Über Das System Ba2Sm0,67U1−xWxO6

On the System Ba₂Sm _0.67U_1?xW_xO₆ The ordered perovskites Ba₂Sm_0.67UO₆ and Ba₂Sm_0.67 WO₆ are forming a complete serie of solid solutions with 4 formula units Ba₂Sm_0.67U_1?xW_xO₆ in the unit cell. By diffuse reflectance and i.r.-spectroscopic measurements the relations between color and constitution are shown.     

Über die Polymorphie der Perowskite Ba2SE0,67WVIO6. II. Die Systeme Ba2Nd0,67(1−x) Y0,67xWO6 und Ba2Nd0,67W1−xUxO6

Polymorphism of Perovskite Compounds Ba₂SE_0.67W^VIO₆. II. The Systems Ba₂Nd_0.67(1?x)Y_0.67xWO₆ and Ba₂Nd_0.67W_1?xU_xO₆ In the system Ba₂Nd_0.67(1?x)Y_0.67xWO₆ the formation of a continuous series of mixed crystals with cubic 1:1 ordered perovskite structure is observed. The existence of a hexagonal modification is confined to the Y-rich side (x ≥ 0,9). In the Ba₂Nd_0.67W_1?xU_xO₆ series only for x ? 0,25 homogeneous cubic perovskites are obtained. In contrast to systems with other rare earths the Nd series show uncommon optical properties.     

Über die Eigenschaftsänderungen beim Einbau von Tav in Ba2Gd0,67UO6

The Variation of Properties by Incorporation of Ta^v in Ba₂Gd_0.67UO₆ In Ba₂Gd□_0.33U^VIO₆ the complete substitution of U^VI by Ta^V is only possible by filling up the gadolinium vacancies (Ba₂Gd_0.67+0.33xU_1?xTa_xO₆), whereas in the series Ba₂Gd_0.67U_1?yTa_yO_6–0.5y the phase boundary is reached with y = 0.1. Depending on x the variation of the properties is studied by X-ray and spectroscopic methods.     

Über Geordnete Perowskite mit Kationenfehlstellen. II. Der Ersatz von UVI durch NbV in Ba2Gd0,67□0,33UO6

On Ordered Perovskites with Cationic Vacancies. II. The Incorporation of Nb^V in Ba₂Gd_0,67□_0,33UO₆ In Ba₂Gd_0.67□_0.33UO₆ a complete substitution of U^VI by Nb^V is possible by filling the cationic vacancies (x-phase: Ba₂Gd_0.67+0.33xU_1?xNb_xO₆). For the y-Phase (Ba₂Gd_0.67U_1?yNb_yO_6?0.5y) solid solutions are formed only for y ? 0.5. The properties of both phases are studied by x-ray and spectroscopic methods. In Ba₂GdNbO₆ – in contrary to the complete ordered Ba₂GdTaO₆ – the order of gadolinium and niobium id partial.     

Gibt es „Wolframylgruppierungen”︁? Über Perowskitphasen im System Ba2Y0,67UO6?Ba2CaWO6

Do ? Wolframyl Groups ”? Exist? On Perovskite Phases in the System Ba₂Y_0,67UO₆ ? Ba₂CaWO₆ In the system Ba₂Y_{0.67(1? x)}Ca_xU_{1? x}W_xO₆ a solid solution series is formed up to x ? 0.85. The properties are studied by x-ray and spectroscopic methods.     

Über Perowskitphasen des Systems Ba2Y0,67U1−xWxO6

On Perovskite Phases of the System Ba₂Y_0,67U_1?xW_xO₆ A solid solution series is formed between the polymorphic perovskites Ba₂Y_0.67UO₆ and Ba₂Y_0.67WO₆ (cubic: a = 8.37₂ Å; hexagonal: a = 4× 5.88₁ Å and c = 4× 7.77₈ Å). The structure is cubic between x = 0.1 and 0.99 and for x > 0.95 hexagonal as well. Strong deviations from the ideal behaviour are detectabel with spectroscopic methods. The shape of the UO₆ and WO₆ octahedrons experiences only minor changes within the series.     

Beiträge zur Chemie der Halogensilan-Addukte. XII. 1,10-Phenanthrolin-N-Oxid-Komplexe von Halogensilanen

On Perovskite Phases in the Systems AO? SE₂O₃? UO_2,x with A =Alkaline Earth Metal and SE = Rare Earths, La and Y. X. The Systems Ba₂CaUO₆? Ba₂CaUO₆? Ba₂Lu_0.67UO₆ and Ba₂SrUO₆? Ba₂Lu_0.67UO₆ In the systems Ba₂B_1?xLu_0,67x UO₆ with B^II = Ca, Sr at the B-rich side rhombic and at the Lu-rich side monoclinic perovskites are formed. The transition is discontinuous and accompanied by order-disorder phenomena.     

Über Perowskitphasen in den Systemen AO-SE2O3-UO2,x mit A = Erdalkali und SE = Seltene Erden,La sowie Y. VI. IR-spektroskopische Untersuchungen an den Verbindungen Ba2SE0,67UO6 und Ba2SE0,67UO5,5

On Perovskite Phases in the Systems AO? SE₂O₃? UO_2,x with A=Alkaline Earth Metal and SE = Rare Earths, La and Y. VI. I.R. spectroscopical Investigations at the Compounds Ba₂SE_0,67UO₆ and Ba₂SE_0,67UO_5,5 According to the results of the i.r. spectroscopic investigations longer and shorter U? O-distances can be distinguished. The HT- and LT-modifications of Ba₂SE_0,67UO₆ contain UO-groups like other ternary uranium oxides. In the O-modifications these groups are only incompletely formed. On the contrary the perovskites Ba₂SE_0,67UO_5,5 with U(V) show two different longer U? O-bonds only.     

Über das System Ba2Zn1−xCuxUO6 — ein schwingungsspektroskopischer Nachweis des Jahn-Teller-Effekts

On the System Ba₂Zn_1?xCu_xUO₆. A Vibrational Spectroscopic Proof of the Jahn Teller Effect The ordered perovskites Ba₂ZnUO₆ (cubic, space group Fm3m) and Ba₂CuUO₆ (tetragonal, space group I₄/mmm) form solid solutions. For small Cu content the lattice symmetry is cubic, with x ≥ 0.25 an increasing tetragonal distortion (c/a √2 > 1) is observed. From the vibrational spectra and in accordance with the factor group analysis the symmetry of the UO₆ octahedra is for small Cu content O_h and on the Cu-rich side D_4h. In the region of the lattice vibrations (T₂ field) the lifting of the degeneracy — due to the Jahn Teller effect of Cu²⁺ — leads to a band separation, which decreases with sinking copper content. Therefore the Jahn Teller effect is easily noticeable with vibrational spectroscopic methods. In the corresponding series with W^VI the vibrational spectroscopic investigations lead qualitatively to the same results as in the U^VI system. As further examples the stacking polytypes Ba₂ZnTeO₆ and Ba₂CuTeO₆ are considered. The vibrational spectra show, that the Jahn Teller effect in this lattice, which is strengthened by partial face-sharing of octahedra, is less pronounced than in the perovskites in which only corner-sharing is present.     

Über den Einfluß von A und B auf die Bindungsverhältnisse in geordneten Perowskiten A2BB′O6. Die Systeme Ba2−xSrxCdUO6 und Ba2−xSrxZnUO6

On the Influence of A and B on the Bonding in Ordered Perovskites A₂BB′O₆. The Systems Ba_2?xSr_xCdUO₆ and Ba_2?xSr_xZnUO₆ In the systems Ba_2?xSr_xBUO₆ for B = Cd a complete substitution of Ba²⁺ by Sr²⁺ is observed, whereas with B = Zn the phase boundary is near x ? 1.25. By measurement of charge transfer and vibrational spectra the influence of the A and B nature on the properties is shown. By comparison with the corresponding Mg- and Ca-perovskites the influence of the electronic configuration (d⁰ or d¹⁰) is studied as well.     

Über Perowskitphasen in den Systemen BaO–SE2O3–UO2,x mit SE = Seltene Erden,La und Y. I. Verbindungen der Zusammensetzung Ba2SE0,67UO6 und Ba2SE0,67UO5,5

In the BaO–SE₂O₃–UO_2,x-system the formation of the polymorphic ordered perovskites Ba₂SE_0,67UO₆ ist observed. At the reduction of the former the ordered perovskites Ba₂SE_0,67UO_5,5 are formed, which contain U(V) only. According to the results of the magnetic and spectroscopic investigations the pentavalent uranium occupies the centers of slightly or strongly distorted octahedrons, while U(VI) is partly forming UO-groups. The rare earths are always present in the trivalent state. – The structural relations to the ordered perovskite A₂BB′O₆ are discussed.     

Über Perowskitphasen in den Systemen AO?SE2O3?UO2.x mit A = Erdalkali und SE = Seltene Erden,La und Y. IV. Verbindungen der Zusammensetzung Sr2SE0,67UO5,5 und Sr2SE0,67UO6

On Perovskite Phases in the Systems AO? SE₂O₃? UO_2,x with A = Alkaline Earth Metal and SE = Rare Earths, La, and Y. IV. Compounds of the Composition Sr₂SE_0,67UO_5,5 and Sr₂SE_0,67UO₆ In the SrO? SE₂O₃? UO_2,x-system the formation of slightly monoclinic distorted rhombic perovskite phases Sr₂SEU⁵⁺O_5,5 is observed. According to the results of the spectroscopic investigations the pentavalent uranium is octahedrally surrounded by oxygen. There are three kinds of U? O-octahedrons to distinguish. By oxydation of Sr₂SE_0,67UO_5,5 the cubic perovskite phases Sr₂SE_0,67UO₆ with hexavalent uranium are obtained. – The structural relations between the perovskites A₂SE_0,67UO_5,5 and A₂SE_0,67UO₆ with A = Ba, Sr are discussed.     

Über Neue Oxoruthenate vom Typ der 6 L-Perowskite: Ba3SrRu2−xTaxO9 (x = 0,8 und 1,4) mit einem Beitrag über Ba3CaRu2O9

On Novel Oxoruthenates of the 6 L-Perovskite Type: Ba₃SrRu_2?xTa_xO₉ (x = 0.8 and 1.4) with a Comment on Ba₃CaRu₂O₉ Single crystals of the phases Ba₃SrRu_2?xTa_xO₉ [(I): x = 0.8 and (II): x = 1.4] and the compound (III): Ba₃CaRu₂O₉ were prepared by a BaCl₂ flux and investigated by X-ray methods. (I)–(III) crystallizes with hexagonal symmetry space group P6 2c with lattice constants: (I) a = 6.003 Å; c = 15.227 Å; (II) a = 5.988 Å; c = 15.220 Å and (III) a = 5.891 Å; c = 14.571 Å. The crystal structures of these substances corresponds to the 6 layer perovskites with the stacking sequence (hcc)₂. All of them show a so far not described slightly distorted oxygen framework caused by the Sr²⁺ and Ca²⁺ ions.     

Über Das System Ba2Gd2/3□1/3U1−xWxO6 sowie hexagonale Perowskite vom 18-

On the System Ba₂Gd_2/3□_1/3U_1?xW_xO₆ and Hexagonal Perovskites of an 18-Layer Type In the system Ba₂Gd_2/3□_1/3U_1?xW_xO₆ the formation of a continuous solid solution series is observed. With x ? 0.9 the mixed crystals have a cubic 1:1 ordered perovskite structure. With x ≥ 0.95 the compounds are polymorphic: besides an cubic 1:1 ordered perovskite type for x = 0.95; 0.99 and 1.00 one hexagonal layer structure exists. This lattice is in all cases rhombohedral (space group R3 m) and represents an 18 L-type. Likewise the compounds Ba₂B□_1/3W^VIO₆ with B^III = Tb-Lu and Y belong to the 18 L-type.     

Determination of oxygen in ternary uranium oxides by a gravimetric alkaline earth addition method

The applicability of a gravimetric method based on alkaline earth metal addition for the determination of oxygen in ternary uranium oxides of the type M—U—O (M=La, Ce and Th) is described. The oxide sample is mixed with MgO or Ba_2.8UO_5.8 and heated in air under suitable conditions. Because uranium is completely oxidized to the hexavalent state during the reaction, oxygen can be determined from the weight change. Oxygen in La_yU_1-y O_2+x is determined up to y = 0.8 with a standard deviation for x of ±0.006 with MgO. For Th_yU_1-y O_2+x, the value of x is determined with Ba_2.8UO_5.8 with a standard deviation of ±0.01 at y = 0.8. For Ce_yU_1-y O_2+x, the method can be applied only for low cerium concentrations where y = 0–0.2; the value for x with Ba_2.8UO_5.8 at y = 0.2 showed a standard deviation of ±0.002.     

Synthesis and Structure of the new Fluoride Bromide Ba6.668(2)Ca0.332(2)F12Br2 and Solid Solutions with Composition Ba7−xCaxF12(ClyBr1−y)2 with x = ∼0.5, 0 < y < 1

Crystals of the chemical composition Ba₇F₁₂Cl₂ were modified by adding a small amount of Ca²⁺ to allow the synthesis of the corresponding bromine compound Ba^[Ca]₇F₁₂Br₂. These samples were prepared in a NaBr flux and characterized by single crystal x‐ray diffraction. The new structure crystallizes in a disordered arrangement in the hexagonal space group P6₃/m (176). The calcium ion has a coordination number of 6. Solid solutions on the heavy halide position can be synthesised in a NaCl/NaBr flux to obtain the compounds Ba_7?xCa_xF₁₂(Cl_yBr_1?y)₂ with x = ～0.5 and 0 < y < 1. Regardless the amount of calcium used in the preparation process, the Ca stoichiometry in the compound is always between 0.3 and 0.5. The lattice parameters differ depending on the Ca‐ and Br‐content between 1053.81(5) ? a = b ? 1058.93(3) pm and 421.21 ? c ? 426.78(3) pm.     

Zur Kenntnis der Fluoride zweiwertiger Lanthanoide. III. Neue Fluoroperowskite vom Typ CsLn1−xLn′xF3 und RbLn1−xLn′xF3 mit Ln = Eu2+ bzw. Sm2+ und Ln′ = Yb2+

On Fluorides of Divalent Lanthanoids. III. New Fluoroperovskites of the MLn_1?xLn′_xF₃ Type with M = Cs, Rb; Ln = Eu²⁺, Sm²⁺; Ln′ Yb²⁺ New fluoroperovskites with divalent lanthanoids have been prepared. They are: CsEu_1?xYb_xF₃, yellow, with x = 0.25, a = 4.737(1) Å; x = 0.50, a = 4.696(1) Å; x = 0.75, a = 4.653(1) Å; CsSm_xYb_1?xF₃, violet, with x = 0.25, a = 4.656(1) Å; x = 0.18, a = 4.645(1) Å, the latter mixed with Sm_0.68Yb_0.32F₃, a = 5.781(1) Å; RbEu_xYb_1?xF₃, orange, with x = 0.25, a = 4.573(1) Å; x = 0.23, a = 4.568(1) Å, the latter mixed with Eu_0.94Yb_0.06F₂, a = 5.827(1) Å; RbSm_0.13Yb_0.87F₃, brown, a = 4.555(1) Å.     

Über Perowskitphasen in den Systemen BaO–SE2O3–UO2,x mit SE = Seltene Erden,La und Y. II. Verbindungen der Zusammensetzung Ba2(SE0,67U0,33)UO6,17

In the BaO–SE₂O₃–UO_2.x system the formation of the compounds Ba₂(SE_0,67U_0.33)UO_6.17 is observed. They crystallize in a pseudocubic ordered perovskite lattice, and contain tetravalent and pentavalent uranium in the ratio 1:3. Their magnetic and spectroscopic properties are reported.     

Synthese,Kristallstruktur und festkörper‐NMR‐spektroskopische Untersuchung neuer Oxonitridosilicate der Mischkristallreihe Ba4−xCaxSi6N10O

The new oxonitridosilicates Ba_4?xCa_xSi₆N₁₀O have been synthesized by means of high‐temperature synthesis in a radio‐frequency furnace, starting from calcium, barium, silicon diimide and amorphous silicon dioxide. The maximum reaction temperature was at about 1450 °C. The solid solution series Ba_4?xCa_xSi₆N₁₀O with a phase width 1.81 ≤ x ≤ 2.95 was obtained. The crystal structure of Ba_1.8Ca_2.2Si₆N₁₀O was determined by X‐ray single‐crystal structure determination (P2₁3, no. 198), a = 1040.2(1) pm, Z = 4, wR2 = 0.082). It can be described as a highly condensed network of corner‐sharing SiN₄ and SiON₃ tetrahedra, the voids of which are occupied by the alkaline earth ions. The structure is isotypic with that of BaEu(Ba_0.5Eu_0.5)YbSi₆N₁₁. In the ²⁹Si solid‐state MAS‐NMR spectrum two isotropic resonances at ?50.0 and ?53.6 ppm were observed.     

Über die Polymorphie der Wolframperowskite Ba2SE0,67WO6

Polymorphism of Tungsten Perovskite Compounds Ba₂SE_0,67WO₆ The compounds Ba₂SE_0,67WO₆ with SE = Gd? Lu are polymorphic. Above 1200°C the instable cubic modification (ordered perovskit with 4 formula units Ba₂SE_0,67□_0,33WO₆ per cell) transforms irreversibly into a hexagonal modification with completely filled cationic lattice. For Ba₂Eu_0,67WO₆ the transformation is incomplete. With SE = Nd and Sm only the cubic modification is formed.