Single Crystals of NaPrTe2 with LiTiO2‐Type Structure

During attempts to synthesize rare‐earth nitride tellurides black and bead‐shaped single crystals of the title compound sodium praseodymium(III) ditelluride (NaPrTe₂) were obtained as a by‐product by reacting a mixture of praseodymium, sodium azide (NaN₃) and tellurium at 900 °C for seven days in evacuated torch‐sealed silica vessels. NaPrTe₂ crystallizes cubic (space group: Fd3¯m, Z = 16; a = 1285.51(9) pm, V_m = 79.96(1) cm³/mol, R₁ = 0.028 for 146 unique reflections) and exhibits the Na⁺ and Pr³⁺ cations in slightly distorted octahedra of six telluride anions (d(Na—Te) = 325 pm, d(Pr—Te) = 317 pm) each. The main characteristics of this new structure type for alkali‐metal rare‐earth(III) dichalcogenides can be derived from the rock‐salt type structure (NaCl, cubic closest‐packed Te^2— arrangement, all octahedral voids occupied with Na⁺ and Pr³⁺) with alternating layers consisting of Na⁺ and Pr³⁺ cations in a ratio of 3:1 and 1:3, respectively, piled along the [111] direction.     

Thiosilicate der Selten‐Erd‐Elemente: III. KLa[SiS4] und RbLa[SiS4] – Ein struktureller Vergleich

Thiosilicates of the Rare‐Earth Elements: III. KLa[SiS₄] and RbLa[SiS₄] – A Structural Comparison Pale yellow, platelet shaped, air‐ and water resistant single crystals of KLa[SiS₄] derived from the reaction of lanthanum (La) and sulfur (S) with silicon disulfide (SiS₂) in a molar ratio of 2 : 3 : 1 with an excess of potassium chloride (KCl) as flux and source of potassium ions in evacuated silica ampoules at 850 °C within seven days. The analogous reaction utilizing a melt of rubidium chloride (RbCl) instead also leads to yellow comparable single crystals of RbLa[SiS₄]. The potassium lanthanum thiosilicate crystallizes monoclinically with the space group P2₁/m (a = 653.34(6), b = 657.23(6), c = 867.02(8) pm, β = 107.496(9)°) and two formula units per unit cell, while the rubidium lanthanum thiosilicate has to be assigned orthorhombically with the space group Pnma (a = 1728.4(2), b = 667.23(6), c = 652.89(6) pm) and four formula units in its unit cell. In both compounds the La³⁺ cations are surrounded by 8+1 sulfide anions in the shape of tricapped trigonal prisms. The Rb⁺ cations in RbLa[SiS₄] show a coordination number of 9+2 relative to the S^2? anions, which form pentacapped trigonal prisms about Rb⁺. This coordination number, however, is apparently too high for the K⁺ cations in KLa[SiS₄], so that they only exhibit a bicapped trigonal prismatic environment built up by eight S^2? anions. The isolated thiosilicate tetrahedra [SiS₄]^4? of the rubidium compound are surrounded by La³⁺ both edge‐ and face‐capping, but terminal as well as edge‐ and face‐spanning by Rb⁺. In the potassium compound there is no change for the La³⁺ environment about the [SiS₄]^4? tetrahedra, but the K⁺ cations are only able to attach terminal and via edges. The whole structure is built up by anionic equation/tex2gif-stack-1.gif{La[SiS₄]}^? layers that are separated by the alkali metal cations. In direct comparison the two thiosilicate structures can be regarded as stacking variants.     

ErF3‐reiche ternäre Erbiumfluoride mit den schweren Alkalimetallen: I. KEr3F10 und RbEr3F10

ErF₃‐Rich Ternary Erbium Fluorides with the Heavy Alkali Metals: I. KEr₃F₁₀ and RbEr₃F₁₀ The conversion of erbium trifluoride (ErF₃) with chlorides of the heavy alkali metals (ACl; A = K, Rb and Cs) at 700–800 °C in tantalum capsules sealed by arc‐welding surprisingly results in the formation of ErF₃‐rich ternary alkali‐metal erbium(III) fluorides with the compositions AEr₃F₁₀ (A = K and Rb) or CsEr₂F₇, respectively. The first‐mentioned compounds are characterized by high coordination numbers at the alkali‐metal cation (CN(A⁺) = 15 and 16) as well as by a uniform surrounding of the Er³⁺ cation (CN = 8, square antiprism). In KEr₃F₁₀ (cubic, Fm3m; a = 1154.06(7) pm, Z = 8) eight (F1)^? anions always arrange as a cube, whose six faces are each capped by an Er³⁺ cation. These [(F1)₈Er₆]¹⁰⁺ groups constitute a cubic closest sphere‐packing with K⁺ cations in all of the tetrahedral interstices. The [Er₆(μ₃‐F1)₈]¹⁰⁺ units are interconnected via the remainder fluoride anions (F2) to build up a three‐dimensional framework so that the characteristic [ErF₈]^5? polyhedra (d(Er³⁺?F^?) = 220 – 235 pm) emerge. In RbEr₃F₁₀ (hexagonal, P6₃mc; a = 818.43(5), c = 1336.54(8) pm, Z = 4) the analogous [ErF₈]^5? polyhedra (d(Er³⁺?F^?) = 219 – 237 pm) initially convene to triple groups [Er₃F₁₉]^10? through cis‐edge condensation, which are then further connected via F^? corners to arrange as a two‐dimensional network perpendicular to the c axis. Finally, the cross‐linking of these layers is achieved by common F^? vertices again, such that large cavities apt to take up the Rb⁺ cations are formed. A second part of these series will report on the syntheses and crystal structures of the ErF₃‐poorer AEr₂F₇‐type representatives with A = K, Rb and Cs.     

Shape‐Induced,Hexagonal, Open Frameworks: Rubidium Ion Complexed Cucurbituril

A honeycomb structure is shown by the one‐dimensional coordination polymer comprising D_6h‐symmetric cucurbituril molecules and rubidium ions (see picture). The cucurbituril molecules stack atop one another and show coordination of their carbonyl groups to the rubidium ions in between. The shape and symmetry of the building blocks encourage the coordination polymer chains to be arranged in such a way as to produce an open‐framework structure with large, linear, hexagonal channels.     

ASc[SeO3]2 (A = Na – Cs): Pure Alkali‐Metal Scandium Oxoselenates(IV) and Their Representatives With Mixed Alkali‐Metal Occupation

Alkali‐metal scandium oxoselenates(IV) ASc[SeO₃]₂ (A = Na – Cs) are known since a few years and a hydrothermal synthesis was used to obtain them. In our new studies we applied a flux‐supported solid‐state reaction and produced colorless single crystals as well. All representatives ASc[SeO₃]₂ with A = Na – Cs crystallize in the orthorhombic space group Pnma, in contrast to earlier reports for hexagonal RbSc[SeO₃]₂. Furthermore we have extended this field with some crystals showing a mixed occupation on the alkali‐metal site, namely (K,Na)Sc[SeO₃]₂, (Rb,K)Sc[SeO₃]₂, and (Cs,Rb)Sc[SeO₃]₂. Since all of them contain [ScO₆]^9– octahedra and [SeO₃]^2– ψ¹‐tetrahedra the diverse connectivity of the distinct alkali‐metal centered oxygen polyhedra differentiates the compounds with the smaller alkali metals (A′ = Na and K) from those with the bigger ones (A′′ = Rb and Cs). For the mixed crystals the amount of smaller or bigger alkali metal is responsible, which design is chosen by the system. This forces the mixed crystal (Rb,K)Sc[SeO₃]₂ with a higher amount of potassium instead of rubidium to crystallize isotypically with KSc[SeO₃]₂ and NaSc[SeO₃]₂, whereas the pure rubidium compound RbSc[SeO₃]₂ adopts the CsSc[SeO₃]₂‐type structure. These findings are supported by single‐crystal Raman spectroscopy.     

Neue Oxocadmate der Alkalimetalle: K6[CdO4],Rb6[CdO4], Rb2CdO2 und Rb2Cd2O3

The crystal structure of K₆[CdO₄] and Rb₂CdO₂ has been determined from single crystal X-ray diffraction data and refined toR=0.058 (K₆[CdO₄]) andR=0.088 (Rb₂CdO₂). K₆[CdO₄] crystallizes hexagonal, space group P6₃mc with lattice constantsa=867.42 (6),c=665.5 (1) pm,c/a=0.767 andZ=2. It is isotypic with Na₆[ZnO₄]. Rb₂CdO₂ is orthorhombic, space group Pbcn witha=1045.0 (2),b=629.1 (1),c=618.3 (1) pm,Z=4, and crystallizes with the K₂CdO₂ structure type. The crystal structures can be deduced from the motif of a closest packed arrangement of O^2– with hexagonal (K₆[CdO₄]) or cubic (Rb₂CdO₂) stacking. The tetrahedra occupied by Cd²⁺ are isolated (K₆[CdO₄]) or edge-shared (formation of infinite SiS₂-like chains [CdO_4/2]) (Rb₂CdO₂). The powder diffraction pattern of Rb₆[CdO₄] [a=906.6 (1),c=694.3 (1) pm] and Rb₂Cd₂O₃ [a=642.6 (2),b=679.0 (1),c=667.9 (2) pm, =115.2 (1)] confirm isotypie with K₆[CdO₄] and K₂Cd₂O₃ respectively.

Herrn Prof. Dr.Gutman zum 65. Geburtstag gewidmet.     

Synthesis and Crystal Structure of the Rubidium Scandium Telluride RbSc5Te8

During attempts to synthesize the rubidium dicopper triscandium hexatelluride RbCu₂Sc₃Te₆ in analogy to CsCu₂Sc₃Te₆ from 2:3:6‐molar mixtures of the elements (Cu, Sc and Te) with an excess of RbBr as flux and rubidium source, after 14 days at 900 °C in torch‐sealed evacuated silica tubes brown lath‐shaped crystals of RbSc₅Te₈ did form instead. This new compound crystallizes monoclinically in space group C2/m (no. 12) with two formula units in a unit cell of the dimensions a = 2130.61(9) pm, b = 413.94(2) pm, c = 1022.03(5) pm and β = 104.392(4)°. The crystal structure of RbSc₅Te₈ consists of a three‐dimensional anionic framework of face‐, edge‐ and vertex‐sharing [ScTe₆]⁹⁻ octahedra that provides one‐dimensional tunnels with a distorted square shape. For charge compensation they are occupied with Rb⁺ cations (CN = 10) coordinated in a trans‐face bicapped cubic fashion by Te²⁻ anions.     

Alkali‐Metal ortho‐Hydroxyphenolates: Syntheses and Crystal Structures from Powder X‐Ray Diffraction

Colorless and highly air‐ and moisture‐sensitive powders of M[o‐C₆H₄O(OH)] with M = K, Rb, or Cs have been synthesized from reaction mixtures of the appropriate alkali metal and catechol in thf. All compounds were structurally characterized by means of powder X‐ray diffraction using the Rietveld profile refinement technique including restraints for the C—C/C—O bond distances and the C—C—C angles. The atomic arrangements of M[o‐C₆H₄O(OH)] (K: monoclinic P2₁/c; Rb/Cs: orthorhombic Pbcm) are characterized by polymeric chains of [M₁^[4]O₂^[2]η⁶] units connected by hydrogen bonds, thereby making up layered structures similar to the one of catechol. The coordinatively unsaturated alkali metals are forming edge‐sharing MO₄ pyramids and exhibit asymmetrical η⁶‐interactions with the phenylene rings. The symmetry of the unit cells increases with increasing size of the cation, and this results in a decrease of the monoclinic angle from 118.5° (catechol) to 93.7° (K compound), eventually leading to orthorhombic cells for the Rb and Cs compounds.     

Synthese und Kristallstruktur des Fluorid‐ino‐Oxosilicats Cs2YFSi4O10

Synthesis and Crystal Structure of the Fluoride ino‐Oxosilicate Cs₂YFSi₄O₁₀ The novel fluoride oxosilicate Cs₂YFSi₄O₁₀ could be synthesized by the reaction of Y₂O₃, YF₃ and SiO₂ in the stoichiometric ratio 2 : 5 : 3 with an excess of CsF as fluxing agent in gastight sealed platinum ampoules within seventeen days at 700 °C. Single crystals of Cs₂YFSi₄O₁₀ appear as colourless, transparent and water‐resistant needles. The characteristic building unit of Cs₂YFSi₄O₁₀ (orthorhombic, Pnma (no. 62), a = 2239.75(9), b = 884.52(4), c = 1198.61(5) pm; Z = 8) comprises infinite tubular chains of vertex‐condensed [SiO₄]^4? tetrahedra along [010] consisting of eight‐membered half‐open cube shaped silicate cages. The four crystallographically different Si⁴⁺ cations all reside in general sites 8d with Si–O distances from 157 to 165 pm. Because of the rigid structure of this oxosilicate chain the bridging Si–O–Si angles vary extremely between 128 and 167°. The crystallographically unique Y³⁺ cation (in general site 8d as well) is surrounded by four O^2? and two F^? anions (d(Y–O) = 221–225 pm, d(Y–F) = 222 pm). These slightly distorted trans‐[YO₄F₂]^7? octahedra are linked via both apical F^? anions by vertex‐sharing to infinite chains along [010] (?(Y–F–Y) = 169°, ?(F–Y–F) = 177°). Each of these chains connects via terminal O^2? anions to three neighbouring oxosilicate chains to build up a corner‐shared, three‐dimensional framework. The resulting hexagonal and octagonal channels along [010] are occupied by the four crystallographically different Cs⁺ cations being ten‐, twelve‐, thirteen‐ and fourteenfold coordinated by O^2? and F^? anions (viz.[(Cs1)O₁₀]^19?, [(Cs2)O₁₀F₂]^21?, [(Cs3)O₁₂F]^24?, and [(Cs4)O₁₂F₂]^25? with d(Cs–O) = 309–390 pm and d(Cs–F) = 360–371 pm, respectively).     

Zur Kenntnis von Unordnungsphänomenen bei Oxiden mit dem „Schmetterlingsmotiv”︁ Über Rb2K4[O2CoOCoO2]

On the Knowledge of Disorder Phenomena in Oxides with the Motive of Butterfly. On Rb₂K₄[O₂CoOCoO₂] For the first time Rb₂K₄Co₂O₅ was obtained by annealing intimate mixtures of the binary oxides as dark red single crystals (Rb:K:Co = 1.2:3.2:1; Ni-tube; 570°C; 20 d). Structure Refinement [fourcircle diffractometer data; PW 1100; AgK radiation; 401 of 607 I₀(hkl); R = 9.9%; R_w = 5.5%; space group P4₂/mnm; Z = 2; a = 674,2(4), c = 1172,2(6) pm] confirms the isotypism to K₂Na₄Co₂O₅, Rb₂Na₄Co₂O₅ [2] and K₂Na₄Be₂O₅ [3]. The Madelung Part of Lattice Energy, MAPLE, Effektive Coordination Numbers, ECoN, these via Mean Fictive Ionic Radii, MEFIR, and the Charge Distribution, ΣQ, were calculated. The isotypism of Rb₂K₄Co₂O₅ and Rb₂Na₄Co₂O₅ is compared graphically.     

Alkali‐Metal meta‐Hydroxyphenolates: Syntheses and Crystal Structures from Powder X‐Ray Diffraction

M[m‐C₆H₄O(OH)] (M = Li—Cs) have been obtained as highly air‐ and moisture‐sensitive powders from reaction mixtures of the appropriate alkali metals and resorcinol in thf. Both the potassium and rubidium compounds were structurally characterized by means of powder X‐ray diffraction using the Simulated Annealing method and the Rietveld profile refinement technique including C—C/C—O bond distance and C—C—C angle restraints. K[m‐C₆H₄O(OH)] (orthorhombic P2₁2₁2₁) forms infinite alternating chains of meta‐hydroxyphenolate anions connected by K—O bonds and short charge‐assisted hydrogen bonds, thereby generating a three‐dimensional network of corrugated layers similar to the structure of pure resorcinol. The potassium cations are surrounded by a triangle of oxygen and, moreover, coordinated by six adjacent phenylene rings to form a distorted octahedron. The complex crystal structure of Rb[m‐C₆H₄O(OH)] (monoclinic Pa) is characterized by layers of hydrogen‐bonded meta‐hydroxyphenolate triple units separated by corrugated rubidium layers. The three crystallographically different Rb atoms are coordinated by three, four, and five oxygens with irregular polyhedra, and the rubidiums are also involved in further electrostatic interactions by up to eight phenylene rings.     

Synthesis and Crystal Structure of the Fluoride‐Rich Rubidium Scandium Fluoride Oxosilicate Rb3Sc2F5Si4O10

The new quinary fluoride‐rich rubidium scandium oxosilicate Rb₃Sc₂F₅Si₄O₁₀ was obtained from mixtures of RbF, ScF₃, Sc₂O₃ and SiO₂ in sealed platinum ampoules after seventeen days at 700 °C. The colourless compound crystallises orthorhombically in space group Pnma with a = 962.13(5), b = 825.28(4), c = 1838.76(9) pm and Z = 4. For the oxosilicate partial structure, [SiO₄]^4– tetrahedra are connected in (001) by vertex‐sharing to form corrugated unbranched vierer single layers ${2}\atop{{\infty}}$ {[Si₄O₁₀]^4–} (d(Si–O) = 158–165 pm, ∠(O–Si–O) = 103–114°, ∠(Si–O–Si) = 125–145°) containing six‐membered rings. Similar oxosilicate layers with 6³‐net topology are well‐known for the mineral group of micas or in sanbornite Ba₂Si₄O₁₀. Regarding other systems, identical tetrahedral layers can be found in the synthetic borophosphate Mg(H₂O)₂[B₂P₂O₈(OH)₂] · H₂O. The Sc³⁺ cations are coordinated octahedrally by four F^– and two O^2– anions. These cis‐[ScF₄O₂]^5– octahedra (d(Sc–F) = 200–208 pm, d(Sc–O) = 202–205 pm) share one equatorial and two apical F^– anions with others to build up slightly corrugated ${1}\atop{{\infty}}$ {[Sc₂F${t}\atop{2/1}$ F${v}\atop{6/2}$ O${t}\atop{4/1}$ ]^7–} double chains along [010]. These are linked with the oxosilicate layers via two oxygen vertices to construct a three‐dimensional framework with cavities apt to host the three crystallographically independent Rb⁺ cations with coordination numbers of eleven, twelve and thirteen.     

Ein neues Selten‐Erd‐Metall(III)‐Fluorid‐Oxoselenat(IV): YF[SeO3]

A New Rare‐Earth Metal(III) Fluoride Oxoselenate(IV): YF[SeO₃] Just two representatives of the rare‐earth metal(III) fluoride oxoselenates(IV) with the formula type MF[SeO₃] (M = La and Lu) exist so far, whereas for the intermediate lanthanoids only M₃F[SeO₃]₄‐type compounds (M = Gd and Dy) were accessible. Because of the similar radius of Y³⁺ to the radii of the heavier lanthanoid cations, a missing link within the MF[SeO₃] series could be synthesized now with the example of yttrium(III) fluoride oxoselenate(IV). Contrary to LuF[SeO₃] with its triclinic structure, YF[SeO₃] crystallizes monoclinically in space group P2₁/c (no. 14, a = 657.65(7), b = 689.71(7), c = 717.28(7) pm, β = 99.036(5)° and Z = 4). A single Y³⁺ cation occupying the general site 4e is surrounded by six oxide and two fluoride anions forming [YO₆F₂]^11? polyhedra (d(Y–O) = 228–243 plus 263 pm, d(Y–F) = 219–220 pm). These are linked via common O···O edges to chains running along [010] and adjacent chains get tied to each other by sharing common O3···O3 and O3···F edges which results in sheets parallel to (100). The Se⁴⁺ cations connect these sheets as ψ¹‐tetrahedral [SeO₃]^2? anions (d(Se–O) = 168–174 pm) for charge balance via all oxygen atoms. Despite the different coordination numbers of seven and eight for the rare‐earth metal(III) cations the structures of LuF[SeO₃] and YF[SeO₃] appear quite similar. The chains containing pentagonal bipyramids [LuO₅F₂]^9? are connected to layers running parallel to the (100) plane again. In fact it is only necessary to shorten the partial structure of the straight chains along [001] to achieve the angular chains in YF[SeO₃]. As a result of this shortening one oxide anion at a time moves into the coordination sphere of a neighboring Y³⁺ cation and therefore adds up the coordination number for Y³⁺ to eight. For the synthesis of YF[SeO₃] yttrium sesquioxide (Y₂O₃), yttrium trifluoride (YF₃) and selenium dioxide (SeO₂) in a molar ratio of 1 : 1 : 3 with CsBr as fluxing agent were reacted within five days at 750 °C in evacuated graphitized silica ampoules.     

K3Er7S12 und Rb3Er7S12: Zwei ternäre Erbium(III)‐sulfide mit Kanalstruktur

K₃Er₇S₁₂ and Rb₃Er₇S₁₂: Two Ternary Erbium(III) Sulfides with Channel Structures The isotypic ternary erbium(III) sulfides K₃Er₇S₁₂ (a = 1185.38(9), b = 2461.5(2), c = 393.59(3) pm) and Rb₃Er₇S₁₂ (a = 1203.51(9), b = 2483.0(2), c = 394.85(3) pm; both orthorhombic, Pnnm, Z = 2) are obtained by reacting erbium metal and sulfur with an excess of alkali chloride (KCl or RbCl, respectively) serving as flux and reagent within seven days at 900 °C. The rod—shaped, yellow, transparent single crystals distinguish themselves in their crystal structure by a framework of corner— and edge—linked [ErS₆] octahedra (d(Er³⁺—S^2—) = 265—285 pm), in which the alkali metal cations (K⁺ and Rb⁺, respectively; CN = 6 and 7 + 1) are inserted into channels running along [001]. Under consideration of the ionic radius quotients r_i(A⁺)/r_i(Ch^2—) (A = K—Cs, Ch = S—Te) the existence range of this Cs₃Y₇Se₁₂—type of structure is discussed.     

New Mixed‐Metal Carbonyl Complexes Containing Bridging 2‐Mercapto‐1‐methylimidazole Ligand

Reaction of [Mn₂(CO)₁₀] with 2‐mercapto‐1‐methylimidazole in the presence of Me₃NO at 25 °C afforded two new dimanganese complexes [Mn₂(CO)₆(μ‐SN₂C₄H₅)₂] ( 1 ) and [Mn₂(CO)₇(μ‐SN₂C₄H₅)₂] ( 2 ). Compound 1 consists of two μ‐SN₂C₄H₅ ligands, each bound through the sulfur atom to two Mn atoms and through the nitrogen atom to one Mn atom forming a four‐membered chelate ring. Compound 2 was found to consist of one μ‐SN₂C₄H₅ ligand in a similar bonding mode to 1 but another μ‐SN₂C₄H₅ ligand coordinates through the sulfur atom to one Mn atom and through the nitrogen atom to another Mn atom. Compound 1 was also obtained as the only product from the reaction of [Mn₂(CO)₈(NCMe)₂] with 2‐mercapto‐1‐methylimidazole. In contrast, a similar reaction of [Re₂(CO)₈(NCMe)₂] with 2‐mercapto‐1‐methylimidazole led to the formation of the di‐, tri‐, and tetranuclear complexes [Re₃(CO)₈(μ‐CO)(μ₃‐SN₂C₄H₅)₂(μ‐H)] ( 3 ), [Re₄(CO)₁₂(μ‐SN₂C₄H₅)₄] ( 4 ), and [Re₂(CO)₆(μ‐SN₂C₄H₅)₂] ( 5 ). Compound 3 provides a unique example of a hydrido trirhenium compound. The reaction of [Cr(CO)₃(NCMe)₃] and [Mo(CO)₃(NCMe)₃] with 1 in refluxing THF afforded the mixed metal complexes [CrMn₂(CO)₈(μ‐CO)₂(μ₃‐SN₂C₄H₅)₂] ( 6 ) and [MoMn₂(CO)₈(μ‐CO)₂(μ₃‐SN₂C₄H₅)₂] ( 7 ), respectively, in which two Mn–M (M = Mo, Cr) bonds were formed. In contrast, a similar treatment of [W(CO)₃(NCMe)₃] with 1 yielded two W‐Mn complexes [Mn₂W(CO)₈(μ‐CO)₂(μ₃‐SN₂C₄H₅)₂] ( 8 ) and [Mn₂W(CO)₇(μ‐CO)₂(SN₂C₄H₅)(μ₃‐SN₂C₄H₅)₂] ( 9 ). Treatment of 1 with [Fe₃(CO)₁₂] at 70‐75 °C afforded the trinuclear mixed‐metal complex [FeMn₂(CO)₈(μ‐CO)(μ₃‐SN₂C₄H₅)₂] ( 10 ) and the diiron side product [Fe₂(CO)₆(μ‐S₂N₂C₄H₅)₂] ( 11 ). Compounds 6 ‐ 10 have a bent open structure of three metal atoms linked by two metal‐metal bonds and all, except 9 and 10 , contain a noncrystallographic two‐fold axis of symmetry. Compound 9 is structurally similar to 8 , but it contains a SN₂C₄H₆ ligand, mono coordinated through the exocyclic sulfur atom to the W atom and a Mn–Mn bond instead of a Mn–W bond. Compound 11 comprises two bridging S₂N₂C₄H₅ ligands, which arise from the coupling of 2‐mercapto‐1‐methylimidazole with sulfur.     

Zr6STe2 – ein zirconiumreiches Sulfidtellurid mit einer Zr3Te‐Teilstruktur vom Re3B‐Typ

Zr₆STe₂ – a Zirconium‐rich Sulfide Telluride with a Zr₃Te Partial Structure of the Re₃B Type Zr₆STe₂ is accessible through the reduction of a mixture of ZrTe₂ and ZrS₂ with zirconium in fused tantalum tubes at 1520 K. The spatially averaged crystal structure of Zr₆STe₂ is described in the space group Cmcm, a = 377.81(4), b = 1156.4(1), c = 887.96(8), Z = 2, Pearson symbol oC18, 320 reflexions (I > 2σ(I)), 22 variables, R_w(I) = 0.088. Zr₆STe₂ crystallizes in a unique structure type, which can be seen as a filled Re₃B type structure. The tellurium atoms are surrounded by nine zirconium atoms situated at the vertices of a distorted, tricapped trigonal prism. The Zr₉Te tetrakaidecahedra are connected by common triangular prism faces parallel [100], edges approximately along [001] and common vertices along [010], thus forming a three‐dimensional tetrakaidecahedral network [Zr_9/3Te], which is decisively stabilized by homonuclear Zr–Zr‐interactions. The tetrakaidecahedra are arranged in such a way, that Zr₆ octahedra occur. The octahedra are arranged into layers by sharing edges parallel [100] and vertices along [001]. As a result of a distortion of the structure, every second octahedron is expanded to such an extent as to be able to smoothly accommodate sulfur atoms. According to the modulation of the diffraction intensities, the vacancy ordering in adjacent layers of octahedra occurs independently of each other.