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1.
This research was done on hureaulite samples from the Cigana claim, a lithium bearing pegmatite with triphylite and spodumene. The mine is located in Conselheiro Pena, east of Minas Gerais. Chemical analysis was carried out by Electron Microprobe analysis and indicated a manganese rich phase with partial substitution of iron. The calculated chemical formula of the studied sample is: (Mn3.23, Fe1.04, Ca0.19, Mg0.13)(PO4)2.7(HPO4)2.6(OH)4.78. The Raman spectrum of hureaulite is dominated by an intense sharp band at 959 cm−1 assigned to PO stretching vibrations of HPO42− units. The Raman band at 989 cm−1 is assigned to the PO43− stretching vibration. Raman bands at 1007, 1024, 1047, and 1083 cm−1 are attributed to both the HOP and PO antisymmetric stretching vibrations of HPO42− and PO43− units. A set of Raman bands at 531, 543, 564 and 582 cm−1 are assigned to the ν4 bending modes of the HPO42− and PO43− units. Raman bands observed at 414, and 455 cm−1 are attributed to the ν2 HPO42− and PO43− units. The intense A series of Raman and infrared bands in the OH stretching region are assigned to water stretching vibrations. Based upon the position of these bands hydrogen bond distances are calculated. Hydrogen bond distances are short indicating very strong hydrogen bonding in the hureaulite structure. A combination of Raman and infrared spectroscopy enabled aspects of the molecular structure of the mineral hureaulite to be understood.  相似文献   

2.
Ab initio coupled Hartree-Fock perturbation theory (CHFPT) calculations on PO43−, PO3F2−, PO2F2, PF3O, PF4+ and HPO42− using large polarized Gaussian bases satisfactorily reproduce experimental trends in 31P magnetic shielding anisotropies.Accurate evaluation of the shielding tensor for HPO42− requires the inclusion of the H atom. Along the series POa Fb−(2a+b−5) the calculated isotropic shielding shows a “sagging” pattern, i.e. the shielding is smallest for the intermediate member of the series PO3F2−. The shielding for this species is, however, a strong function of the P-F and P-O distances. PO3F2− and HPO42− are calculated to be similar in both average shielding and shielding anisotropy.  相似文献   

3.
《Solid State Sciences》2004,6(5):461-468
The hydrothermal reactions of appropriate vanadium oxides and copper(II) salts with bisterpy in the presence of phosphoric acid or fluorophosphoric acid yield the Cu(II)-bisterpy/oxovanadium phosphate materials [{Cu2(bisterpy)}V3O5(HPO4)2(PO4)] (1) and [{Cu2(bisterpy)}V2O5(HPO4)2] (2). Compound 1 is layered material, consisting of inorganic {V3O5(HPO4)2(PO4)}n4n chains propagating parallel to the crystallographic a-axis, linked in the second dimension through binuclear {Cu2(bisterpy)}4+ units. The chain is constructed from corner-sharing {V4O10(PO4)2}6− and {V2O2(PO4)4}6− cluster building blocks. There are two distinct vanadium sites: a tetrahedral {V(V)O4} site and a square pyramidal {V(IV)O5} center. The Cu(II)-bisterpy subunits are linked to the vanadophosphate chains through phosphate oxygen atoms exclusively. In contrast, the structure of 2 is three-dimensional, exhibiting inorganic {Cu2V2O5(HPO4)2}n networks linked through bisterpy bridges to provide the overall three-dimensional connectivity. The oxovanadium subunit consists of the well-documented {V2O7} binuclear unit of corner-sharing tetrahedral.  相似文献   

4.
Two new mixed‐valence iron phosphates, namely heptairon pentaphosphate hydrogen phosphate, Fe6.67(PO4)5.35(HPO4)0.65, and heptairon tetraphosphate bis(hydrogen phosphate), Fe6.23(PO4)4.45(HPO4)1.55, have been synthesized hydrothermally at 973 K and 0.1 GPa. The structures are similar to that of FeII3FeIII4(PO4)6 and are characterized by infinite chains of Fe polyhedra parallel to the [101] direction. These chains are formed by the Fe1O6 and Fe2O6 octahedra, alternating with the Fe4O5 distorted pentagonal bipyramids, according to the stacking sequence ...Fe1–Fe1–Fe4–Fe2–Fe2.... The Fe3O6 octahedra and PO4 tetrahedra connect the chains together. FeII is localized on the Fe3 and Fe4 sites, whereas FeIII is found in the Fe1 and Fe2 sites, according to bond‐valence calculations. Refined site occupancies indicate the presence of vacancies on the Fe4 site, explained by the substitution mechanism FeII + 2(PO43−) = vacancies + 2(HPO42−).  相似文献   

5.
Calcium hydroxylapatite/carbon nanotubes (HA/CNT) composites with various CNT contents have been synthesized by coprecipitation from aqueous solutions in the CaCl2-(NH4)2HPO4-NH3-CNT-H2O system (25°C) under conditions modeling the interaction between HA (Ca10(PO4)6(OH)2), which is an inorganic component of osseous tissue, and multi-walled CNTs. The empirical formula of the composites is Ca10(PO4)6(OH)2 · nCNT · 6H2O, where n = 0.2?C5.0. The synthesis products have been identified by the solubility (Tananaev??s residual concentration) method, pH measurements, chemical analysis, X-ray diffraction, IR spectroscopy, electron spectroscopy for chemical analysis, and scanning and transmission electron microscopy. The effect of the CNT concentration in aqueous solution on the composition of the HA/CNT composites and on the crystallographic and morphological characteristics of HA nanocrystals in HA/CNT has been investigated.  相似文献   

6.
Two new compounds, (H2en)3(H2enMe)4(H3O){CuI[MoV 6O12(OH)3(HPO4)(PO4)3]2}?·?6H2O (1) and (H2enMe)4{CuICuII[MoV 6O12(OH)3(PO4)(HPO4)2(H2PO4)]2}?·?3H2O (2), were hydrothermally synthesized and characterized by elemental analysis, IR, TGA, and single-crystal X-ray diffraction analysis. Crystallographic analysis reveals that 1 is constructed from cluster anions {CuI[MoV 6O12(OH)3(HPO4)(PO4)3]2}15?, protonated organic amines, and water molecules. Each cluster is bridged through hydrogen bonds to form a 3-D supermolecular structure. For 2, {CuI[MoV 6O12(OH)3(PO4)(HPO4)2(H2PO4)]2}11? are connected by CuII cations to form an infinite chain. The formation of 1 and 2 reveals that organoamines influence the structures of the crystals.  相似文献   

7.
The title compound, hexapotassium octairon(II,III) dodecaphosphonate, exhibiting a two‐dimensional structure, is a new mixed alkali/3d metal phosphite. It crystallizes in the space group Rm, with two crystallographically independent Fe atoms occupying sites of m (Fe1) and 3m (Fe2) symmetry. The Fe2 site is fully occupied, whereas the Fe1 site presents an occupancy factor of 0.757 (3). The three independent O atoms, one of which is disordered, are situated on a mirror and all other atoms are located on special positions with 3m symmetry. Layers of formula [Fe3(HPO3)4]2− are observed in the structure, formed by linear Fe3O12 trimer units, which contain face‐sharing FeO6 octahedra interconnected by (HPO3)2− phosphite oxoanions. The partial occupancy of the Fe1 site might be described by the formation of two [Fe(HPO3)2] layers derived from the [Fe3(HPO3)4]2− layer when the Fe1 atom is absent. Fe2+ is localized at the Fe1 and Fe2 sites of the [Fe3(HPO3)4]2− sheets, whereas Fe3+ is found at the Fe2 sites of the [Fe(HPO3)2] sheets, according to bond‐valence calculations. The K+ cations are located in the interlayer spaces, between the [Fe3(HPO3)4]2− layers, and between the [Fe3(HPO3)4]2− and [Fe(HPO3)2] layers.  相似文献   

8.
The synthesis and characterization of a previously unknown, rare organometallic-phosphate complex, {[Bu4N][(1,5-COD)Ir · HPO4]}n (1), is described. Characterization of 1 was accomplished by elemental analysis, electrospray mass spectrometry (ES-MS), and 1H and 13C NMR which established the symmetry of the product as at least C2 or Cs. The ES-MS reveals an interesting, Ir(I) to Ir(III) oxidative process with intense peaks displaying the 191Ir/193Ir isotopic distribution patterns expected for the fragments [(1,5-COD)IrIII(HPO4)2], [(C8H11)2(IrIII)2(PO4)(HPO4)(H2O)], and [(C8H11)2(IrIII)2(PO4)(HPO4)(H2O)2]. These fragments, in turn, provide evidence for a structure with two HPO42− groups attached to a single Ir, for example ring structures (of at least such C2 or Cs symmetry) such as {[Bu4N][(1,5-COD)Ir · HPO4]}2. Complex 1 is significant since it is known to be the preferred, compositionally precise precursor to the prototype example of a recently discovered class of novel, HPO42− and Bu4N+ stabilized nanoclusters, (Bu4N)2n2n+[Ir(0)n · (HPO4)n]2n. Such nanoclusters are being extended, via their analogous hydrogenphosphate-organometallic precursors (1,5-COD)M+ or 2+/HPO42− (M=Rh(I), Ru(II), Pt(II)) to their corresponding, catalytically active [M(0)n · (HPO4)n]2n nanoclusters.  相似文献   

9.
The aqueous chemistry of phosphorus is dominated by P(V), which under typical environmental conditions (and depending on pH and concentration) can be present as the orthophosphate species H3PO 4 0 (aq),H2PO 4 ? (aq),HPO 4 2? (aq) or PO 4 3? (aq). Many divalent, trivalent and tetravalent metal ions form sparingly soluble orthophosphate phases that, depending on the solution pH and concentrations of phosphate and metal ions, can be solubility limiting phases. Geochemical and chemical engineering modeling of solubilities and speciation require comprehensive thermodynamic databases that include the standard thermodynamic properties for the aqueous species and solid compounds. The most widely used sources for standard thermodynamic properties are the NBS (now NIST) Tables (from 1982 and earlier, with a 1989 erratum) and the final CODATA evaluation (1989). However, a comparison of the reported enthalpies of formation and Gibbs energies of formation for key phosphate compounds and aqueous species, especially H2PO 4 ? (aq) and HPO 4 2? (aq), shows a systematic and nearly constant difference of 6.3 to 6.9 kJ?mol?1 per phosphorus atom between these two evaluations. The existing literature contains numerous studies (including major data summaries) that are based on one or the other of these evaluations. In this report we examine and identify the origin of this difference and conclude that the CODATA evaluation is more reliable. Values of the standard entropies of the H2PO 4 ? (aq) and HPO 4 2? (aq) ions at 298.15 K and p?° =1 bar were re-examined in the light of more recent information and data not considered in the CODATA review, and a slightly different value of S m o (H2PO 4 ? , aq, 298.15 K) = (90.6±1.5) J?K?1?mol?1 was obtained.  相似文献   

10.
A new microporous iron (III) phosphate, [H3N(CH2)4NH3]3[Fe8(HPO4)12(PO4)2(H2O)6], has been prepared using low temperature hydrothermal methods and characterized by single-crystal X-ray diffraction, EDAX, infrared spectroscopy, thermogravimetric analysis and bond valence sums. The title compound crystallizes as light pink hexagonal-shaped tabs in the centrosymmetric hexagonal space group 3¯ (No.147) with a = b = 13.495(2) Å, c = 9.396(2) Å, V = 1481.9(4) Å3 and Z = 4 with R/Rw = 0.044/0.048. The compound exhibits a complicated three-dimensional microporous structure with quaternary ammonium ions acting as a template for the framework. It is similar to previously reported [HN(CH2CH2)3NH]3[Fe8(HPO4)12(PO4)2(H2O)6].  相似文献   

11.
A new compound, Ga6(OH)4(HPO4)2(PO4)5·C8H28N5·3H2O (denoted JGP-L1), with a gallophosphate layer and a Ga/P ratio of 6/7 has been synthesized hydrothermally by using tetraethylenepentamine as template. It is characterized by powder X-ray diffraction (XRD), elemental analysis, inductively coupled plasma, and TGA analysis and structurally determined by single-crystal XRD analysis. JGP-L1 crystallizes in the orthorhombic, space group Pna21 (no. 33), with a=16.422(3), b=11.898(2), c=18.730(4) Å, V=3659.6(13) Å3 and Z=4. The structure of JGP-L1 is built up by alternating of Ga(OH)2O4 octahedra, Ga(OH)O4 trigonal bipyramids and PO4 (or HPO4) tetrahedra to form inorganic sheets. It is noteworthy that JGP-L1 was synthesized with extremely low reactant concentration, where the reaction mixture exhibits a H2O:Ga2O3 molar ratio of 2220:1.  相似文献   

12.
The hybrid 2D compound [{Cu(bpy)}2(VO)3(PO4)2(HPO4)2]·2H2O (1), has been investigated due to its interesting magnetic and catalytic properties. Compound (1) acts as an efficient catalyst in the epoxidation of cyclohexene and styrene. The chemoselectivity towards the epoxidation of cyclohexene is notoriously higher than the one observed towards styrene. The bulk antiferromagnetic behaviour of [{Cu(bpy)}2(VO)3(PO4)2(HPO4)2]·2H2O (1) can be well described with a pentanuclear model, using five J values. Both antiferromagnetic and ferromagnetic interactions mediated by phosphate bridges are found to be present in this hybrid copper(II)–vanadium(IV) material.  相似文献   

13.
Two new gallium phosphates, [NH3(CH2)4NH3][Ga4(PO4)4 (HPO4)] (I) and [NH3(CH2)4NH3][Ga(PO4)(HPO4)] (II), have been synthesized under solvothermal conditions in the presence of 1,4-diaminobutane and their structures determined using room-temperature single-crystal X-ray diffraction data. Compound (I) (Mr=844.90, triclinic, space group P-1, a=9.3619(3), b=10.1158(3) and c=12.6456(5) Å, α=98.485(1), β=107.018(2) and γ=105.424(1)°; V=1070.39 Å3, Z=2, R=3.68% and Rw=4.40% for 2918 observed data [I>3(σ(I))]) consists of GaO4 and PO4 tetrahedra and GaO5 trigonal bipyramids linked to generate an open three-dimensional framework containing 4-, 6-, 8-, and 12-membered rings of alternating Ga- and P-based polyhedra. 1,4-Diaminobutane dications are located in channels bounded by the 12-membered rings in the two-dimensional pore network and are held to the framework by hydrogen bonding. Compound (II) (Mr=350.84, monoclinic, space group P21/c, a=4.8922(1), b=18.3638(6) and c=13.7468(5) Å, β=94.581(1)°; V=1227.76 Å3, Z=4, R=2.95% and Rw=3.37% for 2050 observed data [I>3(σ(I))]) contains chains of edge-sharing 4-membered rings of alternating GaO4 and PO4 tetrahedra constituting a backbone from which hang ‘pendant’ PO3(OH) groups. Hydrogen bonding between the GaPO framework and the diamine dications holds the structure together. A previously reported phase, [NH3(CH2)4NH3][Ga4(PO4)4(HPO4)] (V), structurally related but distinct from its stoichiometric equivalent, (I), has been prepared as a pure phase by this method. Two further materials, [NH3(CH2)5NH3][Ga4(PO4)4(HPO4)] (III) (tricli- nic, lattice parameters from PXD: a=9.3565(4), b=5.0156(2) and c=12.7065(4) Å, α=96.612(3), β=102.747(4) and γ=105.277(3)°) and [NH3(CH2)5NH3][Ga(PO4)(HPO4)] (IV) (Mr=364.86, monoclinic, space group P21/n, a=4.9239(2), b=13.2843(4) and c=19.5339(7) Å, β=96.858(1)°; V=1268.58 Å3, Z=4, R=3.74% and Rw=4.44% for 2224 observed room-temperature data [I>3(σ(I))]), were also prepared under similar conditions in the presence of 1,5-diaminopentane. (III) and (IV) are structurally related to, yet distinct from (I) and (II) respectively.  相似文献   

14.
The mineral crandallite CaAl3(PO4)2(OH)5·(H2O) has been identified in deposits found in the Jenolan Caves, New South Wales, Australia by using a combination of X-ray diffraction and Raman spectroscopic techniques. A comparison is made between the vibrational spectra of crandallite found in the Jenolan Caves and a standard crandallite. Raman and infrared bands are assigned to PO43− and HPO42− stretching and bending modes. The predominant features are the internal vibrations of the PO43− and HPO42− groups. A mechanism for the formation of crandallite is presented and the conditions for the formation are elucidated.  相似文献   

15.
The thermal stability of cesium fluorophosphatohafnates (crystalline CsHf2F2(HPO4)2PO4 · 2H2O, CsHfF2PO4 · 0.5H2O, CsHf2F6PO4 · 4H2O and X-ray amorphous Cs2Hf3O1.5F5(PO4)2 · 5H2O, Cs5H4Hf3F7(PO4)3.66(NO3)3 · 5H2O) was determined. The weight ratios Cs+/Hf and PO 4 3? /ZrHf in CsHf2F2(HPO4)2PO4 · 2H2O were confirmed by identifying the calcination production CsHf2(PO4)3 (~1000°C). A new crystalline compound CsHf2F(HPO4)(PO4)2 was found by thermogravimetric and X-ray powder diffraction analysis during heating. A new method for hydrothermal synthesis of CsHf2(PO4)3, which was different from the already known one, was proposed. It was ascertained that CsHf2(PO4)3 possesses a significant X-ray luminescence; whereas in fluorophosphatehafnates show low luminescence intensity.  相似文献   

16.
A new zero-dimensional (0D) aluminophosphate monomer [dl-Co(en)3]2[Al(HPO4)2(H1.5PO4)2(H2PO4)2](H3PO4)4 (designated AlPO-CJ38) with Al/P ratio of 1/6 has been solvothermally prepared by using racemic cobalt complex dl-Co(en)3Cl3 as the template. The Al atom is octahedrally linked to six P atoms via bridging oxygen atoms, forming a unique [Al(HPO4)2(H1.5PO4)2(H2PO4)2]6? monomer. Notably, there exists intramolecular symmetrical O?H?O bonds, which results in pseudo-4-rings stabilized by the strong H-bonding interactions. The structure is also featured by the existence of four different types of monophosphates that have been confirmed by 31P NMR and 1H NMR spectra. The crystal data are as follows: AlPO-CJ38, [dl-Co(en)3]2[Al(HPO4)2(H1.5PO4)2(H2PO4)2](H3PO4)4, M = 1476.33, monoclinic, C2/c (No. 15), a = 36.028(7) Å, b = 8.9877(18) Å, c = 16.006(3) Å, β = 100.68(3)°, U = 5093.2(18) Å3, Z = 4, R1 = 0.0509 (I > 2σ(I)) and wR2 = 0.1074 (all data). CCDC number 689491.  相似文献   

17.
Germanophosphates, as a young class of metal phosphates, have been less reported but might possess more diverse structural types and potential applications. Here, two one‐dimensional (1D) alkali‐metal germanophosphates (GePOs), namely, hydrogen hexakis(μ‐hydrogen phosphato)digermaniumtrirubidium, HRb3Ge2(HPO4)6 ( 1 ), and caesium bis(μ‐hydrogen phosphato)(μ‐hydroxido)germanium, CsGe(HPO4)2(OH) ( 2 ), have been prepared by the solvothermal method. Compound 1 shows 1D [Ge(HPO4)6] chains along the c axis formed by GeO6 octahedra and PO4 tetrahedra, with Rb+ cations dissociated between the chains. Compound 2 also exhibits 1D [Ge(HPO4)4(OH)2] chains constructed from adjacent Ge(HPO4)4(OH)2 octahedra, with Cs+ cations dissociated between the chains. XRD, TGA, IR and UV–Vis–NIR absorption spectra are presented and discussed for both compounds.  相似文献   

18.
Two new inorganic–organic hybrids, (Hampy)Zn2(PO4) (HPO3) (1) and (ampy)Zn2(HPO3)2 (2), where ampy = 3-(aminomethyl)pyridine, have been solvothermally prepared and structurally characterized. Compound 1 exhibits an unusual two-dimensional layer structure, which possesses a central 4.82 zincophosphate sheet wrapped by infinite zincophosphite chains. Left- and right-handed helical chains participate in the formation of the zincophosphate layer. Compound 2 features a three-dimensional pillared-layer structure, in which two-dimensional ZnII(HPO3) inorganic sheets were cross-linked by ampy ligands. The simultaneous occurrence of zinc-amine helical chains in 2 is unique and, to the best of our knowledge, firstly encountered in phosphite/phosphate hybrid materials. Different coordination modes and roles of the same ampy ligand were observed in the formation of the hybrid structures.  相似文献   

19.
《Polyhedron》1987,6(8):1681-1685
Two distinct reaction rates were found in the formation of 12-molybdophosphate complex. These differences in the formation processes were understood by the use of laser Raman spectroscopy. The reaction of isopolymolybdate (MoO4)2−(MoO3)11 with phosphate PO4⋯- proceeds slowly via formation of 11- molybdophosphate then to produce 12-molybdophosphate taken for 8 min. This reaction mechanism is considered to undergo first the replacement between MoO42− and PO43− then the transformation reaction from 11-molybdophosphate into 12-molybdophosphate. On the other hand, the acidification of the mixed solution of molybdate and phosphate rapidly produces 80% of 12-molybdophosphate within 30 s.  相似文献   

20.
Employing 1-(2-Aminoethyl) piperazine as a template, a new organically templated layered zinc phosphate-phosphite (C6H17N3)[Zn4(PO4)2(HPO3)2] has been prepared hydrothermally. Single-crystal X-ray diffraction analysis shows that it crystallizes in the monoclinic space group Cc with a=5.3272(11) Å, b=17.146(3) Å, c=22.071(4) Å, β=94.58(3)°, V=2009.5(7) Å3, Z=4, R1=0.0201 (I>2σ(I)) and wR2=0.0812 (all data). The inorganic network is based on strictly alternating ZnO4 tetrahedral units and P-centered units including PO4 tetrahedra and HPO3 pseudo-pyramids forming a double layered structure that contains columns of double six-membered rings. The diprotonated 1-(2-Aminoethyl) piperazine molecules reside in the interlayer region and interact with the inorganic network through H-bonds.  相似文献   

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