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探讨了热力学基本原理及判据,以及如何利用吉布斯自由能判断变化的方向和限度;并对Fe/Fe_3O_4纳米磁性材料合成过程中的热力学行为进行了较详细的研究。通过热力学分析,认为可以利用歧化反应及以Fe~(2+)离子作为起始物合成Fe/Fe_3O_4磁性材料。  相似文献   

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Novel Beryllates of the Alkali Metals: Na6Be8O11 For the first time transparent, colourless single crystals of Na6Be8O11 have been prepared (Na2O/BeO; Na:Be = 6:8, Ni-tube; 650°, 14 d). The compound crystallizes triclinic (P1 ) with a = 532.1(1) pm, b = 642.4(2) pm, c = 839.1(2) pm, α = 101.7°, γ = 105.8°, Z = 2, dx = 2.42 g/cm3, dpyk=2.51 g/cm3. The crystal structure was solved by four-circle diffractometer data [Siemens AED 2, MoKα , R = 7.9%, Rw = 6.2%, 1429 I0(hkl)]. Effektive Coordination Numbers, ECoN, these via Mean Fictive Ionic Radii, MEFIR, are calculated.  相似文献   

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Standard values of Gibbs free energy, entropy, and enthalpy of Na2Ti6O13 and Na2Ti3O7 were determined by evaluating emf-measurements of thermodynamically defined solid state electrochemical cells based on a Na–β″-alumina electrolyte. The central part of the anodic half cell consisted of Na2CO3, while two appropriate coexisting phases of the ternary system Na–Ti–O are used as cathodic materials. The cell was placed in an atmosphere containing CO2 and O2. By combining the results of emf-measurements in the temperature range of 573⩽T/K⩽1023 and of adiabatic calorimetric measurements of the heat capacities in the low-temperature region 15⩽T/K⩽300, the thermodynamic data were determined for a wide temperature range of 15⩽T/K⩽1100. The standard molar enthalpy of formation and standard molar entropy at T=298.15 K as determined by emf-measurements are ΔfHm0=(−6277.9±6.5) kJ · mol−1 and Sm0=(404.6±5.3) J · mol−1 · K−1 for Na2Ti6O13 and ΔfHm0=(−3459.2±3.8) kJ · mol−1 and Sm0=(227.8±3.7) J · mol−1 · K−1 for Na2Ti3O7. The standard molar entropy at T=298.15 K obtained from low-temperature calorimetry is Sm0=399.7 J · mol−1 · K−1 and Sm0=229.4 J · mol−1 · K−1 for Na2Ti6O13 and Na2Ti3O7, respectively. The phase widths with respect to Na2O content were studied by using a Na2O-titration technique.  相似文献   

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Ferrites Ni0.75Zn0.25Fe2O4 were obtained by polymeric precursor method and calcined in a short time with microwave energy to assess the morphological and microstructural characteristics. Samples were calcined at 500, 650, 800, and 950 °C for 30 min in a microwave oven. The resulting powders were characterized by thermal analysis (TG/DSC), X-ray diffraction (XRD), Fourier transform infrared spectrometer, field-emission gun scanning electron microscope (FEG-SEM), and energy-dispersive X-ray spectroscopy. The XRD results showed the formation of single ferrite phase at temperature of 500 °C for 30 min. The FEG-SEM analysis showed agglomerated particles with formation of non-dense longitudinal plates, with interparticle porosity and agglomerated fine particles. The rapid calcination by microwave energy demonstrated satisfactory results in relatively low temperature of 500 °C for 30 min and appeared to be a promising technique for obtaining nickel–zinc ferrite powders.  相似文献   

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Thermodynamic studies were carried out for the vapor complex of sodium chloride with hafnium tetrachloride at 712-778 K and 0.5-3.1 kPa by using high temperature phase equilibrium-quenching experiments, with closed Pyrex glass ampoules as the reaction containers. The results show that the sole predominant vapor complex is Na2HfCl6 for the HfCl4-NaCl system under the experimental conditions. The thermodynamic equilibrium constants and other thermodynamic functions of the reaction 2NaCl(s)+HfCl4(g)=Na2HfCl6(g) have been derived from the measurements. The results for the changes in enthalpy and entropy are -65.5§1.5 kJ/mol and -99.6§2.0 J/(mol K) in the temperature range.  相似文献   

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Saal JE  Wang Y  Shang S  Liu ZK 《Inorganic chemistry》2010,49(22):10291-10298
The Gibbs energy function of Sr(6)Co(5)O(15) is calculated by first-principles for use in CALPHAD thermodynamic modeling. An efficient method is employed, using the Debye-Gru?neisen model to predict the temperature dependence of the heat capacity and entropy. The equation of state from first-principles and the Debye temperature from harmonic phonon calculations by the supercell approach are taken as input. The effect of using the GGA+U approach on the results is also reported. The properties of Co(3)O(4) are predicted with this method to compare to experiments and quasi-harmonic phonon calculations and are shown to achieve the accuracy necessary for CALPHAD modeling.  相似文献   

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A new perovskite-related oxide with a composition Ca4Fe2Ti2O11 has been found in the Ca2Fe2O5-Ca TiO3 system. Synthesis and characterization by X-ray diffraction and electron microscopy are reported. A model based on a stacking sequence of … OOOTOOOT′ … along theb axis of this material, corresponding to the structure of a compound withn = 4 in theAnMnO3n−1 series, is proposed.  相似文献   

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Structure determination of the molybdenum purple bronze Na0.9Mo6O17 is carried out by single-crystal X-ray diffraction. The crystal is monoclinic with space group A2 and the lattice constants are a = 12.983(2), b = 5.518(1), c = 9.591(2) Å, β = 89.94(1)°, Z = 2. Full-matrix least-squares refinement gives the final values of R(F) = 0.028 and Rw(F) = 0.040 for 1484 independent reflections, in which the occupancy factor of the sodium atom becomes 0.899(12). The present structure is built up of the linkage of the MoO4 and MoO6 polyhedra. There are slabs which consist of four layers of distorted MoO6 octahedra sharing corners. Both the structure and the molybdenum valence distribution estimated from the MoO bond lengths are considered to lead to the two-dimensional electronic transport. This structure is compared with those of other members of molybdenum purple bronzes, K0.9Mo6O17 and Li0.9Mo6O17. The difference of the electronic properties among these compounds can be well understood on the basis of their structural characteristics.  相似文献   

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The crystal structure of synthetic penkvilksite‐2O, disodium titanium tetrasilicate dihydrate, Na2TiSi4O11·2H2O, a microporous titanosilicate, confirms the major features of a previous model that had been obtained by order–disorder (OD) theory from the known structure of penkvilksite‐1M. An important difference from the previous model involves the hydrogen bonding of the water molecule which, on the basis of a Raman spectrum and the finding of only one of the two H atoms, is proposed to be disordered about a fixed O–H direction. The structure of penkvilksite‐2O is based on (100) silicate layers linked by isolated TiO6 octahedra to form a heteropolyhedral framework. The layer is strongly corrugated, based on interlaced spiral chains, and is crossed by two different channels that have an effective channel width of about 3 Å.  相似文献   

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The crystal structures of Na4SiO4 and Na4GeO4 are isotypic, despite a difference in coordination numbers: in Na4SiO4 only one of the four symmetrically independent sodium atoms is four coordinated, in Na4GeO4 two of them are.
Vergleich der Kristallstrukturen von Natriumorthosilikat, Na4SiO4, und Natriumorthogermanat, Na4GeO4 (Kurze Mitteilung)
Zusammenfassung Die Kristallstrukturen von Na4SiO4 und Na4GeO4 sind isotyp, trotz eines Unterschiedes in den Koordinationszahlen: im Na4SiO4 ist nur eines der symmetrisch unabhängigen Natriumatome vierfach koordiniert, während es im Na4GeO4 derer zwei sind.
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The ion exchange behaviour of the exchanger Na4Ti9O20.xH2O was studied with particular emphasis on Sr2+ exchange. Titration of H4Ti9O20.xH2O with 0.1M [Sr/OH/2+SrCl2] solution yielded a strontium ion exchange capacity of 5.30 meq g–1 corresponding well with the theoretical value. When strontium was absorbed on Na4Ti9O20.xH2O from neutral solutions, Sr2Ti9O20.xH2O was formed. This compound decomposed to SrTiO3 and TiO2 when heated to 870 °C. From alkaline solutions strontium was absorbed both as Sr/OH/+ and Sr2+ with the proportion of the former species increasing with pH. At pH 12.8 only exchange of Sr/OH/+ was observed and the exchanged form was Na2/SrOH/2Ti9O20.xH2O. This compound decomposed to Na2Ti6O13 and an unidentified strontium titanate when heated to 870 °C. Distribution coefficients were determined for alkali and alkaline earth metal ions as a function of pH. The selectivity sequence for alkaline earth metal ions was Ba>SrCa>Mg, and that for alkali metal ions was Cs>K>Li /pH 2–6/ and Li>Cs>K /pH 7/.  相似文献   

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