3.1. Evolution of Phase Composition and Microstructure
The phase composition of the prepared Pr-substituted 5YSZ ceramics is defined by the equilibrium phase relationships at the given firing temperature and by the kinetics of the solid-state reaction and cation diffusion. XRD analysis of the as-prepared samples (
Figure 1) shows a prevailing fluorite (F) phase and the onset of a Pr
2Zr
2O
7-based pyrochlore (P) phase. Furthermore, one also observes a clear splitting of the reflections assigned to the fluorite phase (
Figure 2A–C).
The ternary diagrams of the ZrO
2–Y
2O
3–Pr
2O
3 or ZrO
2–Y
2O
3–PrO
y systems have not been reported so far. Still, it is possible to make plausible predictions on equilibrium phase compositions based on the available diagrams of the related ZrO
2–Y
2O
3–Ln
2O
3 systems. As the ionic radius of Nd
3+ is the closest to that of Pr
3+ [
35], the ternary diagram of the ZrO
2–Y
2O
3–Nd
2O
3 system can be expected to resemble that of ZrO
2–Y
2O
3–Pr
2O
3 counterpart in the high-temperature range, when praseodymium is in a 3+ oxidation state in air (T ≥ 1300 °C [
17,
18]). Based on the most recent diagrams of the ZrO
2–Y
2O
3–Nd
2O
3 system by Fabrichnaya [
36,
37], the samples with the nominal cation compositions selected in the present work (
Table 1) are expected to be ternary fluorite-type solid solutions at 1600 °C under equilibrium conditions. The field of fluorite phase narrows with decreasing temperature, and the composition with a lower Pr content (
x = 0.05) at 1400 °C belongs to the two-phase T + F field comprising tetragonal and cubic fluorite ZrO
2-based phases [
36,
37]. According to the earlier diagram of the ZrO
2–Y
2O
3–Nd
2O
3 system at 1600 °C proposed by Hinatsu and Muromura [
38], the
x = 0.05 and
x = 0.15 compositions correspond to the T + F and F regions, respectively, while
x = 0.10 is located at the boundary between the two fields. Furthermore, comparative analysis of available ternary diagrams of the ZrO
2–Y
2O
3–Ln
2O
3 systems, where Ln = La [
39,
40,
41], Nd [
36,
37,
38] and Sm [
42], suggests also that the boundary between the T + F and F fields for a smaller Ln = Pr cation should be shifted towards a slightly higher dopant content compared to the Nd-based system. At the same time, all the inspected diagrams suggest that the praseodymium contents in the sintered ceramic samples are too low for the co-existence of the pyrochlore-type Pr
2Zr
2O
7 phase under equilibrium conditions at 1400–1600 °C.
Further insight into the phase evolution in the course of the direct firing of 5YSZ samples with PrO
y additions is provided by the microstructural studies. All the ceramic samples demonstrate a noticeable porosity (
Figure 3). Visually, the volume fraction of the pores increases with increasing praseodymium content and reasonably decreases with increasing time and temperature of firing. The EDS analysis showed the accumulation of praseodymium near the surface of the pores. Again, the distribution of cations becomes more homogeneous with increasing temperature and duration of firing (
Figure 3).
SEM inspection of the polished and thermally etched samples also revealed inhomogeneities in the grain size distribution (
Figure 4). For lower T
f and shorter t
f, larger grains (1–3 µm) surround the pores, while small grains (0.2–1.2 µm) fill the volume between the pores. The grain size distribution is correlated with praseodymium elemental distribution. As an example,
Figure 5A shows the EDS spectra collected from different points of the P10-1450-4 sample. The results imply that the praseodymium concentration in the large grains is noticeably higher than in the small grains, which is in close agreement with the structural evidence of fluorite peak splitting (
Figure 2), and increases drastically near the pore surface indicating the preferential location of the secondary pyrochlore Pr
2Zr
2O
7 phase. Increasing the time and temperature of firing promotes a more homogeneous distribution of the grain size and praseodymium concentration across the sample volume (
Figure 3 and
Figure 4). Still, the accumulation of Pr near the pore surface is detectable by EDS analysis even in the samples with a longer firing at 1500–1550 °C (
Figure 3 and
Figure 5B).
In combination, the XRD and SEM/EDS data suggest the following scheme of the phase evolution during direct firing. The pores in the ceramic samples may be due to poorer packing near praseodymium oxide agglomerates in the green powder mixture after ball-milling and compaction of the 5YSZ + PrO
y samples or due to hindered shrinkage as reactive firing proceeds. Independently of temperature, the solid-state reaction proceeds through the initial formation of the pyrochlore-type Pr
2Zr
2O
7 phase at the PrO
y/5YSZ contacts. This is followed by the diffusion of praseodymium from the formed layer of the pyrochlore phase into the bulk of the samples, under Pr
2Zr
2O
7/(Zr,Y,Pr)O
2-δ/5YSZ phase gradients inducing grain growth by Pr-enrichment and possibly also the onset of porosity by a Kirkendall-like effect, as demonstrated for interdiffusion in YSZ/YDC (YDC = yttria-doped ceria) [
43]. In addition, local grain growth may hinder microstructural rearrangement, possibly combined with grain boundary pinning by Pr
2Zr
2O
7 particles, preventing the densification and elimination of the remaining porosity. Note also the irregular shape of this porosity (
Figure 3).
The phase evolution is well illustrated by the changes in the XRD peaks shape/splitting with increasing temperature of firing. The substitution by Pr into 5YSZ is expected to increase the lattice parameters due to differences between the ionic radii of Pr
4+ (r
VI = 0.85 Å) and Pr
3+ (r
VI = 0.99 Å) relative to Zr
4+ (r
VI = 0.72 Å) and Y
3+ (r
VI = 0.90 Å) [
35]. In addition to the fluorite (F) phase, the XRD pattern of the P05-1450-1 sample (
Figure 2A) suggests the presence of unreacted tetragonal 5YSZ (T), second praseodymium-enriched fluorite (F2) and pyrochlore (P) phases. Increasing T
f promotes the dissolution of the T and P phases and the merging of the F and F2 phases into a single fluorite-type phase with an intermediate lattice parameter for P05-1550-4. A similar picture is observed for the
x = 0.10 samples (
Figure 2B). In the case of the samples with the largest (
x = 0.15) praseodymia additions, the firing time was insufficient for the full homogenization of the samples. For all T
f, the samples contain the pyrochlore-type intermediate, while the broadening of the peaks seems to imply the transient distribution of the lattice parameters of the fluorite phase (
Figure 2C).
The area ratio of the main peaks of the pyrochlore and fluorite phases, A
(222)P/A
(111)F, was obtained by the integration of the corresponding reflections (
Figure 2D) and used as a criterion for the relative contents of a pyrochlore to fluorite phases and its dependence on the overall composition and firing conditions. The deconvolution of the main and secondary fluorite phase peaks was performed by assuming two Gaussian distributions (
Figure 2E). The peaks of the main contribution at slightly higher 2Θ were used to evaluate the lattice parameters by the Nelson–Riley method [
44] based on extrapolation of:
The results are summarized in
Table 3.
3.2. Praseodymium Oxidation State
Figure 6A illustrates the variations of the average oxidation state of praseodymium cations in selected Pr-substituted 5YSZ samples on temperature cycling in air estimated from the thermogravimetric data. As praseodymium is the only variable-valence cation in the prepared materials, the absolute values of oxygen content in the samples and Pr oxidation state were calculated from the thermogravimetric data on reduction in 10%H
2–N
2 flow (
Figure 6B) assuming the nominal overall cation composition and that all praseodymium cations in the reduced samples are in 3+ state:
Thus, the change of the mass on reduction was assigned to the oxygen release from the oxide sample associated with the Pr4+ → Pr3+ reduction allowing the calculation of the average oxidation state of the praseodymium cations and the fraction of Pr4+ in the oxidized samples.
The results indicate that Pr
3+ prevails in the studied materials; the estimated fraction of Pr
4+ at 600–1000 °C is 1.3–2.1% with respect to the total praseodymium content. Furthermore, the average praseodymium valence shows a very weak temperature dependence in air. This differs from the binary praseodymium oxide where the average oxidation state of praseodymium in air varies between approximately 3.66+ below 300 °C and 3.42+ at 1000 °C [
17,
18], and from Mn-substituted 5YSZ where manganese valence changes reversibly from ~2.9+ at T ≤ 300 °C to (2.50–2.56)+ at 1000 °C in air [
15]. On the other hand, the obtained results are in agreement with the literature reports suggesting the prevailing trivalent state of praseodymium cations in zirconia-rich (ZrO
2)
1-x(PrO
y)
x ceramics [
24,
29] and Pr
2Zr
2O
7-based pyrochlores [
45] sintered at high temperatures.
3.3. Electrical Conductivity in Air
Electrical studies were done using bar-shaped ceramics samples. Impedance spectroscopy of these samples revealed only two contributions in the frequency range 20 Hz–1 MHz: high-frequency (HF) semicircle attributed to the bulk properties of the sample, and a low-frequency (LF) contribution assigned to the electrode process. The spectra were fitted using a simple (R
HFǀǀCPE
HF)(R
LFǀǀCPE
LF) equivalent circuit (where R is the resistance and CPE is the constant phase element [
46]) to extract the total ohmic resistance R
HF of the sample. The calculated specific capacitance for the HF and LF contributions was on the order of ~10
−10 F/cm and ~10
−4 F/cm, respectively. No grain boundary or secondary phase contributions could be detected and extracted from the impedance spectroscopy data for this sample geometry even at temperatures around 500 °C (
Figure 7).
The data on the electrical conductivity of Pr-substituted 5YSZ are summarized in
Figure 8 and
Table 3. The conductivity exhibit nearly linear behavior in Arrhenius coordinates,
lnσT-1/T, similar to yttria-stabilized zirconia electrolytes. The conductivity of prepared ceramics varies in the range 2.0–4.1 S/m at 900 °C and 0.28–0.68 S/m at 700 °C and is lower compared to dense 8YSZ ceramics. The activation energy for electrical conductivity at 500–1050 °C for all the samples varies in a narrow range of 1.0–1.1 eV (
Table 3).
The measurements of oxygen ion transference numbers of selected samples by the modified EMF technique demonstrated that these materials are predominantly oxygen ionic conductors under oxidizing conditions close to atmospheric oxygen pressure (
Table 4). The contribution of electronic conductivity, estimated as σ
e = σ(1 −
), to the total conductivity at 700–900 °C increases with increasing praseodymium content from 0.3–0.4% for P05-1500-9 to 0.9–1.9% for P15-1500-4 at p(O
2) = 0.21–1.00 atm. A minor increase in the electronic contribution can be attributed to the introduction of
p-type electronic transport with an increasing concentration of Pr cations in the zirconia lattice [
23,
24] and/or to the presence of a non-negligible fraction of the pyrochlore-type phase in the latter sample. Stoichiometric Pr
2Zr
2O
7 is known to be a mixed ionic–electronic conductor with prevailing
p-type electronic conductivity under oxidizing conditions [
45,
47]. The total conductivity of Pr
2Zr
2O
7 at 700–1000 °C is 0.5–1.5 orders of magnitude lower compared to 8YSZ and the studied Pr-substituted 5YSZ ceramics (
Figure 8A). Thus, the segregation of the pyrochlore-type phase has a negative impact on the total electrical conductivity of ceramic samples.
3.4. Analysis of the Impact of the Firing Conditions and Pr Content
The results of the firing experiments designed using Taguchi planning to assess the impact of Pr additions and firing conditions on the density ρ
exp, structural features (pyrochlore-to-fluorite peak area ratio A
(222)P/A
(111)F, lattice parameter of the main fluorite phase
aF), and electrical properties (electrical conductivity at 700 °C and corresponding activation energy E
A) of the 5YSZ ceramics are summarized in
Table 3.
A preliminary examination of the changes in the density of the fired ceramics (
Table 3) suggests a prevailing effect of Pr contents, and this is confirmed by the correlation matrix calculated with standard Microsoft Excel formulae (
Table 5). This negative dependence on Pr contents is counterintuitive, taking into account the higher atomic mass of Pr relative to Zr and Y, and indicates a negative impact on sintering, which cannot be reversed by increasing the firing temperature. Note also the negative correlation between density and lattice parameter. In fact, the lattice parameter of the main fluorite phase increases with nominal Pr contents and also with firing conditions, as revealed by the correlation matrix (
Table 5) and as expected for the incorporation of larger Pr
3+ cations into the fluorite YSZ lattice.
The dependence of density on individual parameters is also demonstrated by averaging the results for every level, as shown in
Figure 9A. This confirms the prevailing dependence on Pr contents, and that a poor signal-to-noise ratio prevents statistical relevance for dependence on other parameters.
The relative contents of the pyrochlore phase also increase mainly with nominal Pr contents, as indicated by the area peak ratio A
(222)P/A
(111)F (
Figure 9B). The opposite effects of firing temperature are probably due to kinetic limitations by the direct firing of precursor powder mixtures. As already mentioned, the actual contents of Pr are lower than expected for the onset of the pyrochlore phase in either binary ZrO
2–Pr
2O
3 [
19,
20,
21,
22] or ternary ZrO
2–Y
2O
3–Ln
2O
3 (Ln = La, Nd, Sm) systems [
36,
37,
38,
39,
40,
41,
42] under equilibrium conditions at elevated temperatures.
The impact on the conductivity is mainly ascribed to the contents of Pr (
Figure 9C), and this may be attributed to a combination of microstructural and structural changes, as revealed also by a positive correlation between conductivity and density (and therefore an inverse correlation between conductivity and porosity), and negative correlation with the lattice parameter of the main conducting phase (
Table 5). The effects of activation energy are also consistent with structural changes, which combine the effects of nominal Pr contents and also the effects of firing temperature and firing time (
Table 5), which contribute to an increase in the effective content of the main fluorite phase.
Further confirmation for the dependence of density, structural features and properties on the nominal composition and the firing conditions were obtained by multivariate fitting. However, one performed the following transformation of these variables, as expected for the thermal activation of the sluggish microstructural or structural changes after direct firing. For the effects on density:
This may be linearized by reverting to logarithmic scales:
where T
f is in K, t
f is in h, Pr content is in nominal % (see
Table 1), and the multivariate fitting (
Figure 9D) yields the parameters shown in
Table 6.
Table 6 also shows the overall changes (Δρ) expected on varying each factor independently while keeping the other factors at their intermediate level; this is consistent with the corresponding correlations in
Table 5.
Similar transformations of independent variables were assumed to perform multivariate analysis for changes in conductivity and its activation energy, and also for the lattice parameter. This dependence for a generic property Y is given by:
and the relevant coefficients and impact on these properties are shown in
Table 6. These values confirm the guidelines provided by the correlation matrix. The improved quality of multivariate fitting (
Figure 9D–F) can be assessed by comparing the values of the correlation coefficient
r shown in
Table 6 with the correlation matrix in
Table 5.
Multivariate analysis of the effects on the onset of the pyrochlore phase cannot be based on log-log scales since this phase is absent in some samples or its residual content is below the detection limit of X-ray diffraction. In this case, multivariate analysis was performed without the transformation of independent variables, yielding:
where T
f is in °C, t
f is in h, and Pr content is in nominal %.
The revealed effects of firing conditions and praseodymia additions on the properties of 5YSZ ceramics are in agreement with the proposed pathway of the phase evolution during the direct firing of pelletized precursors and underline the key role of kinetic limitations. Increasing praseodymia additions results mainly in a larger fraction of the low-conducting pyrochlore phase and a lower density (a higher porosity). This, in turn, has a negative effect on the ionic conductivity, which is lower compared to dense 8YSZ ceramics (
Figure 8A). Increasing the time and temperature of firing promotes the homogenization of the samples with corresponding effects on the properties, but the statistical relevance of these variables within the selected ranges is lower compared to PrO
y additions.
3.6. Behavior on Redox Cycling
The exposure to reducing conditions is expected to induce the complete reduction in the fraction of Pr
4+ to Pr
3+ and, therefore, a lattice expansion caused by the difference in ionic radii of tetravalent and trivalent praseodymium. However, as discussed above, the fraction of Pr
4+ in the studied samples is low, ≤2% of the total praseodymium content. As a result, the transformation of the residual Pr
4+ to Pr
3+ on heating in a 10%H
2–N
2 atmosphere has a negligible effect on the thermochemical expansion of Pr-substituted 5YSZ ceramics (
Figure 10B). This behavior is different from, for instance, Mn-substituted 5YSZ ceramics where Mn
3+ ↔ Mn
2+ redox changes cause substantial dimensional variations on thermal cycling between reducing and oxidizing atmospheres [
15].
One should also note that the stabilization of the prevailing 3+ oxidation state of praseodymium cations under oxidizing conditions results in a low oxygen storage capacity. The estimations from the thermogravimetric data (
Figure 6B) showed that the oxygen storage capacity of the samples P05-1500-9 and P10-1550-9 at 900 °C is limited to 2.0–2.5 µmol/g on cycling between oxidizing and highly reducing conditions.
The exposure to a reducing atmosphere results, however, in irreversible changes in electrical conductivity.
Figure 11 illustrates the variations in the electrical conductivity of selected samples in a relatively short reduction–oxidation cycle at 900 °C. Switching from oxidizing to reducing conditions induces a slow decrease in the conductivity with time which cannot be attributed to a drop in partial
p-type electronic conductivity. On returning back to atmospheric oxygen pressure, the level of conductivity is not recovered to the initial level, but remains stable with time.
The changes in electrical conductivity in ox–red–ox cycles coincide with the thermogravimetric data for powdered samples in a similar cycle showing that the weight changes and, therefore, the Pr oxidation state was not fully reversible after re-oxidation at 900 °C (
Figure 6B). In particular, the average oxidation state of Pr cations after one redox cycle at 900 °C dropped irreversibly from 3.021+ to 3.016+ for P05-1500-9 and from 3.013+ to 3.008+ for P10-1550-9. Thus, the changes in electrical conductivity are interrelated with the changes in the oxidation state of praseodymium. At the same time, no structural alterations could be detected by XDR after short-term redox cycles at 900 °C. The variations in the calculated fluorite lattice parameters of P05-1500-9 and P10-1550-9 samples after either thermogravimetric or electrical studies were ≤0.015%.
Note that the aging of conductivity (a slow decrease in ionic conductivity) with time at elevated temperatures, around 1000 °C, is known for yttria-stabilized zirconia [
30,
50]. The proposed mechanisms responsible for aging include a continuous transformation to a lower conducting phase (i.e., cubic to tetragonal) and oxygen vacancy ordering processes. Most likely, similar phenomena are responsible for the conductivity changes in Pr-substituted 5YSZ ceramics. In particular, according to the available phase diagrams [
19,
20,
21], the thermodynamically equilibrium phase composition of the (ZrO
2)
1-x(PrO
y)
x system for
x = 0.02–0.42 at 900 °C corresponds to a mixture of monoclinic ZrO
2- and cubic Pr
2Zr
2O
7-based phases. Apparently, exposure to reducing conditions may facilitate the processes that cause a reduction in conductivity with time.