattice parameters for C12A7 obtained in an inert atmosphere (Ar) were lower when compared with similar samples in the air. These results can be explained by the different levels of oxygen nonstoichiometry in the resulting phase. We noted that sintering and crystallization of mayenite proceeds at lower temperatures in Ar than in the air medium. We found the presence of donor and acceptor active sites on the surface of mayenite, which was detected by the spin probe method. The specific (per unit surface) concentration of such sites (2.5 × 10 m and 1.5 × 10 m for donor and acceptor sites, respectively) is comparable to that of γ-AlO, which is traditionally used as catalyst support. This allows it to be used in adsorption and catalytic technologies, taking into account its high specific surface area (~30-50 m/g at a low synthesis temperature).

摘要

我们研究了在不同气体介质中由氢氧化物前驱体形成钙铝石结构的过程。根据X射线衍射数据,该方法能够在低温(500 - 900°C)下获得结晶良好的钙铝石(CaAlO或C12A7)相,且氧化钙杂质含量极少。结果表明,与在空气中获得的类似样品相比,在惰性气氛(Ar)中获得的C12A7的晶格参数更低。这些结果可以用所得相中不同水平的氧非化学计量来解释。我们注意到,钙铝石在Ar中的烧结和结晶温度比在空气介质中更低。我们通过自旋探针法发现钙铝石表面存在施主和受主活性位点。这些位点的比(每单位表面积)浓度(施主位点和受主位点分别为2.5×10 m和1.5×10 m)与传统用作催化剂载体的γ - AlO相当。考虑到其高比表面积(在低合成温度下约为30 - 50 m/g),这使得它可用于吸附和催化技术。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/57d1/8836596/23a0f843f52c/materials-15-00778-g001.jpg

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