Tom Matsunagaa,
Naoki Tarutani
a,
Kiyofumi Katagiri
*a,
Kei Inumaru
a,
Takuya Sakatab,
Zi Lang Gooc,
Kunihisa Sugimotoc and
Sayako Inoué
d
aGraduate School of Advanced Science and Engineering, Hiroshima University, 1-4-1 Kagamiyama, Higashi-Hiroshima 739-8527, Japan. E-mail: kktgr@hiroshima-u.ac.jp
bWestern Region Industrial Research Center, Hiroshima Prefectural Technology Research Institute, 2-10-1 Aga-Minami, Kure 737-0004, Japan
cDepartment of Chemistry, Faculty of Science and Engineering, Kindai University, 3-4-1 Kowakae, Higashi-Osaka 577-8502, Japan
dGeodynamics Research Center, Ehime University, Matsuyama 790-8577, Japan
First published on 12th August 2025
The synthesis of perovskite-type oxynitride solid solutions has gained significant attention because of their potential applications in advanced materials. This study presents a novel synthetic strategy for obtaining these solid solutions by integrating multiple elements at both the A and B sites within a single crystalline phase. Utilizing liquid-phase processes—specifically sol–gel and polymerizable complex methods—amorphous metal oxide precursors that enhance the nitridation efficiency during ammonolysis are successfully created. The incorporation of alkaline earth metals and lanthanides result in stable, single-phase perovskite structures, such as Ca0.2Sr0.2Ba0.2La0.2Pr0.2Ta(O,N)3, despite substantial differences in the ionic radii of the cations. Effective charge compensation through optimal ratios of O2− and N3− ions is achieved, enabling greater compositional flexibility. The exploration of B-site multi-element perovskite oxynitrides reveals that amorphous precursors facilitate the formation of solid solutions, as exemplified by SrTi1/3Nb1/3Ta1/3(O,N)3, whereas crystalline precursors lead to phase separation. Remarkably, the incorporation of up to eight metal elements in complex compositions such as Ca0.2Sr0.2Ba0.2La0.2Pr0.2Ti1/3Nb1/3Ta1/3(O,N)3 and Ca1/3Sr1/3Ba1/3Ti0.2Zr0.2Hf0.2Nb0.2Ta0.2(O,N)3 is demonstrated. These findings underscore the importance of precursor preparation methods in achieving the desired structural properties and pave the way for the further exploration of perovskite oxynitrides with diverse elemental combinations, thereby enhancing their functionality in various applications.
In recent years, the field of alloys has seen growing interest in high-entropy alloys (HEAs), which represent a contemporary trend in materials science.15–17 HEAs are distinguished by the intentional incorporation of five or more metal elements in nearly equimolar ratios, resulting in exceptional mechanical properties and resistance to wear and corrosion. Notably, the CrMnFeCoNi alloy, commonly referred to as the Cantor alloy, has been extensively studied for its outstanding low-temperature ductility, reaching approximately 71% at room temperature.18,19 Kitagawa et al. developed HEA nanoparticles containing a homogeneous atomic-level mixture of all six platinum-group elements, demonstrating exceptional catalytic activity in ethanol oxidation, surpassing conventional metal catalysts in both activity and durability.20
Furthermore, the concept of high entropy has recently expanded into ceramics, leading to significant research into high-entropy oxides (HEOs).21–23 The first entropy-stabilized HEO, (Co,Cu,Mg,Ni,Zn)O, was synthesized in 2015 and exhibited a stable rock salt structure, underscoring the potential of these materials.24 Although HEOs have emerged only in the past decade, reported examples display a plethora of intriguing functional properties, including colossal dielectric constants,25 low thermal conductivity,26 and high ionic conductivity.27 Known crystalline types of HEOs include spinel,28,29 fluorite,30 bixbyite,31 and perovskite structures.32,33 In 2018, Jiang et al. first reported the formation of HEOs with perovskite structures, considering 13 different compositions with Ba and Sr as A-site metal elements, and a combination of five elements from the Ce, Gd, Hf, Mn, Sn, Y, and Zr groups as B-site metal elements.32 In this case, because alkaline earth metals that act as divalent (+2) cations are chosen as A-site metals, the average positive charge of the B-site cations must be +4 to satisfy charge compensation in the ABO3-type structure, unless there are vacancies in the oxide anion sites. Consequently, in perovskite-type HEOs, achieving a crystal devoid of anion vacancies necessitates fixing the anion charge at −6, thereby limiting the flexibility in selecting A- and B-site elements.
To enhance the degrees of freedom in cation selection, it is essential to adjust the anionic charge within the ABO3-type perovskite structure. Herein, we focus on the concept of mixed-anion compounds.34,35 Most conventional ceramics consist of metallic elements in diverse combinations, yet the anions are typically restricted to a single type, mainly oxide anions (O2−). However, by combining oxide ions with nitride ions (N3−), which possess a different charge of −3, the compositional flexibility can be significantly improved. For example, the formation of a solid solution of LaTaON2 and SrTiO3, both possessing a perovskite-type structure, allows the total anion charge to vary between −6 and −8, enabling various combinations of Sr2+ and La3+ at the A-site, along with Ti4+ and Ta5+ at the B-site.36 This flexibility facilitates precise tuning of the bandgap, thereby enhancing performance as a photocatalyst for water splitting, as previously reported.37,38 Additional examples include the fabrication of LaTaON2 and CaTaO2N solid solutions as environmentally benign inorganic pigments, which are recognized as perovskite-type metal oxynitride solid solutions.39 However, previous studies have primarily described solid solutions with a maximum of three elements at the A site of perovskite-type oxynitrides (AB(O,N)3),40 and there are few examples of AB(O,N)3-type solid solutions containing four or more elements at a single cation site (A or B site), or five or more elements when considering both A and B sites.
Therefore, this study aimed to establish a synthetic strategy for obtaining perovskite-type oxynitride solid solutions by mixing multiple elements into a single crystalline phase. The formation of stable solid solutions necessitates the uniform dispersion of multiple elements, which is particularly challenging in the synthesis of metal oxynitrides owing to the inherent differences in the nitridation behavior of various metals. We consider the homogeneous mixing of metal elements in the precursor to be essential for successful synthesis. Therefore, we employed liquid-phase processes, such as the sol–gel and polymerizable complex (PC) methods,41 to synthesize precursors for the successful preparation of AB(O,N)3-type solid solutions incorporating four or more cations at either the A or B site, or more than eight cations across both sites.
Thermogravimetric and differential thermal analyses (TG-DTA) were conducted using a TG-DTA2000S instrument (Mac Science, Co., Ltd, Tokyo, Japan). Data was collected exclusively during the heating phase, with the samples heated at a linear rate of 5 °C min−1 under a synthetic air flow composed of 80% N2 and 20% O2.
The prepared samples were observed using transmission electron microscopy (TEM; JEM-2010, JEOL, Tokyo, Japan) and scanning TEM (STEM; JEM-2100F, JEOL, Tokyo, Japan) equipped with energy-dispersive X-ray spectroscopy (EDX), operated at 200 kV using carbon film-coated 300-mesh Cu grids.
Ultraviolet–visible (UV-vis) diffuse reflectance spectra (DRS) were obtained using a UV-vis spectrophotometer (V-670; JASCO, Tokyo, Japan). The absorption spectra were processed using the Kubelka–Munk function, F(R∞) = (1 − R∞)2/(2R∞), where R∞ is the absolute diffuse reflectance.42 The band gap energies (Eg) of the samples were calculated by extrapolating the processed absorption edge.
The metal–element ratios were determined using an energy-dispersive X-ray fluorescence (XRF) spectrometer (EDX-7200, SHIMADZU, Kyoto, Japan) and a wavelength-dispersive XRF spectrometer (ZSX Primus IV, Rigaku, Tokyo, Japan).
The chromatic properties of the synthesized samples were evaluated using a chromometer (CR-400, Konica Minolta, Inc., Tokyo, Japan) in accordance with the Commission Internationale de l’Éclairage 1976 colorimetric method. In this method, L*a*b* values quantitatively represent color as points in a three-dimensional space. The L* value denotes lightness, ranging from 0 (black) to 100 (white), while the a* and b* values indicate color directions: +a* (red), −a* (green), +b* (yellow), and −b* (blue).43 Color saturation, C, was calculated using the equation C = [(a*)2 + (b*)2]1/2. The hue angle, h°, was determined using equation the equation h° = tan−1(b*/a*).
A-site multi-element perovskite oxynitrides (ATa(O,N)3; A: Ca, Sr, Ba, La, and Pr) were prepared via ammonolysis using PC-derived precursors. Fig. 1 shows the XRD patterns and Kubelka–Munk-transformed UV-vis DRS of the ATa(O,N)3 samples obtained after nitridation of the precursors for systems employing alkaline earth metals (Ca, Sr, and Ba) as the A site. Binary mixtures of these elements were prepared in a 1:
1 molar ratio, and a ternary mixture containing all three elements was prepared in equimolar proportions. In addition, for the ternary mixture, a sample was prepared using a solid powder mixture as the precursor for comparison, instead of the PC-derived precursor (denoted as “solid mixture” in Fig. 1a).
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Fig. 1 (a) XRD patterns and (b) Kubelka–Munk-transformed UV-vis DRS of ATaO2N (A = Ca/Sr, Sr/Ba, Ca/Ba, and Ca/Sr/Ba) prepared using PC-derived precursors; data for ATaO2N (A = Ca/Sr/Ba) prepared using a solid powder mixture of ACO3 was also shown for comparison. Enlargements of the main reflections at approximately 31° are displayed on the right of panel (a); dashed lines indicate the peak positions of CaTaO2N, SrTaO2N, and BaTaO2N.46 |
For the two-element mixtures, combinations of A = Ca/Sr and Sr/Ba successfully formed single-phase perovskite structures, specifically Ca0.5Sr0.5TaO2N and Sr0.5Ba0.5TaO2N (Fig. 1a). The steep absorption edge observed in the UV-vis DRS further supports the formation of solid solutions (Fig. 1b). The colors of these samples are ochre and vermilion, respectively, which are consistent with those synthesized by Kim et al. using the flux method.40 Conversely, the A = Ca/Ba mixture resulted in two distinct phases, as indicated by the diffraction peaks in the XRD pattern and two absorption edges in the UV-vis DRS. This suggests that a single-phase perovskite Ca0.5Ba0.5TaO2N was not formed; instead, phase separation occurred, producing a mixture of CaTaO2N and BaTaO2N. The significant difference in ionic radii49 between Ca2+ (1.34 Å) and Ba2+ (1.61 Å) likely contributes to this phase separation.
A sample with A = Ca/Sr/Ba, incorporating all three elements, indicated the formation of a single-phase perovskite structure, Ca1/3Sr1/3Ba1/3TaO2N, as confirmed by XRD patterns and UV-vis DRS. This result is particularly noteworthy given the pronounced difference in the ionic radii and observed phase separation between Ca and Ba when only these two elements are mixed. The lattice volumes of the samples exhibiting a single-phase perovskite structure, along with those of each end member, were calculated. When plotted against the average ionic radii of the A-site cations, a linear relationship was observed (Fig. S2). These results indicate that solid solutions with a single-phase perovskite structure can be formed using mixtures of alkaline earth metal cations as the A-site cations in ATaO2N. However, to effectively combine Ca2+ and Ba2+—which have significantly different ionic radii—it is necessary to include Sr2+, which has an intermediate ionic radius, to achieve a solid solution.
To clarify the importance of using precursors synthesized via the PC method, Ca1/3Sr1/3Ba1/3TaO2N was also prepared using a mixture of ACO3 (where A = Ca/Sr/Ba) as the precursor. The resulting XRD pattern showed broader and more asymmetrical peaks compared with that of the PC-derived precursor, whereas the absorption edge in the UV-vis DRS exhibited a more gradual transition. These findings suggest that the sample did not form a single-phase perovskite but instead exhibited phase separation. Kim et al. reported the preparation of Ca1/3Sr1/3Ba1/3TaO2N using a mixture of solid powders as the precursor, which required the addition of KCl flux.40 In their case, the diffusion of metal ions facilitated by the flux was crucial; however, we successfully achieved mixing of the three cations without the use of flux. This demonstrates the effectiveness of preparing the precursor via a liquid-phase process, which enables uniform mixing of metal ions.
Subsequently, four-(A = Ca/Sr/Ba/La) and five-cation mixtures (A = Ca/Sr/Ba/La/Pr) were prepared by introducing alkali metals and lanthanides into the A site of ATa(O,N)3. Fig. 2 represents the XRD patterns and Kubelka–Munk-transformed UV-vis DRS of the samples obtained through the nitridation of the PC-derived precursors. Despite the presence of cations with different valences—divalent Ca2+, Sr2+, and Ba2+, and trivalent La3+ and Pr3+—all samples exhibited diffraction peaks corresponding to a single perovskite phase in the XRD patterns and displayed sharp absorption edge features in the UV-vis DRS (Fig. 2a and b, respectively). These results indicate that Ca0.25Sr0.25Ba0.25La0.25Ta(O,N)3 and Ca0.2Sr0.2Ba0.2La0.2Pr0.2Ta(O,N)3 were successfully synthesized. In perovskite tantalum oxynitride ATa(O,N)3, effective charge compensation can be achieved by incorporating O2− and N3− in an appropriate ratio, even when the average positive charge of the A-site cations varies between +2 and +3. This characteristic allows for greater flexibility in elemental combinations compared with multi-element perovskite metal oxides, ABO3, where the total anion charge is fixed at −6 (O2− × 3).
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Fig. 2 (a) XRD patterns and (b) Kubelka–Munk-transformed UV-vis DRS of ATaO2N (A = Ca/Sr/Ba/La and Ca/Sr/Ba/La/Pr) prepared using the PC-derived precursors. |
A detailed structural analysis was performed on Ca0.2Sr0.2Ba0.2La0.2Pr0.2Ta(O,N)3. The results of the TEM and STEM observations for Ca0.2Sr0.2Ba0.2La0.2Pr0.2Ta(O,N)3 are shown in Fig. 3. The high-resolution (HR) TEM image and fast Fourier transform (FFT) analysis revealed lattice spacings of 0.14, 0.16, 0.28, and 0.39 nm, corresponding to the (224), (312), (112), and (110) planes of the tetragonal perovskite structure, respectively. Elemental mapping was conducted to confirm the successful synthesis of an atomically mixed solid solution. The elemental composition was determined by STEM-EDX and XRF (Table S1). While some discrepancies in the measured values may be present owing to overlapping signals from different elements, the absence of volatile elements supports the conclusion that the molar ratios of the metal cations closely matched the intended composition. To confirm that Ca0.2Sr0.2Ba0.2La0.2Pr0.2Ta(O,N)3 possesses a single crystalline phase rather than a mixture of multiple crystalline phases, high-resolution synchrotron XRD analysis was conducted. Rietveld refinement was performed using the formula Ca0.2Sr0.2Ba0.2La0.2Pr0.2TaO1.6N1.4 based on the elemental analysis (Fig. S3). Note that the ratio of O/N = 1.4/1.6 is not derived from actual measurements but is instead assumed based on the total charge of the cations. The resulting lattice and structural parameters are summarized in Tables S2 and S3. Among the possible space group candidates I2m, I4/mcm, Fmcm, and Pm3m, I4/mcm, which has the lowest R-factor, is presumed to be the most suitable space group.
Next, B-site multi-element perovskite oxynitrides (SrB(O,N)3; B: Ti, Zr, Hf, Nb, and Ta) were prepared. Amorphous mixed metal oxides synthesized by a general sol–gel method using metal alkoxides for the B-site metal combinations were generally employed as precursors. For the five-element combination (B = Ti, Zr, Hf, Nb, and Ta), a precursor was prepared via the PC method by incorporating Sr at the A site. Fig. 4 illustrates the XRD patterns and Kubelka–Munk-transformed UV-vis DRS of SrB(O,N)3 samples featuring combinations of two B-site metals (B = Nb/Ta, Ti/Nb, and Ti/Ta) and a three-metal combination (B = Ti/Nb/Ta). For comparison, data for a sample prepared using precursors containing crystalline TiO2, Nb2O5, and Ta2O5 mixed in the solid phase are also presented. In the case of B = Nb/Ta, a solid solution phase, SrNb0.5Ta0.5O2N, was successfully formed; however, for B = Ti/Nb and Ti/Ta, phase-separated perovskites were obtained, as indicated by the XRD patterns. Upon calculating the lattice constants for the main phase of the sample with B = Ti/Nb from the XRD patterns, the values of a = 5.6530(5) Å and c = 8.025(8) Å were obtained. These values lie between those of SrNbO2N (a = 5.665 Å, c = 8.179 Å) and SrTiO3 (a = 5.534 Å, c = 7.826 Å),47 indicating that a solid solution of Sr(Ti,Nb)(O,N)3 is partially formed. Conversely, the position of the main peak for the impurity phase at 31.2° is relatively close to the main peak of SrNbO2N at 31.3°,48 suggesting phase separation involving SrNbO2N. Similarly, for the sample with B = Ti/Ta, a partial solid solution of Sr(Ti,Ta)(O,N)3 is present; however, achieving a complete solid solution at a 1:
1 composition proved to be impossible. This finding is consistent with our previous report on SrTaO2N–SrTiO3 solid solutions, where a Ti/Ta ratio of 0.15 was identified as the upper limit.45 The ionic radii of six-coordinated Nb5+ and Ta5+ are both 0.64 Å,49 suggesting no significant difference and thus no barrier to solid-solution formation. Conversely, the ionic radius of six-coordinated Ti4+ is 0.605 Å, which is considerably smaller than those of Nb5+ and Ta5+, which likely contributes to the observed phase separation. In contrast, a solid-solution phase, SrTi1/3Nb1/3Ta1/3(O,N)3, was effectively obtained using the three-element combination B = Ti/Nb/Ta. This improvement was attributed to the decrease in the Ti4+ ratio—from 1/2 to 1/3—since Ti4+ has a different ionic radius from Nb5+ and Ta5+. No sample exhibiting a single-phase perovskite structure was obtained when a mixture of crystalline metal oxide powders was used as the precursor. This result parallels the observations for multi-element A-site compositions, even when multiple metal elements occupy the B site, successful solid-solution formation relies on preparing amorphous precursors that uniformly incorporate multiple elements at the atomic scale via a liquid-phase process.
The XRD patterns and UV-vis DRS results for samples containing four (B = Ti/Zr/Nb/Ta) and five (B = Ti/Zr/Hf/Nb/Ta) B-site metals are represented in Fig. 5. The XRD patterns indicate that all samples exhibited diffraction peaks characteristic of single-phase perovskite structures, confirming the formation of SrTi0.25Zr0.25Nb0.25Ta0.25(O,N)3 and SrTi0.2Zr0.2Hf0.2Nb0.2Ta0.2(O,N)3 (Fig. 5a). In contrast, examination of the absorption edge via UV-vis DRS indicated that the sample prepared using a precursor with B-site metals mixed by the sol–gel method displayed a gradual absorption edge (Fig. 5b). The pronounced absorption on the longer-wavelength side suggests the presence of reducible metal ions due to the strong reducing effect of high-temperature NH3 gas, implying incorporation of reduced species within the sample. For example, similar absorption in the longer-wavelength region was observed in the UV-vis DRS of LaTiO2N, SrNbO2N, and BaTaO2N synthesized by ammonolysis, which were attributed to reduced species of Ti, Nb, and Ta (such as Ti3+, Nb4+, Ta4+) as determined by X-ray photoelectron spectroscopy, etc.50–53 It is reasonable to assume that Ti4+, Nb5+, and Ta5+ are also reduced in the samples studied here. Notably, the sample synthesized using the PC-derived precursor comprising five B-site metal elements (B = Ti/Zr/Hf/Nb/Ta) and one A-site metal element (Sr) demonstrated sharper diffraction peaks in the XRD pattern and steeper absorption edges in the UV-vis DRS compared with the sample derived from the sol–gel precursor, despite identical target compositions. This disparity can be attributed to potential heterogeneities in the sol–gel-derived precursors, which are likely due to variations in the hydrolysis and condensation reaction rates of the alkoxides of the five metals during preparation. Furthermore, it is important to note that the sol–gel-derived precursor contained only B-site metals mixed in advance, whereas the PC method-derived precursor incorporated the A-site metal Sr.
Fig. 6 and 7 present TEM and STEM images of SrTi0.2Zr0.2Hf0.2Nb0.2Ta0.2(O,N)3 synthesized using sol–gel- and PC-derived precursors, respectively. The HRTEM images, along with the FFT analyses, reveal lattice spacings of 0.14, 0.16, 0.18, 0.20, 0.28, and 0.39 nm, corresponding to the (224), (312), (222), (220), (112), and (110) planes of the tetragonal perovskite structure, respectively. The elemental mappings shown in Fig. 6d and 7d indicate that the eight constituent elements are homogeneously distributed at the atomic level, with no detectable compositional irregularities. No significant differences were observed between the samples prepared using the two precursor methods. The elemental composition was determined using STEM-EDX and XRF techniques (Tables S4 and S5). As with previous results, no significant differences were observed in the compositions of the samples regardless of the precursor preparation method or elemental analysis technique used. This confirms that the molar ratios of the metal cations effectively retain the intended composition even when the B site consists of multiple elements, similar to the case with multi-element A-site systems. Although the XRD and UV-vis DRS results suggest that the PC-derived precursor may lead to superior properties, SrTi0.2Zr0.2Hf0.2Nb0.2Ta0.2(O,N)3 synthesized using the sol–gel-derived precursor also demonstrates sufficient uniformity.
Fig. 8 presents photographs of the ATa(O,N)3 and SrB(O,N)3 samples, which were successfully synthesized as single-phase, multi-element, mixed perovskite-type oxynitrides. The Commission Internationale de l’Éclairage L*a*b*Ch° color coordinates are summarized in Tables S6 and S7, along with the bandgap energies (Eg) estimated from the UV-vis DRS. The color of ATa(O,N)3 transitions from yellow to orange and eventually to brown, with hue angles (h°) ranging from 40° to 80°. In systems containing three or more elements, the hue angles were within the range of 55° to 60°. Conversely, the color of SrB(O,N)3 shifted towards green as the elements were mixed, resulting in an elevated hue angle. Notably, SrTi0.2Zr0.2Hf0.2Nb0.2Ta0.2(O,N)3 exhibited a hue angle of approximately 100°, the highest among the synthesized samples. The UV-vis DRS of the sample with green color shows an increased background absorption in the longer-wavelength region, as seen in Fig. 5b, suggesting a reduction of B site cations, i.e., Nb5+ to Nb4+ and Ti4+ to Ti3+. The mixed of absorption from these reduced species with band gap absorption resulting in the green color has also been reported in previous syntheses of LaTiO2N.50 Furthermore, the Eg values exhibited relatively minor variations compared with the pronounced color changes, remaining in the range of approximately 2.0 to 2.3 eV. These findings suggest that the strategic combination of multiple elements at both the A and B sites can significant alter the color of perovskite-type oxynitrides. This characteristic highlights their potential application not only as visible light-responsive photocatalysts but also as inorganic pigments for coloring purposes.
Finally, perovskite oxynitrides incorporating multiple elements at both the A and B sites were synthesized. The precursors used were amorphous metal oxides containing all relevant metal elements, prepared via the PC method. Fig. 9 shows the XRD patterns of three AB(O,N)3 samples: “A = Ca/Sr/Ba/La/Pr; B = Ti/Nb/Ta”, “A = Ca/Sr/Ba; B = Ti/Zr/Hf/Nb/Ta”, and “A = Ca/Sr/Ba/La/Pr; B = Ti/Zr/Hf/Nb/Ta”. In the sample containing a mixture of ten elements—specifically, “A = Ca/Sr/Ba/La/Pr; B = Ti/Zr/Hf/Nb/Ta”—peaks not attributable to the perovskite structure were observed and identified as by-products. These peaks correspond closely to the diffraction pattern of A2B2O7 (A = La and/or Pr; B = Zr and/or Hf), characterized by a pyrochlore structure,54–56 indicating the formation of pyrochlore-type oxides as mixed phases or solid solutions. It has been reported that synthesizing LaZrO2N, which contains La at the A site and Zr at the B site, is more challenging than producing other AB(O,N)3-type oxynitrides. The formation of LaZrO2N competes with the generation of pyrochlore-type oxides, necessitating prolonged ammonolysis treatment.57 Consequently, the simultaneous inclusion of La and/or Pr at the A site and Zr and/or Hf at the B site may facilitate the production of oxides other than oxynitrides. To address this, samples were synthesized by combining eight metal elements, excluding La and Pr from the A-site elements and Zr and Hf from the B-site elements—specifically, “A = Ca/Sr/Ba/La/Pr; B = Ti/Nb/Ta” and “A = Ca/Sr/Ba; B = Ti/Zr/Hf/Nb/Ta”. In these cases, the diffraction peaks corresponding to the perovskite-type structure manifested as a single phase, confirming the successful formation of solid solutions containing these elements: Ca0.2Sr0.2Ba0.2La0.2Pr0.2Ti1/3Nb1/3Ta1/3(O,N)3 and Ca1/3Sr1/3Ba1/3Ti0.2Zr0.2Hf0.2Nb0.2Ta0.2(O,N)3. The results of the quantitative analysis of all 10 elements, including cations and anions, for these two types of perovskite-type oxynitrides containing these eight metal elements are summarized in Table 1, using wavelength-dispersive XRF. In addition to the measured wt%, considering that the general formula for perovskite oxynitrides is AB(O,N)3, the molar ratios are presented in parentheses, ensuring that the total for the cation at the A site and the cation at the B site is 1 each, while the total for the anion sites O and N is 3. For Ca0.2Sr0.2Ba0.2La0.2Pr0.2Ti1/3Nb1/3Ta1/3(O,N)3, it can be seen that the five elements at the A site are ca. 20% each, according to the intended ratio, while the three elements at the B site are ca. 33% each. Based on these measured values, the total charge at the cation and anion sites in the formula AB(O,N)3 is about +7.1 and −7.1, respectively, indicating that charge balance is maintained. Similarly, for Ca1/3Sr1/3Ba1/3Ti0.2Zr0.2Hf0.2Nb0.2Ta0.2(O,N)3, it can be seen that the three elements at the A site are ca. 33% each, while the five elements at the B site are ca. 20% each. Based on these measured values, the total charge at the cation and anion sites in the formula AB(O,N)3 is about +6.4 and −6.4, respectively, also indicating that charge balance is maintained. These results demonstrate that even when multiple cations with different valences are mixed at the A and B sites, the ratio of O to N at the anion site can be freely adjusted to maintain the charge balance between cations and anions in the perovskite structure. To the best of our knowledge, no perovskite-type oxynitrides containing these eight metal elements within a single-crystal structure have been synthesized to date, representing the largest combination of elements achieved in a multi-element mixed perovskite-type oxynitride. The key to this achievement was the synthesis of amorphous metal oxides, in which metal elements were uniformly mixed via a liquid-phase method and subsequently used as precursors.
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Fig. 9 XRD patterns of AB(O,N)3 (“A = Ca/Sr/Ba/La/Pr; B = Ti/Nb/Ta”, “A = Ca/Sr/Ba; B = Ti/Zr/Hf/Nb/Ta”, and “A = Ca/Sr/Ba/La/Pr; B = Ti/Zr/Hf/Nb/Ta”) prepared using PC-derived precursors. |
Ca | Sr | Ba | La | Pr | Ti | Zr | Hf | Nb | Ta | O | N | |
---|---|---|---|---|---|---|---|---|---|---|---|---|
The values in the upper row indicates wt%, and the values in parentheses in the lower row indicate the molar ratios of the A site, B site, and anion site, each of which sums to 1, 1, and 3, respectively. | ||||||||||||
Ca0.2Sr0.2Ba0.2La0.2Pr0.2Ti1/3Nb1/3Ta1/3(O,N)3 | 2.56 (0.19) | 5.86 (0.20) | 8.79 (0.19) | 8.32 (0.18) | 11.0 (0.23) | 5.53 (0.34) | — (—) | — (—) | 11.2 (0.35) | 19.6 (0.31) | 17.8 (1.87) | 9.47 (1.13) |
Ca1/3Sr1/3Ba1/3Ti0.2Zr0.2Hf0.2Nb0.2Ta0.2(O,N)3 | 4.64 (0.33) | 10.7 (0.34) | 16.1 (0.33) | — (—) | — (—) | 3.54 (0.21) | 5.75 (0.18) | 12.3 (0.19) | 7.23 (0.22) | 13.2 (0.20) | 23.4 (2.61) | 3.10 (0.39) |
Supplementary information is available: TG-DTA curves and XRD patterns of the precursors, comparison of the average of A-site ion radius and the lattice volume of the sample, elemental compositions, Rietveld-refined XRD pattern, lattice parameters, structure parameters, CIE color coordinates and bandgap energies. See DOI: https://doi.org/10.1039/d5dt01464f.
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