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首页> 外文期刊>ChemistryOpen >Partial Substitution of Potassium with Sodium in the K 2 Ti 2 (PO 4 ) 3 Langbeinite‐Type Framework: Synthesis and Crystalline Structure of K 1.75 Na 0.25 Ti 2 (PO 4 ) 3
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Partial Substitution of Potassium with Sodium in the K 2 Ti 2 (PO 4 ) 3 Langbeinite‐Type Framework: Synthesis and Crystalline Structure of K 1.75 Na 0.25 Ti 2 (PO 4 ) 3

机译:在K 2 Ti 2(PO 4)3中钾被钠部分取代Langbeinite型骨架:K 1.75 Na 0.25 Ti 2(PO 4)3的合成和晶体结构

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The interaction of TiN with Na 2 O–K 2 O–P 2 O 5 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 KTiP 2 O 7 and langbeinite‐type K 2? x Na x Ti 2 (PO 4 ) 3 ( x= 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. K 1.75 Na 0.25 Ti 2 (PO 4 ) 3 was characterized by single‐crystal X‐ray diffraction [ P 2 1 3 space group, a= 9.851(5)??]. The 3D framework is built up by TiO 6 octahedra and PO 4 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 K 1.75 Na 0.25 Ti 2 (PO 4 ) 3 crystals and the preferable occupation sites of Na K cationic substitutions were investigated by DFT‐based electronic structure calculations performed by the plane‐wave pseudopotential method. Melting pot : The interaction of TiN with Na 2 O–K 2 O–P 2 O 5 melts is investigated at different (Na+K)/P and Na/K molar ratios. Interactions in the system lead to the loss of nitrogen and the partial loss of phosphorus to give KTiP 2 O 7 and langbeinite‐type K 2? x Na x Ti 2 (PO 4 ) 3 ( x= 0.22–0.26) solid solutions at T =1173 to 1053?K. The obtained phosphates are fully characterized and DFT calculations confirm cation substitution.
机译: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Na 2 O–K 2 O–P 2 O 5熔体的相互作用。系统中的相互作用导致氮的流失和磷的部分流失,并导致形成KTiP 2 O 7和朗贝氏体型K 2? x Na x Ti 2(PO 4)3(x = 0.22-0.26)固溶体在1173至1053?K的温度范围内。通过X射线衍射(包括Rietveld精炼),扫描电子显微镜(使用能量色散X射线光谱和元素映射),FTIR光谱以及热重分析/差热分析确定所获得样品的相组成。 K 1.75 Na 0.25 Ti 2(PO 4)3用单晶X射线衍射表征[P 2 1 3空间群,a = 9.851(5)? 3D框架由TiO 6八面体和PO 4四面体共享所有的氧顶点并形成被K(Na)阳离子占据的腔体构成。晶体学上两个不等价的钾位中只有一个被钠部分取代,这可以通过计算键合价来确定。通过平面波pseudo势法进行的基于DFT的电子结构计算,研究了K 1.75 Na 0.25 Ti 2(PO 4)3晶体的热力学稳定性以及Na K阳离子取代的优选占据位点。熔炉:在不同的(Na + K)/ P和Na / K摩尔比下研究了TiN与Na 2 O–K 2 O–P 2 O 5熔体的相互作用。系统中的相互作用导致氮的流失和磷的部分流失,从而生成KTiP 2 O 7和朗贝氏体型K 2? x Na x Ti 2(PO 4)3(x = 0.22-0.26)固溶体,T = 1173至1053?K。所获得的磷酸盐已得到充分表征,DFT计算证实了阳离子取代。

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