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1.
The cubic ( c -ZrO2) and tetragonal zirconia ( t -ZrO2) phase stability regions in the system ZrO2–Y2O3–Ta2O5 were delineated. The c -ZrO2 solid solutions are formed with the fluorite structure. The t -ZrO2 solid solutions having a c/a axial ratio (tetragonality) smaller than 1.0203 display high fracture toughness (5 to 14 MPa · m1/2), and their instability/transformability to monoclinic zirconia ( m -ZrO2) increases with increasing tetragonality. On the other hand, the t -ZrO2 solid solutions stabilized at room temperature with tetragonality greater than 1.0203 have low toughness values (2 to 5 MPa · m1/2), and their transformability is not related to the tetragonality.  相似文献   

2.
In the system Ta2O3-Al2O5 solid solutions of metastable δ-Ta2O5 (hexagonal) are formed up to 50 mol% Al2O3 from amorphous materials prepared by the simultaneous hydrolysis of tantalum and aluminum alkoxides. The values of the lattice parameters decrease linearly with increasing Al2O3, content. The to β-Ta2O5 (orthorhombic, low-temperature form) transformation occurs at ∼950°C. The solid solution containing 50 mol% Al2O3 transforms at 1040° to 1100°C to orthorhombic TaAlO4. Orthorhombic TaAlO4 contains octahedral TaO6 groups in the structure.  相似文献   

3.
In the system Nb2O5–Ta2O5, a continuous series of δ-Nb2O5 (δ-Ta2O5) solid solutions with a hexagonal cell is formed while heating amorphous materials prepared by the simultaneous hydrolysis of niobium and tantalum alkoxides. The lattice parameters a and c change linearly with increasing Ta2O5 content; the former value increases from 0.3604 to 0.3620 nm, and the latter value decreases from 0.3923 to 0.3883 nm. They transform to γ-Nb2O5 (β-Ta2O5) solid solutions with an orthorhombic cell at higher temperatures. The changes in lattice parameters a and c as functions of composition are the same as those of hexagonal solid solutions, whereas parameter b is relatively constant.  相似文献   

4.
New phases in the ternary systems ZrO2 (HfO2)-MgO-Nb2O5 (Ta2Os) were identified. These M7O12 compositions have fluorite superstructures isomorphous with the rhombohedral Y6UO12 type.  相似文献   

5.
Fluorite type HfO2 and ZrO2 solid solutions were prepared by doping with 8 to 14 mol% of Ho2O3 and Y2O3, and their lattice parameters were determined. In both HfO2 and ZrO2 systems, the lattice parameters of the solid solutions containing Ho203 were consistently greater than those containing the same amounts of Y2O3. This indicated that the ionic radius of Ho3+ was larger than that of Y3+ in the fluorite structure solid solutions. The effective ionic radius of Y3+ in eightfold coordination was estimated to be 0.1011 nm by using the measured lattice parameters and the empirical equations to predict the lattice parameters of the fluorite-type solid solutions.  相似文献   

6.
A mathematical model of the liquidus surface based on a reduced polynomial method was proposed for the system HfO2-Y2O3-Er2O3. The results of calculations according to this model agree fairly well with the experimental data. Phase equilibria in the system HfO2-Y2O3-Er2O3 were studied on melted (as-cast) and annealed samples using X-ray diffraction (at room and high temperatures) and micro-structural and petrographic analyses. The crystallization paths in the system HfO2-Y2O3-Er2O3 were established. The system HfO2-Y2O3-Er2O3 is characterized by the formation of extended solid solutions based on the fluorite-type (F) form of HfO2 and cubic (C) and hexagonal (H) forms of Y2O3 and Er2O3. The boundary curves of these solid solutions have the minima at 2370°C (15. 5 mol% HfO2, 49. 5 mol% Y2O3) and 2360°C (10. 5 mol% HfO2, 45. 5 mol% Y2O3). No compounds were found to exist in the system investigated.  相似文献   

7.
The phase equilibria in the Y2O3-Nb2O5 system have been studied at temperatures of 1500° and 1700°C in the compositional region of 0-50 mol% Nb2O5. The solubility limits of the C-type Y2O3 cubic phase and the YNbO4 monoclinic phase are 2.5 (±1.0) mol% Nb2O5 and 0.2 (±0.4) mol% Y2O3, respectively, at 1700°C. The fluorite (F) single phase exists in the region of 20.1-27.7 mol% Nb2O5 at 1700°C, and in the region of 21.1-27.0 mol% Nb2O5 at 1500°C, respectively. Conductivity of the Y2O3- x mol% Nb2O5 system increases as the value of x increases, to a maximum at x = 20 in the compositional region of 0 ≤ x ≤ 20, as a result of the increase in the fraction of F phase. In the F single-phase region, the conductivity decreases in the region of 20-25 mol% Nb2O5, because of the decrease in the content of oxygen vacancies, whereas the conductivity at x = 27 is larger than that at x = 25. The conductivity decreases as the value of x increases in the region of 27.5 ≤ x ≤ 50, because of the decrease in the fraction of F. The 20 mol% Nb2O5 sample exhibits the highest conductivity and a very wide range of ionic domain, at least up to log p O2=−20 (where p O2 is given in units of atm), which indicates practical usefulness as an ionic conductor.  相似文献   

8.
On the join LiCrO2-LiAlO2, solid solutions of formulas LiCri- x Al x O2 (0< x <0.6) form. On the spinel join LiAl5O8-"LiCr5O8," solid solutions of formulas LiAl5- x Al x O8 (0< x <3) form and the order-disorder transition, observed in LiAl5O8 at 1295°C, occurs at increasingly lower temperatures with increasing Cr content. No evidence was found for the metastable polymorphs of LiAl5O8 reported by Datta and Roy. Ternary subsolidus equilibria at 1200° to 1300°C were determined for compositions containing <50% Li2O.  相似文献   

9.
The subsolidus phase diagram of the system Bi2O3–ZnO–Ta2O5 in the region of the cubic pyrochlore phase has been determined at 1050°C. This phase forms a solid solution area that includes the ideal composition P, Bi3Zn2Ta3O14; possible solid solution mechanisms are proposed, supported by density measurements of Zn-deficient solid solutions. The general formula of the solid solutions is Bi3+ y Zn2− x Ta3− y O14− x − y , based on the creation of Zn2+, O2− vacancies in Zn-deficient compositions and a variable Bi/Ta ratio.  相似文献   

10.
Tetragonal ZrO2 ( t -ZrO2) solid solutions were prepared with addit ons of 2 mol% Y2O3 plus up to 0.45 mol% Nb2O5. The thermal expansion coefficients in both the a- and c -axis lattice directions increased with Nb2O5 alloying and the thermal expansion in the c -axis direction was greater than that in the a -axis direction over the entire composition range. This anisotropic thermal expansion behavior was related to the 4-fold coordination of Nb5+ with oxygen ions in t -ZrO2 solid solutions in the system ZrO2–Y2O3–Nb2O5. The fracture toughness continuously increased with Nb2O5 alloying and suggested that the c/a axial ratio is a more significant factor than the internal stress that arises from the thermal expansion anisotropy, in the determination of the transformability of t -ZrO2 in this system.  相似文献   

11.
The phase equilibrium relations in the systems Y2O3-Al2O3 and Gd2O3-Fe2O3 were examined. Each system has two stable binary compounds. A 3:s molar ratio garnet-type compound exists in both systems. The 1:1 distorted perovskite structure is stable in the system Gd2O3-Fe2O3 but only metastable in the system Y2O3-AI2O3. This interesting example of metastable formation and persistence of a compound with ions of high Z/r values explains the discrepancies in the literature on the structure of the composition YA1O3. A new 2:1 molar ratio cubic phase has been found in the system Y2O3-A12O3. Since silicon can be completely substituted for aluminum in this compound, the aluminum ions are presumably in fourfold coordination.  相似文献   

12.
Subsolidus phase relations in the low-Y2O3 portion of the system ZrO2-Y2O3 were studied using DTA with fired samples and X-ray phase identification and lattice parameter techniques with quenched samples. Approximately 1.5% Y2O3 is soluble in monoclinic ZrO2, a two-phase monoclinic solid solution plus cubic solid solution region exists to ∼7.5% Y2O3 below ∼500°C, and a two-phase tetragonal solid solution plus cubic solid solution exists from ∼1.5 to 7.5% Y2O3 from ∼500° to ∼1600°C. At higher Y2O3 compositions, cubic ZrO2 solid solution occurs.  相似文献   

13.
The phase relations for the system y2o3–Ta2o5 in the composition range 50 to 100 mol% Y2O3 have been studied by solid-state reactions at 1350°, 1500°, or 17000C and by thermal analyses up to the melting temperatures. Weberite-type orthorhombic phases (W2 phase, space group C2221), fluorite-type cubic phases (F phase, space group Fm3m )and another orthorhombic phase (O phase, space group Cmmm )are found in the system. The W2 phase forms in 75 mol% Y2O3 under 17000C and O phase in 70 mol% Y2O3 up to 1700°C These phases seem to melt incongruently. The F phase forms in about 80 mol% Y2O3 and melts congruently at 2454° 3°C. Two eutectic points seem to exist at about 2220°C 90 mol% Y2O3, and at about 1990°C, 62 mol% Y2O3. A Phase diagram including the above three phases were not identified with each other.  相似文献   

14.
An extensive X-ray study of CeO2–Nd2O3 solid solutions was performed, and the densities of solid solutions containing various concentrations of NdO1.5 were measured using several techniques. Solid solutions containing 0–80 mol% NdO1.5 were synthesized by coprecipitation from Ce(NO3)3 and Nd(NO3)3 aqueous solutions, and the coprecipitated samples were sintered at 1400°C. A fluorite structure was observed for CeO2–NdO1.5 solid solutions with 0–40 mol% NdO1.5, which changed to a rare earth C-type structure at 45–75 mol% NdO1.5. The change in the lattice parameters of CeO2–NdO1.5 solid solutions, when plotted with respect to the NdO1.5 concentration, showed that the lattice parameters followed Vegard's law in both the fluorite and rare earth C-type regions. The maximum solubility limit for NdO1.5 in CeO2 solid solution was approximately 75 mol%. The relationship between the density and the Nd concentration indicated that the defect structure followed the anion vacancy model over the entire range (0–70 mol% NdO1.5) of solid solution.  相似文献   

15.
Compounds in a CaO–Y2O3–SnO2 system were prepared by a solid-state reaction at 1673 K. The phase relation in this system was investigated by powder X-ray diffraction. Besides the previously reported ternary compounds, CaSnO3, Ca2SnO4, Y2Sn2O7, and a quaternary compound Ca0.4Y1.2Sn0.4O3, solid-solution series of Ca2− x Y2 x Sn1− x O4 with 0≤ x ≤0.5, and Ca1− y Y2 y Sn1− y O3 with 0≤ y ≤0.2 and 0.95≤ y ≤1.0 were found. The cell parameters of these solid-solution series were refined. The changes of rhombohedral cell parameters in the samples prepared in the range 0.565< y <0.714 of Ca1− y Y2 y Sn1− y O3 suggested the existence of solid solutions of Ca0.4Y1.2Sn0.4O3, although their single phases could not be prepared, except at y =0.6.  相似文献   

16.
In the binary system PbO–LazO3 only one compound, 4PbO.La2O3, exists; it is flanked by two eutectics. The structure of the compound, although of lower symmetry, is intimately related to the C modification of the rare earths. Below 800° to 1000°C, metastable solid solutions are formed from oxide mixtures coprecipitated from mixed solutions of the nitrates, the cubic parameter a = 5.66 A, if extrapolated to pure La2O3, corresponding to half the a parameter of the C form of La2O3. The solid solutions existing between the compositions La2O3–2Pb0 and pure La2O3 have a cubic face–centered lattice and obey Vegard's rule. The systems of PbO with Sm2O3 and Gd2O8 are quite similar to that with La2O3. The compound Sm2O3.4Pb0 decomposes at 1000°C with evaporation of PbO; Sm2O3 remains in the B modification.  相似文献   

17.
Synthesis of lead tantalate pyrochlores by the reaction of PbO and Ta2O5 in various molar ratios between 1.5 and 4.0 at low temperatures (500–650°C) has been carried out. It has been shown that when PbO is reacted with Ta2O5 in various molar ratios at low temperatures, metastable lead tantalate pyrochlore solid solutions having cubic symmetry are formed. X-ray diffraction data give evidence for an increase in the a lattice parameter with increasing PbO content and partial occupancy of Pb in the Ta sites leading to the formula Pb1.5+ x 2+(Ta2− y Pb y 4+)O7−δ (0.0 < x < 0.5; 0.0 < y < 0.6) for this phase. It has also been found that the intermediate members of the solid solutions are metastable and tend to segregate into Pb-deficient and Pb-excess compositions leading to significant compositional inhomogeneity for the intermediate members.  相似文献   

18.
The subsolidus phase relations in the entire system ZrO2-Y2O3 were established using DTA, expansion measurements, and room- and high-temperature X-ray diffraction. Three eutectoid reactions were found in the system: ( a ) tetragonal zirconia solid solution→monoclinic zirconia solid solution+cubic zirconia solid solution at 4.5 mol% Y2O3 and ∼490°C, ( b ) cubic zirconia solid solutiow→δ-phase Y4Zr3O12+hexagonalphase Y6ZrO11 at 45 mol% Y2O3 and ∼1325°±25°C, and ( c ) yttria C -type solid solution→wcubic zirconia solid solution+ hexagonal phase Y6ZrO11 at ∼72 mol% Y2O3 and 1650°±50°C. Two ordered phases were also found in the system, one at 40 mol% Y2O3 with ideal formula Y4Zr3O12, and another, a new hexagonal phase, at 75 mol% Y2O3 with formula Y6ZrO11. They decompose at 1375° and >1750°C into cubic zirconia solid solution and yttria C -type solid solution, respectively. The extent of the cubic zirconia and yttria C -type solid solution fields was also redetermined. By incorporating the known tetragonal-cubic zirconia transition temperature and the liquidus temperatures in the system, a new tentative phase diagram is given for the system ZrO2-Y2O3.  相似文献   

19.
The system CaO-Ta2O3-SiO2 was studied using a combination of hot-stage microscopy and the quenching technique. Primary crystallization fields were defined for the various calcium silicates, and for the calcium tantalates: CaO·2Ta2O5, CaO·Ta2O5, 2CaO·Ta2O5, and 4CaO·Ta2O5. A congruently melting ternary compound 10CaO·Ta2O5·6SiO2, isostructural with the mineral niocalite, is the only ternary phase in the system. A large twoliquid region extends across the system from the CaO-SiO2 binary to within 1 wt% of the Ta2O3-SiO2 binary but does not cut it, in marked contrast to the analogous CaO-Nb2O5-SiO2 system. Other somewhat unexpected differences were noted between these systems.  相似文献   

20.
α-SiAlONs with equiaxed and elongated microstructures stabilized with Y2O3 and Lu2O3 were produced by hot pressing, and the phase structure and room- and high-temperature mechanical properties were assessed. Additional liquid added to the starting composition in the form of 5 wt% rare-earth monosilicate resulted in the formation of elongated microstructures and improvements in room-temperature strength and fracture toughness. The elongated grain growth was promoted by the additional liquid phase, which crystallized to form a secondary grain-boundary phase thought to be J ' (Re4Si2– x Al x O7+ x N2– x ). For the equiaxed and the elongated samples, those sintered with Lu2O3 showed higher hardness than the comparable Y2O3-sintered materials, and, at elevated temperature, the strength retention of the elongated Lu2O3 SiAlON was much higher than that of the Y2O3 sample, which was attributed to properties of the residual grain-boundary phase associated with the difference in the cationic radius of the stabilizing cation.  相似文献   

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