首页> 外文期刊>International Journal of Quantum Chemistry >Pyrochlore formation, phase relations, and properties in the CaO-TiO2-(Nb,Ta)(2)O-5 systems
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Pyrochlore formation, phase relations, and properties in the CaO-TiO2-(Nb,Ta)(2)O-5 systems

机译:CaO-TiO2-(Nb,Ta)(2)O-5系统中的烧绿石形成,相关系和性质

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Phase equilibria studies of the CaO:TiO2:Nb2O5 system confirmed the formation of six ternary phases: pyrochlore (A(2)B(2)O(6)O') and five members of the (110) perovskite-slab series CanTi,Nb)(n)O3n+2, With n = 4.5, 5, 6, 7, and 8. Relations in the quasibinary Ca2Nb2O7-CaTiO3 system, which contains the Ca-n(Nb)(n)O3n+2 phases, were determined in detail. CaTiO3 forms solid solutions with Ca2Nb2O7 as well as CaNb2O6, resulting in a triangular single-phase perovskite region with corners CaTiO3-70CaTi(2)O(6):30Ca(2) Nb2O7-80CaTiO(3):20CaNb(2)O(6). A pyrochlore solid solution forms approximately along a line from 42.7:42.7:14.6 to 42.2:40.8:17.0 CaO:TiO2:Nb2O5, suggesting formulas ranging from Ca1.48Ti1.48Nb1.02O7 to Ca1.41Ti1.37Nb1.14O7 (assuming filled oxygen sites), respectively. Several compositions in the CaO:TiO2:Ta2O5 system were equilibrated to check its similarity to the mobia system in the pyrochlore region, which was confirmed. Structural refinements of the pyrochlores Ca1.46Ti1.38Nb1.11O7 and Ca1.51Ti1.32V0.04Ta1.10O7 using single-crystal X-ray diffraction data are reported (Fd3m (#227), a = 10.2301(2) angstrom (Nb), a = 10.2383(2) angstrom (Ta)), with Ti mixing on the A-type Ca sites as well as the octahedral B-type sites. Identical displacive disorder was found for the mobate and tantalate pyrochlores: Ca occupies the ideal 16d position, but Ti is displaced 0.7 A to partially occupy a ring of six 96g sites, thereby reducing its coordination number from eight to five (distorted trigonal bipyramidal). The O' oxygens in both pyrochlores were displaced 0.48 angstrom from the ideal 8b position to a tetrahedral cluster of 32e sites. The refinement results also suggested that some of the Ti in the A-type positions may occupy distorted tetrahedra, as observed in some zirconolite-type phases. The Ca-Ti-(Nb,Ta)-O pyrochlores both exhibited dielectric relaxation similar to that observed for some Bi-containing pyrochlores, which also exhibit displacively disordered crystal structures. Observation of dielectric relaxation in the Ca-Ti-(Nb,Ta)-O pyrochlores suggests that it arises from the displacive disorder and not from the presence of polarizable lone-pair cations such as Bi3+. (C) 2007 Elsevier Inc. All rights reserved.
机译:CaO:TiO2:Nb2O5系统的相平衡研究证实了六个三元相的形成:烧绿石(A(2)B(2)O(6)O')和(110)钙钛矿-平板系列CanTi的五个成员, Nb)(n)O3n + 2,n = 4.5、5、6、7和8。准二元Ca2Nb2O7-CaTiO3系统中的关系为Ca-n(Nb)(n)O3n + 2相。详细确定。 CaTiO3与Ca2Nb2O7以及CaNb2O6形成固溶体,形成具有角CaTiO3-70CaTi(2)O(6):30Ca(2)Nb2O7-80CaTiO(3):20CaNb(2)O( 6)。烧绿石固溶体大约沿42.7:42.7:14.6至42.2:40.8:17.0 CaO:TiO2:Nb2O5的线形成,表明分子式为Ca1.48Ti1.48Nb1.02O7至Ca1.41Ti1.37Nb1.14O7(假设充满氧气)网站)。平衡CaO:TiO2:Ta2O5系统中的几种成分,以检查其与烧绿石区域​​中Mobia系统的相似性,这已得到证实。报告了使用单晶X射线衍射数据对烧绿石Ca1.46Ti1.38Nb1.11O7和Ca1.51Ti1.32V0.04Ta1.10O7的结构进行了精炼(Fd3m(#227),a = 10.2301(2)埃(Nb) ,a = 10.2383(2)埃(Ta)),Ti混合在A型Ca位点和八面体B型位点上。发现mobate和钽酸盐的烧绿石具有相同的置换性紊乱:Ca占据理想的16d位置,但Ti置换0.7 A以部分占据六个96g的环,从而将其配位数从8减少至5(变形的三角双锥体)。两种烧绿石中的O'氧都从理想的8b位移至32e位的四面体簇中0.48埃。细化结果还表明,如在某些锆钛矿型相中所观察到的,A型位置的某些Ti可能占据扭曲的四面体。 Ca-Ti-(Nb,Ta)-O烧绿石均表现出与某些含Bi烧绿石相似的介电弛豫,后者也表现出位移无序的晶体结构。 Ca-Ti-(Nb,Ta)-O烧绿石中介电弛豫的观察表明,它是由位移异常引起的,而不是由极化的孤对阳离子(例如Bi3 +)的存在引起的。 (C)2007 Elsevier Inc.保留所有权利。

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