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在钾霞石型框架中用钠部分替代钾:KNaTi(PO)₄的合成与晶体结构

Partial Substitution of Potassium with Sodium in the KTi(PO) Langbeinite-Type Framework: Synthesis and Crystalline Structure of KNaTi(PO).

作者信息

Zatovsky Igor V, Strutynska Nataliia Yu, Hizhnyi Yuriy A, Nedilko Sergiy G, Slobodyanik Nickolai S, Klyui Nickolai I

机构信息

College of Physics Jilin University 2699 Qianjin St. 130012 Changchun P. R. China.

Taras Shevchenko National University 64/13 Volodymyrska Str. 01601 Kyiv Ukraine.

出版信息

ChemistryOpen. 2018 Jun 20;7(7):504-512. doi: 10.1002/open.201800059. eCollection 2018 Jul.

DOI:10.1002/open.201800059
PMID:30003004
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6031861/
Abstract

The interaction of TiN with NaO-KO-PO melts was investigated at (Na+K)/P molar ratios of 0.9, 1.0, and 1.2 and at Na/K molar ratios of 1.0 and 2.0. Interactions in the system led to the loss of nitrogen and the partial loss of phosphorus and resulted in the formation of KTiPO and langbeinite-type K Na Ti(PO) (0.22-0.26) solid solutions over the temperature range of 1173 to 1053 K. The phase compositions of the obtained samples were determined by using X-ray diffraction (including Rietveld refinement), scanning electron microscopy (using energy-dispersive X-ray spectroscopy and element mapping), FTIR spectroscopy, and thermogravimetric analysis/differential thermal analysis. KNaTi(PO) was characterized by single-crystal X-ray diffraction [23 space group, 9.851(5) Å]. The 3D framework is built up by TiO octahedra and PO tetrahedra sharing all the oxygen vertices with the formation of cavities occupied by K(Na) cations. Only one of the two crystallographically inequivalent potassium sites is partially substituted by sodium, and this was confirmed by calculating the bond-valence sum. The thermodynamic stability of KNaTi(PO) crystals and the preferable occupation sites of Na cationic substitutions were investigated by DFT-based electronic structure calculations performed by the plane-wave pseudopotential method.

摘要

在(Na + K)/P摩尔比为0.9、1.0和1.2以及Na/K摩尔比为1.0和2.0的条件下,研究了TiN与NaO-KO-PO熔体的相互作用。该体系中的相互作用导致氮的损失以及磷的部分损失,并在1173至1053 K的温度范围内形成了KTiPO和磷钾钠石型KNaTi(PO)(0.22 - 0.26)固溶体。通过使用X射线衍射(包括Rietveld精修)、扫描电子显微镜(使用能量色散X射线光谱和元素映射)、傅里叶变换红外光谱以及热重分析/差示热分析来确定所得样品的相组成。KNaTi(PO)通过单晶X射线衍射进行表征[23空间群,9.851(5) Å]。三维骨架由TiO八面体和PO四面体构成,它们共享所有氧顶点,形成了由K(Na)阳离子占据的空穴。两个晶体学上不等价的钾位点中只有一个被钠部分取代,这通过计算键价和得到了证实。通过基于密度泛函理论(DFT)的平面波赝势方法进行的电子结构计算,研究了KNaTi(PO)晶体的热力学稳定性以及Na阳离子取代的优选占据位点。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e0af/6031861/3a093feb4196/OPEN-7-504-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e0af/6031861/ef49e7c3c22b/OPEN-7-504-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e0af/6031861/abfd7f7b4754/OPEN-7-504-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e0af/6031861/485f39155a1b/OPEN-7-504-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e0af/6031861/3ed3f681fefb/OPEN-7-504-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e0af/6031861/21d71f3f1638/OPEN-7-504-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e0af/6031861/3a093feb4196/OPEN-7-504-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e0af/6031861/ef49e7c3c22b/OPEN-7-504-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e0af/6031861/abfd7f7b4754/OPEN-7-504-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e0af/6031861/485f39155a1b/OPEN-7-504-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e0af/6031861/3ed3f681fefb/OPEN-7-504-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e0af/6031861/21d71f3f1638/OPEN-7-504-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e0af/6031861/3a093feb4196/OPEN-7-504-g006.jpg

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