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1.
The phase diagrams in the Al2O3–Cr2O3 and V2O3–Cr2O3 systems have been assessed by thermodynamic modeling with existing data from the literature. While the regular and subregular solution models were used in the Al2O3–Cr2O3 system to represent the Gibbs free energies of the liquid and solid phases, respectively, the regular solution model was applied to both phases in the V2O3–Cr2O3 system. By using the liquidus, solidus, and/or miscibility gap data, the interaction parameters of the liquid and solid phases were optimized through a multiple linear regression method. The phase diagrams calculated from these models are in good agreement with experimental data. Also, the solid miscibility gap and chemical spinodal in the V2O3–Cr2O3 system were estimated.  相似文献   

2.
Activity–composition relations in Al2O3–Cr2O3 solid solutions at 1500° and 1600°C were determined by equilibrating members of this solid-solution series with Mo–Cr alloys of known activity–composition relations and a gas phase of known oxygen potentials. The oxide solid solution shows considerable positive deviation from ideality.  相似文献   

3.
Subsolidus phase equilibria in the system Fe2O3–Al2O3–TiO2 were investigated between 1000° and 1300°C. Quenched samples were examined using powder X-ray diffraction and electron probe microanalytical methods. The main features of the phase relations were: (a) the presence of an M3O5 solid solution series between end members Fe2TiO5 and Al2TiO5, (b) a miscibility gap along the Fe2O3–Al2O3 binary, (c) an α-M2O3( ss ) ternary solid-solution region based on mutual solubility between Fe2O3, Al2O3, and TiO2, and (d) an extensive three-phase region characterized by the assemblage M3O5+α-M2O3( ss ) + Cor( ss ). A comparison of results with previously established phase relations for the Fe2O3–Al2O3–TiO2 system shows considerable discrepancy.  相似文献   

4.
Activities of NiO were measured in the oxide and spinel solutions of the system MnO–NiO–Al2O3 at 1300° and 1400° C with the aim of deriving information on the thermodynamic properties of the spinel phases. Synthetic samples in selected phase assemblages of the system were equilibrated with metallic nickel and a gas phase of known oxygen partial pressures at a total pressure of 1 atm. The data on NiO activities and directions of conjugation lines between coexisting oxide and spinel phases were used to establish the activity–composition relations in spinel solid solutions at 1300° and 1400°C. The MnAl2O4–NiAl2O4 solid solutions exhibit considerable negative deviations from ideality at these temperatures. The free energy of formation of MnAl2O4 from its oxide components (MnO + Al2O3) at 1300° and 1400°C is calculated to be −24.97 and −26.56 kJ. mol−1, respectively. The activities determined in the stoichiometric spinel solid solutions are more negative as compared with those predicted from cation distribution models.  相似文献   

5.
Thermal and X-ray studies show that there is complete solid solution between MgO.Cr2O3 and MgO.Al2O3 and that the spinel solid solutions are stable with no exsolution down to temperatures as low as 510°C. There is no solid solution of excess Cr2O3 in MgO.Cr2O3 nor of MgO.Cr2O3 in Cr2O3. The join MgO.Cr2O3–Al2O3 is found to be nonbinary; compositions along that join yield mixtures of a chromium oxide-alumina solid solution and a spinel solid solution on firing to temperatures high enough to promote solid-state reaction. Chromium oxide loss by volatilization increases at higher temperature. At a given temperature, chromium oxide loss is found to vary directly with the partial pressure of oxygen in the furnace atmosphere and with the ratio of MgO to SiO2 in the charges heated.  相似文献   

6.
An isothermal section of the ternary system MgO–Al2O3-Cr2O3 was determined at 1700°± 15°C to delineate the stability field for spinel crystalline solutions (cs). Crystalline solutions were found between the pseudobinary joins MgAl2O4–Cr2O3 and MgCr2O4-Al2O3, and the binary join MgAl2O4-MgO. The first two crystalline solutions exhibit cation vacancy models while the latter can probably be designated as a cation interstitial model. Precipitation from spinel cs may proceed directly to an equilibrium phase, (Al1-xCrx)2O3, with the corundum structure or through a metastable phase of the probable composition Mg(Al1-xCr)26O40. The composition and temperature limits were defined where the precipitation occurs via metastable monoclinic phases. The coherency of the metastable monoclinic phase with the spinel cs matrix can be understood by considering volume changes with equivalent numbers of oxygens and known crystallographic orientation relations. Electron probe and metallographic microscope investigations showed no preferential grain boundary precipitation.  相似文献   

7.
Schairer's study (1954) on phase relations in the system KalSi2O6–Mg2SiO4–SiO2 was extended to include the system KalSiO4–Mg2SiO4–KalSi2O6. It is shown that this join is ternary; however, the relatively high vapor pressure of the condensed phases prohibits study by the usual quenching techniques. The apparent intersection of the (KalSiO4–Mg2SiO4–SiO3) join with the primary phase volume of spinel is attributed to loss of the alkali-silicate constituents by vapor transport. This results in the effective bulk composition being moved away from this join toward the primary phase volume of spinel in the system K2O–MgO–Al2O3–SiO2.  相似文献   

8.
Phase equilibria in the system MnO–CoO–Cr2O3 were investigated at 1300°C under controlled oxygen partial pressures by using the gas equilibration technique. The CoO activities in various phase assemblages of the system were measured by determining the partial pressures of oxygen in the gas phase for coexistence with metallic cobalt. The activity data revealed that at 1300°C, MnO–CoO and MnCr2O4–CoCr2O4 solid solutions exhibit mild positive departures from ideal behavior. The activities in the stoichiometric spinel solutions were found to be in good agreement with those predicted from a model based on cation distribution equilibria. The standard free energy of formation of the compound CoCr2O4 from its oxide components at 1300°C was determined as −37 636 J/mol, while that for MnCr2O4 was found as −44 316 J/mol.  相似文献   

9.
Liquidus phase equilibrium data are presented for the system Al2O3-Cr2O3-SiO2. The liquidus diagram is dominated by a large, high-temperature, two-liquid region overlying the primary phase field of corundum solid solution. Other important features are a narrow field for mullite solid solution, a very small cristobalite field, and a ternary eutectic at 1580°C. The eutectic liquid (6Al2O3-ICr2O3-93SiO2) coexists with a mullite solid solution (61Al2O3-10Cr2O3-29SiO2), a corundum solid solution (19Al2O3-81Cr2O3), and cristobalite (SO2). Diagrams are presented to show courses of fractional crystallization, courses of equilibrium crystallization, and phase relations on isothermal planes at 1800°, 1700°, and 1575°C. Tie lines were sketched to indicate the composition of coexisting mullite and corundum solid solution phases.  相似文献   

10.
The isoplethal sections CaAl2O4–MgO and CaAl4O7–MgO of the Al2O3–MgO–CaO ternary system have been experimentally established at 1 bar total pressure and air of normal humidity. The sections obtained provide new data and information that are in disagreement with thermodynamic evaluations and optimizations of the Al2O3–MgO–CaO ternary system published to date. These differences arise mainly from the inclusion, or exclusion, of the binary compound Ca12Al14O33, mayenite, as a stable phase in the reported studies of the system. The presence or absence of this compound within the system has an important impact on the solid state and melting relationships of the whole ternary system. The present study confirms the solid-state compatibility CaAl2O4–MgO and CaAl2O4–MgO–MgAl2O4 up to 1372°± 2°C, the peritectic melting point of the later mentioned subsystem.  相似文献   

11.
Phase relations and lattice constants in the MgO–Al2O3–Ga2O3 system at 1550°C have been determined experimentally. In a large part of this system, only a nonstoichiometric spinel is stable. Compositions as extreme as 12.5 mol% MgO–20.5 mol% Ga2O3–67 mol% Al2O3 for a homogeneous spinel are possible. In the bordering phase diagrams of MgO–Al2O3 and MgO–Ga2O3, the composition of the spinel is as high as 63 mol% Al2O3 or Ga2O3, respectively. The contributions of all simple ionic exchange reactions on the lattice constant of the spinel have been deduced from X-ray diffractometry data.  相似文献   

12.
The phase relations at a temperature below "subsolidus" in the system Al2O3–B2O3–Nd2O3 are reported. Specimens were prepared from various compositions of Al2O3, B2O3, and Nd2O3 of purity 99.5%, 99.99%, and 99.9%, respectively, and fired at 1100°C. There are six binary compounds and one ternary compound in this system. The ternary compound, NdAl3(BO3)4 (NAB), has a phase transition at 950°C ± 15°C. The high-temperature form of NAB has a second harmonic generation (SHG) efficiency of KH2PO4 (KDP) of the order of magnitude of the form which has been used as a good self-activated laser material, and the low-temperature form of NAB has no SHG efficiency.  相似文献   

13.
Liquidus equilibrium relations for the air isobaric section of the system Y2O3–Fe2O3–FeO–Al2O3 are presented. A Complete solid-solution series is found between yttrium iron garnet and yttrium aluminum garnet as well as extensive solid solutions in the spinel, hematite, orthoferrite, and corundum phases. Minimum melting temperatures are raised progressively with the addition of alumina from 1469°C in the system Y–Fe–O to a quaternary isobaric peritectic at 1547°C and composition Y 0.22 Fe 1.08 Al 0.70 O 2.83* Liquidus temperatures increase rapidly with alumina substitutions beyond this point. The thermal stability of the garnet phase is increased with alumina substitution to the extent that above composition Y 0.75 Fe 0.65 Al 0.60 O 3 garnet melts directly to oxide liquid without the intrusion of the orthoferrite phase. Garnet solid solutions between Y 0.75 Fe 1.25 O 3 and Y 0.75 Fe 0.32- Al 0.93 O 3 can be crystallized from oxide liquids at minimum temperatures ranging from 1469° to 1547°C, respectively. During equilibrium crystallization of the garnet phase, large changes in composition occur through reaction with the liquid. Unless care is taken to minimize temperature fluctuations and unless growth proceeds very slowly, the crystals may show extensive compositional variation from core to exterior.  相似文献   

14.
The quenching method has been used to determine approximate phase relations in the system iron oxide-Cr2O3 in air. Only two crystalline phases, a sesquioxide solid solution (Fe2O3–Cr2O3) with corundum structure and a spinel solid solution (approximately FeO ·Fe2O3–FeO – Cr2O3), occur in this system at conditions of temperature and O2 partial pressure (0.21 atm.) used in this investigation. Liquidus temperatures increase rapidly as Cr2O3 is added to iron oxide, from 1591°C. for the pure iron oxide end member to a maximum of approximately 2265°C. for Cr2O3. Spinel(ss) is the primary crystalline phase in iron oxide-rich mixtures and sesquioxide (ss) in Cr2O3–rich mixtures. These two crystalline phases are present together in equilibrium with a liquid and gas (po2= 0.21 atm.) at approximately 2075°C.  相似文献   

15.
Solid-state compatibility and melting relations of MgAl2O4 in the quaternary system Al2O3–CaO–MgO–SiO2 were studied by firing and quenching selected samples located in the 65 wt% MgAl2O4, plane followed by microstructural and energy dispersive X-ray analysis. A projection of the liquidus surface of the primary crystallization volume of MgAl2O4 was constructed from CaO, SiO2 and exceeding Al2O3, not involved in stoichiometric MgAl2O4 formation; those three amounts were recalculated to 100 wt%. The temperature and character of six invariant points, where four solids co-exist with a liquid phase, were defined. One maximum point was localized and the positions of the isotherms were tentatively established. The effect of CaO, SiO2, and Al2O3 impurities on the high temperature behavior of spinel materials was also discussed.  相似文献   

16.
The UO2–Al2O3 phase equilibrium system was found to contain no new compounds or solid solutions. Uranium dioxide melted at 2878°± 22°C. and Al2O3 melted at 2034°± 16°C. The eutectic temperature was approximately 1930°C. There is an indication that two immiscible liquids formed above the eutectic temperature between 53 and 74 mole % Al2O3.  相似文献   

17.
Al2O3–ZrO2–SiC whisker composites were prepared by surface-induced coating of the precursor for the ZrO2 phase on the kinetically stable colloid particles of Al2O3 and SiC whisker. The fabricated composites were characterized by a uniform spatial distribution of ZrO2 and SiC whisker phases throughout the Al2O3 matrix. The fracture toughness values of the Al2O3–15 vol% ZrO2–20 vol% SiC whisker composites (∼12 MPa.m1/2) are substantially greater than those of comparable Al2O3–SiC whisker composites, indicating that both the toughening resulting from the process zone mechanism and that caused by the reinforced SiC whiskers work simultaneously in hot-pressed composites.  相似文献   

18.
The sintering of a composite of MgO–B2O3–Al2O3 glass and Al2O3 filler is terminated due to the crystallization of Al4B2O9 in the glass. The densification of a composite of MgO–B2O3–Al2O3 glass and Al2O3 filler using pressureless sintering was accomplished by lowering the sintering temperature of the composite. The sintering temperature was lowered by the addition of small amounts of alkali metal oxides to the MgO–B2O3–Al2O3 glass system. The resultant composite has a four-point bending strength of 280 MPa, a coefficient of thermal expansion (RT—200°C) of 4.4 × 10−6 K−1, a dielectric constant of 6.0 at 1 MHz, porosity of approximately 1%, and moisture resistance.  相似文献   

19.
Amorphous films in the system Al2O3–Y2O3 were prepared by the rf sputtering method in the range of 0–76 mol% Y2O3, and their density, refractive index, and elastic constants were measured. All of the physical properties of the amorphous Al2O3–Y2O3 films had a similar compositional dependence; that is, they increased continuously, but not linearly with increasing Y2O3 content. To confirm the coordination states of aluminum and yttrium ions in the amorphous Al2O3–Y2O3 films, the Al K α X-ray emission spectra and the X-ray absorption near edge structures (XANES) were measured. The average coordination number of aluminum ions in the amorphous films containing up to about 40 mol% Y2O3 content was 5, that is a mixture of 4-fold- and 6-fold-coordinated states. In the region of more than about 50 mol% Y2O3, the fraction of the 6-fold-coordinated aluminum ions increased with increasing Y2O3 content, while the results led to the conclusion that the coordination number of yttrium ions was always 6, regardless of composition. These results indicate that, in amorphous films in the system Al2O3–Y2O3, the change of the coordination state of aluminum ions has an important effect on physical properties.  相似文献   

20.
Refractory bodies of 65 wt% Al2O3 were prepared from a mixture of calcined alumina and raw kaolin with the addition of Cr2O3 up to 15 wt%. The Cr2O3 addition effectively enhances slag resistance and reduces mullite formation. Petrographic analysis of the refractories after the slag test suggests that Cr2O3 increases the viscosity of both the glassy phase in the refractory as well as the slag, thereby retarding slag penetration and reaction at elevated temperature.  相似文献   

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