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首页> 外文期刊>Zeitschrift fur Anorganische und Allgemeine Chemie >A NEW STRUCTURE TYPE FOR THE RARE EARTH OXOTUNGSTATE FECE(WO4)W2O8=FECE(WO4)(3) German
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A NEW STRUCTURE TYPE FOR THE RARE EARTH OXOTUNGSTATE FECE(WO4)W2O8=FECE(WO4)(3) German

机译:稀土氧钨酸盐粪便(WO4)W2O8=粪便(WO4)(3)的新结构类型德语

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摘要

Single crystals of the hitherto unknown compound FeCe(WO4)(3) have been prepared by crystallization from melts of Fe2O3, CeO2 and WO3. It crystallizes with triclinic symmetry, space group P (1) over bar, a = 7,486(3); b = 7,528(1); c = 16,502(4) Angstrom, alpha = 101,00(2); beta = 96,62(3); gamma = 98,62 degrees; Z = 2. Tungsten shows octahedral and tetrahedral coordination by oxygen. The crystal structure is characterized by layers related to the Scheelite and Wolframite type. Thermogravimetric measurements led to a lost of oxygen during reaction. It results in a decrease of the oxidation states of Fe3+ and Ce4+ respectively, as will be discussed using magnetic measurements and calculations of the Coulomb terms of lattice energy. The structure contains a one-fold coordinated oxygen. References: 28
机译:迄今为止未知的化合物FeCe(WO4)(3)的单晶是通过Fe2O3、CeO2和WO3的熔体结晶制备的。它以三斜对称性结晶,空间群 P (1) 在棒上,a = 7,486(3);b = 7,528(1);c = 16,502(4) 埃,alpha = 101,00(2);贝塔 = 96,62(3);伽玛 = 98,62 度;Z = 2。钨在氧的作用下表现出八面体和四面体的配位。晶体结构的特征是与白钨矿和黑钨矿类型相关的层。热重测量导致反应过程中氧气损失。它导致 Fe3+ 和 Ce4+ 的氧化态分别降低,正如将使用磁性测量和晶格能库仑项的计算进行讨论的那样。该结构包含一倍配位氧。[参考文献: 28]

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