Abstract
This work describes the synthesis, structural characterization and electrical properties of solid solutions with the general formula Gd2Hf2−xBxO7, where B = Ti4+, Sn4+ and Zr4+. All samples were successfully prepared in ~ 30 h, via a mechanochemical reaction in a planetary ball mill, using the corresponding elemental oxides as starting chemicals. The XRD and Raman spectroscopy analysis of the title samples revealed that on firing at 1500 °C Hf4+ substitution by Sn4+ and Ti4+ produces better ordered pyrochlore structures and decreases the electrical conductivity of Gd2Hf2O7 by more than two orders of magnitude (from 2.7 × 10−4 at 700 °C to 8.71 × 10−7 and 1.12 × 10−6 Sm cm−1, for Gd2Sn2O7 and Gd2Ti2O7, respectively). By contrast, the Gd2Hf2−xZrxO7 system remains disordered with conductivity increasing by almost an order of magnitude and reaching a value for Gd2Zr2O7 of 1.55 × 10−3 Sm cm−1 at 700 °C, whereas the activation energy for oxygen migration decreases in both, the Sn- and Ti-containing systems, and increases slightly in the Zr-containing solid solution. These changes cannot be only explained when taking into account the cations size ratio criteria; the covalency of the <B–O> metal bond plays also a key role in determining the structural characteristics and electrical properties of the title three systems.
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Introduction
The pyrochlore structure is widely adopted by synthetic A2B2O7 multicomponent oxides because it can accommodate a broad range of cation combinations, mixed site populations, and vacancies [1]. Thus, the A-site can be occupied by a great variety of large cations (rA = 0.9–1.2 Å) in different oxidation states such as Bi3+, Pb2+ or Ln3+ (lanthanide ions) to name a few. The B-site might host almost any medium size (~ 0.6–0.75 Å) and positively charged ion capable of adopting a sixfold coordination, such as Sn4+, Zr4+, Hf4+, Ti4+, Nb5+, or Ir4+. Some oxygen- and cation-deficient pyrochlores show gross deviations from the ideal A2B2O7 stoichiometry and yet remain thermodynamically stable even without a significant distortion of the ideal isometric unit cell [2,3,4]. Coupled to such interesting structural and compositional features, pyrochlore oxides display a rather unique set of exciting physical and chemical properties. Thus, pyrochlores electrochemical properties span from metallic or even superconducting behavior, to fast ion and mixed ionic-electronic conduction, semiconductors and insulators [5,6,7,8]. Some of these properties are mediated by subtle electronic features or by the presence of structural defects and disorder, which occur easily in this family of oxides. Moreover, the pyrochlore structure offers a unique playground to examine the interplay between chemical composition, defect chemistry and properties.
This contribution addresses some of these issues by analyzing the effect of isovalent substitutions on the structure and oxygen ion conducting properties of a pyrochlore-type hafnate, Gd2Hf2O7. Pyrochlore-type lanthanide-containing oxides Ln2B2O7, where B is a tetravalent cation, have attracted a great deal of interest in recent years for both, fundamental science and practical applications in fields such as energy conversion and storage, thermal insulation or even, immobilization of high-level radioactive waste [9,10,11]. We have recently engaged in a study of the synthesis, structural characteristics and physicochemical properties of otherwise, insufficiently studied lanthanide hafnates [12,13,15], and this work is part of this effort.
The pyrochlore structure might be considered a fluorite-related superstructure [1]. The fluorite structure [S.G. = Fm\( \bar{3} \)m (#225)] can be described as a face-centered cubic (fcc) array of cations in which all the available tetrahedral interstices are filled with anions. Although retaining the fcc array, cations in the pyrochlore structure [S.G. = Fd\( \bar{3} \)m (#227)] are ordered on two nonequivalent sites. Furthermore, anions are also located as in fluorites, in the tetrahedral interstices of the cation framework although they are all no longer equivalent, but occupy two symmetry-independent positions. Both structures are compared in Table 1 and in Fig. 1.
Different attempts have been made in the literature to rationalize the formation and stability of the pyrochlore structure, in terms of simple geometrical requirements such as the cations radii and their size mismatch [1, 16,17,18]. Thus, the radius ratio constraints in A2B2O7 oxides result in the formation of the pyrochlore structure when 1.46 ≤ rA/rB ≤ 1.78. Outside this range, the size mismatch favors different structure types such as perovskite-related monoclinic layered structures (rA/rB > 1.78) and anion deficient fluorite structures (rA/rB < 1.46). However, geometric and electrostatic criteria only are not enough to fully explain the formation and stability of pyrochlore-type phases. Additional factors, such as bonding character, processing conditions, and thermal history, play also an important role in stabilizing/destabilizing the pyrochlore structure and, indeed, in determining its properties.
The use of mechanical energy to stimulate physical and chemical processes in the solid state, the so-called mechanochemical methods (MM), has attracted great deal of interest in materials science for different reasons [19,20,21,22]. First, they are simple to implement and capable of providing large volumes of the target material in a cost-effective manner. Furthermore, as far-from-equilibrium processing techniques, MM frequently yield highly defective and metastable phases; additional processing allows obtaining fairly stable intermediate states with intriguing and potentially interesting characteristics, which are inaccessible by more conventional processing techniques. Having in mind the extremely refractory nature of lanthanide hafnates and the importance of some structural defects on transport properties of ion conducting materials, we selected this powder processing method, to obtain all the samples analyzed in this work.
Experimental
The samples preparation and characterization procedure followed in this work has been described in detail elsewhere [12,13,14]. Different compositions in the three Gd2(Hf2−xBx)2O7 systems (B = Ti4+, Sn4+ and Zr4+; x = 0, 0.4, 0.8, 1.2, 1.6 and 2) were prepared by dry milling at room temperature, stoichiometric mixtures of the corresponding high purity (≥ 99%) elemental oxides, baddeleyite-type HfO2 and ZrO2, anatase-TiO2, cassiterite-SnO2, and C-Gd2O3. Milling was carried out in a Retsch PM400 planetary ball mill (rotation speed = 350 rpm), using YPSZ (5 wt% Y2O3) containers (volume = 125 ml; sample size = 20 g), and grinding media (20 mm ∅; balls-to-powder mass ratio = 10:1). The evolution of selected reacting mixtures with milling time was followed by using X-ray diffraction (XRD). Mechanochemical reactions were considered completed when no traces of the starting chemicals were observed by this technique. As-prepared samples were subjected to post-milling thermal treatments at 1500 °C and analyzed as described below. The structural and microstructural features were obtained from precise diffraction data collected by using a Bruker D8 high-resolution X-ray powder diffractometer equipped with a Ge(111) primary monochromator (CuKα1 radiation, λ = 1.5406 Å), and a LynxEye® rapid detector. The angular range, step size and counting times were adjusted to obtain good resolution (the step size should be, at least, 1/10th of the FWHMs), and statistics. The instrumental contribution to peak broadening was evaluated by using NIST LaB6 standard reference material (SRM 660a). The structural refinements were undertaken by using the Rietveld method and the FullProf program [23], to determine the lattice parameter, atomic positions (O in x48f) and the isotropic thermal factors (Debye–Waller); the chemical composition was included as constraint during the refinements since no additional phases were ever detected. Furthermore, the distribution of metal ions was allowed to move between the 16d and 16c site although always having in mind that smaller ions would prefer to sit at the 16d site, and correspondingly, larger ions would tend to occupy the 16c site. The samples microstructure was determined by the phenomenological approach described in detail elsewhere [24,25,26,27]. The oxygen array in our structural refinements is assumed to be ordered, as in the ideal pyrochlore structure. Raman spectra were collected in a Horiba Scientific LabRAM HR Evolution NIR spectrometer, equipped with an Olympus BX41 confocal microscope, a solid-state blue excitation laser (473 nm) and a liquid N2-cooled CCD detector.
The electrical characterization was carried out in pressed powders (applied pressure = 7 Tons cm−2; pellets size = 10 mm diameter and ~ 1 mm thickness) sintered at 1500 °C for 12 h (heating/cooling rate = 5 °C min−1). Pellets density was determined by using the Archimedes method and deionized water as the immersion medium; measurements were carried out in an Ohaus Discovery DV314C analytical balance (± 0.1 mg), equipped with a density determination accessory (P/N 77402-00). AC impedance measurements were carried out in air, as a function of frequency (100 Hz to 1 MHz) and temperature (250–700 °C), using a Solartron 1260 Frequency Response Analyzer and a ProboStat® sample holder system. Electrodes for impedance spectroscopy were made by coating opposite faces of the pellets, with conductive Pt paste and firing in air at 800 °C to eliminate organic components and harden the Pt residue.
Results and discussion
Synthesis
Figure 2 presents selected XRD patterns, collected at different stages of the synthesis of the Gd2Hf2−xSnxO7 system. The synthesis of the Gd2Hf2−xTixO7 and Gd2Hf2−xZrxO7 systems were presented elsewhere and would be referred here only for comparison purposes [13, 14]. Figure 2a shows the XRD pattern of a Gd2O3:HfO2:SnO2 reacting mixture (1:1.6:0.4 molar ratio), selected as representative of the series. Numbers in parenthesis are the Miller indexes of the most intense reflections, characteristic of the three starting chemicals: i.e., MH = baddeleyite m-HfO2; CG = C-Gd2O3 and T = cassiterite-SnO2; vertical lines at the bottom part of this figure represent the Bragg peaks of these oxides, as reported in the ICDD®. Figure 2b shows the evolution of this mixture with milling time, whereas Fig. 2c shows the XRD patterns of all compositions that were prepared in the Gd2Hf2−xSnxO7 system, as taken out of the mill (decreasing Hf4+ content from top to bottom); dashed lines in Fig. 2b, c are provided as a guide to the eye. As observed in 2b, diffraction lines belonging to C-Gd2O3, which are the most intense in the XRD pattern of the starting mixture (Fig. 2a), have almost disappeared after milling for only 1 h (e.g., the (440) line at ~ 47.5° (2θ) shows more than 80% reduced intensity), whereas characteristic lines of m-HfO2 [e.g., (111) line at 31.6°, 2θ] and SnO2 [e.g., (110) line at 26.6°, 2θ] are still very much evident, after milling for 6 or even 9 h. The rapid weakening and apparent disappearance of C-Gd2O3 diffraction lines from the pattern in such a short milling time is probably due to its polymorphic transformation to monoclinic B-Gd2O3, which might be activated by temperature (~ 1100 °C), but also by high-energy milling [28]; in our mixture, the most intense reflections characteristic of B-Gd2O3, which are found between 28 and 33° (2θ), is obscured between the two strongest lines of m-HfO2, the (− 111) and (111) lines.
By contrast, no evidence was ever found by XRD of an m- to t- or c-HfO2 (tetragonal or cubic) polymorphic transformation, probably because much higher energy is required in this case (transformation temperatures to t- or c-HfO2, are ~ 1720 °C and ~ 2600 °C, respectively). Although these HfO2 higher symmetry forms might be also stabilized at lower temperatures by the incorporation of lanthanide ions such as Gd3+, that does not happen apparently in our reacting mixtures. The formation of a reaction product and therefore the existence of a mechanochemical reaction becomes clear after milling for 6 h with new strong reflections emerging at ~ 30°, ~ 34°, ~ 49° and ~ 58° (2θ); this new set of reflections becomes narrower and more intense, with increasing milling time. Finally, the XRD pattern obtained after milling for 30 h is similar to that characteristic of a fluorite lattice, with no evidence of the starting chemicals, additional phases or any other impurity suggesting then, a complete reaction at this point. Very broad diffraction peaks as those observed in these patterns are characteristic of materials prepared by mechanosynthesis because of the small crystallite size and the high density of structural defects induced by milling. These results highlight the advantages of using mechanochemical methods to obtain extremely refractory compounds such as these lanthanide hafnates, which require very high temperatures (typically ≥ 1600 °C) and long and repeated firing cycles, when prepared by the traditional ceramic method. According to Fig. 2c, all the compositions prepared in this system seem to be either highly disordered pyrochlore or fluorite-like materials since none of the superlattice reflections characterizing the long-range ordering of cations, anions and vacancies in the pyrochlore structure [29], are evident by XRD: e.g., the (111), (311), (331) and (511) lines at, respectively, ~ 15°, ~ 29°, ~ 39° and ~ 46° (2θ). Therefore, Miller indexes shown in Fig. 2c are characteristic of fluorite-like phases, whereas Fig. 2d shows the XRD patterns of the same six compositions, after firing them at 1500 °C. As we have shown before in previous works [13, 30], Gd2Hf2O7- or Gd2Zr2O7-based powders prepared by mechanosynthesis present a fluorite-like structure; depending on the firing temperature, post-milling thermal treatments facilitate the relaxation (at least partially) of mechanically induced defects and the transformation to more ordered pyrochlore-type structures, in a top-down approach to the corresponding equilibrium phase diagrams. Although the XRD patterns shown in Fig. 2d are apparently similar to those of fluorite-like phases, a deeper inspection using precise X-ray diffraction data collected with a high-resolution diffractometer showed a different picture.
Structural refinement by the Rietveld method
Table 2 presents the rA/rB values for the end limit compositions of the three systems analyzed in this work, calculated using the ionic radii values given by Shannon [31]. Therefore, according to the size mismatch criteria, Hf4+ substitution by Ti4+ and to a lesser extent by Sn4+ should increase the stability of the pyrochlore structure and produce better ordered phases (increasing rA/rB), whereas introducing Zr4+ instead of Hf4+ should barely affect the degree of structural disorder in Gd2Hf2O7. Moreover, all intermediate compositions should also crystallize on the pyrochlore structure; Tables 3, 4 and 5 show a summary of the results obtained by the Rietveld method in the three systems, Gd2Hf2−xSnxO7, Gd2Hf2−xZrxO7 and Gd2Hf2−xTixO7; those of the Gd2Hf2−xTixO7 solid solution were already discussed in a previous paper [13] and are included here only for comparison purposes. Figure 3 shows the graphical results of fitting two different samples: (a) Gd2Hf0.4Zr1.6O7 and (b) Gd2Hf0.4Zr1.6O7.
All patterns were successfully refined to the pyrochlore structure, as expected according to Table 2. However, not all of them show the same degree of structural disorder. Therefore, as Table 3 shows, the unit cell parameter in the Gd2Hf2−xSnxO7 system hardly changes with increasing Sn4+ content, as expected from the small difference in ionic radii between VIHf4+ and VISn4+, whereas disorder decreases drastically across the entire system, with little cation anti-site disorder present in Gd2Sn2O7, i.e., after firing the as-prepared Gd2Sn2O7 powders at high temperature, the cation distribution is very close to that expected from the thermodynamic equilibrium configuration, with Gd3+ confined to the eightfold coordinated 16c site, and Hf4+ and Sn4+, both sharing the sixfold coordinated 16d site. Our results are in agreement with neutron diffraction studies carried out in lanthanide stannates, which have shown no evidence of cation anti-site defects or anion disorder but considerable covalency of the <Sn–O> bond [32]. Even in those Hf-rich compositions showing some cation anti-site defects, the best structural refinement results were obtained when assuming that Sn4+ ions remain at the sixfold coordinated site and allowing both Gd3+ and Hf4+ to disorder between the 16d and 16c positions. Comparable results have been recently obtained by 119Sn MAS NMR and Sn L3-edge XANES studies carried out in the Y2Sn2−xZrxO7 system [33], where despite a pyrochlore-to-fluorite phase transition taking place on increasing Zr4+ content, Sn4+ showed a strong preference to occupy the sixfold coordinated 16d site in the entire system, i.e., its first coordination sphere remains always basically as SnO6. By contrast, Gd2Hf2O7 presents a highly disordered structure even after firing at 1500 °C with almost 30% of all Gd3+ atoms occupying the “wrong” sixfold site, whereas an equal number of Hf4+ atoms are located at the eightfold coordinated 16c position. As shown in Table 4, this disordered structure is hardly affected when the replacing cation is Zr4+, and the entire system shows a defect pyrochlore structure, with a significant density of cation anti-site defects. A complex cation distribution among the two cation sites is observed, most likely due to the history (mechanical and thermal) of each sample; the only clear point is that Zr4+ tends to occupy the sixfold coordination. As the cell parameter of the pyrochlore structure is mostly determined by the size of the BO6 trigonal antiprism, the average size of the cations located in the 16d sites mainly determines the cell dimensions. In the case of the Gd2Hf2−xZrxO7 series, since Hf4+ and Zr4+ cations present similar size, the population of large Gd3+ determines the unit cell dimension, i.e., higher concentration of cation anti-site defects (higher structural disorder) results in larger unit cells.
For the Gd2Hf2−xTixO7 system due to the small size of Ti4+ that ensures a strong tendency to sixfold coordination, the population of Gd3+ ions at the 16d-site decreases rapidly on Hf4+ substitution and remains below 15% throughout the whole system. Finally, cation distribution in Gd2Ti2O7 corresponds to that expected based only in thermodynamic reasons.
The importance of bonding characteristics in pyrochlore disordering has been confirmed by experimental data. Despite of having almost the same cations size mismatch, the Gd2Ti2−xSnxO7 and Gd2Ti2−xZrxO7 systems show different evolution upon Ti substitution, whereas no significant change in the degree of structural disorder was observed in the Sn-containing system, a high number of defects evolve with increasing Zr content. The higher covalency of the <Sn–O> bonds as compared with <Ti–O> and <Zr–O> has been suggested to explain such differences [9].
Since XRD gives only an averaged structure, we used Raman spectroscopy to obtain more information about the local structure.
Raman spectroscopy
As structural disorder within the pyrochlore structure breaks up its translational symmetry and has a significant impact in the spectra, Raman spectroscopy is frequently used to obtain information about disordering trends in pyrochlore-type systems. It is noteworthy that such disruption allows more phonons to contribute to the optical spectra causing a general broadening of all Raman-active modes on disordering.
Therefore, according to the selection rules, the disordered anion deficient fluorite structure should have only one Raman-active mode of F2g symmetry, with the form of oxygen anions vibrating against the symmetry-fixed cations [34]. By contrast, A2B2O7 pyrochlore-type phases should have six Raman-active modes. Five of them (i.e., A1g + Eg + 3F2g) are commonly assigned to vibrations of O48f ions, which are bonded to two A and two B cations; the remaining one (F2g), to vibrations of the O8a ions, bonded only to four A cations [34,35,36]. Specifically, only O48f ions vibrate (predominantly bending) in A1g and Eg modes; furthermore, A1g is directly related to the only free parameter of the pyrochlore crystal structure, the x48f positional parameter. Figure 4 presents the evolution of the Raman spectrum of Gd2Hf2O7, when replacing Hf4+ by isovalent (a) Ti4+ (Gd2Hf2−xTixO7), (b) Sn4+ (Gd2Hf2−xSnxO7) and (c) Zr4+ (Gd2Hf2−xZrxO7); to ease the discussion, the top spectrum in (a), (b) and (c) is always that of pristine Gd2Hf2O7. As observed in this figure, the spectrum of Gd2Hf2O7 (i.e., x = 0) is dominated by two strong bands centered at 337 and 412 cm−1. Similar bands have been observed for pyrochlore-type La2Hf2O7 and they can be assigned to (F2g + Eg) and F2g modes, respectively [37]. As discussed in our previous work [13], the weak band at 543 cm−1 can be assigned to the A1g mode, whereas the remaining two F2g modes are located near 602 and 490 cm−1. Worth mentioning is that all bands are very broad and the A1g mode characteristic of the pyrochlore structure is very weak. Since these two features are considered to stem from structural disorder, the Raman spectrum of Gd2Hf2O7 is consistent with the highly disordered pyrochlore structure observed by XRD for this compound. Increasing Ti4+ content (from top to bottom in Fig. 4a) induces some important changes in the Raman-active bands of Gd2Hf2O7. Thus, all bands in the spectra exhibit important shifts with increasing substitution, most of them toward lower wavenumbers (e.g., from 337, 543 and 602 cm−1 to 309, 515 and 577 cm−1 for x = 2, i.e., Gd2Ti2O7), although some bands shift also toward higher wavenumbers (e.g., from 412 to 446 cm−1). Furthermore, the band near 490 cm−1 is absent in Gd2Ti2O7, and those at 446 and 577 cm−1, present a considerable reduction in intensity.
By contrast, the A1g band shows increased intensity with higher Ti4+ content; overall, most bands show significant narrowing with increasing level of Hf4+ substitution. These two later characteristics have been related to higher structural ordering [13, 34, 38], and they suggest that doping with Ti4+ leads to a considerable growth of the pyrochlore-like domains. Note that the spectrum of Gd2Hf2O7 shows additional very broad bands near 730 and 830 cm−1. The intensity of these bands strongly increases when x = 0.4 and 0.8, and then decreases gradually for Ti4+-rich compositions. As discussed previously, these bands can be attributed mainly to disorder-activated oxygen vibrations and a partial occupation of the 8a sites, which are completely empty in an ideal pyrochlore structure [13, 39]. Thus, our Raman results suggest that the x = 0.4 and 0.8 samples show the highest degree of oxygen disorder in this system, and that this disorder decreases for higher Ti4+ contents. These observations are in very good agreement with our own XRD data analysis shown before.
As for the Gd2Hf2−xSnxO7 system, Fig. 4b shows that the Raman bands of Gd2Hf2O7 also exhibit important shifts with increasing Sn4+ content (i.e., from 337, 412 and 543 cm−1 in Gd2Hf2O7, to 309, 414 and 501 cm−1 for Gd2Sn2O7). As in the Gd2Hf2−xTixO7 system, the intensity of the band near 602 cm−1 shows reduced intensity with increasing tin content and it is absent in Gd2Sn2O7 (bottom spectrum). Furthermore, a new weak and narrow band appears at 533 cm−1. This behavior strongly suggests that our previous assignment of the 602 cm−1 band in the Gd2Hf2−xTixO7 system to a F2g mode [13] is probably not correct. Most likely, this F2g mode in the Ti-containing system should be located near 530 cm−1 but it is obscured by the large width of the A1g band; as this A1g band is significantly narrower in the Gd2Hf2−xSnxO7 system, the F2g mode is clearly visible for samples with x ≥ 0.8. Although the origin of the band near 600 cm−1 is not so clear, the fact that it exhibits decreasing intensity with increasing Ti4+ or Sn4+ content suggests that it should be related to oxygen disorder. Finally, for Sn-rich compositions (x = 1.6 and x = 2), the Gd2Hf2−xSnxO7 system also shows an additional weak band at 345 cm−1, not resolved for other chemical compositions, which can be attributed most likely to the Eg mode. As observed by XRD, this behavior supports the evolution of the Gd2Hf2−xSnxO7 system into a very well-ordered pyrochlore structure, upon Sn4+ doping. In general, the Raman spectra of the Gd2Hf2−xSnxO7 system show similar behavior as the Ti-containing system although the effects associated to higher structural ordering, i.e., narrowing of Raman bands and increasing intensity of the A1g band with lower Hf4+ content are much more pronounced.
Contrary to these two systems, Gd2Hf2−xSnxO7 and Gd2Hf2−xTixO7, doping with Zr4+ ions has almost no effect on the Raman bands of Gd2Hf2O7, i.e., the Raman spectra of Gd2Hf2O7 and Gd2Zr2O7 (top and bottom spectra in Fig. 4c) are very similar and unambiguously assigned to highly defective pyrochlore structures. Therefore, all Raman bands in the Gd2Hf2−xZrxO7 solid solution remain very broad irrespective of the Hf4+/Zr4+ ratio, which is consistent with the system maintaining a highly disordered pyrochlore-type structure as discussed in the previous section.
In summary, the Raman study shows clearly that oxygen disorder in the Gd2Hf2−xBxO7 title systems decreases with increasing Ti4+ or Sn4+ content, but remains largely unaffected when the replacing cation is Zr4+.
Electrical properties
Figure 5a–d shows some representative examples of the electrical characterization carried out in the title samples. Hf4+ substitution has also a significant influence on density. When firing at the same temperature, Ti4+ produces samples with higher density (83–91%) than Zr4+ (77–90%) or Sn4+ (67–91%). Nevertheless, impedance spectroscopy which is the technique used to study the electrical properties of these materials allows separating individual contributions from different regions of a sample, and determine its intrinsic conductivity. Figure 5a shows the frequency and temperature dependence of the real component of the electrical conductivity of Gd2Hf1.6Sn0.4O7, in a log–log representation. Similar graphs were obtained for the remaining samples. Two different conductivity regimes are clearly observed in this graph; on the one hand, there is this region at low temperatures (e.g., ≤ 380 °C) and high frequencies, where conductivity shows a power-law type dependence with frequency, which has been linked to the hopping dynamics of mobile ions.
With increasing temperature, this region shifts to higher frequencies and out of the experimental window (≥ 500 °C). On the other hand, there is a plateau region at every temperature, where the conductivity is frequency independent; such regime which dominates this sample’s response for measuring temperatures ≥ 500 °C is associated with the bulk conductivity, σdc. Figure 5b shows the frequency and temperature dependence of the real component of the dielectric permittivity also in a log–log representation, for the same sample. Ion blocking effects at grain boundaries and electrodes which are characteristic of ionic conduction are very much evident in this graph as significant increments in permittivity values shifting to higher frequencies with increasing temperature. Therefore, Fig. 5b confirms that conductivity in this system is mainly ionic. Figure 5c shows a complex impedance plot of the same sample (measuring temperature = 380 °C), which is similar to those characteristic of most solid electrolyte materials and features two semicircles, with capacitance values characteristic of grain boundary (low frequencies) and bulk contributions (high frequencies). Figure 5d shows the temperature dependence of the bulk conductivity for the whole Gd2Hf2−xSnxO7 system; dashed lines in these graphs are least squares best fits to an Arrhenius-type law of the form of σdc=(σ0/T)exp(− Edc/kT), where Edc is the activation energy for ion migration; σ0 is the pre-exponential factor which is proportional to the number of mobile charge carriers in the structure; k is the Boltzmann constant and T is the absolute temperature (K). This figure confirms that ion diffusion in the system is thermally activated. The activation energy (eV) as obtained from the slope of the Arrhenius graphs is shown in Table 6 and compared with that of the other two systems Gd2Hf2−xTixO7 and Gd2Hf2−xZrxO7. Table 6 also shows the bulk conductivity of each composition, σdc, measured at 700 °C, whereas Fig. 6 depicts the effect of Hf4+ substitution by Ti4+ (Fig. 6a), Sn4+ (Fig. 6b) and Zr4+ (Fig. 6c), on the Edc and log(σT)700 of Gd2Hf2O7.
Worth mentioning, Edc and σdc values obtained in this work are comparable with those found in similar systems [40,41,42]. As observed in Table 6, the effect of Zr4+ is significantly different from that of Ti4+ and Sn4+. Thus, σdc at 700 °C in the Gd2Hf2−xZrxO7 series increases by almost an order of magnitude on increasing zirconium content (from 2.7 × 10−4 to 1.55 × 10−3 Sm cm−1) whereas decreasing more than two orders of magnitude, when the replacing cation is either titanium (to 1.12 × 10−6 Sm cm−1) or tin (to 8.71 × 10−7 Sm cm−1). This effect is also graphically illustrated in the log(σT)700 representation of Fig. 6 (red solid squares). It is noteworthy that the Edc and σdc trends within each system are not correlated and lower Edc does not necessarily render higher σdc. Thus, Edc in the Gd2Hf2−xZrxO7 system (6c) is hardly affected by substitution since both end limits display similar values (~ 1.2 eV); even though, the lowest Edc value is obtained when x = 0.8 (1.035 eV). By contrast, the Edc in the Gd2Hf2−xTixO7 system (6a) decreases almost continuously on increasing Ti content, reaching a minimum at x = 1.6 (0.716 eV) and then increasing again for Gd2Ti2O7 (0.898 eV), whereas the Edc in the Gd2Hf2−xSnxO7 system (6b) decreases abruptly at first, reaching a minimum when x = 0.4 and then increases for higher Sn4+ contents ending at 1.07 eV for Gd2Sn2O7. Finally, we found also of interest to plot in Fig. 6d the σdc versus the cations size mismatch for the three systems. This graphs shows, indeed, that changes in the cations size ratio rA/rB cannot fully explain the trends in conductivity of these systems.
Worth mentioning, Edc and σdc values obtained in this work are comparable with those found in similar systems [40,41,42]. As observed in Table 6, the effect of Zr4+ is significantly different from that of Ti4+ and Sn4+. Thus, σdc at 700 °C in the Gd2Hf2−xZrxO7 series increases by almost an order of magnitude on increasing zirconium content (from 2.7 × 10−4 to 1.55 × 10−3 Sm cm−1) whereas decreasing more than two orders of magnitude, when the replacing cation is either titanium (to 1.12 × 10−6 Sm cm−1) or tin (to 8.71 × 10−7 Sm cm−1). This effect is also graphically illustrated in the log(σT)700 representation of Fig. 6 (red solid squares). It is noteworthy that the Edc and σdc trends within each system are not correlated and lower Edc does not necessarily render higher σdc. Thus, Edc in the Gd2Hf2−xZrxO7 system (6c) is hardly affected by substitution since both end limits display similar values (~ 1.2 eV); even though, the lowest Edc value is obtained when x = 0.8 (1.035 eV). By contrast, the Edc in the Gd2Hf2−xTixO7 system (6a) decreases almost continuously on increasing Ti content, reaching a minimum at x = 1.6 (0.716 eV) and then increasing again for Gd2Ti2O7 (0.898 eV), whereas the Edc in the Gd2Hf2−xSnxO7 system (6b) decreases abruptly at first, reaching a minimum when x = 0.4 and then increases for higher Sn4+ contents, ending at 1.07 eV for Gd2Sn2O7. Finally, we found also of interest to plot in Fig. 6d the σdc versus the cations size mismatch for the three systems. This graphs shows, indeed, that changes in the cations size ratio rA/rB cannot fully explain the trends in conductivity of these systems.
Discussion
The most striking feature of the A2B2O7 pyrochlore structure when compared to the ideal BO2 fluorite structure is perhaps the fact that 1/8th of the anions are missing from the oxygen sublattice, i.e., as the stoichiometry changes from BO2 to A2B2O7, the anion-to-cation ratio decreases from 2 to 1.75, and anion vacancies are created to preserve electroneutrality. Using the Wyckoff’s notation, such oxygen vacancies are ordered in the 8b site (3/8 3/8 3/8); interestingly, this site which is nominally empty in ideal (ordered) pyrochlore structures can be easily occupied by anions in defect (disordered) structures, mainly coming from the neighboring 48f site. On moving to the vacant 8b site, O48f leave behind a continuous path for the migration of oxygen vacancies along the 48f position, transforming some defect pyrochlore-type oxides, into intrinsic oxygen ion conducting materials at high temperature. Correspondingly, the prevailing ion transport mechanism in this structure consists basically of consecutive 48f → 48f jumps along the <100> and <110> directions. Interestingly, anion disorder is favored by the presence of disorder also in the cation sublattice, which in turn, is mainly controlled by the A to B size mismatch, i.e., the rA/rB ratio. Another important factor determining the stability of the pyrochlore structure and its oxide ion conducting properties is the type (i.e., ionic vs. covalent) and strength of the metal–oxygen bonds, i.e., <A–O> but mostly, <B–O> bonds. Moreover, recent calculations have shown that migration along the <100> direction would be controlled by the strength of the <B–O> bond, whereas migration along the <110> direction would be governed by the size mismatch [43]. Our results confirm, indeed, that both characteristics are important when determining the electrical properties of Gd2Hf2O7-based systems. The three substituting tetravalent cations selected for this study, Zr4+, Sn4+ and Ti4+, covered both factors; the first two have very similar ionic radii to Hf4+ although the <Sn–O> bonding is significantly more covalent than <Zr–O> and <Hf–O>, whereas Ti4+ have a smaller ionic radius than Hf4+ and at the same time, its bonding to oxygen has a higher covalent contribution.
According to our structural study, all compositions prepared by mechanochemical synthesis in these three systems Gd2Hf2−xBxO7 (B = Ti, Sn, Zr) present an averaged pyrochlore-like structure after firing at 1500 °C, in agreement with the rA/rB size ratio criteria for pyrochlore stability, i.e., the pyrochlore structure is thermodynamically favored at room temperature, over the anion deficient fluorite structure in all four end members of the three systems targeted in the present study. As for the evolution of the unit cell size on substitution, Zr4+ and Sn4+ do not produce major changes since both have very similar ionic radii to Hf4+. By contrast, the unit cell size decreases significantly when the substituting cation is Ti4+. As for the degree of structural disorder, XRD results also show that cation distribution in Gd2Hf2−xZrxO7 is highly disordered with a significant amount of Gd3+ ions (c.a. 25%) occupying the 16d octahedral site and correspondingly equal number of (Hf4+/Zr4+) ions located at the eightfold coordinated site. Therefore, both end members seem to present a highly disordered pyrochlore structure when obtained by mechanical milling, even after firing at 1500 °C and slow cooling to room temperature. Cation distribution in the Gd2Hf2−xSnxO7 and Gd2Hf2−xTixO7 systems is another story. Therefore, the first one shows a continuous trend toward better ordered structures with increasing Sn4+ content and Gd2Sn2O7 features an almost perfect pyrochlore structure, in agreement with previous studies [32]. Raman spectroscopy confirms the XRD analysis results and show that although the averaged structure in every case is of pyrochlore-type, each system shows a very different degree of oxygen disorder. Thus, disorder is high in Gd2Hf2O7, decreases when the replacing cation is Sn4+ or Ti4+ but remains high when using Zr4+. As for the electrical properties, we have also shown that in general both Sn4+ and Ti4+ substitutions have a detrimental effect in conductivity, whereas Zr4+ incorporation increases σdc, by almost half an order of magnitude. Nevertheless, the highest conductivity in the Gd2Hf2−xTixO7 system was obtained for Gd2Hf1.6Ti0.4O7. Changes in the size ratio cannot explain σdc values since change in it seems, however, to be correlated with decreasing covalency in the B4+–O bonds. The observed behavior cannot be related to change in the ionic radius of the B4+ ion.
Conclusions
We have successfully prepared at room temperature, highly refractory and pyrochlore-type HfO2-based oxides, using a mechanochemical reaction and the corresponding elemental oxides as reagents. Our results have shown that milling for 30 h in a planetary ball mill is enough to obtain single-phase multicomponent oxides of general formula Gd2Hf2−xBxO7 (B = Ti, Sn, Zr) and with a fluorite-like structure. XRD analysis and Raman spectroscopy have also shown that all of them present a pyrochlore-like structure after firing at 1500 °C although with different degree of structural disorder. Thus, Hf4+ substitution by Sn4+ and Ti4+ produce better ordered pyrochlore oxides, whereas Zr4+ substitution does not have much influence in disorder. Impedance spectroscopy analysis have confirmed that composition in the Gd2Hf2−xZrxO7 system is high-temperature oxygen ion conducting materials with conductivities in the order of 10−3 Scm−1 at 700 °C, whereas Sn4+ and Ti4+ substitutions have a detrimental effect in conductivity. Both, the cations size ratio rA/rB and the ionic/covalent character of the <B–O> bonding influence the structural characteristics and the electrical conductivity of these oxides.
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Acknowledgements
This work was financially supported by CONACYT (Grants CB2013-01-221701). The authors acknowledge Prof. Maik Lang for providing the opportunity to carry out the Raman spectroscopy measurements at the University of Tennessee (Knoxville, TN), and Igor M. Gussev for his help when collecting the spectra.
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Cepeda-Sánchez, N.M., Díaz-Guillén, J.A., Maczka, M. et al. Cations size mismatch versus bonding characteristics: synthesis, structure and oxygen ion conducting properties of pyrochlore-type lanthanide hafnates. J Mater Sci 53, 13513–13529 (2018). https://doi.org/10.1007/s10853-018-2402-5
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DOI: https://doi.org/10.1007/s10853-018-2402-5