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1.
All available oxygen potential-temperature-composition data for the calcium fluorite-structure 〈PuO2?x★★ phase were retrieved from the literature and utilized in the development of a binary solid solution representation of the phase. The data and phase relations are found to be best described by a solution of [Pu43O2] and [PuO2] with a temperature dependent interaction energy. The fluorite-structure 〈U1?zPuzOw〉 is assumed to be represented by a combination of the binaries 〈PuO2?x〉 and 〈UO2 ± x〉, and thus treated as a solution of [Pu43O2], [PuO2], [UO2], and either [U2O4.5] or [U3O7]. The resulting equations well reproduce the large amount of oxygen potential-temperature-composition data for the mixed oxide system, all of which were also retrieved from the literature. These models are the first that appear to display the appropriate oxygen potential-temperature-composition and phase relation behavior over the entire range of existence for the phases.  相似文献   

2.
Homogenisation in mixed UO2-PuO2 compacts has been studied by X-ray diffraction. It is observed that the homogenisation proceeds, mainly, by the assimilation of UO2 into PuO2. This near one-way flow of material, from UO2 to PuO2, is shown to be due to high activity (large BET surface area) of the PuO2 powder as compared with that of the UO2 powder.An X-ray line profile analysis method of determining various mixed composition fractions in sintered mixed compacts has been used to evaluate homogeneity in terms of the fraction of UO2 that has gone into PuO2. A concentric core-shell diffusion model, in which UO2 forms a solute core and PuO2 forms a solvent shell, was used to determine cation interdiffusion coefficients from the homogenisation data. The temperature dependence of cation diffusivity in the range 1573–1873 K is obtained as D = 2.55 × 10?11exp(?2.22 × 105/8.31 T) m2/s. The low value (222 kJ/mole) of activation energy for cation interdiffusion is attributed to the hypostoichiometry of the mixed compacts studied.The diffusivity values at 1573 and 1673 K separately give an activation energy of 126 kJ/mole, which suggests grain-boundary diffusion as the primary mechanism of homogenisation in this temperature range.  相似文献   

3.
UO2 pellets were sintered in flowing H2-N2-H2O gas mixtures at temperatures between 1000 and 1300°C. Sintered density increased with increasing ratio R = partial pressureH2O/partial pressureH2. The results provide a method of produ dense stoichiometric UO2 pellets by means of a single-stage sintering process.  相似文献   

4.
Phase relations in the composition range from UO2+x to U3O8?z were studied by electrical-conductivity measurements and X-ray diffraction in the ranges 1025°C ? T ? 1140°C and 10?7atm ? PO2 ? 10?3atm. The plot of log σ versus log PO2 showed straight lines with distinct slopes, which corresponded to four regions (UO2+x, U4O9?y, U4O9+y and U3O8?z). The existence of the hyperstoichiometric U4O9+y phase was suggested in the temperature range from 1025 to 1126°C. The peritectoid temperature (U4O9±y = UO2+x + U3O8?z) was estimated to be present between 1126 and 1131°C. The partial free enthalpies and entropies for the two-phase equilibrium (U4O9+y + U3O8?z, and U4O9?y + UO2+x) were calculated and compared with previous results. From the dependence of the electrical conductivity on the oxygen partial pressure the nonstoichiometric defect structures of UO2+x and U4O9±y were interpreted as consisting of doubly charged oxygen interstitials (Oi'') and doubly charged oxygen vacancies (VO''). At room temperature, the homogeneity range of the U4O9 phase was investigated with a Debye-Scherrer camera.  相似文献   

5.
A new high-energy laser technique, including fast temperature recording in the microsecond range, was developed for measuring the vapour pressure of fast breeder uranium-plutonium oxide fuels up to 7000 K. In the ternary system, the pressure of uranium-plutonium oxide above its melting point was determined to be log p (atm) = 7.966 ? (28137/T), yielding a high-temperature heat of evaporation of ΔHevap = 128.7 kcal/mol. Measurement of the UO2 partial pressure over the solid gave log p (atm) = 9.365 ? (32436/T), resulting in a heat of sublimation of ΔHsub = 148.4 kcal/mol. The difference of these heats yields the heat of fusion ΔHf = 19.7 kcal/mol, which is in good agreement with the literature value of 19.4 kcal/mol. In the binary UO2 system, the pressure above the melting point was determined to be log p (atm) = 7.7 ? (27900/T),giving a heat of evaporation of ΔHevap = 127.6 kcal/mol. An assessment of literature data for below the melting point yielded log p (atm) = 8.846 ? (31506/T), and a heat of sublimation of ΔHsub = 144.1 kcal/mol. The resulting heat of fusion, ΔHf = 16.5 kcal/mol, is only slightly below the published value of ΔHf = 17.7 kcal/mol.  相似文献   

6.
Using Schuhmann's method the chemical potentials of three components in nonstoichiometric ternary uranium oxides MyU1?yO2+x(M = Mg and Pu) have been calculated. The obtained results are shown in the form of equi-chemical-potential curves (surface of partial molar free energy) in the composition triangle. In the hypostoichiometric region the contour lines of the surface are dense and run parallel with each other. Taking account of this fact the difficulty in attainment of homogeneity in the fabrication of mixed oxide fuel is discussed.  相似文献   

7.
The electrical conductivities of UO2+x. ThO2 and their solid solutions, in thermodynamic equilibrium with the gas phase, were measured as a function of temperature, and of oxygen partial pressure in the temperatnre range 800 to 1200°C. The slope of the plot log α versus 1/T for UO2+x and UO2-rich solid solutions exhibits a single region, whereas in the ThO2-rich solid solutions it exhibits two regions. The pressure dependence of the conductivity (σ) in the UO2-rich solid solutions can be represented by σ ∝ [Oi] ∝ po212 in the range of 0.01 < x < 0.1. Here, Oi is an interstitial oxygen and po2 the partial pressure of oxygen, and it varies with the ThO2 content. At greater deviation from stoichiometry (x ? 0.1) the presence of U4O9 or (Th U)4O9 phases influences the conductivity data. In ThO2 or ThO2-rich solid solutions. P-type conduction at high oxygen pressures is interpreted as arising from the incorporation of excess oxygen into oxygen vacancies.  相似文献   

8.
A model has been developed for calculating oxygen pressures for uranium oxide compositions in the range from the UO2?x metal-rich boundary to UO2,1. The model is based on the law of mass action, the free energy of formation of UO2 and U4O9, and phase boundary data. Oxygen pressures calculated with the model are in excellent agreement with experimental observations.  相似文献   

9.
The entire 〈UO2 ± x★★ data base for the dependence of the nonstoichiometry, x, on temperature and chemical potential of oxygen (oxygen potential) was retrieved from the literature and represented. This data base was interpreted by least-squares analysis using equations derived from the classical thermodynamic theory for the solid solution of a solute in a solvent. For hyperstoichiometric oxide at oxygen potentials more positive than ?266700 + 16.5T J/mol, the data were best represented by a [UO2]-[U3O7] solution. For O/U ratios above 2 and oxygen potentials below this boundary, a [UO2]-[U2O4.5] solution represented the data. The 〈UO2?x data were represented by a [UO2]-[U13] solution. The resulting equations represent the experimental ln(PO2)?ln(x) behavior and can be used in thermodynamic calculations to predict phase boundary compositions consistent with the literature. Collectively, the present analysis permits, for the first time, a mathematical representation of the behavior of the total data base.  相似文献   

10.
The nonstoichiometric composition of Cr2O3±x was measured by means of thermogravimetry in the range of 1173 ≦ T/K ≦ 1318 and 10?15 ≦ PO2/Pa ≦ 105. The compositional deviation from stoichiometry, x, in the hyperstoichiometric Cr2O3+x phase was observed to be smaller than 2 × 10?4, irrespective of temperatures, provided that the hyperstoichiometric Cr2O3+x exists. The existence of the hypostoichiometric Cr2O3?x phase was first established in this study in the region of low oxygen partial pressure below 10?5 Pa. From the oxygen partial pressure dependence of x in Cr2O3?x, the defect structure was discussed with the neutral chromium interstitials in the composition near stoichiometry and with the triply charged ones far from stoichiometry. The partial molar enthalpy and entropy of oxygen of Cr2O3?x showed the complex compositional dependences, suggesting the change of the type of the predominant defect.  相似文献   

11.
12.
The electrical conductivity and nonstoichiometric composition of UO2+x and (U1?yNby)O2+x (y = 0.01, 0.05 and 0.10) were measured in the range 1282 ≦ T ≦ 1373 K and 10?16 ≦ Po2 ≦10?2 Pa by tie four inserted wires method and thermogravimetry, respectively. The electrical conductivity of (U1?yNby)O2+x plotted against the oxygen partial pressure indicated a minimum corresponding to the transition between n- and p-type cone uction. The band-gap energy of (U1?yNby)O2+x was calculated to be (248 ± 12) kJmol.?1, independent of niobium content, which is nearly the same as that of UO2+x. From the oxygen partial pressure dependences of both the electrical conductivity and the deviation x of UO2+x and (U1?yNby)O2+x, the defect structures in these oxides were discussed with the complex defect model consisting of oxygen vacancies and two kinds of interstitial oxygens.  相似文献   

13.
14.
To resolve discrepancies between the existing low temperature ΔG?O2 data for solid solution mixed (U, Pu)-oxide nuclear fuel material, additional measurements have been performed on U0.75Pu0.25O2±x employing a combined thermogravimetric (TGA) and solid-electrolyte galvanic cell technique. These measurements, which were performed at temperatures between 800 and 1000°C, and for O : M ratios in the range 1.940 to 2.028, are reasonably self-consistent and show good agreement with the results of previous TGA measurements. However, they do not corroborate the earlier EMF cell measurements of Markin and McIver. Possible explanations for errors in these earlier EMF cell results are examined. The new results indicate that the ΔG?O2 of stoichiometric mixed oxide at typical outer surface fuel temperatures is close to ?100 kcal/mol O2 (?419 kJ/mol O2). Attempts have been made to fit the new ΔG?O2 data to two equations derived from recent defect models, and it is shown that neither equation accurately represents the experimental po2 ?x data over more than a short range of x.  相似文献   

15.
The high-temperature specific heat of solid UO2, ThO2, and Al2O3 can be represented by an equation of the form Cp(s) = 3nRF(?D/T) + dT3, (1) where ?D is the Debye temperature, F(?D/T) is the Debye function, d represents contributions of the anharmonic vibrations within the lattice, and n denotes the number of atoms per molecule. In the liquid the corresponding equation is Cp(1) = 3nRF(?D/T) + hT2, (2) where h is the anharmonic term. It is shown that for Al2O3 and UO2, where experimental data for the liquid phase are also available, dh has the same value, Indicating that both materials behave identically. If we compare the thermodynamic relationship Cp ? Cv = Vα2KT, (3) where V is the volume, α the volume expansion coefficient, and K the bulk modulus, with equation (1), It follows that d must be equal to 2KT2; the value of 2KT2 is calculated in the temperature region where d was obtained; within experimental error they are equal.  相似文献   

16.
The hot pressing behavior of hyperstoichiometric UO2 and (U, Pu)O2 powders has been evaluated. Specimens with densities in excess of 99% ρth can be fabricated with this technique at temperatures of 1000°C or less.  相似文献   

17.
The vapor pressures over UO2.000 and (U1?yNby)O2+x (y = 0.01, 0.05, x = 0.000–0.022) were measured by the mass-spectrometric method in the temperature range 2025–2343 K. The main gas species over UO2.000 were observed to be UO3(g) and UO2(g) and those over (U1?yNby)O2+x were NbO2(g), NbO(g), UO3(g) and UO2(g). The partial vapor pressures of almost all gas species over (U1?yNby)O2+x increased with increasing O/M (M = U + Nb) ratio. With increasing Nb content in (U1?yNby)O2.000, the partial vapor pressures of UO2(g) and UO3(g) decreased and those of NbO(g) and NbO2(g) increased. The congruently vaporizing composition in the (U1?yNby)O2+x phase was estimated to be (U0.985±0.005Nb0.015±0.005)O2.000 from the compositional dependence of the total vapor pressures. The partial molar enthalpy and entropy of oxygen of (U1?yNby)O2+x calculated from the partial pressures of gaseous species NbO2(g) and NbO(g) were in fairly good agreement with those previously obtained by the present authors with a thermobalance.  相似文献   

18.
19.
Isothermal and isobaric conductivities of UO2+x nave been measured as a function of oxygen pressure and temperature. Intrinsic disorder predominates at low-oxygen pressures. The pressure dependence of the conductivity can be expressed as σ = PO212 in the intermediate oxygen pressure range in which more than one type of charge carrier predominate. At high oxygen pressures, it has been proposed that oxygen vacancy-interstitial trios in association with U+5 ions faciliate the fast transport of oxygen interstitials in the region.  相似文献   

20.
Pressed samples of initial compositions “UC2” + 1 C and “UC2” + 2 C were made to undergo progressive reaction under a gradually increasing pressure of nitrogen (10?3 Torr ≤ PN2 ≤ 760 Torr) in a high-temperature X-ray diffraction apparatus which operated in the range 800–2000°C. In this way, the various equilibrium domains [ α or β “UC2”, C, N2], [α or β “UC2”, UCyNx, C, N2] and [ UCyNx, C, N2], were successively made manifest; this permitted the lattice parameters and equilibrium pressures of the carbonitrides to be determined, and also their standard free enthalpies of formation and compositions to be evaluated. It was established, in particular, that the “dicaibide” and the “monocarbonitride” in equilibrium on the monovariant “plateau” are hypostoichiometric and hyperstoichiometric, respectively; the stability of these compounds is enhanced by their large nitrogen contents, which increase with the temperature. It was also shown that above 1410°C, a temperature rise leads to a substantial drop in the nitrogen content of the virtually stoichiometric monocarbonitride which is in equilibrium with graphite under PN2 ~ 760 Torr. Between 800°C and 1410°C and PN2 ~ 760 Torr, an excess of carbon coexists with α “U2N3” and β “U2N3”, and the lattice parameters of these phases were likewise determined.  相似文献   

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