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New calcium tantalate polytypes in the system Ca2Ta2O7-Sm2Ti2O7

机译:Ca2Ta2O7-Sm2Ti2O7系统中的新钽酸钙多型

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New calcium tantalate poly types with weberite-related structures have been prepared by doping Ca2Ta2O7 with Sm2Ti2O7. Trigonal 6-layer (6T) and monoclinic 5-layer (5M) polytypes containing similar to 6 and 10 mol%, respectively of the Sm2Ti2O7 component were prepared and the structures were determined and refined using S-ray data on flux-grown single crystals. The 6T phase, Ca1.89Ta1.86Sm0.16Ti0.10O7, has a = 7.353(1), c = 36.264(1) Angstrom, Z = 12, space group P3(1), and the 5M phase, Ca1.80Ta1.80Sm0.24Ti0.17O7 has a = 12.763(1), b = 7.310(1), c = 30.190(1) Angstrom, beta = 94.09 degrees(1), Z = 20, space group C2. The 6T structure is related to the 3T weberite structure, having a cubic close packed metal atom array as in fluorite and a stacking of (001) metal atom layers (={111}(f)) that alternately have the composition Ta3Ca and Ca3Ta. Hexagonal tungsten bronze type layers of corner-connected octahedra are interconnected by isolated TaO6, octahedra in the Ca3Ta layers, giving an octahedral framework of composition [Ta2O7](4-) in which the eight- coordinated calcium atoms are distributed. The octahedra in the Ca3Ta layers have only four anions involved in corner sharing. The different weberite polytypes are distinguished by the geometry of the two terminal anions, cis- or trans. In the 6T structure there is an alternation of cis- and trans- octahedra in successive Ca3Ta layers. The 5M polytype differs from the weberite polytypes in having regular twinning of the metal atom lattice on (001), giving a stacking sequence hccchccccc.... The c-stacked blocks alternatively have the weberite and pyrochlore structures, with ordering of Sm into the Ca sites in the pyrochlore blocks. (C) 2000 Acadmic Press. [References: 21]
机译:通过用Sm2Ti2O7掺杂Ca2Ta2O7,可以制备出具有与韦伯石相关结构的新型钽酸钙多晶类型。制备分别含有分别为6和10 mol%的Sm2Ti2O7组分的三角6层(6T)和单斜晶5层(5M)多型体,并使用助熔剂生长的单晶上的S射线数据确定和精炼结构。 6T相Ca1.89Ta1.86Sm0.16Ti0.10O7具有a = 7.353(1),c = 36.264(1)埃,Z = 12,空间群P3(1)和5M相Ca1.80Ta1。 80Sm0.24Ti0.17O7具有a = 12.763(1),b = 7.310(1),c = 30.190(1)埃,β= 94.09度(1),Z = 20,空间组C2。 6T结构与3T韦伯石结构有关,具有萤石中的立方紧密堆积的金属原子阵列和(001)金属原子层(= {111}(f))的堆叠,它们交替具有成分Ta3Ca和Ca3Ta。角连接的八面体的六角形钨青铜型层通过Ca3Ta层中的孤立的TaO6,八面体相互连接,形成了组成为[Ta2O7](4-)的八面体骨架,其中八配位的钙原子分布。 Ca3Ta层中的八面体只有四个阴离子参与角共享。不同的韦伯石多型体的特征是两个末端阴离子为顺式或反式。在6T结构中,连续的Ca3Ta层中有顺式和反式八面体的交替。 5M多型与Weberite多型的不同之处在于(001)上的金属原子晶格有规则的孪生,给出了堆积顺序hccchccccc...。c堆积的块体也具有Weberite和烧绿石结构,Sm顺序为烧绿石块中的钙位点。 (C)2000年学术出版社。 [参考:21]

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