J. Am. Ceram. Soc., 83 [4] 919 –27 (2000) journal Ternary System Al2O3–MgO–CaO: Part II, Phase Relationships in the Subsystem Al2O3–MgAl2O4–CaAl4O7 Antonio H. De Aza,† Juan E. Iglesias,‡ Pilar Pena,† and Salvador De Aza*,† Instituto de Cerámica y Vidrio, CSIC, Madrid, Spain; and Instituto de Ciencia de Materiales, CSIC, Madrid, Spain (CaAl12O19 or CA6§) or through the existence of a new ternary phase within the above-mentioned ternary system, whose stoichiometric composition is tentatively assigned as CaMg2Al16O27 (CM2A8). Göbbels et al.2 and Iyi et al.3 have published articles on this topic. In the first article, the authors studied the subsolidus phase relations in the Al2O3-rich part of the system Al2O3–MgO–CaO and found two new compounds. These compounds are located on the joint connecting CA6 and spinel (MgAl2O4). Their stoichiometric compositions are given as Ca2Mg2Al28O46 (C2M2A14) and CaMg2Al16O27 (CM2A8), denoted as CAM I and CAM II by Göbbels et al. Both compositions show limited solid solubility range. On the other hand, in the second article, the structure models of both compounds were established by high-resolution electron microscopy, and structure refinements were conducted using single-crystal X-ray diffractometry (XRD) data. However, these works provide no detailed information on the melting relationships of the new crystalline phases. Furthermore, a theoretical study of the solid-state compatibilities in the Al2O3-rich part of the system Al2O3–MgO–CaO published by Göbbels et al.2 showed that, once the “Law of Adjoining Phase Regions” of Palatnick and Landau4 was taken into account, several errors in the isothermal sections were obvious. Despite these errors, these works were of significant assistance on clarifying the results of the above-mentioned preliminary experiments conducted in the present investigation. The goal of the present work is to determine solid-state compatibilities and melting relationships in the subsystem Al2O3– MgAl2O4–CaAl4O7. The results obtained in Part I1 and literature data are used to establish a phase diagram of the entire system Al2O3–MgO–CaO. Solid-state compatibility and melting relationships in the subsystem Al2O3–MgAl2O4–CaAl4O7 were studied by firing and quenching selected samples located in the isopletal section (CaO䡠MgO)–Al2O3. The samples then were examined using X-ray diffractomtery, optical microscopy, and scanning and transmission electron microscopies with wavelength- and energy-dispersive spectroscopies, respectively. The temperature, composition, and character of the ternary invariant points of the subsystem were established. The existence of two new ternary phases (Ca2Mg2Al28O46 and CaMg2Al16O27) was confirmed, and the composition, temperature, and peritectic character of their melting points were determined. The isothermal sections at 1650°, 1750°, and 1840°C of this subsystem were plotted, and the solid-solution ranges of CaAl4O7, CaAl12O19, MgAl2O4, Ca2Mg2Al28O46, and CaMg2Al16O27 were determined at various temperatures. The experimental data obtained in this investigation, those reported in Part I of this work, and those found in the literature were used to establish the projection of the liquidus surface of the ternary system Al2O3–MgO–CaO. I. Introduction in the Part I of this work,1 the ternary system Al2O3–MgO–CaO is extremely important in many technological applications, in particular, refractories. In Part I, the spinel primary phase field of crystallization in the subsystem MgAl2O4–CaAl4O7–CaO–MgO was established to understand why spinel addition to high-Al2O3 concretes significantly improves the wear resistance of these materials in secondary steel refining ladles. In the present research, the work is mainly focused on determining the solid-state compatibility and melting relationships in the subsystem Al2O3–MgAl2O4–CaAl4O7 to understand properly phase constitution of the matrices of these materials and, consequently, their melting behavior. Preliminary experiments, conducted in the subsolidus region of the system, showed that the solid-state compatibilities and melting relationships within this part of the system Al2O3–MgO–CaO are complexed, mainly because of the existence of phases whose microanalyses (scanning electron microscopy–wavelengthdispersive spectroscopy (SEM-WDS)) agreed with none of the compositions of the expected phases. The data could be explained either as a wide but limited solid solution of MgO in the magnetoplumbite structure of the calcium hexa-aluminate A S DISCUSSED II. Experimental Procedure With the purpose of establishing the Al2O3-rich part of the system Al2O3–MgO–CaO, nine selected compositions (Table I) located in the isopletal section doloma¶–alumina ((CaO䡠MgO)– Al2O3) in the range 76.04 –100 wt% Al2O3 were prepared and studied. An additional composition to those studied in the isopletal section (CaO䡠MgO)–Al2O3 was also prepared. This composition corresponded to the compound CaMg2Al16O27 (CM2A8). Calculated batches were weighed, starting from the materials described in Part I of this work,1 and were processed in the manner described in the previous paper. The samples were thermally treated between 1625° and 1950°C. Treatments up to 1725°C were made under the conditions described in Part I. Thermal treatments between 1725° and 1950°C were conducted in an argon atmosphere in a Brew furnace (200 mm diameter and 200 mm high; LBL, Berkeley, CA) with tantalum heating elements. The samples (5 mm diameter and R. S. Roth—contributing editor Manuscript No. 189562. Received February 12, 1999; approved September 20, 1999. Supported by Plan Nacional de Materiales CICYT and European Union under Project Nos. MAT97–0728 and BRPR-CT97–0427, respectively. *Member, American Ceramic Society. † Instituto de Cerámica y Vidrio. ‡ Instituto de Ciencia de Materiales. § Cement notation is used in the text and figure captions of this article; i.e., C is CaO, M is MgO, and A is Al2O3 (e.g., CA6 is CaO䡠6Al2O3 or CaAl12O19). ¶ Product derived from the burning or calcining of dolomite or dolomite rock. It contains a mixture of MgO and CaO relative to proportions of originally existing carbonates. 919 920 Journal of the American Ceramic Society—De Aza et al. Table I. Selected Compositions in the Isopletal Section (CaO䡠MgO)–Al2O3† in the Range of 76.04 wt% up to 100 wt% Al2O3 Designation CaO Composition (wt%) MgO Al2O3 77 79 81 83 85 88 (Ca2Mg2Al28O46) 89 91 94 CaMg2Al16O27‡ 13.3815 12.2179 11.0543 9.8907 8.7270 6.9225 6.3998 5.2362 3.4908 5.8884 9.6185 8.7821 7.9457 7.1093 6.2730 4.9759 4.6002 3.7638 2.5092 8.4651 77 79 81 83 85 88.1016 89 91 94 85.6465 † In the range 76.04–100 wt% Al2O3. ‡Additional composition outside of the isopletal section. 6 mm long) were placed into molybdenum crucibles (15 mm long and 8 mm in diameter) that were hermetically sealed by welding. Temperature was controlled by a W5Re–W26Re thermocouple (maximum temperature of 2320°C) encapsulated in a beryllium sheath and connected to an electronic digital controller (⫾1°C; Vol. 83, No. 4 Model Eurotherm 900, EPC, Edinburgh, U.K.). The temperature of the furnace was frequently checked against the melting points of platinum and rhodium, using an optical pyrometer. At temperatures ⬍1725°C, the samples, after heat treatment, were air quenched.1 In thermal treatments conducted above 1725°C in the Brew furnace, the samples were quenched inside the furnace by switching off the power. This provided a very fast cooling of the furnace chamber and of the samples, because the furnace walls were refrigerated by a continuous flux of cold water. Occasionally, the samples were reground after quenching, then pressed and fired again to ensure the attainment of equilibrium. After the samples were quenched, they were removed from the platinum or molybdenum crucibles and mounted in epoxy resin. The samples then were polished to 1 m. The phases present in the equilibrated specimens were determined and analyzed using the techniques described in Part I. However, the two new phases (Ca2Mg2Al28O46 and CaMg2Al16O27) were prepared by ion-beam thinning and were studied by transmission electron microscopy (TEM; Model JEM-2010, JEOL, Tokyo, Japan) at 200 kV using a high-resolution technique (HR-TEM) involving lattice plane imaging. All TEM samples were carbon coated to ensure specimen stability in the electron beam. X-ray powder pattern lattice parameter refinements of the two new compounds were conducted (see Appendix). Fig. 1. Experimental isopletal section (CaO䡠MgO)–Al2O3 in the range 76.04 –100 wt% Al2O3. Symbols represent samples studied (see Table I). April 2000 Ternary System Al2O3–MgO–CaO 921 Fig. 2. SEM micrographs of typical samples within various fields of crystallization: (a) sample 77 at 1712° ⫾ 1°C for 4 ⫹ 7 h with coexisting phases CaAl4O7 (CA2) ⫹ MgAl2O4(ss) (MA); (b) sample 79 at 1712° ⫾ 1°C for 4 ⫹ 7 h with coexisting phases CaAl2O4 (CA2) ⫹ MgAl2O4(ss) (MA) ⫹ CaMg2Al16O27(ss) (CM2A8); (c) sample 88 at 1725° ⫾ 1°C for 4 ⫹ 4 h with coexisting phases Ca2Mg2Al28O46(ss) (C2M2A14) ⫹ CaMg2Al16O27(ss) (CM2A8); and (d) sample 94 at 1750° ⫾ 1°C for 12 ⫹ 12 h with coexisting phases Al2O3 ⫹ MgAl2O4(ss) (MA) ⫹ Ca2Mg2Al28O46(ss) (C2M2A14). Solid-state compatibilities and melting relationships in the subsystem Al2O3–MgAl2O4–CaAl4O7 were established using the experimental procedure described in Part I.1 III. Results and Discussion The experimental segment 76.04 –100 wt% Al2O3 of the isopletal section of(CaO䡠MgO)–Al2O3 that was plotted with the results obtained, after heat treatment at various temperatures of the selected compositions, is shown in Fig. 1. The data obtained confirmed the existence of the two new compounds Ca2Mg2Al28O46 and CaMg2Al16O27 proposed by Göbbels et al.2 These compounds were clearly identified by XRD (see Appendix), SEM-WDS, and HR-TEM. HR-TEM also allowed us to confirm the laminar structure of both compounds, being polytypoids with structures derived from that of CA6. In the case of the CaMg2Al16O27, the stacking sequence (MS)n†† also has †† M is CA6 blocks; S is spinel blocks. been confirmed; however, this is not the case for Ca2Mg2Al28O46, which requires further studies (see Appendix). The obtained section provides new information that is in disagreement with published literature data. The isopletal section shows the existence of the solid-state compatibility Ca2Mg2Al28O46(ss)–Al2O3 that was omitted by Göbbels et al.2 These phases are compatible up to 1725° ⫾ 10°C. Above this temperature, the solid-state compatibility changes; the phases Al2O3, MgAl2O4(ss), and Ca2Mg2Al28O46(ss) coexist up to 1830°⫾10°C. At this temperature, the compatibility changes again; Al2O3, MgAl2O4(ss), and CaAl12O19(ss) are in equilibrium with each other. This compatibility change is not indicated by Göbbels et al. Finally, the phases Al2O3, MgAl2O4(ss), and CaAl12O19(ss) coexist up to 1850° ⫾ 10°C, which is the temperature of the peritectic melting point of this subsystem. The solid-state compatibility changes can be explained by changes in the free energy of formation of the phases Ca2Mg2Al28O46, CaMg2Al16O27, and MgAl2O4 as a consequence of the variation of their solid solutions with the temperature. The remaining ternary subsystems, indicated in the isopletal section (Fig. 1), are in agreement with those reported by Göbbels 922 Journal of the American Ceramic Society—De Aza et al. Vol. 83, No. 4 Table II. Samples Analyzed by SEM–WDS Temperature (°C) Time of treatment (h) 1650 26 ⫹ 25 26 ⫹ 25 26 ⫹ 25 26 ⫹ 25 26 ⫹ 25 26 ⫹ 25 1750 10 ⫹ 14 10 ⫹ 14 10 ⫹ 14 10 ⫹ 14 4 10 ⫹ 14 10 ⫹ 14 10 ⫹ 14 ⫹ 20 1840 4 4 4 3⫹7 Composition Phases in equilibrium 77 79 85 88 91 CaMg2Al16O27 MgAl2O4(ss) ⫹ CaAl4O7 MgAl2O4(ss) ⫹ CaAl4O7 ⫹ CaMg2Al16O27 CaAl4O7 ⫹ CaMg2Al16O27(ss) ⫹ Ca2Mg2Al28O46 CaMg2Al16O27(ss) ⫹ Ca2Mg2Al28O46(ss) Ca2Mg2Al28O46(ss) ⫹ Al2O3 CaMg2Al16O27(ss) ⫹ MgAl2O4(ss)? 77 79 81 83 85 88 89 91 MgAl2O4(ss) ⫹ liquid MgAl2O4(ss) ⫹ CaMg2Al16O27(ss) ⫹ liquid MgAl2O4(ss) ⫹ CaMg2Al16O27(ss) ⫹ liquid MgAl2O4(ss) ⫹ CaMg2Al16O27(ss) ⫹ liquid CaMg2Al16O27(ss) ⫹ Ca2Mg2Al28O46(ss) ⫹ liquid CaMg2Al16O27(ss) ⫹ Ca2Mg2Al28O46(ss) CaMg2Al16O27(ss) ⫹ Ca2Mg2Al28O46(ss) MgAl2O4(ss) ⫹ Ca2Mg2Al28O46(ss) ⫹ Al2O3 81 88 89 94 Liquid MgAl2O4(ss) ⫹ CaAl12O19(ss) ⫹ liquid MgAl2O4(ss) ⫹ CaAl12O19(ss) ⫹ liquid MgAl2O4(ss) ⫹ CaAl12O19(ss) ⫹ Al2O3 et al.2 The temperature and character of the ternary subsystem invariant points also are indicated in Fig. 1. (These data and their compositions are presented later in Table V.) Figures 2(a)–(d) show typical SEM microstructures, within different fields of crystallization, of samples after quenching from various annealing temperatures. To determine the projection of the liquidus surface of the subsystem Al2O3–MgAl2O4–CaAl4O7, the composition of the various phases coexisting at equilibrium in selected samples, within the isopletal section (Fig. 1) at different temperatures, were quantitatively determined by SEM-WDS. Table II shows the selected compositions, their temperatures, the times of treatment, and the coexisting phases. For the sake of simplicity, the analyzed samples and the results obtained for a series of isothermal sections at 1650°, 1750°, and 1840°C are discussed below. (1) Isothermal Section at 1650°C The isothermal section at 1650°C was plotted by projecting the data obtained from compositions treated at 1650°C (see Fig. 1) together with data reported by Göbbels et al.2 This section, shown in Fig. 3, is subsolidus throughout. The various solid-state compatibility relationships have been indicated and described in the figure caption. Numbers in italic represent experimental samples used to construct the figure (see Fig. 1 and Table II). The data of the solid-solution ranges determined and used to plot the isothermal section are shown in Table III. This experimental section obeys the “Law of the Adjoining Phase Regions.”4 (2) Isothermal Section at 1750°C The isothermal section at 1750°C is shown in Fig. 4. It was plotted using data obtained in the study of compositions treated at Fig. 3. Isothermal section at 1650°C of the subsystem Al2O3–MgAl2O4–CaAl4O7. Coexisting phases are (a) CaAl4O7 ⫹ MgAl2O4(ss), (b) CaAl4O7 ⫹ MgAl2O4(ss) ⫹ CaMg2Al16O27(ss), (c) MgAl2O4(ss) ⫹ CaMg2Al16O27(ss), (d) MgAl2O4(ss) ⫹ CaMg2Al16O27(ss) ⫹ Al2O3, (e) CaMg2 Al16O27(ss) ⫹ Al2O3, (f) CaMg2Al16O27(ss) ⫹ Al2O3 ⫹ Ca2Mg2Al28O46(ss), (g) Al2O3 ⫹ Ca2Mg2Al28O46(ss), (h) Al2O3 ⫹ Ca2Mg2Al28O46(ss) ⫹ CaAl12O19 (ss), (i) Al2O3 ⫹ CaAl12O19(ss), (j) CaAl12O19(ss), (k) CaAl12O19(ss) ⫹ CaAl4O7, (l) CaAl12O19(ss) ⫹ CaAl4O7 ⫹ Ca2Mg2Al28O46(ss), (m) CaAl4O7 ⫹ Ca2Mg2Al28O46(ss), (n) CaAl4O7 ⫹ Ca2Mg2Al28O46(ss) ⫹ CaMg2Al16O27(ss), (o) CaAl4O7 ⫹ CaMg2Al16O27(ss), (p) CaMg2Al16O27(ss), (q) CaMg2Al16O27(ss) ⫹ Ca2Mg2Al28O46(ss), (r) Ca2Mg2Al28O46(ss), and (s) Ca2Mg2Al28O46(ss) ⫹ CaAl12O19(ss). Numbers in italics are experimental compositions (see Fig. 1). April 2000 Ternary System Al2O3–MgO–CaO 923 Table III. Solid-Solution Ranges at 1650°C Solid-state compatibilities † Mg1–3zAl2⫹2zVazO4 (1) CaAl4O7–MgAl2O4(ss) (2) CaMg2Al16O27(ss) ⫹ MgAl2O4(ss) ⫹ CaAl4O7 (3) CaMg2Al16O27(ss)–MgAl2O4(ss) (16) CaMg2Al16O27(ss) (18) Ca2Mg2Al28O46(ss) Ca2Mg2–3xAl28⫹2xO46 0 ⱕ z ⱕ 0.07 z ⫽ 0.07 0.07 ⱕ z ⱕ 0.12 0 ⱕ x ⱕ 0.30 CaMg2–3yAl16⫹2yO27 y⫽0 0 ⱕ y ⱕ 0.15 0 ⱕ y ⱕ 0.20 CaAl4O7 CaAl4O7 CaAl4O7 †Numbers in parantheses correspond to those assigned in to the different solid-state compatibilities Fig. 3. Fig. 4. Isothermal section at 1750°C of the subsystem Al2O3–MgAl2O4–CaAl4O7. Coexisting phases are (a) MgAl2O4(ss) ⫹ liquid, (b) MgAl2O4(ss) ⫹ CaMg2Al16O27(ss) ⫹ liquid, (c) MgAl2O4(ss) ⫹ CaMg2Al16O27(ss), (d) MgAl2O4(ss) ⫹ CaMg2Al16O27(ss) ⫹ Ca2Mg2Al28O46(ss), (e) MgAl2O4(ss) ⫹ Ca2Mg2Al28O46(ss), (f) MgAl2O4(ss) ⫹ Ca2Mg2Al28O46(ss) ⫹ Al2O3, (g) Ca2Mg2Al28O46(ss) ⫹ Al2O3, (h) Ca2Mg2Al28O46(ss) ⫹ Al2O3 ⫹ CaAl12O19(ss), (i) Al2O3 ⫹ CaAl12O19(ss), (j) CaAl12O19(ss), (k) CaAl12O19(ss) ⫹ CaAl2O7, (l) CaAl12O19(ss) ⫹ CaAl2O7 ⫹ Ca2Mg2Al28O46(ss), (m) CaAl2O7 ⫹ Ca2Mg2Al28O46(ss), (n) CaAl2O7 ⫹ Ca2Mg2Al28O46(ss) ⫹ liquid, (o) Ca2Mg2Al28O46(ss) ⫹ liquid, (p) Ca2Mg2Al28O46(ss) ⫹ CaMg2Al16O27(ss) ⫹ liquid, (q) CaMg2Al16O27(ss) ⫹liquid, (r) CaMg2Al16O27(ss), (s) CaMg2Al16O27(ss) ⫹ Ca2Mg2Al28O46(ss), (t) Ca2Mg2Al28O46(ss), and (u) Ca2Mg2Al28O46(ss) ⫹ CaAl12O19(ss). Numbers in italics are experimental compositions (see Fig. 1). 1750°C within the isopletal section (Fig. 1). The different phase relationships are indicated in the figure and described in the figure caption. The solid-solution ranges determined and used to plot the isothermal section are shown in Table IV. In the isothermal section at 1750°C, liquid phases already appear, which implies that the isopletal section at 1800°C proposed by Göbbels et al.2 is not accurate. In this section the “Law of the Adjoining Phase Regions”4 is also fulfilled. The composition of the spinel and CA6 coexisting with liquid at 1840°C correspond to Mg1–3zAl2⫹2zVazO4 with z ⫽ 0.24 and CaMgxAl12–2x/3O19 with x ⫽ 0.18. However, the solid solutions in Al2O3 and CA6 coexisting with spinel at 1840°C are negligible and within experimental error. For simplicity, as previously presented, the different phase relations have been marked in the figure and described in the figure caption This experimental section also obeys the “Law of the Adjoining Phase Regions.”4 (3) Isothermal Section at 1840°C The isothermal section at 1840°C was plotted with data obtained from experimental compositions treated at the mentioned temperature (see Fig. 1). Figure 5 shows this isothermal section. (4) Liquidus Surface of the Subsystem Al2O3–MgAl2O4– CaAl4O7 With all the information obtained, the projection of the liquidus surface of the subsystem Al2O3–MgAl2O4–CaAl4O7 was established. Figure 6 shows the outline of this liquidus surface. The Table IV. Solid-Solution Ranges at 1750°C Coexisting phases † (1) MgAl2O4(ss) ⫹ liquid (2) MgAl2O4(ss) ⫹ CaMg2Al16O27(ss) ⫹ liquid (3) MgAl2O4(ss) ⫹ CaMg2Al16O27(ss) (6) MgAl2O4(ss) ⫹ Ca2Mg2Al28O46(ss) ⫹ Al2O3 (16) CaMg2Al16O27(ss) ⫹ Ca2Mg2Al28O46(ss) ⫹ liquid † Mg1–3zAl2⫹2zVazO4 0 ⱕ z ⱕ 0.09 z ⫽ 0.09 0.09 ⱕ z ⱕ 0.19 z ⫽ 0.21 Numbers in parentheses correspond to those assigned to the different phase compatibilities in Fig. 4. Ca2Mg2–3xAl28⫹2xO46 x ⫽ 0.26 x⫽0 CaMg2–3yAl16⫹2yO27 y⫽0 0 ⱕ y ⱕ 0.20 y ⫽ 0.05 Al2O3 924 Journal of the American Ceramic Society—De Aza et al. Vol. 83, No. 4 Fig. 5. Isothermal section at 1840°C of the subsystem Al2O3–MgAl2O4–CaAl4O7. Coexisting phases are (a) MgAl2O4(ss) ⫹ liquid, (b) MgAl2O4(ss) ⫹ CaAl12O19(ss) ⫹ liquid, (c) MgAl2O4(ss) ⫹ CaAl12O19(ss), (d) MgAl2O4(ss) ⫹ CaAl12O19(ss) ⫹ Al2O3, (e) CaAl12O19(ss) ⫹ Al2O3, (f) CaAl12O19(ss), and (g) CaAl12O19(ss) ⫹ liquid. Numbers in italics are experimental compositions (see Fig. 1). Fig. 6. Projection of the liquidus surface of the subsystem Al2O3–MgAl2O4–CaAl4O7. For composition, temperature, and character of the invariant points, see Table V. compositions, temperatures, and character of the various invariant points within the subsystem are shown in Table V. For the sake of simplicity, the solid-state compatibility triangles have been omitted at the temperature of the corresponding invariant points. The new phases Ca2Mg2Al28O46 and CaMg2Al16O27 (see Appendix) melt incongruently at 1830° ⫾ 10°C and 1820° ⫾ 10°C, respectively, according to the reactions Ca2Mg2Al28O46 3 MgAl2O4 ⫹ CaAl12O19 ⫹ liquid CaMg2Al16O27 3 MgAl2O4 ⫹ Ca2Mg2Al28O46 ⫹ liquid High temperatures are observed for the first liquid formation (ⱖ1730°C) in this region of the ternary system Al2O3–MgO–CaO. This justifies the high refractoriness of materials designed in this area of the system, especially if they are formulated in the subsystem Al2O3–MgAl2O4(ss)–CaAl12O19, where the temperature of first liquid formation is 1850°⫾10°C (Table V). (5) Liquidus Surface of the System Al2O3–MgO–CaO The experimental data obtained in Parts I and II of this investigation and the data collected from the literature were used to establish the entire projection of the liquidus surface of the ternary system Al2O3–MgO–CaO (Fig. 7). The composition, temperatures, and character of all the invariant points within the system are indicated in Table V. The liquidus surface shows a large primary field of crystallization of the spinel within the ternary system Al2O3–MgO–CaO, as compared with those of calcium aluminates, which means low April 2000 Ternary System Al2O3–MgO–CaO 925 Table V. Composition, Temperature, and Character of Invariant Points within Ternary System Al2O3–MgO–CaO† Points p1 e1 e2 e3 e4 p2 e5 e6 e7 P1 E1 E2 E3 P2 P3 P4 E4 P5 P6 P7 P8 P9 Al2O3 CaO MgO † Temperature (°C) 1539 1400 1390 1590 1776 1883 1995 1975 2370 1450 1321 1346 1344 1350 1372 1567 1730 1760 1740 1820 1830 1850 2045 2625 2825 Al2O3 ⫾5 42.8 48.31 53.03 65.75 79.74 87.37 55 96.01 ⫾5 42.3 47.85 50 50.74 51.11 52.5 63.2 78.25 79.25 78.75 80.0 81.2 86.0 100 ⫾3 ⫾ ⫾ ⫾ ⫾ ⫾ ⫾ ⫾ ⫾ ⫾ 2 2 10 10 10 10 10 10 5 Composition (wt%) CaO MgO 57.2 51.69 46.97 34.25 20.26 12.63 67 51.5 46.40 44.26 43.88 42.59 40.55 33.3 18.0 19.75 19.0 14.5 12.5 6.5 45 3.99 33 6.20 5.75 5.74 5.38 6.30 6.95 3.50 3.75 1.0 2.25 5.5 6.3 7.5 100 100 Comments and references Peritectic (Nurse et al.6) Eutectic (Chatterjee and Zhmoidin7) Eutectic (Chatterjee and Zhmoidin7) Eutectic (Rolin and Pham8,9) Eutectic (Rolin and Pham8,9 and Hallstedt10) Peritectic (Hallstedt10) Eutectic (Alper et al.11) Eutectic (Viechnicki et al.12) Eutectic (Doman et al.13) Peritectic (Ranking and Merwin14) Eutectic (Majundar15) Eutectic (Majundar15) Eutectic (Majundar15) Peritectic (Majundar15) Peritectic Peritectic Eutectic Peritectic Peritectic Peritectic Peritectic Peritectic In Ar (Viechnicki et al.12) (Doman et al.13) In N2 (McNally et al.16) Points whose text is italicized are those determined in the present investigation and in Part I of this work.1 solubility and adequate chemical resistance to slags containing CaO–MgO. IV. Conclusions (a) The projection of the liquidus surface of the subsystem Al2O4–MgAl2O4–CaAl4O7 has been experimentally established. The solid-state compatibility relations, compositions, temperatures, and character of the various invariant points and the extension of the primary phase fields of crystallization of the various phases also have been determined. (b) The existence of two new ternary phases Ca2Mg2Al28O46 and CaMg2Al16O27 within the subsystem have been confirmed. The temperature, composition, and peritectic character of their melting points also have been established. (c) The range of the solid solutions, at different temperatures, of the phases CaAl4O7, CaAl12O19, MgAl2O4, Ca2Mg2Al28O46, and CaMg2Al16O27 also have been determined within the various compatibility triangles. (d) The high temperatures of first liquid formation involved (ⱖ1730° ⫾ 10°C) in the Al2O3-rich part of the ternary system Al2O3–MgO–CaO justifies the high refractory characteristics of materials designed in this area of the system, particularly if they are formulated within the subsystem Al2O3–MgAl2O4– CaAl12O19, where the temperature of first liquid formation is 1850°⫾10°C. (e) The results obtained confirm the greater refractoriness of the high-Al2O3 refractory concretes bonded with spinel and calcium aluminate cements, as compared with that of the traditional high-Al2O3 concretes bonded only with calcium aluminate cements, in which the highest temperature of initial liquid-phase formation is ⬃1547° ⫾ 5°C. (f) The phase diagram of the entire ternary system Al2O3– MgO–CaO has been established using all the experimental and literature information obtained. Appendix (1) Phase Characterization of Ca2Mg2Al28O46 and CaMg2Al16O27 Ca2Mg2Al28O46 and CaMg2Al16O27 were obtained from stoichiometric amounts of 99.99-wt%-pure Al2O3 (Fluka AG, Buchs, Switzerland), 99.5-wt%-pure CaCO3, and 99.9-wt%-pure MgO (E. Merk, Darmstadt, Germany). The samples were homogenized, isostatically pressed at 200 MPa, and solid-state reacted at 1700°C for various lengths of time with repeated millings and reheatings. The powder patterns of these materials were obtained on a diffractometer (R ⫽ 230 mm, Model X⬘pert, Philips, Eindhoven, The Netherlands) fitted with an incident-beam Ge (111) monochromator of the symmetric Johansson type using CuK␣1 ( ⫽ 1.5405981 Å) radiation. Soller slits of 1.1° axial divergence were placed in the path of the diffraction beam; the equatorial divergence was 0.5°. The /2 scan mode was used, and intensities were measured for 10 s at 0.03° intervals while the sample was rotated around an axis normal to its plane at ⬃2 Hz. The patterns were obtained using the silicon powder 2/d spacing standard for XRD (Reference Material 640b, a ⫽ 5.430940 Å, National Institute for Standards and Technology, Gaithersburg, MD).17 (2) CaMg2Al16O27 The powder pattern in Göbbels et al.2 was used to assign Miller indexes to the strongest reflections at low Bragg angles. With our 2 values for 16 reflections thus indexed, lattice parameters were determined by a least-squares procedure. With these parameters and the atom coordinates found in space group P⫺6m2 by Iyi et al.,3 the powder pattern was computed. Subsequently weaker reflections were unambiguously assigned. The procedure was repeated several times, finally obtaining 80 indexed reflections, 11° ⱕ 2 ⱕ 90°, 39 of which are not listed in the pattern of Göbbels et al. The reflections 2 0 15 and 1 2 10 are calculated as moderately strong, and their Bragg angles differ by ⬍0.03°; consequently, the uniquely observed 2 value was assigned to both reflections, and they were each given half-weight in the leastsquares lattice parameters refinement. Other incompletely resolved reflections are duly marked in Table AI,‡‡ where the indexed pattern is presented. The quality of the indexing can be judged from the estimator R ⫽ 兺兩2obs – 2calc兩/兺2obs, R ⫽ 0.00017, and from the usual5 figure of merit M20 ⫽ 50 (具ε典 ⫽ 0.000034(sin2 ), N ⫽ 30). The ‡‡ For Table AI, order ACSD–333 from Data Depository Service, The American Ceramic Society, 735 Ceramic Place, Westerville, OH 43081. 926 Journal of the American Ceramic Society—De Aza et al. Vol. 83, No. 4 Fig. 7. Projection of the liquidus surface of the system Al2O3–MgO–CaO. For composition, temperature, and character of the invariant points, see Table V. maximum deviation between calculated and observed values is 兩⌬2兩max ⫽ 0.04°, which occurs four times in 80 reflections; the average value is 兩⌬2兩 ⫽ 0.01°. From this indexing, we obtained the lattice parameters a ⫽ 5.6002(2) Å and c ⫽ 31.350(1) Å. Although the sample used was quite pure, seven weak reflections were impossible to index, and they were later recognized as the seven strongest reflections of spinel, MgAl2O4; two more reflections at 2 ⫽ 23.53° (I ⫽ 2) and 63.22 (I ⫽ 9) were left unindexed. (3) Ca2Mg2Al82O46 The indexing of the powder pattern was more difficult in this case because of the presence of a significant quantity of CaMg2Al16O27 in our sample. In fact, of 68 peaks measured to 2 ⫽ 60°, at least 26 belong to CaMg2Al16O27. Nevertheless, the successive-approach method outlined above for CaMg2Al16O27 also converged adequately, producing an indexing with many differences from that of Göbbels et al.,2 which appeared to be indexed on cell geometric information only, before structure determination. Calculated intensities in space group R3 m, using the model of Iyi et al.,3 lead, for many observed peaks, to Miller indexes different from those assigned by Göbbels et al. Our lattice parameters, obtained from least-squares refinement of 39 reflections unambiguously assigned to Ca2Mg2Al82O46 are a ⫽ 5.5812(3) Å and c ⫽ 79.921(5) Å. (4) Discussion We obtained lattice parameters for CaMg2Al16O27 greater than those given by Göbbels et al.2 (a ⫽ 5.5926(2) Å and c ⫽ 31.297(14) Å). The difference in a is 0.007 Å, which represents ⬃35, independent of standard deviation used; the difference in c is 0.05 Å, which represents 5 if the value of Göbbels et al. is used, or 50 with our value of the standard deviation. In this connection, our values correspond to relative errors of the same order of magnitude in both parameters, i.e., c/a ⫽ 5, because c/a ⫽ 5.6, which is considered normal. On the contrary, c/a ⫽ 70 in Göbbels et al. indicates some pathologic condition in their data; moreover, Göbbels et al. offer no explanation for the differences between their powder lattice parameters and those obtained (by Iyi et al.3) from single-crystal data. We conclude that our indexed pattern for CaMg2Al16O27 (see Table AI) represents an improvement over that previously published. The same conclusion cannot drawn for Ca2Mg2Al82O46, because we could not obtain a sample of sufficient purity. Our larger values for a and c (Göbbels et al.2 found a ⫽ 5.5710(1) Å and c ⫽ April 2000 Ternary System Al2O3–MgO–CaO 79.770(12) Å) represent a difference of ⬃30 if our values of the standard deviation are used, which can be attributed to the fact that we were measuring, in all probability, a solid solution. Again, our ratio, c/a ⫽ 17, is more reasonable (c/a ⫽ 14) than that of Göbbels et al., c/a ⫽ 120. The Göbbels et al. powder pattern can be improved upon, because many reflections are incorrectly indexed. Acknowledgments The authors wish to thank Dr. A. P. Tomsia and Dr. Eduardo Saiz of Lawrence Berkeley Laboratory for the use of the Materials Science Division facilities and their help and assistance during the SEM-WDS analyses. Thanks are also expressed to Dr. Z. B. Luklinska of the Materials Science Department, Queen Mary and Westfield College, University of London, for providing help with HR-TEM experiments. References 1 A. H. De Aza, P. Pena, and S. De Aza, “Ternary System Al2O3–MgO–CaO: Part I, Primary Phase Field of Crystallization of Spinel in the Subsystem MgAl2O4– CaAl4O7–CaO–MgO,” J. Am. Ceram. Soc., 82 [8] 2193–203 (1999). 2 M. Göbbels, E. Woermann, and J. Jung, “The Al-Rich Part of the System CaO–Al2O3–MgO, Part I. Phase Relationships,” J. Solid State Chem., 120, 358 – 63 (1995). 3 N. Iyi, M. Göbbels, and Y. Matsui, “The Al-Rich Part of the System CaO–Al2O3– MgO, Part II. Structure Refinement of Two New Magnetoplumbite-Related Phases,” J. Solid. State Chem., 120, 364 –71 (1995). 927 4 L. S. Palatnick and A. I. Landau, “Fazovye Ravnovesiya v Mnogokomponentny Sistemakh (Phase Equilibria in Multicomponent Systems),” Kar’kov State University, Kar’kv, 1961. Translation edited by J. Joffe; published by Holt, Rinehart, and Winston, New York, 1964. Also extensively cited by A. Prince, Alloy Phase Equilibria, Ch. 14; pp. 230 — 48. Elsevier, New York, 1966. 5 P. M. De Wolff, “A Simplified Criterion for the Reliability of a Powder Pattern Indexing,” J. Appl. Crystallogr., 1, 108 –13 (1968). 6 R. W. Nurse, J. H. Welch, and A. J. Majumdar, “The CaO–Al2O3 System in a Moisture-Free Atmosphere,” Trans. Br. Ceram. Soc., 64 [9] 409 –18 (1965). 7 A. K. Chatterjee and G. I. Zhmoidin, “The Phase Equilibria Diagram of the System CaO–Al2O3–CaF2,” J. Mater. Sci., 7 [1] 93 (1972). 8 M. Rolin and H. T. Pham, “Phase Diagram of Mixtures not Reacting with Molybdenum,” Rev. Int. Hautes. Temp. Refract., 2, 175– 85 (1965). 9 M. Rolin and H. T. Pham, “Le Systeme Aluminate de Calcium—Alumine,” Rev. Int. Hautes. Temp. Refract., 2 [2] 181 (1965). 10 B. Hallstedt, “Assessment of the CaO–Al2O3 System,” J. Am. Ceram. Soc., 73 [1] 15–23 (1990). 11 A. M. Alper, R. N. Mc Nally, P. H. Ribbe, and R. C. Doman, “The System MgO–MgAl2O4,” J. Am. Ceram. Soc., 45 [6] 263– 68 (1962). 12 D. Viechnicki, F. Schmind, and J. W. McCauley, “Liquidus–Solidus Determination in the System MgAl2O4–Al2O3,” J. Am. Ceram. Soc., 57 [1] 47– 48 (1974). 13 R. C. Doman, J. B. Barr, R. N. MacNally, and A. M. Alper, “Phase Equilibria in the System CaO–MgO,” J. Am. Ceram. Soc., 46 [7] 313–16 (1963). 14 (a)G. A. Ranking and H. E. Merwin, “The Ternary System CaO–Al2O3–MgO,” Z. Anorg. Allg. Chem., 96, 309 (1916). (b)ibid., J. Am. Chem. Soc., 38, 568 (1916). 15 A. J. Majumdar, “The Quaternary Phase in High-Alumina Cement,” Trans. Br. Ceram. Soc., 63 [7] 347– 64 (1964). 16 R. N. MacNally, F. I. Peters, and P. H. Ribbe, “Laboratory Furnace for Studies in Controlled Atmospheres; Melting Points of MgO in N2 Atmosphere and Cr2O3 in N2 and in Air Atmospheres,” J. Am. Ceram. Soc., 44 [10] 491–93 (1961). 17 C. R. Hubbard, H. E. Swanson, and F. A. Mauer, “A Silicon Powder Diffraction Standard Reference Material,” J. Appl. Crystallogr., 8, 45 (1975). 䡺
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