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1.
The structure of SiO2-Al2O3 glasses with up to 60 wt% Al2O3 was investigated using the radial distribution function together with the correlation method based on X-ray scattering intensity data. Radial distribution curves are interpreted on the basis of glass-in-glass separation with the constituents of SiO2-rich and Al2O3-rich glasses. The structure of the Al2O3-rich glass has a short-range ordering similar to the crystal structure of mullite. The calculated S- i (S) curve of this model gives good agreement with the observed one.  相似文献   

2.
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   

3.
Thermodynamic data on activities, activity coefficients, and free energies of mixing in SiO2-Al2O3 solutions were calculated from the phase diagram. Positive deviations from ideal mixing in the thermodynamic data suggest a tendency for liquid immiscibility in both SiO2- and Al2O3-rich compositions. The calculated data were used to estimate regions of liquid-liquid immiscibility. A calculated metastable liquid miscibility gap with a consolute temperature of ∼1540°C at a critical composition of ∼36 mol% Al2O3 was considered to be thermodynamically most probable; the gap extended from ∼11 to °49 mol% Al2O3 at 1100°C. SiO2-rich glass compositions showed evidence of glass-in-glass phase separation when examined by direct transmission electron microscopy.  相似文献   

4.
The independent crystallization sequence of an Al2O3 component is modified in the presence of SiO2 and vice versa. Mixed SiO2-Al2O3, gel (28 wt% SiO2 and 72 wt% Al2O3) forms neither cristobalite nor γ-Al2O3 and corundum at 1000°C but forms Si-Al spinel; an amorphous aluminosilicate phase invariably also forms after the gel is heated. However, the composition of this amorphous aluminosilicate phase is not as yet known.  相似文献   

5.
The phase development, microstructure development, and Curie temperature of PbO-BaO-TiO2-Al2O3-SiO2 glass- ceramics were investigated by X-ray diffractometry, electron microscopy, and dilatometry. The primary crystalline phase was perovskite titanate, which exhibited bulk nucle- ation. When the samples were heated at low temperatures, the Curie inversion was hindered and cubic perovskite was obtained. Increased heating temperature/time resulted in tetragonal perovskite. Growth of a surface layer due to the crystallization of the secondary crystalline phase PbO- Al2O3-2SiO2 resulted in the coexistence of coarse and fine perovskite particles. The increase in the relative number of coarse-to-fine perovskite particles with the heating temperature/time was the major factor responsible for increased spontaneous deformation and higher Curie temperature of the perovskite phase. Substitution of barium for lead in the lead titanate phase probably occurred and is explained by the use of SiO2 instead of B2O3 as the glass former in the present study.  相似文献   

6.
NiAl2O4/SiO2 and Co2+-doped NiAl2O4/SiO2 nanocomposite materials of compositions 5% NiO – 6% Al2O3– 89% SiO2 and 0.2% CoO – 4.8% NiO – 6% Al2O3– 89% SiO2, respectively, were prepared by a sol–gel process. NiAl2O4 and cobalt-doped NiAl2O4 nanocrystals were grown in a SiO2 amorphous matrix at around 1073 K by heating the dried gels from 333 to 1173 K at the rate of 1 K/min. The formations of NiAl2O4 and cobalt-doped NiAl2O4 nanocrystals in SiO2 amorphous matrix were confirmed through X-ray powder diffraction, Fourier transform infrared spectroscopy, differential scanning calorimeter, transmission electron microscopy (TEM), and optical absorption spectroscopy techniques. The TEM images revealed the uniform distribution of NiAl2O4 and cobalt-doped NiAl2O4 nanocrystals in the amorphous SiO2 matrix and the size was found to be ∼5–8 nm.  相似文献   

7.
SiO2-Al2O3 melts containing 42 and 60 wt% A12O3 were homogenized at 2090°C (∼10°) and crystallized by various heat treatment schedules in sealed molybdenum crucibles. Mullite containing ∼78 wt% A12O3 precipitated from the 60 wt% A12O3 melts at ∼1325°± 20°C, which is the boundary of a previously calculated liquid miscibility gap. When the homogenized melts were heat-treated within this gap, the A12O3 in the mullite decreased with a corresponding increase in the Al2O3 content of the glass. A similar decrease of Al2O3 in mullite was observed when crystallized melts were reheated at 1725°± 10°C; the lowest A12O3 content (∼73.5 wt%) was in melts that were reheated for 110 h. All melts indicated that the composition of the precipitating mullite was sensitive to the heat treatment of the melts.  相似文献   

8.
The densities of binary aluminosilicate melts were measured X-radiographically as a function of Al2O3, concentration between 1800° and 2000°C. Within this temperature range, the density curves vary linearly and are parallel from fused SiO2 to ≊30 to 45 mol% Al2O3, depending on the temperature. At higher Al2O3 contents, negative deviation from linearity increases with increasing temperature. Recent supplementary research efforts on various aspects of the system SiO2-Al2O3 indicate that the changing coordination and structural role of the aluminum ion may be a primary factor in determining the shapes of the density curves.  相似文献   

9.
Alumina reacts with 1 atm of SiF4 below 660°± 7°C to form A1F3 and SiO2. At higher temperatures the product is a mixture of fluorotopaz and AIF3. Mixtures of fluorotopaz and AIF3 decompose in 1 atm of SiF4 at 973°± 8°C and form tabular α-alumina. The equilibrium vapor pressure of SiF4 above mixtures of fluorotopaz and AlF3 is log p (atm) = 9.198 – 11460/ T (K). Fluorotopaz itself decomposes at 1056°± 5°C in 1 atm of SiF4 to give acicular mullite, 2Al2O3.1.07SiO2. Alumina and mullite are stable in the presence of 1 atm of SiF4 above 973° and 1056°C, respectively. The phase diagram of the system SiO2-Al2O3-SiF4 shows only gas-solid equilibria.  相似文献   

10.
The system Na3AlF6-AlF3-Al2O3 was investigated by a combination of quenching, optical microscopy, and X-ray powder diffraction techniques in order to define liquidus temperatures, univariant lines, and invariant points. Phase fields for the primary crystallization of cryolite, chiolite, aluminum fluoride, α-alumina, and η-alumina were located. A ternary peritectic point contained 28.3% AlF3-4.4% Al2O3-67.3% Na3AlF6 at 723°C. A eutectic point of composition 37.3% AlF3-3.2% Al2O3-59.5% Na3AlF6 occurs at 684°C.  相似文献   

11.
The coordination and bond character of the cations in amorphous SiO2-Al2O3 films prepared by rf sputtering were examined by studying chemical shifts in the SiK and AlK X-ray emission spectra. The coordination number of Si ions in these films was always 4, regardless of composition, whereas the average coordination number of Al ions changed from 4 to 5, depending onAl2O3 content. TheSi-O-Al bond type seemed to appear as Al2O3 was introduced into amorphous SiO2 films or vice versa.  相似文献   

12.
Mechanical mixture of γ-Al2O3 and amorphous SiO2, and diphasic Al2O3/SiO2 gels of three different compositions were synthesized. They were subjected to heat treatment to various temperatures in the range 900°–1600°C. Qualitative X-ray diffraction data show that these diphasic gels do not crystallize to a combined mixture of θ-Al2O3 and α-Al2O3 polymorphs at the intermediate stage, prior to mullite formation. Estimated mullite formation data show that the course of its formation from mixed oxides was different from that of diphasic gels. Results are compared with previous findings and the concept of Al–Si spinel formation in the phase transformation of stoichiometric diphasic gel system is substantiated.  相似文献   

13.
The crystallization of several Nb2O5-catalyzed glasses in the Na2O.Al2O.SiO2 system was studied using DTA, X-ray diffraction, and electron microscopy. The Nb2O5 was an effective nucleation catalyst; fine-grained body-nucleated glass-ceramic materials containing hexagonal nepheline and NaNbO3 were obtained. The crystallization sequence and final crystalline phases in these compositions were quite different from those found in the equivalent TiO2 analogs. The addition of small amounts of carbides and nitrides at the expense of oxides in the initial glass batch markedly affected the final crystalline phases.  相似文献   

14.
SiO2, Al2O3, and 3Al2O3.2SiO2 powders were synthesized by combustion of SiCl4 or/and AlCl3 using a counterflow diffusion flame. The SiO2 and Al2O3 powders produced under various operation conditions were all amorphous and the particles were in the form of agglomerates of small particles (mostly 20 to 30 nm in diameter). The 3Al2O3.2SiO2 powder produced with a low-temperature flame was also amorphous and had a similar morphology. However, those produced with high-temperature flames had poorly crystallized mullite and spinel structure, and the particles, in addition to agglomerates of small particles (20 to 30 nm in diameter), contained larger, spherical particles 150 to 130 nm in diameter). Laser light scattering and extinction measurements of the particle size and number density distributions in the flame suggested that rapid fusion leading to the formation of the larger, spherical particles occurred in a specific region of the flame.  相似文献   

15.
The chemical composition of mullite which was termed from 2SiO23Al2O3 xerogel by firing was examined by analytical TEM. Mullite formed at 950°C firing showed around 66 mol% Al2O3, which was fairly Al2O3 rich compared with the bulk composition. The chemical composition of mullite gradually approached the bulk composition as the firing temperature increased to 1400°C and slightly departed again above that firing temperature.  相似文献   

16.
Stoichiometric mullite (71.38 wt% Al2O3-28.17 wt% SiO2) and 80 wt% Al2O3-20 wt% SiO2 gels were prepared by the single-phase and/or diphasic routes. Dense sintered bodies were prepared from both sets of gels in the Al2O3-SiO2 system. Apparent densities of 96% and 97% of theoretical density were measured for the diphasic (using two sols) mullite samples sintered at 1200° and 1300°C for 100 min, respectively; this compared with 85% and 94% for the single-phase xerogels under the same conditions, and to much lower values for mullite prepared from conventional mixed powders. The microstructure of the mullite pellets from diphasic xerogel precursors is also considerably finer.  相似文献   

17.
Transmission electron microscopy (at 100 and 1000 kV potential) and analytical scanning transmission electron microscopy were used to study α-Al203 second-phase particles and their interactions with grain boundaries in two high-conductivity Y203/Yb203 stabilized zirconia ceramics containing deliberate additions of the alumina as a sintering aid. Most of the Al203 particles were intragranular and microanalysis showed that they contained inclusions rich in Zr or Si plus Zr. Al2O3 particles at grain boundaries were frequently associated with amorphous cusp areas rich in Si and Al. The results suggest that the Al203 acts as a scavenger for SiO2, removing it from grain-boundary localities. A model is proposed whereby this process occurs as the boundaries meet the second-phase particles, assisted by rapid grain-boundary diffusion. Such an ZrO2-Al2O3-SiO2 interaction and partitioning is predicted thermodynamically and offers a possible explanation for the improvements in ionic conductivity brought about by Al2O3 additions, as reported in the literature.  相似文献   

18.
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   

19.
In this study, the isothermal section of a Cu2O–Al2O3–SiO2 pseudo-ternary phase diagram at 1150°C was analyzed by means of a scanning electronic microscope and powder X-ray diffraction of the quenched samples qualitatively, and the compositions of the tie-points of the tie-planes as well as their regions were determined by in situ high-temperature quantitative X-ray diffraction analysis and energy-dispersive X-ray spectroscopy. Then, the isothermal section of the Cu2O–Al2O3–SiO2 pseudo-ternary phase diagram at 1150°C was constructed; it was found that the isothermal section is composed of two single liquid-phase regions, five two-phase regions, and six three-phase regions.  相似文献   

20.
On the basis of 190 runs made up to 1860°C in sealed noble-metal containers the following revisions have been made in the equilibrium diagram for the system A12O3–SiO2. Mullite melts congruently at 1850°C. The extent of equilibrium solid solution in mullite at solidus temperature is from approximately 60 mole % Al2O3 (3/2 ratio) to 63 mole % A12O3. Metastable solid solutions can be prepared up to about 67 mole % Al2O3. There is no evidence for stable solubility of excess SiO2 beyond the 3/2 composition at pressures below 3 kbars. Refractive indices are presented for glasses containing up to 60 mole % Al2O3 and from them the composition of the eutectic is confirmed at 5 mole % SiO2. The variation in lattice constants of the mullite solid solution is not an unequivocal guide to composition since mullites at one composition produced at different temperatures show differences in spacing, no doubt reflecting Al-Si ordering phenomena. The possibility of quartz and corundum being the stable assemblage at some low temperatures and pressures cannot be ruled out. A new anhydrous phase in the system is described, which was previously thought to be synthetic andalusite; it is probably a new polymorph of the Al2SiO5 composition with ortho-rhombic unit-cell dimensions a =7.55 A, b =8.27 A, and c = 5.66 A.  相似文献   

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