Disilberoxotellurat(VI), Ag2TeO4

Disilver Oxotellurate(VI), Ag₂TeO₄ Ag₂TeO₄ was synthesised by reaction of Ag₂O and TeO₂ applying an elevated oxygen pressure. According to a single crystal structure determination (C2/c, a = 9.0588(9), b = 9.2456(8), c = 13.623(1) Å, β = 91.758(8)°, Z = 12, 1289 independent reflections, R1 = 2.32 %, wR2 = 5.51 %), Ag₂TeO₄ contains a novel chain‐like polyanion with tellurium in an octahedral coordination. The TeO₆ octahedra are connected via common edges and vertices in a way that the resulting polyanion represents a section of the rutile structure type. Ag₂TeO₄ shows diamagnetic and insulating behaviour, it decomposes at 560 °C into Ag₂TeO₃ and oxygen.     

Synthese und Kristallstruktur von Te3O3(PO4)2, einer Verbindung mit fünffach koordiniertem Tellur(IV)

Synthesis and Crystal Structure of Te₃O₃(PO₄)₂, a Compound with 5‐fold Coordinate Tellurium(IV) Polycrystalline Te₃O₃(PO₄)₂ is formed during controlled dehydration of (Te₂O₃)(HPO₄) with (Te₈O₁₀)(PO₄)₄ as an intermediate product. Colourless single crystals were prepared by heating stoichiometric amounts of the binary oxides P₂O₅ und TeO₂ in closed silica glass ampoules at 590 °C for 8 hours. The crystal structure (P2₁/c, Z = 4, α = 12.375(2), b = 7.317(1), c = 9.834(1)Å, β = 98.04(1)°, 1939 structure factors, 146 parameters, R[F² > 2σ(F²)] = 0.0187, wR2(F² all) = 0.0367) was determined from four‐circle diffractometer data and consists of [TeO₅] polyhedra und PO₄ tetrahedra as the main building units. The framework structure is made up of cationic zigzag‐chains of composition [Te₂O₃]²⁺ which extend parallel to [001] and anionic [Te(PO₄)₂]^2— units linked laterally to these chains. This leads to the formation of [Te₂O₃][Te(PO₄)₂] layers parallel to the bc plane which are interconnected via weak Te‐O bonds.     

Synthesis and Structure Determination of Ag5HgSbO6, Comparison with AgHg3SbO6 and Ag5Pb2O6

From solid state reactions of Ag₂O, HgO, and Sb₂O₃ at high temperatures under elevated oxygen pressures a new silver mercury antimonate, Ag₅HgSbO₆, has been obtained. According to a single crystal structure determination Ag₅HgSbO₆ crystallizes in space group P$\bar{3}$ 1c (no. 163) with a = 5.9263(4), c = 12.3023(7) Å, V = 374.18(4) ų, Z = 2, 498 independent reflections, R1 = 0.030, wR2 = 0.059 (I ≥ 2 σ (I). Ag₅HgSbO₆ consists of HgSbO₆ layers, analogous to BiI_3, which are separated by Kagome nets formed by Ag⁺ ions. Perpendicular to these layers and along the c axis linear strings of Ag⁺ ions run through the large voids of the layers. Accordingly, Ag₅HgSbO₆ adopts the Ag₅Pb₂O₆ type of structure where the lead positions are occupied by mercury and antimony alternatingly. The finding of mercury in octahedral coordination, particularly besides the lower charged Ag⁺ cations in linear coordination, which is also highly preferred by Hg²⁺ ions, is rather unexpected. Ag₅HgSbO₆ starts to decompose at 450 °C and, in contrast to subvalent and metallic Ag₅Pb₂O₆, the new compound is charge balanced and semiconducting (ρ = 5.7 Ωcm at ambient temperature, E_a = 0.047 eV).     

Two Modifications of (TeO)(HAsO4) and its Dehydration Product (Te3O3)(AsO4)2 – Three more Examples of Tellurium(IV) with a Fivefold Oxygen Coordination

Two modifications of (TeO)(HAsO₄) were obtained by reacting tellurium dioxide with arsenic acid under boiling conditions (modification I, acid concentration 80 wt‐%) or under hydrothermal conditions (modification II, acid concentration 50 wt‐%). The crystal structures of the two modifications were determined from single‐crystal X‐ray data [modification I: P2₁/c, Z = 4, a = 7.4076(10), b = 5.9596(7), c = 9.5523(11) Å, β = 102.589(8)°, 2893 structure factors, 68 parameters, R[F² > 2σ(F²)] = 0.0247, wR₂(F² all) = 0.0530; modification II: P2₁/c, Z = 4, a = 6.2962(4), b = 4.7041(3), c = 13.9446(8) Å, β = 94.528(3)°, 2549 structure factors, 69 parameters, R[F² > 2σ(F²)] = 0.0207, wR₂(F² all) = 0.0462)]. Dehydration of (TeO)(HAsO₄)‐II at temperatures above 260 °C results in the formation of polycrystalline (Te₃O₃)(AsO₄)₂. Single crystals of the anhydrous product were grown either by heating stoichiometric amounts of the binary oxides TeO₂ and As₂O₅ in closed silica glass ampoules or with higher concentrated arsenic acid (80 wt‐%) under hydrothermal conditions at 220 °C. The common features in the crystal structures of (Te₃O₃)(AsO₄)₂ [P$\bar{1}$ , Z = 4, a = 6.5548(4), b = 7.6281(6), c = 15.0464(15) Å, α = 140.212(6), β = 102.418(9)°, γ = 77.346(5)°, 5718 structure factors, 146 parameters, R[F² > 2σ(F²)] = 0.0351, wR₂(F² all) = 0. 1093] and in that of the two modifications of acidic (TeO)(HAsO₄) are [TeO₅] square‐pyramids and [AsO₄] tetrahedra. In anhydrous (Te₃O₃)(AsO₄)₂ and in (TeO)(HAsO₄)‐II, a layered arrangement of the building units is found, whereas in the (TeO)(HAsO₄)‐I structure strands are formed. Different hydrogen bonding interactions are present in the two modifications of (TeO)(HAsO₄).     

Dimers of Ag2+ Ions – Synthesis and Characterization of the Quaternary Silver Fluoride Ag2ZnZr2F14 with [Ag2F7]3– Units

Deep blue‐violet colored powder samples of Ag₂ZnZr₂F₁₄ were synthesized by heating Zn(NO₃)₂·4H₂O, Ag and ZrOCl₂·8H₂O at 300 °C under fluorine atmosphere. The crystal structure of Ag₂ZnZr₂F₁₄ was refined from X‐ray powder diffraction data using the Rietveld method (C2/m, a = 9.0206(1) Å, b = 6.6373(1) Å, c = 9.0563(1) Å, β = 90.44(1)°, Z = 2). The structure is derived from the isotypic Ag₃Zr₂F₁₄ by replacing only one of the two crystallographically different Ag²⁺ ions with Zn²⁺ ions, thus leading to discrete Ag₂F₇ dimers. These dimers are connected via nearly linear Ag–F···F–Ag bridges with short F···F distances of 2.33 Å to form two‐legged ladders. Magnetic susceptibility measurements and density functional calculations show that the two Ag²⁺ ions in each Ag₂F₇ dimer are strongly coupled antiferromagnetically.     

Preparation and Crystal Structures of the Hydrous Mercury Tellurates,HgII(H4TeVIO6) and HgI2(H4TeVIO6)(H6TeVIO6)·2H2O

Single crystals of Hg^II(H₄Te^VIO₆) (colourless to light‐yellow, rectangular plates) and Hg^I₂(H₄Te^VIO₆)(H₆Te^VIO₆)·2H₂O (colourless, irregular) were grown from concentrated solutions of orthotelluric acid, H₆TeO₆, and respective solutions of Hg(NO₃)₂ and Hg₂(NO₃)₂. The crystal structures were solved and refined from single crystal diffractometer data sets (Hg^II(H₄Te^VIO₆): space group Pna2₁, Z = 4, a =10.5491(17), b = 6.0706(9), c = 8.0654(13)Å, 1430 structure factors, 87 parameters, R[F² > 2σ(F²)] = 0.0180; Hg^I₂(H₄Te^VIO₆)(H₆Te^VIO₆)·2H₂O: space group P1¯, Z = 1, a = 5.7522(6), b = 6.8941(10), c = 8.5785(10)Å, α = 90.394(8), β = 103.532(11), γ = 93.289(8)°, 2875 structure factors, 108 parameters, R[F² > 2σ(F²)] = 0.0184). The structure of Hg^II(H₄Te^VIO₆) is composed of ribbons parallel to the b axis which are built of [H₄TeO₆]^2— anions and Hg²⁺ cations held together by two short Hg—O bonds with a mean distance of 2.037Å. Interpolyhedral hydrogen bonding between neighbouring [H₄TeO₆]^2— groups, as well as longer Hg—O bonds between Hg atoms of one ribbon to O atoms of adjacent ribbons lead, to an additional stabilization of the framework structure. Hg^I₂(H₄Te^VIO₆)(H₆Te^VIO₆)·2H₂O is characterized by a distorted hexagonal array made up of [H₄TeO₆]^2— and [H₆TeO₆] octahedra which spread parallel to the bc plane. Interpolyhedral hydrogen bonding between both building units stabilizes this arrangement. Adjacent planes are stacked along the a axis and are connected by Hg₂²⁺ dumbbells (d(Hg—Hg) = 2.5043(4)Å) situated in‐between the planes. Additional stabilization of the three‐dimensional network is provided by extensive hydrogen bonding between interstitial water molecules and O and OH‐groups of the [H₄TeO₆]^2— and [H₆TeO₆] octahedra. Upon heating Hg^I₂(H₄Te^VIO₆)(H₆Te^VIO₆)·2H₂O decomposes into TeO₂ under formation of the intermediate phases Hg^II₃Te^VIO₆ and the mixed‐valent Hg^IITe^IV/VI₂O₆.     

Synthesis,Crystal Structure and Properties of Ag4CuTeO6

The new quaternary oxide Ag₄CuTeO₆ has been obtained by solid state reaction starting from stoichiometric amounts of the binary oxides at elevated temperatures and oxygen pressures. Ag₄CuTeO₆ crystallises in space group C2/c with a = 11.3021(8), b = 9.6875(6), c = 5.7082(5) Å, β = 99.301(7)°, V = 616.77(8) ų, Z = 4; the structure refinement was based on 747 independent reflections and resulted in R₁ = 3.26 %, wR₂ = 7.29 %. The crystal structure consists of isolated TeO₆ octahedra which are connected by distorted CuO₄ squares, thus forming one‐dimensional, infinite heteropolyanions, extending along the c axis. According to the approximately fcc packing and a distorted octahedral oxygen environment of all the cations, the structure may be regarded a derivative of the NaCl structure type. Ag₄CuTeO₆ is paramagnetic between 300 K and 7 K, where it develops antiferromagnetic ordering. An evaluation according to the Curie‐Weiss law yielded a magnetic moment of 1.86 μ_B per copper ion. The electronic conductivity shows a maximum at ～ 75 K, below a temperature characteristic of a semiconductor, above of a metal.     

Synthesis and Crystal Structure of Cs(VO2)3(TeO3)2, a New Layered Cesium Vanadium(V) Tellurite

Synthetic Cs(VO₂)₃(TeO₃)₂ is built up from infinite sheets of distorted octahedral V^VO₆ groups, sharing vertices. These octahedral layers are “capped” by Te atoms (as parts of pyramidal [Te^IVO₃]^2– groups) on both faces of each V/O sheet, with inter‐layer, 12‐coordinate, Cs⁺ cations providing charge compensation. Cs(VO₂)₃(TeO₃)₂ is isostructural with M(VO₂)₃(SeO₃)₂ (M = NH₄, K). Crystal data: Cs(VO₂)₃(TeO₃)₂, M_r = 732.93, hexagonal, space group P6₃ (No. 173), a = 7.2351(9) Å, c = 11.584(2) Å, V = 525.1(2) ų, Z = 2, R(F) = 0.030, wR(F ²) = 0.063.     

Complex Topology of Uranyl Polyphosphate Frameworks: Crystal Structures of α‐, β‐K[(UO2)(P3O9)] and K[(UO2)2(P3O10)]

Three new uranyl polyphosphates, α‐K[(UO₂)(P₃O₉)] ( 1 ), β‐K[(UO₂)(P₃O₉)] ( 2 ), and K[(UO₂)₂(P₃O₁₀)] ( 3 ), were prepared by high‐temperature solid‐state reactions. The crystal structures of the compounds have been solved by direct methods: 1 – monoclinic, P2₁/m, a = 8.497(1), b = 15.1150(1), c = 14.7890(1) Å, β = 91.911(5)°, V = 1898.3(3) ų, Z = 4, R₁ = 0.0734 for 4181 unique reflections with |F₀| ≥ 4σ_F; 2 – monoclinic, P2₁/n, a = 8.607(1), b = 14.842(2), c = 14.951(1) Å, β = 95.829(5)°, V = 1900.0(4) ų, Z = 4, R₁ = 0.0787 for 3185 unique reflections with |F₀| ≥ 4σ_F; 3 – Pbcn, a = 10.632(1), b = 10.325(1), c = 11.209(1) Å, V = 1230.5(2) ų, Z = 4, R₁ = 0.0364 for 1338 unique reflections with |F₀| ≥ 4σ_F. In the structures of 1 and 2 , phosphate tetrahedra share corners to form infinite [PO₃]^? chains, whereas, in the structure of 3 , tetrahedra form linear [P₃O₁₀]^5? trimers. The structures are based upon 3‐D frameworks of U and P polyhedra linked by sharing common O corners. The infinite [PO₃]^? chains in the structures of 1 and 2 are parallel to [100] and [–101], respectively. The uranyl polyphosphate frameworks are occupied by host K⁺ cations.     

Silver Vanadyl(IV) ortho‐Pyrophosphate: Synthesis,Crystal Structure,and Characterization of the (V≡O)2+ Group

Ag₆(V^IVO)₂(PO₄)₂(P₂O₇) was obtained by reaction of Ag₃PO₄ and (VO)₂P₂O₇ (sealed ampoule, 550 °C, 3 d). The crystal structure of the new mixed ortho‐pyrophosphate was determined from X‐ray single‐crystal data [Pnma, Z = 4, a = 12.759(3) Å, b = 17.340(4) Å, c = 6.418(1) Å, R₁ = 0.071, wR₂ = 0.184 for 3174 unique reflections with F_o > 4σ(F_o), 141 variables]. Ag⁺ ions are located in between layers [(V^IVO)₂(PO₄)₂(P₂O₇)]^6–. Equilibrium relations of the new phosphate to neighboring phases were determined. The electronic structure of the (V^IV≡O)²⁺ group was investigated by polarized electronic absorption spectroscopy (ν̃_1a = 9450 cm^–1, ν̃_1b = 9950 cm^–1, ν̃₂ = 14750 cm^–1), EPR spectroscopy [X‐ and Q‐band, powder and single crystal, orthorhombic crystal g‐tensor with g₁ = 1.9445(3), g₂ = 1.9521(3), g₃ = 1.9695(3)], and magnetic measurements (powder, μ_exp/μ_B = 1.71, Θ_p = –1.7 K).     

Preparation,Thermal Behaviour and Crystal Structure of the Basic Mercury(II) Tetraoxotellurate(VI), Hg2TeO5, and Redetermination of the Crystal Structure of Mercury(II) Orthotellurate(VI), Hg3TeO6

Single crystals of Hg₂TeO₅ were obtained as dark‐red parallelepipeds by reacting stoichiometric amounts of Hg(NO₃)₂ · H₂O and H₆TeO₆ under hydrothermal conditions (250 °C, 10d). The crystal structure (space group Pna2₁, Z = 4, a = 7.3462(16), b = 5.8635(12), c = 9.969(2)Å, 1261 structure factors, 50 parameters, R[F² > 2σ(F²)] = 0.0295) is characterized by corner‐sharing [TeO₆] octahedra forming isolated chains [TeO_4/1O_2/2] which extend parallel to [100]. The two crystallographically independent Hg atoms are located in‐between the chains and interconnect the chains via common oxygen atoms. Amber coloured single crystals of Hg₃TeO₆ were prepared by heating a mixture of Hg, HgO and TeO₃ together with small amounts of HgCl₂ as mineralizer in an evacuated and sealed silica glass tube (520 °C). The previously reported crystal structure has been re‐investigated by means of single crystal X‐ray data which reveal a symmetry reduction from Ia3¯d to Ia3¯ (Z = 16, a = 13.3808(6) Å, 609 structure factors, 33 parameters, R[F² > 2σ(F²)] = 0.0221). The crystal structure is made up of a body‐centred packing of [TeO₆] octahedra with the Hg atoms situated in the interstices of this arrangement. Upon heating, both title compounds decompose in a one‐step mechanism under formation of TeO₂ and loss of the appropriate amounts of elementary mercury and oxygen.     

Weak Interactions in Silver Complexes of 15-Crown-5

Abstract

The X-ray crystal structures of two closely related Ag(I) complexes of 15-crown-5 and benzo-15-crown-5 are reported. In the case of [Ag(15-crown-5)₂][SbF₆] 1, pointing one of its oxygen atoms away from the Ag⁺ cation enables one of the crown ligands to take part in an intermolecular C?H…O hydrogen bond. The analogous benzo-15-crown-5 species, [Ag(benzo-15-crown-5)₂][SbF₆] 2, is too rigid to attain the necessary conformation. Crystal data for 1: P2_1/c, a = 8.4481(3), b = 25.5813(9), c = 13.2773(4) Å, β = 101.354(2)°. Z = 4, unique data: 5187 R ₁ [F ² > 2σ(F ²)] 0.0259. Compound 2: P1, a = 8.6511 (15) Å, b =10.2322(18) Å, c = 19.291(3) Å, α = 103.704 (2)°, β = 101.274(2)°, γ = 95.952(2)°, Z = 2, unique data: 5803 R ₁ [F ²>2σ(F ²)] 0.0931.     

Structural Phase Transitions in Ag2Se (Naumannite)

Ag₂Se (naumannite) was investigated by means of temperature dependent synchrotron powder diffraction and DTA. Upon heating in air the known 1^st order phase transition from orthorhombic low‐temperature Ag₂Se (P2₁2₁2₁, Z = 4) to cubic ion conducting high‐temperature Ag₂Se (Im3m, Z = 2) was observed at approx. 140 °C. Upon cooling a small hysteresis was detected (T_PU = 120 °C). It was found that when heated in air Ag₂Se segregates elemental selenium. After cooling to ambient temperature the resulting low‐temperature Ag₂Se can no longer be described in the known structural model with harmonic terms, the use of anharmonic terms is probably necessary. The phase transition and the segregation of selenium are accompanied by an increased crystallinity of the sample, as the halfwidths of the reflections become significantly smaller. Approaching the phase transition the lattice parameters of orthorhombic Ag₂Se show a distinct anisotropic behaviour: b and c show a positive and a a negative thermal expansion. When heated in argon the segregation of selenium is not observed.     

Hydrothermal Synthesis of a New Vanadium Tellurate(VI) with a Novel Chain Structure: (NH4)4{(VO2)2[Te2O8(OH)2]}·2H2O

A new ammonium vanadium tellurate, (NH₄)₄{(VO₂)₂[Te₂O₈(OH)₂]}·2H₂O ( 1 ) was hydrothermally synthesized and characterized by elemental analyses, IR spectrum, TG analysis, and single crystal X–ray diffraction. Compound 1 crystallizes in the monoclinic system, space group P2₁/n, a = 7.3843(15) Å, b = 17.111(3) Å, c = 7.3916(15) Å, β = 118.88(3)°, V = 817.9(3) ų, Z = 2, R1 (I>2σ(I)) = 0.0235, wR2 (all data) = 0.0462. The structure of 1 consists of infinite anionic chains, {(VO₂)₂[Te₂O₈(OH)₂]}^4? which contain octahedral VO₆ and TeO₅OH units. Each octahedral VO₆ and TeO₅OH unit is connected by sharing an edge to form V₂O₁₀ and Te₂O₈(OH)₂ binuclear units. The V₂O₁₀ and Te₂O₈(OH)₂ binuclear units are alternatively connected to one another, creating complete infinite {(VO₂)₂[Te₂O₈(OH)₂]}^4? chains along the c direction. The anionic chains are separated by ammonium cations and water molecules that link the chains through a network of hydrogen bonds. In addition, the structure contains an extended network of O–H·····O hydrogen bonds between the chains.     

Crystal structure of a new gallium tellurite: Ga2Te4O11

Ga₂Te₄O₁₁ crystallises with triclinic symmetry (space group P1) and unit cell parameters: a = 5.125(1) Å, b = 6.559(1) Å, c = 8.173(2) Å, α = 75.06(2), β = 89.25(2), γ = 69.62(2), Z = 1. Its crystal structure has been refined by a full matrix least-squares process to R₁ = 0.023 and wR₂ = 0.060 values, on the basis of 2931 independent single crystal X-ray reflections. It can be described as a three-dimensional polyhedral network of independent Te₂O₆ groups of TeO₃ trigonal pyramids and TeO₄ disphenoids sharing corners, and infinite (Te₂O₅)_∞ quasi-linear chains of the same corner-sharing TeO₃ and TeO₄ units, linked one to the other via common corner or common edge by GaO₄ and GaO₅ polyhedra. The stereochemical activity of the lone pair of each Te atom has been analysed and a comparison is made with all the known other M₂Te₄O₁₁ crystal structures.     

Die Kristallstruktur der Tieftemperaturmodifikation von Ag5Te2Cl

The Crystal Structure of the Low‐Temperature Form of Ag₅Te₂Cl Crystals of trimorphic Ag₅Te₂Cl were obtained by solid state reaction from a stoichiometric mixture of silver, tellurium, and tellurium(IV)chloride (480 °C, 4–10 days). The crystals were cooled down to –80 °C without decomposition and data collection was carried out at this temperature. The low temperature form of the title compound crystallizes in space group P2₁/c with lattice constants of a = 19.359(1) Å, b = 7.713(1) Å, c = 19.533(1) Å, β = 90.6°(1), V = 2916.4(1), and Z = 16. The refinement converged to residual values of R₁ = 0.0381 and wR₂ = 0.0847, respectively. Te and Cl atoms form empty, distorted octahedra interconnected by common vertices to give a 3D‐network. Ag atoms form clusters with Ag–Ag distances between 2.83 Å and 3.10 Å.     

Über Ag2SnO3, das erste Silberstannat

On Ag₂SnO₃, the First Silver Stannate For the first time, crystals of red Ag₂SnO₃ have been obtained by solid state reaction of freshly prepared K₂Sn(OH)₆ and Ag₂O at 430°C while applying an oxygen pressure of 350 bar. Ag₂SnO₃ shows a one dimensional incommensurate superstructure with a′ = 33.1 Å. Here we report on the basic structure of Ag₂SnO₃. According to the results of X-ray crystal structure determination the basic structure of Ag₂SnO₃ may be described in P6₃22 (a = 5.6230(4) Å, c = 12.6694(14) Å, Z = 4, 968 independent reflections, R1 = 5.6%, wR2 = 12.5%). Within the layered “SnO₃” partial structure two third of the octahedral voids are occupied by tin. Those SnO₃ layers are connected to each other by almost linearly coordinated silver atoms. Additionally, silver occupies the free octahedral voids within the SnO₃ sheets. As expressed by the formula Ag[Ag_1/3Sn_2/3]O₂ the structure may be described as a super structure of Delafossite CuFeO₂.     

Ag9I(GeO4)2 – Containing Two‐dimensionally Linked [IAg12] Metallo Complexes

Ag₉I(GeO₄)₂ was obtained for the first time by reacting a stoichiometric mixture of Ag₂O, AgI, and GeO₂, at elevated oxygen pressures, adding a small portion of distilled water. The synthesis was done at 480 °C and 110 MPa of oxygen pressure. It crystallizes in space group C2/m, with the unit cell dimensions a = 17.3736(9) Å, b = 6.9177(4) Å, c = 5.7176(3) Å, β = 105.501(3)°, V = 662.18(6) ų, and Z = 2. The structure refinement was based on 638 independent reflections and resulted in R₁ = 6.26 %. The crystal structure consists of isolated (GeO₄)^4– ions and [IAg₁₂] metallo complexes, the latter are interconnected through each two common edges and corners corresponding to [IAg_6/1Ag_6/2], thus forming infinite layers within the (100) plane. The Ag/I slabs are stacked perpendicular to the a‐axis with an interlayer distance of about 3.4 Å. The (GeO₄)^4– anions are located in the gaps between the silver iodide layers. According to the results of impedance measurements, Ag₉I(GeO₄)₂ is a good silver ion conductor. The compound shows an increase in the ionic conductivity in the temperature range of 30 to 310 °C, and has a silver ion conductivity of 1.1 × 10^–3 Ω^–1 cm^–1 at room temp. The activation energy for silver ion conduction is 0.35 eV, in the temperature range from 25 to 190 °C.     

MII(C4H12N2)[B2P3O12(OH)] (MII = Co,Zn): Synthesis and Crystal Structure of Novel Open Framework Borophosphates

Two novel borophosphates, M^II(C₄H₁₂N₂)[B₂P₃O₁₂(OH)] (M^II = Co, Zn), exhibiting open frameworks, have been synthesized by hydrothermal reactions (T = 165 °C). The crystal structures of the isotypic compounds have been determined both at 293 K (orthorhombic, Ima2 (no. 46), Z = 4; M^II = Co: a = 12.4635(4) Å, b = 9.4021(4) Å, c = 11.4513(5) Å, V = 1341.90 ų, R₁ = 0.0202, wR₂ = 0.0452, 2225 observed reflections with I > 2σ(I); M^II = Zn: a = 12.4110(9) Å, b = 9.4550(5) Å, c = 11.4592(4) Å, V = 1344.69 ų, R₁ = 0.0621, wR₂ = 0.0926, 1497 observed reflections with I > 2σ(I)). Distorted CoO₆‐octahedra and ZnO₅‐square‐pyramids, respectively, share common oxygen‐corners with BO₄‐, PO₄‐ and (HO)PO₃‐tetrahedra. The tetrahedral groups are linked via common corners to form infinite loop‐branched borophosphate chains [B₂P₃O₁₂(OH)^4–]. The open framework of M^II‐coordination polyhedra and tetrahedral borophosphate chains contains a three‐dimensional system of interconnected structural channels running along [100], [011] and [011], respectively, which are occupied by di‐protonated piperazinium ions.     

Synthesis and Crystal Structure of a Decanuclear Silver（I）-thiolate Compound Ag10S[S2P（OEt）2]8

A new decanuclear silver(I) compound Ag₁₀(μ₈‐S)(dtp)₈ [dtp=S₂P(OEt)₂] was isolated from a reaction mixture containing W₂S₄(dtp)₂ and AgN0₃, and its solid‐state molecular structure was determinated by X‐ray crystallography. The crystallographic study revealed that the compound contains a distorted mono‐capped quasi‐prism [Ag_io] with an octat‐bridging S atom at the center of the prism. The compound (C₃₂H₈₀Ag₁₀O₁₆P₈S₁₇, M_r=2592.46) crystallizes in the monoclinic P2₁/n space group, with a = 1.5111(5) nm, b=2.3656(8) nm, c=2.284(1) nm, β= 96.88(3)°, V=8.107(5) nm³, Z=4 and D,=2.12 g · cm^?3. The solution using direct method and full‐matrix least‐squares refinement led to R=0.066, Rw=0.078 for 3928 reflections with I3σ(I).