High‐temperature mass spectrometric study of the vaporization processes of V2O3 and vanadium‐containing slags

A Knudsen effusion mass spectrometric method was used to study the vaporization processes and thermodynamic properties of pure V₂O₃ and 14 samples of vanadium‐containing slags in the CaO‐MgO‐Al₂O₃‐SiO₂ system in the temperature range 1875–2625 K. The system was calibrated using gold in the liquid state as the standard. Vaporization was carried out from double tungsten effusion cells. First it was shown that, in vapor over V₂O₃ and the vanadium‐containing slags in the temperature range 1875–2100 K, the following vapor species were present: VO₂, VO, O, WO₃ and WO₂, with the latter two species being formed as a result of interaction with the tungsten crucibles. The temperature dependencies of the partial pressures of these vapor species were obtained over V₂O₃ and the slags. The ion current comparison method was used for the determination of the V₂O₃ activities in slags as a function of temperature with solid V₂O₃ as a reference state. The V₂O₃ activity coefficients in the slags under investigation indicated positive deviations from ideality at 1900 K and a tendency to ideal behavior at 2100 K. It was shown that the V₂O₃ activity as a function of the slag basicity decreased at 1900 K and 2000 K and was practically constant in the slag melts at 2100 K. The results are expected to be valuable in the optimization of slag composition in high‐alloy steelmaking processes as well as for their environmental implications. Copyright © 2010 John Wiley & Sons, Ltd.     

Zur Kenntnis eines gemischtvalenten Oxochromats(III,IV): Sr4Cr3O9

About a Mixed-Valence-Oxochromate(III, IV): Sr₄Cr₃O₉ Single crystals of the hitherto unknown compound Sr₄Cr₃O₉ were prepared and examined by four circle diffractometer technique (space group C–P3, a = 9.6182; c = 7.8736 Å, Z = 3). The point positions of chromium are occupied statistically by Cr³⁺ and Cr⁴⁺. The Cr³⁺/Cr⁴⁺-coordination is partly unusual, there are one dimensional chains of CrO₆-polyhedra incorporated in a [Sr₄O₉]^10?-network.     

Schwingungsspektren und Kraftkonstanten von Chrom(VI)-Sauerstoff-Verbindungen

The infrared and RAMAN spectra of Cr₃O, CrO₄O and CrO₃ have been measured and assigned. The force constant of a modified valence force field have been calculated and compared with the force constants of CrO, Cr₂O, CrO₃F^?, CrO₃Cl^?, CrO₂F₂ and CrO₂Cl₂. The valence force constant f_CrO depends almost linearly on the distance d(CrO). The bending frequency δ(CrOCr) has to be reassigned. The unit cell parameters of α- and β-Cs₂Cr₃O₁₀ and Cs₂Cr₄O₁₃ have been determined by means of Guinier X-ray powder techniques.     

Synthese und Kristallstruktur von Terbium(III)‐meta‐Oxoborat Tb(BO2)3 (≡ TbB3O6)

Synthesis and Crystal Structure of Terbium(III) meta‐Oxoborate Tb(BO₂)₃ (≡ TbB₃O₆) The terbium meta‐oxoborate Tb(BO₂)₃ (≡ TbB₃O₆) is obtained as single crystals by the reaction of terbium, Tb₄O₇ and TbCl₃ with an excess of B₂O₃ in gastight sealed platinum ampoules at 950 °C after three weeks. The compound appears to be air‐ and water‐resistant and crystallizes as long, thin, colourless needles which tend to growth‐twinning due to their marked fibrous habit. The crystal structure of Tb(BO₂)₃ (orthorhombic, Pnma; a = 1598.97(9), b = 741.39(4), c = 1229.58(7) pm; Z = 16) contains strongly corrugated oxoborate layers {(BO₂)^‐} built of vertex‐linked [BO₄]^5‐ tetrahedra (d(B‐O) = 143 ‐ 154 pm, ?(O‐B‐O) = 102‐115°) which spread out parallel (100). The four crystallographically different Tb³⁺ cations all exhibit coordination numbers of eight towards the oxygen atoms (d(Tb‐O) = 228‐287 pm). The corresponding metal cation polyhedra [TbO₈]¹³⁺ too convene to layers (composition: {(Tb₂O₁₁)^16‐}) which are likewise oriented parallel to the (100) plane.     

Rb2Co3(H2O)2[B4P6O24(OH)2]: Ein Borophosphat mit ‐Tetraeder‐Anionenteilstruktur und Oktaeder‐Trimeren (CoO12(H2O)2)

Rb₂Co₃(H₂O)₂[B₄P₆O₂₄(OH)₂]: A Borophosphate with ‐Tetrahedral Anionic Partial Structure and Trimers of Octahedra (Co O₁₂(H₂O)₂) Rb₂Co₃(H₂O)₂[B₄P₆O₂₄(OH)₂] is formed under mild hydrothermal conditions (T = 165 °C) from mixtures of RbOH_(aq), CoCl₂, H₃BO₃, and H₃PO₄ (molar ratio 1 : 1 : 1 : 2). The crystal structure (orthorhombic system) was solved by X‐ray single crystal methods (space group Pbca, No. 61; R‐values (all data): R1 = 0.0699, wR2 = 0.0878): a = 950.1(1) pm, b = 1227.2(2) pm, c = 2007.4(2) pm; Z = 4. The anionic partial structure consists of tetrahedral [B₄P₆O₂₄(OH)₂^8–] layers, which contain three‐ and nine‐membered rings. Co^II is octahedrally coordinated by oxygen and oxygen and H₂O ligands, respectively (coordination octahedra CoO₆ and CoO₄(H₂O)₂). Three adjacent coordination octahedra are condensed via common edges to form trimeric units (CoO₁₂(H₂O)₂). The oxidation state +2 of cobalt was confirmed by magnetic measurements. The octahedral trimers are quasi‐isolated. No long‐range magnetic ordering occurs down to 2 K. Rb⁺ is disordered over three crystallographically independent sites within channels of the structure running parallel [010]; the coordination sphere of Rb⁺ is formed by nine oxygen species of the tetrahedral layers, one OH group and one H₂O molecule.     

Ein neuartiges Polyoxocobaltat(II)‐Anion in Rb2Co2O3

A New Polyoxocobaltate(II) Anion in Rb₂Co₂O₃ Rb₂Co₂O₃ was prepared via the azide/nitrate route. Mixtures of the precursors Co₃O₄, RbN₃ and RbNO₃ in the molar ratios 6:17:1 were heated in a special regime up to 450 °C and annealed at this temperature for 50 h in silver crucibles. Single crystals have been grown by subsequent annealing of prepared powder at 450 °C for 500 h in silver crucibles, which were sealed in glass ampoules under dried Ar. According to the X‐ray analysis of the crystal structure (Pnma, Z = 8, 11.729(2), 6.058 (1), 8.004(1) Å) cobalt is trigonal planar coordinated by oxygen atoms. The CoO₃‐units share through all corners and build up an infinite two‐dimensional Co₂O₃‐network.     

Die Photolumineszenz der dreiwertigen Seltenen Erden in den Perowskitstapelvarianten Ba2La2−xSE MgW2□O12, Ba6Y2−xSEW3□O18 und Sr8SrGd2−x SEW4□O24

Photoluminescence of Trivalent Rare Earths in Perovskite Stacking Polytypes Ba₂La_2?x RE MgW₂□O₁₂, Ba₆Y_2?x RE W₃□O₁₈, and Sr₈SrGd_2?xRE W₄□O₂₄ Rhombohedral 12 L stacking polytypes Ba₂La_2?xREMgW₂□O₁₂ show with RE³⁺ = Pr, Sm, Eu, Tb, Dy, Ho, Er, Tm; the 18 L stacking polytypes Ba₆Y_2?xREW₃□O₁₈ and the polymorphic perovskites Sr₈SrGd_2?xREW₄□O₂₄ with RE³⁺ = Sm, Eu, Dy, Ho, Er visible photoluminescence. The concentration dependence and the influence of the coordination number of the rare earth are reported.     

The adsorption of CO2, H2CO3, HCO3− and CO32− on Cu2O (111) surface: First‐principles study

The adsorption of CO₂, and its derivatives, H₂CO₃, HCO, and CO, on Cu₂O (111) surface has been investigated by first‐principles calculations based on the density functional theory at B3LYP hybrid functional level. The Cu₂O (111) surface has been modeled using an embedded cluster method,in which the quantum clusters plus some ab initio ion model potentials were inserted in an array of point charges. On the surface, H₂CO₃ was dissociated into an H⁺ and an HCO ion. Among the CO₂ species, HCO was the only activated species on the surface. The results suggest that the reduction of CO₂ on Cu₂O (111) surface can start from the form of HCO. © 2011 Wiley Periodicals, Inc. Int J Quantum Chem, 2011     

Sur la Stoechiométrie de la Variété Allotropique γ de Bi2O3

On the Stoichiometry of the Allotropic Variation γ-Bi₂O₃ The study of the solid solutions Bi₁₂[BBi□_1/5]O₂₀ (B^+V = As, V) with 0 ? x ? 0,80 leads for x = 0,77 to a phase whose cubic centered symmetry and parameter (10.255 Å) correspond to those previously announced for γ-Bi₂O₃. The présence of impurities seems required to obtain such a phase whose theoretical stoichiometry should be Bi₁₂[Bi□_1/5]O₂₀ i. e. Bi₂O_3,125.     

Ho2O[SiO4] und Ho2S[SiO4]: Zwei Chalkogenid‐Derivate von Holmium(III)‐ortho‐ Oxosilicat

Ho₂O[SiO₄] and Ho₂S[SiO₄]: Two Chalcogenide Derivatives of Holmium(III) ortho‐Oxosilicate Ho₂O[SiO₄] crystallizes monoclinically with the space group P2₁/c (a = 904.15(9), b = 688.93(7), c = 667.62(7) pm, β = 106.384(8)°, Z = 4) in the A‐type structure of rare‐earth(III) oxide oxosilicates. Yellow platelet‐shaped single crystals were obtained as by‐product during an experiment to synthesize Ho₃Cl[SiO₄]₂ by reacting Ho₂O₃ and SiO₂ in the ratio 4 : 6 with an excess of HoCl₃ as flux at 1000 °C for seven days in evacuated silica ampoules. Both crystallographically different Ho³⁺ cations show coordination numbers of 8+1 and 7 with coordination figures of 2+1‐fold capped trigonal prisms and octahedra, in which one of the vertices changes to an edge by two instead of one coordinating atoms, respectively. The O^2— anion not linked to silicon is surrounded tetrahedrally by four Ho³⁺ cations which built a layer parallel (100) by vertex‐ and edge‐sharing of the [OHo₄]¹⁰⁺ units according to {[(O5)(Ho1)_1/1(Ho2)_3/3]⁴⁺}. Within rhombic meshes of these layers the isolated oxosilicate tetrahedra [SiO₄]^4— come to lie. Ho₂S[SiO₄] crystallizes orthorhombically in the space group Pbcm (a = 605.87(5), b = 690.41(6), c = 1064.95(9) pm, Z = 4). It also emerged as a single‐crystalline by‐product obtained during the synthesis of Ho₂OS₂ by reaction of a mixture of Ho₂O₃, Ho and S with the wall of the evacuated silica tube used as container with an excess of CsCl as flux at 800 °C. The structure of the yellow platelet‐shaped, air and water resistant crystals also distinguishes two Ho³⁺ cations with bicapped trigonal prisms and trigondodecahedra as coordination polyhedra for CN = 8. The S^2— anions are almost square planar surrounded by four Ho³⁺ cations, but situated completely outside this plane. The [SHo₄]¹⁰⁺ squares form strongly corrugated layers perpendicular to [100] by corner‐sharing according to {[(S)(Ho1)_2/2(Ho2)_2/2]⁴⁺}. Contrary to the oxide oxosilicates the isolated oxosilicate tetrahedra [SiO₄]^4— do not lie within the rhombic meshes of these layers, but above and below the (Ho2)³⁺ cations while viewing along [100].     

Thermoanalytical study of the solid-state reactions in MgO-Cr2O3 and ZnO-Cr2O3 systems

The solid-state reactions in MgO-Cr₂O₃ and ZnO-Cr₂O₃ systems under atmospheres of oxygen, air and nitrogen were investigated by means of DTA and isothermal kinetic techniques. It was shown that the application of DTA to the solid-state reactions affords useful information with respect to the initial reaction stage: oxidation of Cr₂O₃ to CrO₃ in the presence of MgO or ZnO, followed by the formation of a thin layer of spinel, which consisted of an imperfect lattice, on the surface of the MgO or ZnO grains.     

Das Kupfer(II)‐indium‐oxidphosphat CuInOPO4 mit α‐Fe2OPO4‐Struktur,dargestellt durch die Oxidation einer Cu/In/P‐Legierung im Sauerstoffstrom

The Copper(II) Indium Oxide Phosphate CuInOPO₄ with α‐Fe₂OPO₄ Structure, prepared by Oxidation of a Cu/In/P Alloy with Oxygen Green single crystals of CuInOPO₄ (orthorhombic, Pnma, a = 774.5(1) pm, b = 661.0(1) pm, c = 730.6(1) pm, Z = 4) were prepared by reaction of Cu/In/P‐alloys with oxygen. The compound is isotypic with α‐Fe₂OPO₄. The structure contains isolated [CuO_4/2O₂]‐chains running along [010] formed by CuO₆‐octahedra which are connected by common edges. The chains are linked by phosphate groups and by [InO₄O_2/2]‐chains along [100] consisting of trans vertex connected InO₆‐octahedra.     

Collision-induced emission of O2(b1Σ → a1Δg) in the gas phase

In flow tube studies of the quenching of O₂(b¹Σ), broad band emission of O₂(b):M collision complexes was found to appear under the discrete rotational lines of the 0–0 band of the b¹Σ → a¹Δ_g electric quadrupole transition at higher oxygen pressures and on addition of foreign gases. Bimolecular rate constants for the collision-induced emission processes have been derived from the ratio of the intensities of the discrete lines and the continuum as well as from low-resolution measurements of the relative intensities of the b → a and b → X bands as a function of O₂ and added gas pressure. They range from ≈10^?21 cm³ s^?1 for He to ≈4 × 10^?19 cm³ s^?1 for PCl₃ vapor.     

LaCl(BO2)2 und Er2Cl2[B2O5]: Zwei Chlorid‐Oxoborate dreiwertiger Lanthanide

LaCl(BO₂)₂ and Er₂Cl₂[B₂O₅]: Two Chloride Oxoborates of Trivalent Lanthanides Er₂Cl₂[B₂O₅] is obtained as single crystals by the reaction of ErCl₃, Er₂O₃ and B₂O₃ with an excess of ErCl₃ as flux in evacuated silica tubes after two weeks at 850 °C. The compound crystallizes as long, pale pink needles and appears to be air‐ and water‐resistant. Single‐crystalline LaCl(BO₂)₂ emerges from the reaction of La₂O₃, LaCl₃, and B₂O₃ with an excess of B₂O₃ as flux in evacuated silica tubes after four weeks at 900 °C. LaCl(BO₂)₂ crystallizes as thin, colourless, air‐ and water‐resistant needles which tend to severe twinning due to their fibrous habit. The crystal structure of Er₂Cl₂[B₂O₅] (orthorhombic, Pbam; a = 1489.65(9), b = 1004.80(6), c = 524.86(3) pm; Z = 4) contains two crystallographically different erbium cations. (Er1)³⁺ resides in pentagonal‐bipyramidal coordination of seven anions while (Er2)³⁺ is surrounded by only six anions with the shape of an octahedron. The planar oxodiborate units [B₂O₅]^4— consisting of two vertex‐shared [BO₃]^3— triangles are isolated according to {([BOO]₂)^4—}. LaCl(BO₂)₂ crystallizes isostructurally with PrCl(BO₂)₂ in the triclinic space group P1¯ (a = 423.52(4), b = 662.16(7), c = 819.33(8) pm; α = 82.081(8), β = 89.238(9), γ = 72.109(7)°; Z = 2). The characteristic unit consists of endless chains built up by corner‐linked [BO₃]^3— triangles. These quasi‐planar zigzag chains of the composition {[(B1)OO(B2)OO]^2—} (≡ {[BO₂]^—} run parallel [100]. The La³⁺ cations exhibit coordination numbers of ten and are coordinated by three Cl^— and seven O^2— anions.     

Neutral and Cationic Hexanuclear Rhenium Phosphine Clusters with μ3‐(Phosphido‐Chalcogenido), μ3‐(Arsenido‐Chalcogenido), and μ3‐(Imido or Oxo‐Chalcogenido) Hetero Ligand Shells

Reactions of dry THF/MeCN solutions of Ca[Re₆SCl(Cl^a)₆] with silylated derivatives E(SiMe₃)₂ (E = PhAs, PSiMe₃, HN, O, S) and addition of trialkylphosphine PPr₃ afford in high yields and at room temperature either the neutral clusters [Re₆SX(PPr₃)] ( 1 : X = As, 2 : X = P) or the ionic compounds [Re₆SX(PPr₃)]²⁺ · [Re₆S₆Cl₈]^2– ( 3 : X = NH, 4 : X = O, 5 : X = S). The compounds 1 – 5 were characterised by X‐ray crystal structure analysis. A di‐substitution reaction occurs on the {Re₆SCl}⁴⁺ cluster core, where the two inner μ₃‐chloro ligands Clⁱ are substituted by X (X = As, P, NH, O, S) and all six terminal chloro ligands Cl^a are exchanged by terminal PPr₃‐ligands.     

Zur Kenntnis einer modifizierten Form des β-CuNdW2O8-Typs: γ-CuTbW2O8

On a Modified Form of the β-CuNdW₂O₈ Type: γ-CuTbW₂O₈ Single crystals of γ-CuTbW₂O₈ were prepared by flux in closed copper tubes. X-ray investigations show triclinic symmetry, space group C-P1 , with a = 6.722, b = 9.831, c = 15.352 Å, α = 72.82, β = 88.53, γ = 71.76°, Z = 6. γ-CuTbW₂O₈ is closely related to β-CuNdW₂O₈. One significant difference can be seen in an alternate staggered location of Tb³⁺ ions along [110].     

Density and surface tension of the systems CaO-FeO-Fe2O3-MgO, CaO-FeO-Fe2O3-ZnO and CaO-Fe2O3-Cu2O

The density and surface tension of melts of the systems CaO-FeO-Fe₂O₃ MgO at the temperature 1623 K, CaO-FeO-Fe₂O₃-ZnO at 1573 K, and CaO-Fe₂O₃-Cu₂O at 1573 K were determined using the maximum bubble pressure method. The molar volume, the excess molar volume, and the excess surface tension were calculated on the basis of the obtained data. From these properties information on the interactions of components and possible chemical reactions between them was obtained. Due to the absence of silica and the low concentration of other network-forming oxides, only isolated FeO ₄ ⁵⁻ tetrahedra and the CaO·FeO ionic pairs are formed in these basic melts, the donor of the oxygen atoms being either CaO, FeO, or both CaO+FeO oxides. Even the observed ternary interactions may be attributed to the formation of the anions FeO ₄ ⁵⁻ only.     

Glycerol catalytic cyclocondensation with ethanediamine to pyrazinyl compounds over the modified SiO2‐Al2O3

The Fe, Zn, and Mn‐modified SiO₂‐Al₂O₃ catalysts for the glycerol vapor‐phase cyclocondensation with ethanediamine (ED) to 2‐pyrazinemethanol (2‐PMol) and 2‐methylpyrazine (2‐MP) in a fixed‐bed system were prepared by coprecipitation and characterized by N₂ adsorption–desorption, X‐ray powder diffraction, and NH₃ temperature‐programmed desorption (NH₃‐TPD) in the present work. The results showed that the Mn‐modified SiO₂‐Al₂O₃ catalyst with a SiO₂/Al₂O₃ molar ratio 15.84 and 6% Mn gave the highest catalytic activity for formation of 2‐PMol (53.1%) and 2‐MP (42.9%). Mn species could cause the modulation of the acidic species of catalysts, improving the glycerol cyclocondensation with ED to 2‐PMol, and also acted as the catalytic centers for the hydrodehydration of 2‐PMol to 2‐MP. However, too many strong acidic sites could lead to ED self‐cyclocondensation to form a by‐product pyrazine. The optimum temperature was tested to be 380°C for the cyclocondensation over a 6%Mn‐SiO₂‐Al₂O₃ catalyst. © 2012 Wiley Periodicals, Inc. Heteroatom Chem 23:377–382, 2012; View this article online at wileyonlinelibrary.com . DOI 10.1002/hc.21026     

Stable complex C2H4Al4Li3− and its similarity with bicyclo[2.2.0]hex‐2‐ene: A DFT study

We propose that complexation of all metal antiaromatic Al₄Li with C₂H₄ may lead to stable C₂H₄Al₄Li species [II(b)]. Complexation leads to the electron transfer from Al₄Li moiety to C₂H₄ and development of aromatic character in the Al₄ ring. Our proposed compound C₂H₄Al₄Li [II(b)] is very similar to the existing organic compound bicyclo[2.2.0]hex‐2‐ene [I(b)]. The complex C₂H₄Al₄Li [II(b)] can be imagined as an analogue of bicyclo[2.2.0]hex‐2‐ene [I(b)] achieved by a simple replacement of C₄H₄ in the later with π‐isoelectronic Al₄Li moiety in the former. © 2010 Wiley Periodicals, Inc. Int J Quantum Chem, 2010     

Untersuchungen an SrYb2O4, CaYb2O4 und CaLu2O4; ein Beitrag zur Kristallstruktur des Calciumferrat(III)-Typs

Single crystals investigations at SrYb₂O₄, CaYb₂O, and CaLu₂O₄, and investigations at the systems CaO? Yb₂O₃ and CaO? Gd₂O₃ show, that the condition R > R must be fullfilled for the formation of compounds of the CaFe₂O₄-type. The anionic frame [MeO₄]^2? is inflexible. Any changing in volume of Me²⁺ is transmitted up to the limitation of the unit cell.