Incorporation and Conduction of Protons in Ca, Sr, Ba-Doped BaLaInO4 with Ruddlesden-Popper Structure

The new phases BaLa0.9M0.1InO3.95 (M = Ca2+, Sr2+, Ba2+) with a Ruddlesden-Popper structure were obtained. It was established that all investigated samples were capable for the water uptake from the gas phase. The ability of water incorporation was due to not only by the presence of oxygen vacancies, but also due to the presence of La-O blocks in the structure. The degree of hydration of the samples was much higher than the concentration of oxygen vacancies and the composition of the samples appear to be BaLaInO3.42(OH)1.16, BaLa0.9Ca0.1InO3.25(OH)1.4, BaLa0.9Sr0.1InO3.03(OH)1.84, BaLa0.9Ba0.1InO2.9(OH)2.1. The degree of hydration increased with an increase in the size of the dopant, i.e., with an increase in the size of the salt blocks. It was proven that doping led to the increase in the oxygen ionic conductivity. The conductivities for doped samples BaLa0.9M0.1InO3.95 were higher than for undoped composition BaLaInO4 at ~1.5 order of magnitude. The increase in the conductivity was mainly attributed to the increase of the carrier concentration as a result of the formation of oxygen vacancies during doping. The proton conductivities of doped samples increased in the order Ca2+–Sr2+–Ba2+ due to an increase in the concentration of protons. It was established that all doped samples demonstrated the dominant proton transport below 450 °C.


Introduction
Protonic ceramics are important materials for using as electrolytes in proton-conducting solid oxide fuel cells (H-SOFCs) [1][2][3][4][5][6]. The application of the proton-conducting complex oxides in comparison with oxygen-ion conductors (in oxygen ion-conducting solid oxide fuel cells O-SOFCs) has several advantages. First, the proton electrolytes have lower activation energies of charge carriers (~0.5 eV) than the oxygen-ion conductors (~1 eV). Consequently, they have higher conductivities. This allows us to decrease the operating temperatures from 900-1000 • C (O-SOFCs) to 500-700 • C (H-SOFCs) [7] and provides the decrease of the production cost of H-SOFCs at 27-37% [8]. Secondly, the water vapor in the H-SOFCs is produced at the air-side electrode (the cathode side) and this avoids the dilution of fuel by steam [9], and, consequently, increases the energy conversion efficiency [10,11]. Therefore, the discovery of a new structure family of proton conductors is important both in terms of the development of scientific materials and in the applied aspect.
The most studied protonic conductors are the complex oxides with perovskite or perovskite-related structures. Further development of proton conductors suggests investigations of materials with new types of structures, including Ruddlesden-Popper structure. It is common understanding that oxygen-deficient compounds are capable of manifesting not only oxygen-ionic conductivity, but also protonic conductivity in a humid atmosphere. Therefore, perovskite-related structures with oxygen-ion

Materials and Methods
The phases BaLa 0.9 M 0.1 InO 3.95 (M = Ca 2+ , Sr 2+ , Ba 2+ ) and the parent composition BaLaInO 4 were prepared by a solid-state method. The preliminary dried high-purity powders of CaCO 3 , SrCO 3, BaCO 3 , In 2 O 3 , and La 2 O 3 were used. Prior to weighing, the starting materials were dried. The stoichiometric powder mixtures were manually milling in an agate mortar and then calcined at 800, 900, 1000, 1100, 1200, and 1300 • C for 24 h. Intermediate grindings were made for every following heating step.
Phase purity was monitored by powder X-ray diffraction (XRD) on a Bruker Advance D8 diffractometer with CuK α radiation. The crystal structures of dry and hydrated samples were determined by Rietveld refinement [25]. The dry samples were prepared for XRD by heat treated at 1100 • C for 4 h and then cooled in dry Ar (pH 2 O = 3.5 × 10 −5 atm). The hydrated samples were obtained at slow cooling from 1100 to 150 • C (1 • C/min) under a flow of wet Ar (99.999% purity, pH 2 O = 2 × 10 −2 atm). Ar atmosphere was used to avoid any carbonization of the samples.
TG-analysis was carried out on a STA 409 PC analyzer (Netzsch, Selb, Germany) coupled with a quadrupole mass spectrometer QMS 403 C Aëolos (Netzsch, Selb, Germany) in order to determine the degree of hydration. The samples were heated at the rate of 10 • C/min in a corundum crucible under a flow of dry Ar at temperatures ranging from 40 to 1100 • C. Before TG-measurements, the powder samples were initially hydrated as described above. The number of moles of water per one formula unit was determined and the notation of the total composition as BaLa 0.9 M 0.1 InO 3.95 ·nH 2 O was used for convenience of comparison. To indicate that H 2 O incorporation gives OH − -groups, the formulas were also written in another representation as BaLa 0.9 M 0.1 InO 3.95−n (OH) 2n .
The ceramics used for the electrical measurements were prepared by pressing cylindrical pellets and sintering them at 1300 • C for 24 h in dry air. The samples typically had a relative density of around ∼92% (density of the sintered samples was determined by the Archimede method). After polishing, the platinum paste electrodes were fired at 900 • C for 3 h. The ac conductivity of the samples (two-probe method) was measured over the frequency range of 1 kHz-1 MHz using a Z-1000P (Elins, RF) impedance spectrometer at an applied voltage of 150 mV. The least squares refinement program ZView (Scribner Associates Inc., Southern Pines, NC, USA) was used to fit the impedance data to an (RQ) equivalent circuit, where R is resistance and Q is the constant phase element. The bulk resistance was calculated from the impedance data and then the bulk conductivity was calculated and discussed below. From the fitted resistances and, together with the geometrical dimensions, the total conductivity can be calculated using the following equation.
where l and S are the thickness and surface area of the sample. The measurements of the temperature dependencies of conductivities were performed in the temperature range from 200 to 1000 • C every 10 to 20 • C with a cooling rate of 1 • C/min. During the measurement, the sample was held at each temperature until the resistances became constant. The conductivity measurements were carried out under dry and wet air or Ar.
The «wet» gas was obtained by bubbling the gas at room temperature first through distilled water and then through a saturated solution of KBr (pH 2 O = 2 × 10 −2 atm). The «dry» gas was produced by circulating the gas through P 2 O 5 (pH 2 O = 3.5 × 10 −5 atm). The humidity of gases was measured by the H 2 O-sensor ("Honeywell" HIH-3610, Charlotte, NC, USA).

X-ray Characterization
The X-ray diffraction (XRD) results for the parent compound BaLaInO 4 and its doped analogs BaLa 0.9 M 0.1 InO 3.95 (M = Ca 2+ , Sr 2+ , Ba 2+ ) showed that the samples were single phase (orthorhombic symmetry, space group Pbca). The obtained lattice parameters for the sample BaLaInO 4 were in good agreement with previously reported data [24]. The substitution of M 2+ ions for La +3 ion led to changes in structural parameters ( Table 1). The lattice parameters and cell volumes increased with an increasing ionic radius of the dopant [26]. It should be noted that a more significant increase in parameters and cell volume in comparison with the undoped sample was observed for the Ba 2+ -doped sample. At the same time, for the Ca 2+ -doped sample (as the closest-sized ion to lanthanum), an increase and decrease in the lattice parameters was observed. It is known that the formation of oxygen vacancy is also accompanied by decreases of the lattice parameter because of the size relationship of oxygen vacancy and the oxide ion [27]. We can assume that, for the Ca 2+ -doped sample, the overall effect of the influence of the size of the B-cation and oxygen vacancy occurred and no monotonic change of the parameters was observed. The hydration processes led to the changes in the crystal structure for the samples compared with anhydrous samples. All hydrated samples BaLaInO 4 ·nH 2 O and BaLa 0.9 M 0.1 InO 3.95 ·nH 2 O belonged to the monoclinic symmetry (space group P2/m). The increase in the ionic radii of alkaline earth metal led to the increase in the cell volume of hydrate samples (Table 1).
It should be noted that XRD-patterns for all obtained samples were refined by the Rietveld analysis. Results for anhydrous BaLa 0.9 Sr 0.1 InO 3.95 and hydrated BaLa 0.9 Sr 0.1 InO 3.95 ·nH 2 O are presented in Figure 1a,b as an example of fitting.   Figure 1a,b as an example of fitting.

Thermal Properties
The water uptake was established by TG-analysis in combination with differential scanning calorimetry (DSC) and mass-spectrometry (MS).
As is well known, the possibility of water uptake from the gas phase for perovskite-type oxide conductors is due to the presence of oxygen vacancies in the structure and can be described as follows.

Thermal Properties
The water uptake was established by TG-analysis in combination with differential scanning calorimetry (DSC) and mass-spectrometry (MS).
As is well known, the possibility of water uptake from the gas phase for perovskite-type oxide conductors is due to the presence of oxygen vacancies in the structure and can be described as follows.  Figure 2, for all the investigated samples, the mass loss was observed, which is attributed to a loss of water, in accordance with MS data. Water uptake of the samples was much higher than the concentration of oxygen vacancies and the composition of the samples appears to be BaLaInO 4 ·0.58H 2 O (or BaLaInO 3.42 (OH) 1 Figure 2, for all the investigated samples, the mass loss was observed, which is attributed to a loss of water, in accordance with MS data. Water uptake of the samples was much higher than the concentration of oxygen vacancies and the composition of the samples appears to be BaLaInO4•0.58H2O (or BaLaInO3.42(OH)1. 16 Figure 3 represents the comparison of TG-curves, DSC-curves, and MS-curves for the hydrated sample BaLaInO4•nH2O. As can be seen, the sample underwent a mass decrease in the temperature from 200 to 800 °C, which was accompanied by a three endothermic DSC-signals (two well pronounced and one weak signal) at ~320 °C, ~500 °C , and ~700 °C. The MS analysis indicated that the mass change can be attributed by the water loss . No other volatile components (CO2, O2) were detected. The doped samples BaLa0.9M0.1InO3.95 showed the similar TG-curves, DSC-curves, and MScurves ( Figure 2).
It is known that the ability of water incorporation is ensured not only by the presence of oxygen vacancies, but also by the features of the crystal structure [28]. For layered structures, it can be explained by the ability of water incorporation by the salt La−O blocks, which alternates with blocks of the perovskite matrix. For example, the formation of hydrated phases based on the Ruddlesden-Popper-type layered oxide Ba2ZrO4 [29] was proven. During hydration, this phase can incorporate up to 1.7 mol of water Ba2ZrO4•1.7H2O. The effects of water incorporation into layered structures were summarized in the dissertation [30]. It was shown that RP phases can adopt up to two water molecules per formula unit/rock-salt block. At the same time, the large amount of water molecules in some RP-phases can be explained by the formation of hydrates and, in addition, not all RP  Figure 3 represents the comparison of TG-curves, DSC-curves, and MS-curves for the hydrated sample BaLaInO 4 ·nH 2 O. As can be seen, the sample underwent a mass decrease in the temperature from 200 to 800 • C, which was accompanied by a three endothermic DSC-signals (two well pronounced and one weak signal) at~320 • C,~500 • C, and~700 • C. The MS analysis indicated that the mass change can be attributed by the water loss. No other volatile components (CO 2 , O 2 ) were detected. The doped samples BaLa 0.9 M 0.1 InO 3.95 showed the similar TG-curves, DSC-curves, and MS-curves ( Figure 2). compounds react with water under ambient conditions. This shows that the elemental composition of an RP compounds has a significant effect on the stability, and atoms with the biggest influence are the cations present in the rock-salt block. If the majority of cations in the rock-salt block are large cations, e.g., Ba, K, Rb or Cs, then the compounds have a higher tendency for the intercalation of wa ter into the rock-salt block [30]. As can be seen from Figure 2, the degree of hydration increases in the order of BaLaInO4-BaLa0.9Ca0.1InO3.95-BaLa0.9Sr0.1InO3.95-BaLa0.9Ba0.1InO3.95. We can suggest that, with an increase in the size of the dopant, the size of the salt block increases . This contributes to the placement of a larger number of OH − -groups, which occupy interstitial sites within the rock salt layers. Therefore, we can conclude that investigated samples BaLaInO4 and BaLa0.9M0.1InO3.95 can show the ability for water uptake not only in accordance with reaction (2), but also due to the presence in the structure of La-O blocks (rock-salt blocks).
Thus, the results show the ready ability of the RP-structure to incorporate extra water as OH −groups, located in the sites of the rock salt layers. This ability can lead to proton transport. In addition, it is important to note that these results also show that it is possible to regulate the concentration of intercalated water by the nature of the dopant introduced into the salt layers.

Electrical Properties
For all the samples in this study, one semicircle, starting from zero coordinates of the complex Z-Z′ plane and corresponding to the bulk component, was observed. Typical impedance spectroscopy diagrams for the BaLa0.9Sr0.1InO3.95 sample, recorded at various temperatures, are given in Figure 4. The capacitance of the observed arc was estimated to be about 10 −11 F•cm −1 , which is typical of a bulk response. According to the experimental data obtained for other phases with an RP structure It is known that the ability of water incorporation is ensured not only by the presence of oxygen vacancies, but also by the features of the crystal structure [28]. For layered structures, it can be explained by the ability of water incorporation by the salt La−O blocks, which alternates with blocks of the perovskite matrix. For example, the formation of hydrated phases based on the Ruddlesden-Popper-type layered oxide Ba 2 ZrO 4 [29] was proven. During hydration, this phase can incorporate up to 1.7 mol of water Ba 2 ZrO 4 ·1.7H 2 O. The effects of water incorporation into layered structures were summarized in the dissertation [30]. It was shown that RP phases can adopt up to two water molecules per formula unit/rock-salt block. At the same time, the large amount of water molecules in some RP-phases can be explained by the formation of hydrates and, in addition, not all RP compounds react with water under ambient conditions. This shows that the elemental composition of an RP compounds has a significant effect on the stability, and atoms with the biggest influence are the cations present in the rock-salt block. If the majority of cations in the rock-salt block are large cations, e.g., Ba, K, Rb or Cs, then the compounds have a higher tendency for the intercalation of water into the rock-salt block [30].
As can be seen from Figure 2, the degree of hydration increases in the order of BaLaInO 4 -BaLa 0.9 Ca 0.1 InO 3.95 -BaLa 0.9 Sr 0.1 InO 3.95 -BaLa 0.9 Ba 0.1 InO 3.95 . We can suggest that, with an increase in the size of the dopant, the size of the salt block increases. This contributes to the placement of a larger number of OH − -groups, which occupy interstitial sites within the rock salt layers.
Therefore, we can conclude that investigated samples BaLaInO 4 and BaLa 0.9 M 0.1 InO 3.95 can show the ability for water uptake not only in accordance with reaction (2), but also due to the presence in the structure of La-O blocks (rock-salt blocks).
Thus, the results show the ready ability of the RP-structure to incorporate extra water as OH − -groups, located in the sites of the rock salt layers. This ability can lead to proton transport. In addition, it is important to note that these results also show that it is possible to regulate the concentration of intercalated water by the nature of the dopant introduced into the salt layers.

Electrical Properties
For all the samples in this study, one semicircle, starting from zero coordinates of the complex Z-Z plane and corresponding to the bulk component, was observed. Typical impedance spectroscopy diagrams for the BaLa 0.9 Sr 0.1 InO 3.95 sample, recorded at various temperatures, are given in Figure 4. The capacitance of the observed arc was estimated to be about 10 −11 F·cm −1 , which is typical of a bulk response. According to the experimental data obtained for other phases with an RP structure (for example, LaSrInO 4 [19,20] and NdBaInO 4 [13]), two contributions can be observed in the typical impedance spectroscopy diagrams. The semicircle in the high-frequency range, corresponding to the contribution from bulk resistance, and very small low-frequency semicircle, attributed to the contribution of grain-boundary resistance. It should be noted that the grain-boundary arc was manifested in the frequency range of 100 mHz to 100 Hz. In comparison with the presented data for doped BaLaInO 4 (Figure 4), the observed one semicircle is realized in the frequency range of 1 to 1000 kHz. Therefore, the arc corresponding to the grain boundary response, which appears at lower frequencies (in comparison with bulk semicircle), cannot be observed due to the instrumental limitations of the frequency range. (for example, LaSrInO4 [19,20] and NdBaInO4 [13]), two contributions can be observed in the typical impedance spectroscopy diagrams. The semicircle in the high-frequency range, corresponding to the contribution from bulk resistance, and very small low-frequency semicircle, attributed to the contribution of grain-boundary resistance. It should be noted that the grain-boundary arc was manifested in the frequency range of 100 mHz to 100 Hz. In comparison with the presented data for doped BaLaInO4 (Figure 4), the observed one semicircle is realized in the frequency range of 1 to 1000 kHz. Therefore, the arc corresponding to the grain boundary response, which appears at lower frequencies (in comparison with bulk semicircle), cannot be observed due to the instrumental limitations of the frequency range.

Dry Conditions
The temperature dependencies of total conductivities for investigated samples BaLaInO4 and BaLa0.9M0.1InO3.95 (M = Ca 2+ , Sr 2+ , Ba 2+ ) are shown in Figure 5. For dry air (pH2O = 3.5 × 10 −5 atm) ( Figure  5), the conductivities for doped samples BaLa0.9M0.1InO3.95 are higher than those for undoped composition BaLaInO4 at a ~1.5 order of magnitude. To evaluate the contribution of electronic conductivity of investigated phases, the measurements were performed in the Ar atmosphere (that is, at lower pO2 where ionic conductivity dominates). The comparison of total conductivities in air and Ar under dry conditions was shown in Figure 6. The conductivities in Ar atmosphere were lower than the conductivities, measured in air. The conductivity enhancement in air can be ascribed to the electronic conduction because of formation of holes in air, as shown by the quasi-chemical reaction.
For the undoped sample, the conductivity in Ar atmosphere were lower than the conductivities, measured in air, over the whole temperature range studied. This proves the mixed oxygen ionicelectronic character of conductivity of BaLaInO4. For Sr 2+ , Ba 2+ -doped samples, the conductivity exhibited the same character, but, for the Ca 2+ -doped sample, the differences were more significant at higher temperatures and the conductivity values were comparable at low temperatures, which indicates that the electron contribution decreases with a falling temperature and this phase exhibited the dominant oxygen-ionic character of conductivity below 500 °C. These results also showed that for the Sr 2+ , Ba 2+ -substituted phases, the contribution of the electronic conductivity was greater when compared to the Ca 2+ -substituted phase.

Dry Conditions
The temperature dependencies of total conductivities for investigated samples BaLaInO 4 and BaLa 0.9 M 0.1 InO 3.95 (M = Ca 2+ , Sr 2+ , Ba 2+ ) are shown in Figure 5. For dry air (pH 2 O = 3.5 × 10 −5 atm) ( Figure 5), the conductivities for doped samples BaLa 0.9 M 0.1 InO 3.95 are higher than those for undoped composition BaLaInO 4 at a~1.5 order of magnitude. To evaluate the contribution of electronic conductivity of investigated phases, the measurements were performed in the Ar atmosphere (that is, at lower pO 2 where ionic conductivity dominates). The comparison of total conductivities in air and Ar under dry conditions was shown in Figure 6. The conductivities in Ar atmosphere were lower than the conductivities, measured in air. The conductivity enhancement in air can be ascribed to the electronic conduction because of formation of holes in air, as shown by the quasi-chemical reaction.
For the undoped sample, the conductivity in Ar atmosphere were lower than the conductivities, measured in air, over the whole temperature range studied. This proves the mixed oxygen ionic-electronic character of conductivity of BaLaInO 4 . For Sr 2+ , Ba 2+ -doped samples, the conductivity exhibited the same character, but, for the Ca 2+ -doped sample, the differences were more significant at higher temperatures and the conductivity values were comparable at low temperatures, which indicates that the electron contribution decreases with a falling temperature and this phase exhibited the dominant oxygen-ionic character of conductivity below 500 • C. These results also showed that for the Sr 2+ , Ba 2+ -substituted phases, the contribution of the electronic conductivity was greater when compared to the Ca 2+ -substituted phase.     increase of the carrier concentration as a result of the formation of oxygen vacancies during doping. The M 2+ -cations are incorporated into the lattice at La 3+ sites with the creation of oxygen vacancies as charge-compensating defects. This doping process can be represented by the following defect reaction.
Comparing the ionic conductivities of the doped phases, we can note the tendency of its increase in the order of BaLa 0.9 Ca 0.1 InO 3.95 −BaLa 0.9 Sr 0.1 InO 3.95 −BaLa 0.9 Ba 0.1 InO 3.95 , i.e., in the order of increasing the ionic radius of dopants. The concentration of the oxygen vacancies was the same for the doped samples, so the difference in the conductivity of the BaLa 0.9 M 0.1 InO 3.95 might be attributed to their mobilities. In this respect, effect of the dopant nature on the conductivity should be considered.
The authors [13] have investigated NdBaInO 4 , doped with Ca 2+ , Sr 2+ , Ba 2+ . Their results show another trend in comparison with the data obtained in this work: σ ion of Ca 2+ > Sr 2+ > Ba 2+ . Their conductivities showed the tendency to increase with a decrease in the ionic radii of the M site ions, i.e., Ca 2+ is the most favorable dopant on Nd 3+ sites. The authors [13] indicate that the replacement of Nd 3+ by the cations with the most comparable size may minimize local structural relaxation and this main reason may explain the enhancement of the oxygen vacancy conductivity in the order of Ca 2+ > Sr 2+ > Ba 2+ . Taking into account the differences in the radii of La 3+ and Ca 2+ , Sr 2+ , and Ba 2+ , we could expect a similar trend in the change in conductivity of doped BaLaInO 4 . However, this is not the case. Clearly, other reasons should be considered.
There are not many reports in the literature on the relationships of O 2− -transport in phases with the RP-structure. However, for the ABO 3 perovskites, there is a lot of information on the influence of the nature of A-cations, B-cations, and dopants on the mobility of oxygen vacancies. In the general case, there are many factors that affect the mobility of oxygen vacancies. For phases with the same structure and with the same concentration of dopants, the main factors are generally identified.
(1) Geometric characteristics. It is well known that the size proportion of the A-cations and B-cations is an important factor for high ionic conductivity. The relationship of structure parameters and oxygen-ion transport properties had been studied by Wakamura [31]. The author plotted the activation energy (E a ) versus lattice volume (V) for numerous ion conductors, and found a simple inverse correlation between them, according to the expression E a = A v /V 2/3 , where A v is a constant. The relationship indicates that the E a value is decreased with a weakened long-range force due to the volume expansion. A similar tendency was observed for the ionic conductivity of mixed ionic-electronic conductors. For example, for Ln 0.5 M 0.5 FeO 3-δ (M = Sr 2+ , Ba 2+ ) [32], increasing the mismatch between La 3+ and M 2+ radii weakens the metal-oxygen bonding and increases the oxygen mobility.
Returning to the analysis of the experimental data, presented in this paper, we can make the assumption concerning the reason for the enhancement of the oxygen vacancy conductivity in the order of Ca 2+ -Sr 2+ -Ba 2+ for doped BaLaInO 4 . The observed increase in the lattice volume and the lattice parameters weakens the metal-oxygen bonding, and, as a consequence, increases the oxygen mobility. It should be noted that the activation energy for oxygen ion conduction in doped BaLaInO 4 decreased in the order of Ca 2+ (0.86 eV)-Sr 2+ (0.85 eV)-Ba 2+ (0.82 eV).
As can be seen, the results obtained for changes in oxygen-ion conductivity are consistent with the main trends described for perovskites. At the same time, it should be emphasized that the nature of the dopant has little effect on the oxygen ionic conductivity of doped BaLaInO 4 . The differences reached less than 0.3 order at low temperatures. This is due to the fact that the replacement of cations is carried out in the salt block and the change in geometrical parameters also occurs mainly in the salt block. The formation of oxygen vacancies and their migration occurs in the perovskite block. Therefore, the nature of the dopant introduced into the salt block does not significantly affect the oxygen ionic conductivity.
(2) Binding energies for dopant−oxygen vacancy pair clusters. It is well-known that interactions between dopant ions and their charge-compensating defects can lead to the formation of clusters, which can trap the migrating species. This implies that the oxide ion vacancies might be strongly bound to the dopant species, and the migration of the oxygen vacancy might depend on the binding energy of the dopant-oxygen vacancy, which, consequently, leads to lower oxide ion conductivities. As for the calculations for dopant-vacancy clusters in Ca 2+ -, Sr 2+ -, and Ba 2+ -doped NdBaInO 4 with RP-structure, it was shown [13] that the calculated binding energies are comparable to ca.-0.9 eV, which indicates that trapping for the migrating oxygen vacancies in NdBaInO 4 from the Ca 2+ , Sr 2+ , and Ba 2+ dopants could be comparable. If we assume that the same tendency is observed for the doped phase BaLaInO 4 , then it can also be said that the reason for the cluster formation does not explain the change in conductivity due to the nature of the dopant.
This result shows that the nature of the dopant, by occupying sites within the rock salt layers, does not have a very significant effect on the oxygen-ion conduction and that the key parameter governing the oxygen-ion conductivity of these materials is the concentration of oxygen vacancies. Likely, the variation in the concentration of oxygen vacancies of solid solutions, which will be studied in the future, will reveal new regularities of ionic transport in phases with the RP-structure.
The comparison of the conductivities of the investigated samples based on BaLaInO 4 with Nd-structural analogues BaNdInO 4 [13] showed the total and ionic conductivities were in good agreement and comparable for Sr 2+ and Ba 2+ doped phases at low temperatures, but Nd-structural analogues exhibited higher conductivities at higher temperatures [13]. Figure 5 shows a comparison of the temperature dependencies of conductivity for undoped phases BaLaInO 4 and BaNdInO 4 and Ba 2+ doped phases BaLa 0.9 Ba 0.1 InO 3.95 (or Ba 1.1 La 0.9 InO 3.95 ), Ba 1.1 Nd 0.9 InO 3.95 [13]. Figure 7 shows a comparison of the temperature dependencies of conductivity of investigated samples in Ar under dry and wet conditions. For wet Ar (pH 2 O = 2 × 10 −2 atm) ( Figure 7, curves with open signs), the conductivities of all samples were higher than those in dry Ar. Clearly, this behavior was a result of the insertion of water and the formation of proton charge carriers. The conductivity differences were more significant at lower temperatures as the hydration increased with decreasing temperature. We can suppose that the nature of dopant does not have significant effects on the type of dominant charge carrier, and increasing in the conductivity values in wet atmospheres is due to the appearance of proton carriers for all investigated samples.  The proton conductivity was calculated as the difference between the conductivity in wet and dry Ar, that is, σ H = σ (wet Ar) − σ (dry Ar), and the temperature dependencies are shown in Figure 8. The proton transport numbers were calculated according to the formula tH = σH/σ (wet air) and were plotted as a function of temperatures in Figure 9. It can be seen that the proton transport numbers increased with decreasing temperature and the investigated samples were nearly pure proton conductors below 450 °C. As can be seen from Figure 8, the proton conductivities of doped samples increased in the order Ca 2+ -Sr 2+ -Ba 2+ . We can assume that these differences were due to an increase in the concentration of protons in the same order. The activation energies decreased in the order of Ca 2+ (0.70 eV)-Sr 2+ (0.68 eV)-Ba 2+ (0.65 eV). These values are greater than the activation energy of proton transport in doped perovskites~0.5 eV [33]. As was discussed above in the analysis of TG data, during hydration, the main part of the protons was in the salt block. This situation is like hydroxides. It is well known that proton mobility is dependent on the strength of hydrogen bonds with the next-nearest oxygen atoms and energy barriers are high for proton transport in non-H-bonded systems [34,35]. It is clear that proton migration in the layer of salt block is a difficult in comparison with the proton migration in the bulk of perovskite block. Moreover, from a general point of view, four key steps for hydration can be distinguished [36]: these are (1) water adsorption on the oxide surface, (2) proton migration from the surface to the bulk of the oxide, (3) proton migration in the bulk, and (4) oxide ion vacancy migration in the bulk. The proton migration from the surface to the bulk is difficult. For investigated systems, the proton migration from the salt layer is assumed to be the same as the proton migration from the surface to the bulk of the perovskite structure. Taking into account these differences in the structures of perovskites and phases with the RP-structure, as well as differences in hydration mechanisms, it can be concluded that the proton transport in the investigated phases is realized with higher activation energies compared to the substituted ordinary perovskites.

Wet Conditions
The proton transport numbers were calculated according to the formula t H = σ H /σ (wet air) and were plotted as a function of temperatures in Figure 9. It can be seen that the proton transport numbers increased with decreasing temperature and the investigated samples were nearly pure proton conductors below 450 • C.
The results indicate that new phases BaLa 0.9 M 0.1 InO 3.95 (M = Ca 2+ , Sr 2+ , Ba 2+ ) might be a promising proton-conducting oxide in future applications. Further modification of the composition will improve the H + -conductivity. The results indicate that new phases BaLa0.9M0.1InO3.95 (M = Ca 2+ , Sr 2+ , Ba 2+ ) might be a promising proton-conducting oxide in future applications. Further modification of the composition will improve the H + -conductivity.

Conclusions
The new phases BaLa0.9M0.1InO3.95 (M = Ca 2+ , Sr 2+ , and Ba 2+ ) with the Ruddlesden-Popper structure were obtained. The analysis of the effect of nature of dopant (alkaline earth metals) on the hydration processes and on the transport properties of BaLaInO4 was carried out. It was established that all investigated samples were capable of water uptake from the gas phase. The ability of water incorporation was due to, not only the presence of oxygen vacancies, but also due to the presence in the structure of La-O blocks. The degree of hydration increased with a growth in the size of the dopant, i.e., with an increase in the size of the salt blocks, that contributed to the placement of a larger number of OH − -groups, which occupied interstitial sites within the rock salt layers.
It was proven that doping led to the increase of the oxygen ionic conductivity values. The conductivity values for doped samples BaLa0.9M0.1InO3.95 were higher than for undoped composition BaLaInO4 at a ~1.5 order of magnitude. The increase in the conductivity values was mainly attributed to the increase of the carrier concentration as a result of the formation of oxygen vacancies during doping. The oxygen ionic conductivity of doped samples increased in the order of BaLa0.9Ca0.1InO3.95-BaLa0.9Sr0.1InO3.95-BaLa0.9Ba0.1InO3.95, i.e., in the order of increasing the ionic radius of dopants. The increase in the lattice volume and the lattice parameters weakens the metal-oxygen bonding, and, as a consequence, increases the oxygen mobility. The activation energy for oxygen ion conduction decreased in the same order.
The conductivity increased in wet conditions as a result of the insertion of water and the formation of proton charge carriers. The proton conductivity was estimated by subtracting the conductivity data for dry Ar from the corresponding data in wet Ar. The proton conductivities of doped samples increased in the order Ca 2+ -Sr 2+ -Ba 2+ due to an increase in the concentration of protons. The activation energies for the proton conductivities were 0.70-0.68-0.65 eV, respectively.

Conclusions
The new phases BaLa 0.9 M 0.1 InO 3.95 (M = Ca 2+ , Sr 2+ , and Ba 2+ ) with the Ruddlesden-Popper structure were obtained. The analysis of the effect of nature of dopant (alkaline earth metals) on the hydration processes and on the transport properties of BaLaInO 4 was carried out. It was established that all investigated samples were capable of water uptake from the gas phase. The ability of water incorporation was due to, not only the presence of oxygen vacancies, but also due to the presence in the structure of La-O blocks. The degree of hydration increased with a growth in the size of the dopant, i.e., with an increase in the size of the salt blocks, that contributed to the placement of a larger number of OH − -groups, which occupied interstitial sites within the rock salt layers.
It was proven that doping led to the increase of the oxygen ionic conductivity values. The conductivity values for doped samples BaLa 0.9 M 0.1 InO 3.95 were higher than for undoped composition BaLaInO 4 at a~1.5 order of magnitude. The increase in the conductivity values was mainly attributed to the increase of the carrier concentration as a result of the formation of oxygen vacancies during doping. The oxygen ionic conductivity of doped samples increased in the order of BaLa 0.9 Ca 0.1 InO 3.95 -BaLa 0.9 Sr 0.1 InO 3.95 -BaLa 0.9 Ba 0.1 InO 3.95, i.e., in the order of increasing the ionic radius of dopants. The increase in the lattice volume and the lattice parameters weakens the metal-oxygen bonding, and, as a consequence, increases the oxygen mobility. The activation energy for oxygen ion conduction decreased in the same order.
The conductivity increased in wet conditions as a result of the insertion of water and the formation of proton charge carriers. The proton conductivity was estimated by subtracting the conductivity data for dry Ar from the corresponding data in wet Ar. The proton conductivities of doped samples increased in the order Ca 2+ -Sr 2+ -Ba 2+ due to an increase in the concentration of protons. The activation energies for the proton conductivities were 0.70-0.68-0.65 eV, respectively.