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镧锶锗酸镧电解质磷灰石中的拟单相转变 2A-->2M-->2H。

Pseudomorphic 2A--> 2M--> 2H phase transitions in lanthanum strontium germanate electrolyte apatites.

机构信息

Nanyang Technological University, School of Materials Science and Engineering, 50 Nanyang Avenue, 639798, Singapore.

出版信息

Dalton Trans. 2009 Oct 21(39):8280-91. doi: 10.1039/b907704a. Epub 2009 Aug 24.

DOI:10.1039/b907704a
PMID:19789780
Abstract

Apatite-like materials are of considerable interest as potential solid oxide fuel cell electrolytes, although their structural vagaries continue to attract significant discussion. Understanding these features is crucial both to explain the oxide ion conduction process and to optimise it. As the composition of putative P6(3)/m apatites with ideal formula [A(I)(4)][A(II)(6)][(BO(4))(6)]X is varied the [A(I)(4)(BO(4))(6)] framework will flex to better accommodate the [A(II)(6)X(2)] tunnel component through adjustment of the A(I)O(6) metaprism twist angle (varphi). The space group theory prescribes that framework adaptation during phase changes must lead to one of the maximal non-isomorphic subgroups of P6(3)/m (P2(1), P2(1)/m, P1[combining macron]). These adaptations correlate with oxygen ion conduction, and become crucial especially when the tunnels are filled by relatively small ions and/or partially occupied, and if interstitial oxygens are located in the framework. Detecting and completely describing these lower symmetry structures can be challenging, as it is difficult to precisely control apatite stoichiometry and small departures from the hexagonal metric may be near the limits of detection. Using a combination of diffraction and spectroscopic techniques it is shown that lanthanum strontium germanate oxide electrolytes crystallise as triclinic (A), monoclinic (M) and hexagonal (H) bi-layer pseudomorphs with the composition ranges: [La(10-x)Sr(x)][(GeO(4))(5+x/2)(GeO(5))(1-x/2)][O(2)] (0 <or=x<or= 1) apatite-2A[La(10-x)Sr(x)][(GeO(4))(5+x/2)(GeO(5))(1-x/2)][O(2)] (1 <or=x<or= 2) apatite-2M[La(10-x)Sr(x)][(GeO(4))(6)][O(2)][H(delta)] (2 <or=x<or= 2.96) apatite-2M[La(10-x)Sr(x)][(GeO(4))(6)][O(2)][H(delta)] (2.96 <or=x<or= 5.32) apatite-2HFurthermore, at typical fuel cell operating temperatures apatite-2A and apatite-2M will transform to apatite-2H, with the latter showing the highest conduction. The results show that small twist angles and high symmetry enhance oxygen mobility with these properties tailored by adjusting the relative size of the framework to tunnel. This information can hence aid in the design of new materials with improved oxide ion conductivity.

摘要

磷灰石类似物作为潜在的固体氧化物燃料电池电解质具有相当大的兴趣,尽管它们的结构变化仍然引起了广泛的讨论。了解这些特征对于解释氧离子传导过程和优化氧离子传导过程至关重要。随着假定的具有理想分子式 [A(I)(4)][A(II)(6)][(BO(4))(6)]X 的 P6(3)/m 磷灰石的组成变化,[A(I)(4)(BO(4))(6)] 骨架将通过调整 A(I)O(6) 变形棱锥的扭曲角度 (varphi) 来更好地适应 [A(II)(6)X(2)] 隧道组件。群论规定,在相变过程中,骨架的适应性必须导致 P6(3)/m(P2(1)、P2(1)/m、P1[连字符]) 的最大非同构子群之一。这些适应性与氧离子传导相关,如果隧道被相对较小的离子填充并且/或者部分占据,如果间隙氧位于骨架中,则这些适应性变得尤为重要。检测和完全描述这些低对称结构可能具有挑战性,因为很难精确控制磷灰石的化学计量,并且偏离六方度量的微小偏差可能接近检测极限。使用衍射和光谱技术的组合表明,镧锶锗酸盐氧化物电解质结晶为具有组成范围的三斜 (A)、单斜 (M) 和六方 (H) 双层准同型物:[La(10-x)Sr(x)][(GeO(4))(5+x/2)(GeO(5))(1-x/2)][O(2)](0 <or=x<or= 1) 磷灰石-2A[La(10-x)Sr(x)][(GeO(4))(5+x/2)(GeO(5))(1-x/2)][O(2)](1 <or=x<or= 2) 磷灰石-2M[La(10-x)Sr(x)][(GeO(4))(5+x/2)(GeO(5))(1-x/2)][O(2)][H(delta)](2 <or=x<or= 2.96) 磷灰石-2M[La(10-x)Sr(x)][(GeO(4))(6)][O(2)][H(delta)](2.96 <or=x<or= 5.32) 磷灰石-2H此外,在典型的燃料电池工作温度下,磷灰石-2A 和磷灰石-2M 将转变为磷灰石-2H,后者表现出最高的传导性。结果表明,小的扭曲角度和高对称性通过调整骨架与隧道的相对大小来提高氧迁移率,这些特性可以通过调整来实现。这些信息可以帮助设计具有更高氧离子电导率的新材料。

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