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Preparation and Properties of (CF3)2EMn(CO)5 (E ? P, As) The complexes (CF3)2EMn(CO)5 (E ? P, As) are formed by the reaction of E2(CF3)4 with HMn(CO)5. They can be converted quantitatively to the binuclear compounds [Mn(CO)4E(CF3)2]2 in a thermal (E ? P) or photochemical (E ? P, As) process. u. v. irradiation of a 1:1 mixture gives the mixed derivative Mn2(CO)8As(CF3)2P(CF3)2 together with the symmetrical systems. The Mn? E bond is less reactive with HBr and Me3SnBr than the M? E bond in derivatives of the type Me3ME(CF3)2 (M ? Si, Ge, Sn; Me ? CH3). The terminal (CF3)2E groups are found to be strong π-acceptor ligands.  相似文献   

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Molecular and Crystal Structures of (CO)4W(μ-S-t-C4H9)2W(CO)4, η7-C7H7W(μ-SC6H4CH3)3W(CO)3 and η7-C7H7W(μ-S-n-C4H9)3W(CO)(μ-S-n-C4H9)2W(CO)4 The molecular structures of the two binuclear complexes (CO)4W(μ-S-t-C4H9)2W(CO)4 and η7-C7H7W(μ-SC6H4CH3)3W(CO)3 and of the tungsten cluster η7-C7H7W(μ-S-n-C4H9)3W(CO)-(μ-S-n-C4H9)2W(CO)4 respectively are described. In the nonlinear trinuclear cluster the central tungsten atom is connected to the two tungsten atoms by two and three μ-S-n-C4H9 bridges respectively and additionally by one W? W bond each. The coordination sphere of the W atoms is completed by a η7-C7H7 ring and four CO groups respectively; the central tungsten carries an additional CO group.  相似文献   

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Decarbonation curve for the synthetic dolomite analogues; (Cd-dolomites) were determined for CdMg(CO3)2, CdMn(CO3)2 and CdZn(CO3)2 under CO2 pressure of up to 2.5 kbar. All the three double carbonates were completely disordered at the decomposition temperatures and hence the thermodynamic data (Standard enthalpy; ΔH f o, Standard free energy; ΔG f o) retrieved from the univariant decarbonation curve corresponds to the disordered phases. They are: The mixing enthalpies and free energies for the formation of the disordered 1∶1 solid solution phases are: The thermodynamic data (ΔH f o, ΔG f o and ΔH r o, ΔG r o) showed a positive correlation with the decomposition temperatures. The mixing energies of the disordered double carbonates also show a direct correlation with the cationic size differences.  相似文献   

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Three new carbonate halides, Cs3Pb2(CO3)3I, KBa2(CO3)2F and RbBa2(CO3)2F have been synthesized with hydrothermal and solid‐state methods. Cs3Pb2(CO3)3I is the first product in the lead carbonate iodides family; KBa2(CO3)2F and RbBa2(CO3)2F are the first two centrosymmetric compounds found in the alkaline–alkaline earth carbonate fluorides family. Cs3Pb2(CO3)3I crystallizes in a centrosymmetric space group C2/m, and exhibits a two‐ dimensional layered structure which is formed by [Cs4Pb4(CO3)6I2] double‐layers consisting of [Pb2(CO3)3I] single‐layers bridged by the Cs atoms. KBa2(CO3)2F and RbBa2(CO3)2F, which are isostructural, crystallize in a trigonal crystal system with a centric space group of R featuring a honeycomb‐like framework. First principle calculations indicate that Cs3Pb2(CO3)3I has a moderate birefringence and explain the difference between the band gaps of the title compounds from electron structures. The effects of cations and halogens on the structures and properties of the title compounds are also discussed.  相似文献   

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The solution obtained by reduction of [(triphos)CO(μ-Cl)2Co(triphos)]+2 (triphos = CH3C(CH2PPh2)3) with Na/Hg reacts with CO2, CS2 and SO2 to give (triphos)Co(O2CO), (triphos)Co(S2CO), and (triphos)Co(O2SO), respectively. The molecular structure of the last has been established by X-ray difraction.  相似文献   

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Summary The stabilities of rosasite, (Cu, Zn)2 (CO3)(OH)2, and aurichalcite, (Zn, Cu)5(CO3)2(OH)6, have been determined by solution experiments with computer calculations of aqueous species in equilibrium with the solid phases. G f o values for rosasite and aurichalcite have been calculated as –1100 and –2766 kJ mol–1 respectively for specific samples of the two minerals. Most of the difference between the free energies of the compounds and those of malachite, Cu2(CO3)(OH)2, and hydrozincite, Zn5(CO3)2(OH)6 arises from substitution of the minor cation in the crystal lattice. Malachite, zincian malachite and rosasite should be considered as a single isomorphous series.Part II: A. K. Alwan and P. A. Williams,Transition Acct. Chem., 4, 319 (1979).  相似文献   

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Since S. Trofimenko introduced these isosteric and isoelectronic ligands with poly(1-pyrazolyl)borates[1],the poly (pyrazolyl)alkane ligands have attracted much attention. Their coordinating behaviour with transition and main group metals has been extensively investigated in recent years[2]. The coordinating behaviour of bis(3,5-dimethylpyrazol-1-yl)ethane is often different from other poly(pyrazolyl) alkanes[3]. The VIB metals carbonyl complexes bonded with poly (pyrazolyl)alkanes have novel structures and unusual reactivities[4,5,6],which encourages us to investigate M-Sn bimetallic complexes with poly(pyrazolyl)alkanes. In this paper, we report the synthesis, characterization and reactivities of poly (pyrazol-1-yl)alkane tetracarbonylmolybdenum (tungsten) with R'SnCl3(R'=Ph,Cl).  相似文献   

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CO, O(2), and H(2) adsorption on a clean W(2)C(0001)√13×√13 R ± 13.9° reconstructed surface at room temperature (RT) were investigated using high-resolution electron energy loss spectroscopy (HREELS). The W(2)C(0001) adsorbs CO molecularly and adsorbs O(2) dissociatively, but does not adsorb H(2) at RT. In the CO adsorption system, two C-O stretching (antisymmetric CCO stretching) modes were found at 242.3 meV (1954 cm(-1)) and at 253.0 meV (2041 cm(-1)). The low-frequency site is occupied at first with subsequent conversion to the high-frequency site with increasing coverage. Additionally, a small peak was apparent at 104.5 meV (843 cm(-1)), and a middle peak at 50-51 meV (400-410 cm(-1)), which are assignable to a symmetric stretching mode and a hindered translational mode, respectively, of a CCO (ketenylidene) species. These observations are consistent with the CO adsorption model on top of the surface carbon. For oxygen adsorption, two adsorption states were found at 65.2-68.1 meV (526-549 cm(-1)) and 73.6 meV (594 cm(-1)): typical frequencies to oxygen adsorption on metal surfaces. Results suggest that atomic oxygen adsorption occurred on a threefold hollow site of the second W layer.  相似文献   

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