1. Introduction
Aluminium titanate, or tialite, is a ceramic material used in aluminium metallurgy, mainly due to its low reactivity to aluminium alloys and high thermal shock resistance [
1]. The disadvantage of tialite, especially in high-temperature applications, consists in its thermal instability in the temperature range 750–1280 °C, in which it tialite decomposes into its initial oxides, i.e., Al
2O
3 and TiO
2. The specific structure of tialite is the direct cause its thermal instability of [
2,
3].
Tialite crystallizes in to a pseudobrukite structure. Austin and Schwartz [
4] found that tialite is a material isomorphic to pseudobrukite (Fe
2TiO
5), with a theoretical density of 3.71 g cm
−3. Pseudobrukite crystallizes into an orthorhombic arrangement, in the Cmcm space group. Tialite differs slightly in its coordination of its constituent cellular atoms, with lattice parameters a = 3.557 Å, b = 9.436 Å, and c = 9.648 Å. Tialite’s structure consists of distorted octahedra with a central metal cation, surrounded by six oxygen atoms. The unusual combination of octahedra in pseudobrukite-type structures, leading to their deformation, allowed the authors to obtain Me
3O
5-type structures instead of Me
3O
6-type structures, which are characteristic of octahedra [
5]. The TiO
6 and AlO
6 octahedra form a network of chains that are weakly connected by their edges in the b and c directions, and by vertices in the a direction. The metal cations forming the deformed octahedra in the pseudobrukite structure tend to occupy positions in their center. This causes their displacement and a decrease in the bond angle O-Me-O to values below 180°, which has a direct effect on the lattice parameter a, whose length is related to the height of the octahedra. Hence, the greater the difference between the ionic radii of the individual metals forming the octahedra, the more they are distorted in the a and c directions [
5]. This is particularly evident in the structure of tialite, for which the coefficient of thermal expansion in the a direction takes negative values. A significant deformation of the pseudobrukite structure is the cause of the instability of its compounds. Scala [
6] found a relationship between the thermal stability of tialite and its lattice parameter a. The phenomenon, in this case, consists in the decrease in the lattice constant a with the increase in temperature. Thus, the larger the lattice constant a, the higher the thermal stability of the tialite. This constant corresponds to the height of the deformed MeO
6 octahedra. Increasing its value leads to a decrease in the deformation of the tialite structure. As the elementary cells of tialite are deformed and, therefore, suffers internal stresses, tialite shows thermal instability at temperatures between 750 and 1280 °C. This means that in this temperature range, tialite disintegrates into its constituent oxides, i.e., Al
2O
3 and TiO
2. The introduction of magnesium cations into the structure of tialite leads to the formation of aluminum magnesium titanate (MAT) solid solutions with the structural formula Mg
xAl
2(1−x)Ti
1+xO
5 [
7]. In solid solutions with magnesium, the magnesium cation and the titanium cation simultaneously substitute two aluminum cations; for iron-containing structures, the exchange occurs between Fe
3+ and Al
3+ cations [
8]. Both mechanisms lead to a reduction in the stresses in the structure, reducing the number and size of micro-cracks, i.e., increasing the thermal stability of tialite. In MAT solid solutions, the elemental cell deformation is lower; thus, the solid solutions exhibit less anisotropy in linear thermal expansion compared to pure tialite. Consequently, lower thermal stresses are generated during their cooling, resulting in fewer and smaller microcracks. Therefore, the obtained materials can be expected to exhibit higher flexural strength while maintaining high thermal shock resistance compared to pure tialite [
7].
Tialite is characterized by the high anisotropy of its thermal expansion coefficients [
5]. As a result of the formation of a complex stress state in the material, micro and macro cracks are formed in the material during its cooling after reaction sintering [
9,
10,
11,
12,
13,
14,
15,
16,
17,
18,
19,
20,
21]. These cracks provide desirable properties, such as a low macroscopic thermal expansion coefficient [
22], low thermal conductivity [
23,
24,
25], and, thus, high resistance to thermal shock [
1,
11,
26,
27]. Tialite also has high resistance to microcrack propagation [
28]. The micro and macro cracks present in the material reduce its flexural strength [
20,
29,
30] and its values for Young’s modulus and Poisson’s number [
31]. Therefore, it is necessary to optimize the reactive sintering process and to select stabilizing additives in order to obtain a material characterized by the optimum size and number of micro-cracks, due to which it will have a characteristic resistance to thermal shock while maintaining its mechanical properties.
The synthesis and reaction sintering of tialite solid solutions can be combined by means of the classical solid-phase reaction technique [
32,
33]. Equimolar mixtures of alumina and titanium oxide are then annealed together with an additive introducing magnesium cations, e.g., MgO or talc [
33]. The synthesis using heterogeneous nucleation is a different case in which tialite solid solution is obtained by addition ofisostructural magnesium titanate MgTi
2O
5 (MT). This allows the activation energies of the process to be lowered [
34,
35,
36,
37], and, thus, the synthesis temperature of the solid solutions to be reduced. In [
38], it was shown that reaction sintering leads to an improvement in the homogeneity and density of the sinter. Due to the lower synthesis temperature, the grain size of the obtained sinters is smaller. As a result, finer micro-cracks are formed in the material and its strength is improved [
39].
The paper presents changes in lattice parameters of tialite and its solid solutions obtained by reaction sintering. The samples were synthetized with and without stabilizing additives, such as structure-stabilizing additives in the form of magnesium oxide or heterogeneous magnesium titanate nuclei, and with the addition of magnesium cations and silica. The objectives of this work were to investigate whether the method of stabilizer introduction affects the magnitude of the changes occurring in the elementary cells of tialite, whether the addition of SiO2 affects the incorporation of Mg2+ cations into the tialite’s structure, and to determine the mechanism of incorporation of stabilizer cations into the tialite structure. For this purpose, the results obtained experimentally were compared with the results of the DFT simulations.
4. Discussion of Results
The solid-phase synthesis of tialite using oxide substrates can be influenced by many factors. Some of the most important include the synthesis temperature, final temperature annealing time, and substrate grain size. However, controlling only the above synthesis parameters, without the deliberate introduction of magnesium and silica compounds, allows only a 67% yield at 1350 °C. Thermodynamic instability of tialite in the temperature range of 780–1280 °C is an additional parameter worsening the efficiency of the synthesis in the reference systems. It can cause the decomposition of the formed tialite into starting oxides. As was shown in this study, an almost complete conversion of the substrates, of 94–95%, is possible if magnesium cations are introduced into the reaction mixtures in the form of magnesium compounds, i.e., MgO and MgTi
2O
5, magnesium titanate isostructural with tialite. For the sample with 4% MgO addition, the synthesis efficiency was already 89% y at the lowest sintering temperature (1250 °C), and from 1300 °C onwards, it was constant at about 96%. Equally high yields were obtained for reaction sintering of the tialite using heterogeneous nucleation. At the lowest temperature, for the compositions AT 9MT and AT 18MT, 85 to 87% of tialite was obtained, at 1300 °C the values ranged from 91 to 93%, and about 95% was obtained at the highest temperatures. Thus, it can be concluded that the presence of magnesium cations effectively activates the synthesis of MAT solid solutions regardless of the form in which they are introduced. The high conversion is particularly important due to the fact that the unreacted grains of the substrate phases in the decomposition temperature range can act as decomposition nuclei, accelerating the decomposition of tialite. Thus, fully reacted systems containing trace amounts of phases other than the MAT solid solution should exhibit much higher thermal stability. The second additive, nanosilica, introduced in an amount of 4 mass %, slightly decreased the amount of the obtained MAT solid solutions. This was probably a result of the formation of the so-called diffusion barriers by silica on the grain boundaries of the crystalline or amorphous phases, hindering the incorporation of Mg
2+ cations into the tialite structure, i.e., hindering the formation of Mg
xAl
2(1−x)Ti
1+xO
5 solid solutions. (
Table 2). The occurrence of spinels in the systems synthesized using magnesium oxide may indicate that the synthesis of tialite in the systems containing magnesium cations proceeded through the formation of a spinel transition-phase MgAl
2O
4. Subsequently, magnesium was incorporated into the tialite structure, and solid solutions of MAT—Mg
xAl
2(1−x)Ti
1+xO
5 were then formed, in which, according to the literature, one magnesium cation together with one titanium cation probably substituted two aluminum cations simultaneously. Although the inclusion in the stoichiometry of the solid solutions meant that the magnesium cation together with the titanium cation simultaneously probably substituted two aluminum cations in the synthesized products, slight amounts of unreacted oxides, mainly aluminum oxide, were visible (
Table 2). This fact can be explained by the higher solubility of the titanium cations in the structures of the resulting solid solutions compared to the aluminum cations. To confirm the above conjecture, an additional experiment was conducted in which compositions were prepared, amounts of alumina that were 2.5, 5, and 10% mol. Less than the stoichiometry of the reaction to form MAT solid solutions. In this way, 100% solid-solution MAT was obtained (
Figure 7a). The SEM observations of the sinter made of polycrystal consisting of 100% of MAT solid solution showed that the grain boundaries were very weak, and a significant amount of crumbling of the whole grains of the MAT solution was observed (
Figure 7b). This observation suggests that the sintered polycrystal may exhibit low strength. The problem of improving the mechanical parameters of tialite-made polycrystals is now widely discussed in the literature [
20,
21,
27].
The presented analysis of the changes in the lattice parameters of the tialite elemental cell clearly shows that when magnesium is introduced into the systems, both in the form of MgO and MgTi
2O
5 alone or together with the addition of nanosilica, MAT solid solutions are formed. A significant increase in the elemental cell volume was observed (
Figure 8), in comparison to the elemental cells of the tialite synthesized without additives. The increase in the volume of the elemental cells was larger the more Mg
2+ cations substituted the aluminum cations, which was in agreement with the reports in the literature. Mg
2+ (0.078 nm) cations have the largest ionic radius a compared to Ti
4+ (0.067 nm) and Al
3+ (0.053 nm) cations, which explains the increase in the elemental cell volume of tialite if substitutions occur.
A careful analysis of
Figure 2,
Figure 3 and
Figure 4, which shows the changes in the lattice parameters (a, b and c), reveals their increase in the systems with the additives compared to the parameters of the elementary tialite cells without any additives (AT). From the point of view of stability, the increase in the value of parameter a is important; due to this increase, the deformation of oxygen octahedra, forming the tialite structure, reduced, the stresses associated with differences in the thermal expansion of the differently oriented grains reduced, fewer micro-cracks formed, and the structure of the MAT solid solutions showed higher stability [
1,
27,
30,
33]. It is still worth noting that the increase in the reaction sintering temperature of the tialite or its MAT solid solutions and the associated increase in the synthesis yield resulted in a slight increase in the value of the lattice parameter a, with a slight decrease in the values of the parameters b and c, which can be explained by the formation of the proper structure of the tialite or MAT solid solutions. Furthermore, in the case of the simultaneous application of additives introducing magnesium cations as well as nanosilica additives (AT 4M 4S; AT 9MT 4S and AT 18MT 4S), lower values of lattice parameter a (
Figure 2,
Figure 3 and
Figure 4) and higher values of parameters b and c (
Figure 2,
Figure 3 and
Figure 4) were observed in comparison with the analogous systems not containing nanosilica (AT 4M; AT 9MT and AT 18MT). It can also be seen that the differences in the values of the lattice parameters of the systems with and without silica were negligible when compared to the significant increase in the values of these parameters, relative to the reference system. These observations suggest that silicon does not build into the structure of tialite, while nanosilica forms a kind of “diffusion barrier” on the grain boundaries, limiting the grain size, reducing the number of micro-cracks formed, and decreasing the susceptibility to thermal decomposition, while, on the other hand, hindering the incorporation of Mg
2+ cations into the structure of aluminum titanate [
1,
19,
27,
30,
33]. These suggestions were confirmed by the surface phase composition analysis, according to which silicon-rich phases were present at the grain boundaries, at triple points, and between the obtuse grains of the tialite (
Figure 9).
The literature data [
40,
43], used as the basis for the theoretical calculations (
Table 3), differ from the obtained results in terms of the values of the lattice constants (structure A—Al
2TiO
5 and D—MgTi
2O
5 in
Table 4). Nevertheless, the crystal structure optimization, using the VASP program, reduced these differences. The lattice constants a and b were smaller by 0.3% and the lattice constant c was larger by 0.24% compared with the values obtained in our experimental studies (
Table 5, structure AT). The results obtained for the different Ti and Mg configurations indicate that the Al
2TiO
5 structure is highly sensitive to the Al exchange position. The deformation of the elementary cells also changes, depending on the substitution site. A comparison between the differences in the lattice constants in the theoretical modeling and those in the experimental studies indicates that for the exchange of single Al by Ti or Mg, the smallest deviations in the lattice constants, compared to experimental data, were obtained for structures B and E (
Table 4 and
Table 5). The Ti and Mg positions in structures B and E were used for structure I, whose lattice constants were closest to the experimental data of the AT 18 MT and AT 4M structures. The other structure, H, showed larger deviations, but only up to 0.5%. These results indicate that a configuration in which the exchanged atoms are not in close proximity to each other is preferable. On this basis, as well as on the basis of the literature data, the most probable substitutions are the substitutions of the two aluminum atoms with one magnesium atom and one titanium atom. Moreover, as the simulations show, substitutions are more likely when atoms do not contact each other (
Table 4, structure H). The simulations also showed that when the amount of magnesium cation added (AT 9MT) is halved, the values of the real lattice parameters are close to the structures with substitutions of one aluminum cation for one magnesium cation (
Table 4, structure E) or one aluminum cation for one titanium cation (
Table 4, structure B).
From the presented model (
Figure 5H) and its comparison with the real data, it is clear that the current view in the literature [
8], starting with the proposition that two aluminum atoms are substituted simultaneously by one magnesium atom and one titanium atom, is highly probable. The elemental cell parameters calculated on this basis are very close to the values obtained from the X-ray data (
Table 3). It also seems reasonable to simultaneously apply a structural stabilization with magnesium cations and a microstructural stabilization with silica. Therefore, it is reasonable to believe that the simultaneous substitution of two aluminum atoms with a magnesium atom and a titanium atom increases the volume of the elemental cell and, thus, reduces its distortion, resulting in a less stressed and more stable macroscopic system. These statements are confirmed by the thermal stability studies of the AT tialite and MAT solid solutions. These are illustrated in
Figure 6, which shows the amount of tialite or MAT solid solution after an appropriate annealing time.
The almost complete decomposition of the reference sample AT after 24 h of annealing confirms the instability of pure aluminum titanate and indicates the need for stabilizing additives [
44,
45]. It is reasonable to believe that the lower stability of the AT 18MT and AT 4M4S systems was due to the higher amount of decomposition nuclei, primarily alumina grains and micro-cracks. The sample showing the highest stability of AT 18MT 4S had a highly homogeneous microstructure (
Figure 10a), with negligible amounts of unreacted oxide grains and the lowest amount of micro-cracks (
Figure 10a). The AT 4M sample, to which magnesium cations in the form of MgO were added and no nanosilica was added, also showed a homogeneous microstructure, although much more micro-cracks were visible (
Figure 10b). As a result, after 96 h of annealing, ~40 mass % mass of MAT solid solutions was present (
Figure 6).
Figure 10c,d shows SEM microstructure images of the AT 4M and AT 18MT 4S samples after 96 h of annealing at 1100 °C. In the case of the sample containing 4 mass % magnesium oxide additive (AT 4M), a clear decomposition and recrystallization of the starting oxides, i.e., TiO
2 (brightest areas) and Al
2O
3 (darkest areas) can be observed. In the AT 18MT 4S sample, on the other hand, the decomposition process was much slower. A few areas can be distinguished in which the recrystallization of the rutile had started (the brightest areas), while the rest of the microstructure consisted of grains of MAT solid solutions, mullite, and spinel [
44,
45].