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1.
The structure of a KxP2W4O16 (x ? 0.4) crystal was established by X-ray analysis. The solution in the cell of symmetry P21m, with a = 6.6702(5), b = 5.3228(8), c = 8.9091(8) Å, β = 100.546(7)°, Z = 1, has led to R = 0.033 and Rw = 0.036 for 2155 reflections with σ(I)I ≤ 0.333. This structure can be described as two octahedra-wide ReO3-type slabs connected through “planes” of PO4 tetrahedra. A new structural family KxP2W2nO6n+4 can be foreseen which is closely related to the orthorhombic P4W8O32 and the monoclinic RbxP8W8nO24n+16 series.  相似文献   

2.
The crystal structure of KxP4W14O50 (x = 1.4) has been solved by three-dimensional single crystal X-ray analysis. The refinement in the cell of symmetry A2m, with a = 6.660(2) Å, b = 5.3483(3) Å, c = 27.06(5) Å, and β = 97.20(2)°, Z = 1, has led to R = 0.036 and Rw = 0.039 for 2436 reflections with σ(I)I ≤ 0.333. This structure belongs to the structural family KxP4O8(WO3)2m, called monophosphate tungsten bronzes (MPTB), which is characterized by ReO3-type slabs of various widths connected through PO4 single tetrahedra. This bronze corresponds to the member m = 7 of the series and its framework is built up alternately of strands of three and four WO6 octahedra. The structural relationships with the P4O8(WO3)2m series, called M′PTB, are described and the possibility of intergrowth between these two structures is discussed.  相似文献   

3.
The crystal structure of KP8W40O136, the tenth member of the series KxP4O8(WO3)2m, has been resolved by three-dimensional single-crystal X-ray analysis. The space group is P21c and the cell parameters are a = 19.589(3) Å, b = 7.5362(4) Å, c = 16.970(3) Å and β = 91.864(14)°. The framework is built up from ReO3-type slabs connected through pyrophosphate groups. The structure is compared to those of the other members of the series: although the ReO3-type slabs show a different type of tilting of the WO6 octahedra, the dispersion of WO distances is always higher for the octahedra linked to one or two P2O7 groups and decreases in proportion as W is farther from these groups. The perovskite cages of the slabs are described and compared to those encountered in the structures of WO3 and of the bronzes AxWO3.  相似文献   

4.
During the investigation of the phosphate bronzes (PO2)4(WO3)2m [MPTBP] and Kx(P2O4)2WO3)2m [DPTBH] crystals of a new type were observed. HREM images of these crystals showed twinned ReO3-type slabs the junction of which was parallel to the (102)ReO3 plane. The proposed model identified the twin boundary as built from P2O7 groups involving the formation of pentagonal tunnels. The structure of this new type of extended defects is quite original: it corresponds to a new structural type named “diphosphate tungsten bronzes with pentagonal tunnels” [DPTBP], for which no regular member could be synthesized. Image calculations were performed to confirm the junction model. Apart from the disordered stacking of the ReO3-type slabs, very few defects were observed and shear planes were only obtained in reduced samples. This new structural type takes its place in the large family of phosphate tungsten bronzes where all members (DPTBH, MPTBH, MPTBP) are very closely related.  相似文献   

5.
The phase relations in the cross-section of the K2W2O7-K2WO4-KPO3 containing 15 mol% Bi2O3 were undertaken using flux method. Crystallization fields of K6.5Bi2.5W4P6O34, K2Bi(PO4)(WO4), Bi2WO6, KBi(WO4)2 and their cocrystallization areas were identified. Novel phase K6.5Bi2.5W4P6O34 was characterized by single-crystal X-ray diffraction: sp. gr. P−1, a=9.4170(5), b=9.7166(4), c=17.6050(7) Å, α=90.052(5)°, β=103.880(5)° and γ=90.125(5)°. It has a layered structure, which contains {K7Bi5W8P12O68} layers stacked parallel to ab plane and sheets composed by potassium atoms separating these layers. Sandwich-like {K7Bi5W8P12O68} layers are assembled from [W2P2O13] and [BiPO4] building units, and are penetrated by tunnels with K/Bi atoms inside. FTIR-spectra of K2Bi(PO4)(WO4) and K6.5Bi2.5W4P6O34 were discussed on the basis of factor group theory.  相似文献   

6.
The solid-state synthesis of the oxyfluoride Nb3O5F5, its crystal structure determined from X-ray powder diffraction data as well as some physical characterizations, are reported. Nb3O5F5 constitutes the term n=3 of the NbnO2n−1Fn+2 series related to the Dion-Jacobson phases. It crystallizes, at room temperature, in the tetragonal system (space group I4/mmm (no. 139); Z=4; a=3.9135(1) Å, c=24.2111(2) Å, and V=370.80(3) Å3). The crystal structure appears to be an in-between of the three-dimensional network of NbO2F and the two-dimensional packing of NbOF3 (term n=1 of the NbnO2n−1Fn+2 series). This layered structure consists of slabs made of three Nb(O,F)6 corner-linked octahedra in thickness (n=3) shifted one from another by a ()/translation. Oxygen and fluorine atoms are randomly distributed over all the ligand sites.  相似文献   

7.
Ba11W4O23 was synthesized at 1300 °C, followed by quenching with liquid nitrogen. The crystal structure, which was known to be cryolite-related but has remained unclear, was initially determined by single-crystal X-ray diffraction for the isostructural Ru-substituted compound Ba11(W3.1Ru0.9)O22.5, which was discovered during exploratory synthesis in the Ba-Ru-O system. The structure of Ba11W4O23 was refined by a combined powder X-ray and neutron Rietveld method (Fd-3m, a=17.1823(1) Å, Z=8, Rp=3.09%, Rwp=4.25%, χ2=2.8, 23 °C). The structure is an example of A-site vacancy-ordered 4×4×4 superstructure of a simple perovskite ABO3, and it may be written as (Ba1.750.25)BaWO5.750.25, emphasizing vacancies on both metal and anion sites. The local structure of one of two asymmetric tungsten ions is the WO6 octahedron, typical of perovskite. The other tungsten, however, is surrounded by oxygen and anionic vacancies statistically distributed over three divided sites to form 18 partially occupied oxygen atoms (∼30% on average), represented as WO18/3. The A-site cation-vacancies are ordered at the 8a (, , ) site in between adjoining WO18/3 polyhedra which form 1-D arrangements along [110] and equivalent directions. In situ high-temperature XRD data have shown that the quenched Ba11W4O23 at room temperature is isostructural to the high-temperature phase at 1100 °C.  相似文献   

8.
Single crystal X-ray diffraction photographs taken with a Buerger precession camera, at temperatures 250, 214, and 122 K, corroborate the existence of three low-temperature phases of Ag26I18W4O16. These phases are labeled α′, β, and γ in order of decreasing temperature. The α′ phase is monoclinic, space group P21, Z = 2; the β phase is triclinic, space group P1 or P1, Z = 2; and the γ phase is triclinic, space group P1, Z = 1. Lattice constants at the aforementioned temperatures are given. Twins in the β and γ phases are related by the albite and pericline laws, as are twins in the feldspars. The highest symmetry known to be attained by the (W4O16)8? entity is 2(C2), which, strictly, it must lose at the transition to the α′ phase.  相似文献   

9.
Intercalation behavior of n-alkylamines into a protonated form of an A-site defective layered perovskite H2W2O7 has been investigated. Results from XRD indicate these materials are layered with the corresponding interlayer spacing governed by the n-alkylamine chain length, and a reversible intercalation and deintercalation property is observed among these intercalation compounds. The IR spectra of the intercalation compounds with n-alkylamines clearly show that n-alkyl chains possess an all-trans conformation, and H2W2O7 accommodate n-alkylamines (CnH2n+1NH2: n=3, 4, 7, 8, 12, 16) to form intercalation compounds via an acid-base mechanism. A linear relationship between the interlayer distance and the number of carbon atoms in n-alkyl chains is observed to show a bilayer arrangement of the n-alkyl chains with a tilt angle of ∼71.6°. Elemental analysis studies reveal that the amounts of intercalated n-alkylamines are about 2.0 mol per [W2O7]. Despite the surface geometry of H2W2O7 is almost identical to those of layered perovskites H2[An−1BnO3n+1], the amounts of intercalated n-alkylamines of them are different. A reasonable explanation is given through our research.  相似文献   

10.
Pyrolysis of rare earth (R) polyoxomolybdate, [R2(H2O)12Mo8O27xH2O (R=La, Nd and Sm), at 750°C for 2-8 h results in crystallization of R2Mo4O15 compounds. β-La2Mo4O15 crystallizes together with an α-form in monoclinic P21/a (No. 14), a=13.8893(5), b=13.0757(4), c=20.0927(8) Å, β=95.199(2)°, V=3634.1(2) Å3, Z=12, R1(I>2σ(I))=0.048, Rw (all data)=0.116. The structure is built up with {LaOn} (n=9, 10) and {MoOn′} (n′=4-6) polyhedral units. The {LaOn} units are polymerized into a linear {La6O39} chain, while the {MoOn} are connected together to form {Mo4O15} and {Mo7O26} groups. The structure can be related to the α-form by partial rearrangement of O atoms and small shifts of La and Mo atoms. The R2Mo4O15 (R=Nd and Sm) compounds are isomorphous with the previously reported R=Eu and Gd analogs, crystallizing in triclinic, (No. 2), a=9.4989(5) and 9.4076(7), b=11.0088(7) and 10.9583(8), c=11.5665(6) and 11.5234(8) Å, α=104.141(3) and 104.225(3), β=109.838(3) and 109.603(3), γ=108.912(3) and 108.999(3)°, V=987.3(1) and 970.5(1) Å3, Z=3, R1(I>2σ(I))=0.028 and 0.030, Rw (all data)= 0.079 and 0.094, respectively. The crystal structure is composed of {RO8} and {MoOn′} (n′=4-6) polyhedral units. The molybdate units are condensed to give a corrugated {Mo4O17} chain. The square-antiprismatic {RO8} units share their trigonal and square faces, forming {R2O13} and {R2O12} groups, respectively. A very short R?R distance (3.557(6) Å for R=Nd; 3.4956(6) Å for R=Sm) is achieved in the latter unusual {R2O12} group. A common cationic arrangement was found in all the structures in the R2Mo4O15 family: a R-R pair with the shortest separation and surrounding 12 Mo atoms. The symmetry of the cationic arrangement was reduced with an increase of atomic number of R, viz. La>Ce, Pr>Nd-Gd≈Tb, Ho.  相似文献   

11.
A one-dimensional coordination polymer [Cu(en)2]2[Cu(en)2(H2O)]2{[Cu(en)2]2[Cu2Si2W22O78]}·4.5H2O (en=ethylenediamine), which represents the first example of one-dimensional organic-inorganic hybrid based on the bimolecular Keggin polyoxometalates {[Cu(en)2]2[Cu2Si2W22O78]}8− has been hydrothermally synthesized and characterized by elemental analyses, IR, TG and single crystal X-ray diffraction. Crystal data: C24H85Cu8N24O84.5Si2W22, monoclinic, P21/c, a=18.8126(3), b=23.0896(4), c=26.0711(4) Å, β=96.3790(10)°, V=11254.5(3) Å3, T=293(2) K; Z=4, μ=23.983 mm−1, R1=0.0628, wR2=0.1210 [I>], R1=0.0854, wR2=0.1285 (all data ).  相似文献   

12.
A series of monophosphate tungsten bronzes of composition P4O8(WO3)2m with pentagonal tunnels, MPTBP, have been investigated by high resolution electron microscopy. Most of the micrographs of the integral m members exhibit an asymmetrical contrast which could not be explained qualitatively by the structural models derived from X-ray diffraction studies of some members of the series. Image calculations were thus performed on the m = 4 member (P4W8O32), which showed that the unexpected symmetry does not result from a structural anomaly, but could be due to a titled electron beam. The observations revealed that ordered crystals can be obtained up to m = 16. The investigation of the nonintegral m compositions showed two sorts of intergrowths: disordered intergrowths of different m members belonging to the MPTBP series and ordered intergrowths of the MPTBP structure with a related phosphate tungsten bronze structure based upon hexagonal tunnels.  相似文献   

13.
The crystal structure of Na7Mg4.5(P2O7)4 has been solved by direct methods from the three-dimensional X-ray data. The space group is P1. The crystal structure consists of Mg2+, Na+, and P2O4?7 ions. One magnesium atom at symmetry center (0,0,0) and two sodium atoms at ±(?0.0421, ?0.0596, 0.2230) display occupation factors 0.5 each. A short interatomic distance between these Na+ and Mg2+ ions (1.80 ± 0.01 Å) excludes the occupation of both sites in the same unit cell. The crystal structure of Na7Mg4.5(P2O7)4 consists of unit cells containing Na8Mg4(P2O7)4 or Na6Mg5(P2O7)4 with a statistical occurrence 1:1.Each Mg2+ ion is octahedrally coordinated by six O2? ions at distances 1.979 – 2.270 Å. The coordination polyhedra around the Na+ ions are ill-defined. The bond angles POP in the P2O4?7 groups are 126.6 and 133.6° (±0.3°). The final reliability factor R is 7.1%.  相似文献   

14.
Ce2(MoO4)2(Mo2O7) crystallizes in the triclinic system with unit cell dimensions (from single-crystal data) a = 11.903(8), b = 7.509(5), c = 7.385(5) Å, α = 94.33(8), β = 97.41(8), γ = 88.56(7)°, and space group P1, z = 2. The structure was solved using Patterson (“P1 method”) and Fourier techniques. Of the 8065 unique reflections measured by counter techniques, 6314 with I ≥ 3σ(I) were used in the least-squares refinement of the model to a conventional R of 0.035 (Rw = 0.034). The structure of Ce2(MoO4)2(Mo2O7) consists of dimolybdate chains of the K2Mo2O7 and (NH4)2Mo2O7 type separated by isolated MoO4 tetrahedra and cerium(III) polyhedra.  相似文献   

15.
Crystals of P4W12O44 and P4W16O56 have been synthesized. They are orthorhombic, space group P212121 with a = 5.2927(7), b = 6.5604(7), c = 23.549(3)Å for P4W12O44 and a = 5.2943(5), b = 6.5534(4), c = 29.700(4)Å for P4W16O56. Structures were solved by the heavy-atom method and refined to R = 0.033 (Rw = 0.044) with 2031 independent reflections for P4W12O44 and R = 0.043 (Rw = 0.052) with 2272 independent reflections for P4W16O56. The structures are related to that of P4W8O32 and can be described by the association of zig-zag chains of octahedra and tetrahedra. The members of the series (PO2)4(WO3)2m differ from one another by the length of the links in the chains of polyhedra. Pentagonal tunnels and O18 cages are formed at the junction between the ReO3-type slabs and the slices of PO4 tetrahedra. The surroundings of P and W have been studied and compared with those of other phosphate tungsten bronzes; the relation with the apparent oxidation state of tungsten is discussed.  相似文献   

16.
Complex bismuth oxides with layered structure are prepared with a series of compositions in the system Bi2CaNb2O9-NaNbO3. It is found by X-ray powder diffraction that each compound is composed of more than two phases, which are described by a formula Bi2CaNan?2NbnO3n+3, e.g., in the sample with the nominal composition Bi2CaNb2O9 · 8NaNbO3, the phases with n = 6 to 8 appear predominantly. These phases are closely intergrown to each other. Moreover, high-resolution electron microscopy reveals that microsyntactic intergrowth frequently occurs in the phases with n > 5. The occurrence of the latter intergrowth is explained in terms of the bond length obtained.  相似文献   

17.
KSbP2O8 crystallizes in the rhombohedral system, space group R3, with a = 4.7623(4) Å, c = 25.409(4)Å, and Z = 3. The structure was determined from 487 reflexions collected on a NONIUS CAD4 automatic diffractometer with MoK?α radiation. The final R index and weighted Rw index are 0.030 and 0.038, respectively. This structure is built up from layers of SbO6 octahedra and PO4 tetrahedra sharing corners. These (SbP2O?8)n layers are very similar to the (ZrP2O2?8)n layers in the well-known α-ZrP compound.  相似文献   

18.
The thermal evolution and structural properties of fluorite-related δ-Bi2O3-type Bi9ReO17 were studied with variable temperature neutron powder diffraction, synchrotron X-ray powder diffraction and electron diffraction. The thermodynamically stable room-temperature crystal structure is monoclinic P21/c, a=9.89917(5), b=19.70356(10), c=11.61597(6) Å, β=125.302(2)° (Rp=3.51%, wRp=3.60%) and features clusters of ReO4 tetrahedra embedded in a distorted Bi–O fluorite-like network. This phase is stable up to 725 °C whereupon it transforms to a disordered δ-Bi2O3-like phase, which was modeled with δ-Bi2O3 in cubic Fmm with a=5.7809(1) Å (Rp=2.49%, wRp=2.44%) at 750 °C. Quenching from above 725 °C leads to a different phase, the structure of which has not been solved but appears on the basis of spectroscopic evidence to contain both ReO4 tetrahedra and ReO6 octahedra.  相似文献   

19.
A single crystal of ordered LiAl5O8 has been prepared by image furnace melting and its structure has been determined; 400 X-ray reflections were collected on an automatic counter diffractometer (Mo radiation). The structure is of the spinel type. The space group is P4332 (or P4132); the lattice parameter is a = 7.908(2), Å, Z = 4. The value of R is 0.022. The distribution of cations shows the absence of Li+ ions in tetrahedral cation sites and 1–3 imperfect ordering of Li+ and Al3+ in octahedral cation sites of spinel.  相似文献   

20.
The structure of Cu2Fe2Ge4O13, previously thought to be CuFeGe2O6, has been determined from single-crystal X-ray diffraction data to be monoclinic, P21/m, a=12.1050(6), b=8.5073(4), c=4.8736(2) Å, β=96.145(1)°, Z=2, with R1=0.0231 and wR2=0.0605. The unique structure has an oligomer of four germanate tetrahedra, cross-linked laterally by square-planar copper ions, joined end-to-end by a zigzag chain of edge-sharing iron oxide octahedra. Running along the a-direction the metal oxide chain consists of alternating Cu-Cu and Fe-Fe dimers. A hypothetical series of homologous structures (Cun−2Fe2GenO3n+1 with n=3,4,…,∞) with different length germanate oligomers is proposed, where as n increases, the infinite chain of the CuGeO3 is approached. In this context, Cu2Fe2Ge4O13 is viewed as being built from blocks of CuGeO3 and the Fe oxide chains. This material has significance to the study of low-dimensional mixed-spin systems.  相似文献   

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