Open Access Article
Fang Zhang†
a,
Yuchen Cui†b,
Jingxin Gaob,
Hao Zhangb,
Yi Bianb,
Chen Liuc,
Nuofu Chen*a and
Jikun Chen
*b
aSchool of Renewable Energy, North China Electric Power University, Beijing 102206, China. E-mail: nfchen@ncepu.edu.cn
bSchool of Materials Science and Engineering, University of Science and Technology Beijing, Beijing 100083, China. E-mail: jikunchen@ustb.edu.cn
cBeijing Synchrotron Radiation Facility, Institute of High Energy Physics, Chinese Academy of Sciences, Beijing 100049, China
First published on 27th March 2026
Although an intriguing metal-insulator transition (MIT) stemming from spin-state transition was discovered for cobaltite double-perovskites (REBaCo2O5+δ), its regulatory mechanism is yet unclear owing to the intertwined dual-determinants from cationic and anionic perspectives. Herein, we demonstrate that the occurrence of abrupt MIT for REBaCo2O5+δ relies on the synergistic coordination between the RE ionic-radius-induced CoO6 octahedral distortion and the oxygen-vacancy-modulated Co valence-state for low structural symmetry. A gradual shift in the transportation behavior from metal to insulator is observed for REBaCo2O5+δ synthesized in air with REs from Pr to Ho, while the MIT emerges for middle REs (e.g., Sm, Eu, Gd and Tb). Nevertheless, the MIT was could be further extended to more RE compositions from an anionic perspective by annealing the insulating (RE: Dy and Ho) or metallic (RE: Pr and Nd) REBaCo2O5+δ at MPa-high oxygen or nitrogen pressure, respectively. Further estimation the oxygen composition via their thermopowers indicates that their MIT behaviors were coincide with a narrow distribution of δ around 0.5 and descendent structural symmetry towards Pmmm from P4/mmm. This unveils the distinctiveness in spin-state transition-driven MIT compared to the Bloch–Wilson, Mott, or Peierls transitions, providing a versatile platform for fundamental explorations beyond conventional correlated electron systems.
To gain a better fundamental understanding of the determinant of the orbital configuration of REBaCo2O5+δ, it is urgent to decouple the respective influence from the perspectives associated with the cation (e.g., rare-earth compositions) and anion (e.g., oxygen vacancy). Although decreasing rRE was known to distort the CoO6 octahedra more to reduce the orbital overlapping between O-2p and Co-3d, it meanwhile exacerbated the formation of oxygen vacancies within REBaCo2O5+δ that reduces the valence of Co. This is attributed to the intermediate valence state of Co within REBaCo2O5+δ that is susceptible to both structural distortions and reaction atmospheres. Consequently, such entangled regulations from both the band gap regulation and orbital filling control impedes further comprehending the relationship among the charge, spin, orbital, and lattice underlying the MIT behavior of REBaCo2O5+δ. To address this core issue, further systematic studies of the electronic structure and transportation properties of the as-synthesized REBaCo2O5+δ sample at various oxygen partial pressures (pO2) are needed.
In this work, we disentangle the role of RE ionic radius-induced CoO6 octahedral distortion and oxygen vacancy-modulated Co valence state in the MIT behavior of REBaCo2O5+δ by their first synthesis in air followed by post-annealing in various atmospheres, covering a large variety of RE compositions. The resulting variations in electronic transportation properties (e.g., resistivity and thermopower) were systematically investigated, and further related to the ones observed in crystal and electronic structures. We highlight the synergistic coordination between the RE ionic radius and the oxygen composition, resulting in the emergence of abrupt MIT for REBaCo2O5+δ, unveiling the distinctiveness in spin-state transition-driven MIT, compared to the Bloch–Wilson, Mott, or Peierls transitions.
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| Fig. 1 (a) Illustration of the crystal structure of REBaCo2O5+δ (RE represents rare-earth elements) containing light (Pr and Nd), middle (Sm, Eu, Gd and Tb) and heavy (Dy and Ho) rare-earth elements, where RE, Ba and Co atoms are represented by purple, green, and dark blue, respectively. From left to right, there are schematic diagrams of the structures of RELBaCo2O5+δ (REL = Pr and Nd), REMBaCo2O5+δ (REM = Sm, Eu, Gd and Tb), and REHBaCo2O5+δ (REH = Dy and Ho). (b) X-ray diffraction (XRD) patterns of REBaCo2O5+δ synthesized via a solid-state reaction in air. (c) Lattice parameters of the as-synthesized REBaCo2O5+δ sample (solid symbols) plotted as a function of the ionic radius of rare-earth elements compared to the previous reports (hollow symbols).11,14 The RELBaCo2O5+δ and REHBaCo2O5+δ samples were refined using the P4/mmm space group, while the REMBaCo2O5+δ sample was refined using the Pmmm space group. | ||
Fig. 1(c) shows the lattice parameters of REBaCo2O5+δ from the Rietveld refinement as a function of rRE, where the solid symbols represent our experimental data and the hollow symbols represent the data from references.11,14 Notably, the refinement of RELBaCo2O5+δ and REHBaCo2O5+δ was performed using the P4/mmm space group, while that of REMBaCo2O5+δ was performed using the Pmmm space group. It more clearly demonstrates the diversity in 2a and b for REBaCo2O5+δ containing middle rare-earth elements, giving rise to a descended symmetry in the structure. We also tried to perform refinement for REBaCo2O5+δ containing the heavy or light rare-earth elements using the Pmmm space group (see more details in Table S1 and Fig. S2), the operation of which results in similar magnitudes in 2a and b. Our results are in consistency with the previous reports by T. V. Aksenova et al.,11 T. Dasgupta et al.,16 and I. O. Troyanchuk et al.13
The temperature dependence of resistivity was further measured for the as-synthesized REBaCo2O5+δ, as shown in Fig. 2(a). It can be seen that the light rare-earth element-containing samples (REL = Pr and Nd) exhibit metallic behavior, while the heavy rare-earth element-containing samples (REH = Dy and Ho) show semiconducting behavior. More intriguingly, abrupt MITs are observed for the middle rare-earth element-containing REMBaCo2O5+δ (REM = Sm, Eu, Gd, and Tb), which coincides with a low symmetry in their ground-state crystal structures (e.g., Pmmm compared to P4/mmm), in agreement with the previous observations.
The variations in carrier types and concentrations of the air-synthesized REBaCo2O5+δ with various rare-earth compositions were also indicated by their different temperature dependence of S, as shown in Fig. 2(b). At low temperatures (e.g., 100 K), the absolute magnitude |S| shows an increasing tendency along the lanthanide sequence with reduced rRE until Tb. However, when the ionic radius continues to decrease, the S of DyBaCo2O5+δ begins to decrease. It is interesting to note that HoBaCo2O5+δ manifests a negative magnitude in S indicating the electron as a major carrier, which differs from the rest REBaCo2O5+δ. With an elevation in temperature, a reducing tendency is generally observed for the |S| of all REBaCo2O5+δ, and this is in agreement with their negative temperature dependence in resistivity. Abrupt transitions are observed in |S|–T for REMBaCo2O5+δ in the range of 330–360 K, and this is in consistency with their MIT behaviors. In contrast, a gradual reduction in |S| is observed for DyBaCo2O5+δ and HoBaCo2O5+δ with the heavier rare-earth composition showing insulating transportation behavior, while PrBaCo2O5+δ shows a small magnitude in |S| with low-temperature dependences owing to the metallic transportation behavior.
The above observation is in consistency with the previous reports, and was attributed to the variation in oxygen stoichiometry across rare-earth substitutions. According to references,16,17 this is likely due to its oxygen content δ being closest to, and slightly greater than, 0.5. In fact, the δ value of TbBaCo2O5+δ synthesized in this experiment is approximately 0.53.18 In contrast, the δ value of other REBaCo2O5+δ compounds (RE ≠ Tb) deviates more significantly from 0.5, with δ in PrBaCo2O5+δ around 0.7,14 in SmBaCo2O5+δ around 0.61 (ref. 19) and in DyBaCo2O5+δ around 0.3.14
The electronic structure of the as-synthesized REBaCo2O5+δ sample with various rare-earth compositions (RE = Sm, Tb, and Ho) was further probed by the near-edge X-ray absorption fine structure (NEXAFS), and their Co L-edge spectrum is shown in Fig. 2(c). Compared with the Co L3-edge spectra of Co2+, Co3+, and Co4+ in reference,20 Co is predominantly in the +3 oxidation state across all four samples, with no noticeable presence of Co2+ or Co4+. This suggests that, despite varying δ in the REBaCo2O5+δ samples synthesized in air, the structural and unit cell differences stabilize Co near the +3 oxidation state. Furthermore, the A peak position for all samples is consistent at ∼780.4 eV, confirming that the oxidation state of Co remains largely unchanged (higher oxidation states shift the A peak to higher energies). The ref. 19 indicates that SmBaCo2O5+δ, with a δ value of approximately 0.61 after sintering in air at 1100 °C, has an average Co oxidation state of 3.11, suggesting the presence of Co4+. For HoBaCo2O5+δ, δ is typically around 0.3,14 resulting in an average Co oxidation state of 2.8, which indicates the presence of Co2+.
In contrast to REBaCo2O5+δ (RE = Tb and Ho), SmBaCo2O5+δ shows a distinct small peak at the left edge of the A peak, corresponding to high-spin Co3+ (HS Co3+) as identified in ref. 21–23, while other samples predominantly exhibit intermediate-spin (IS Co3+) or low-spin Co3+ (LS Co3+). This is consistent with SmBaCo2O5+δ exhibiting metallic-like resistivity (5.5 × 10−5 Ω m) at room temperature, while the other REBaCo2O5+δ samples show higher resistivity characteristic of semiconductors. Additionally, HoBaCo2O5+δ displays a small peak at the right shoulder of the A peak, corresponding to LS Co3+, consistent with its semiconducting behavior at room temperature.
Fig. 3(a) shows the powder XRD pattern of REBaCo2O5+δ (RE = Gd, Tb, Dy, and Ho) after oxygen annealing, the process of which results in the broadening of diffraction peaks (see Fig. S3) without introducing secondary phases. The variation in the magnitudes of their lattice parameters was further determined by the Rietveld refinement (see more details in Table S3 and Fig. S4), as plotted as a function of rRE in Fig. 3(b). It clearly demonstrates a symmetry descending in the structure of heavy rare-earth element-containing REBaCo2O5+δ (RE: Dy and Ho) from the tetragonal (P4/mmm) to the orthorhombic (Pmmm) structure, owing to post-annealing at MPa-high oxygen pressures. It is also interesting to note that pronounced MIT behaviors manifest in both DyBaCo2O5+δ and HoBaCo2O5+δ upon post-annealing at high-oxygen pressures, as shown in Fig. 3(c) and S7(a). This feature corresponds to a decrease in the symmetry of REBaCo2O5+δ (RE: Dy and Ho). After oxygen annealing, the phase transition of GdBaCo2O5+δ disappears, which is associated with the increase in δ of GdBaCo2O5+δ after annealing, leading to a deviation of the Co oxidation state from +3.
Fig. 3(d) shows the temperature dependence of S of REBaCo2O5+δ (RE = Gd, Tb, Dy, and Ho) with middle and heavy rare-earth compositions after annealing at MPa-high oxygen pressure to compensate their oxygen composition. It can be seen that the oxygen annealing converted the previously negative magnitude in S for HoBaCo2O5+δ towards positive magnitudes. Compared to their air-synthesized counterparts, the magnitude of |S| of all REBaCo2O5+δ decreases at 100 K, indicating that after oxygen doping, the δ value deviates from 0.5 (as reported in the literature,17 where it is known that the absolute value of |S| increases as δ approaches 0.5). Meanwhile, the temperature dependence of S becomes more gradual and abrupt transitions are observed in DyBaCo2O5+δ and HoBaCo2O5+δ, as shown in Fig. S7(b). With an elevation in temperature, a reducing tendency is generally observed for the S of all REBaCo2O5+δ, and this is in agreement with their negative temperature dependence in resistivity.
Fig. 4(a) shows the powder XRD pattern of REBaCo2O5+δ (RE = Pr, Nd, Sm, and Eu) after nitrogen annealing, the process of which results in the broadening of diffraction peaks (see Fig. S5) without introducing secondary phases. The variation in the magnitudes of their lattice parameters was further determined by the Rietveld refinement, as plotted as a function of rRE in Fig. 4(b).
The top image of Fig. 4(b) shows the crystal structure of RELBaCo2O5+δ. On the left is the structural diagram of RELBaCo2O5+δ synthesized in air, and on the right is the structural diagram of RELBaCo2O5+δ after nitrogen annealing. After nitrogen annealing, RELBaCo2O5+δ transitions from the original tetragonal structure to a lower-symmetry orthorhombic structure (similar to the oxygen-annealed REHBaCo2O5+δ). At the same time, the δ value decreases (opposite to the trend observed in oxygen-annealed REHBaCo2O5+δ).
Fig. 4(b) demonstrates the lattice parameters obtained from the Rietveld refinement of REBaCo2O5+δ (RE = Pr, Nd, Sm, and Eu) after nitrogen annealing (see more details in Table S4 and Fig. S6). A comparison with the oxygen-annealed and as-sintered samples shows that after annealing, for REL (Pr and Nd), the b is significantly larger than 2a. This causes the original P4/mmm space group, obtained by sintering in air, to transition to the lower-symmetry Pmmm space group, likely due to oxygen vacancies inducing distortions in the crystal structure. For RE = Sm and Eu, after annealing, the a-axis slightly decreases, while the b-axis slightly increases, leading to a further reduction in structural symmetry. The c-axis remains relatively unchanged before and after annealing for all REBaCo2O5+δ compounds.
Fig. 4(c) shows the temperature-dependent resistance (ρ–T) relationship of REBaCo2O5+δ (RE = Pr, Nd, Sm, and Eu) after nitrogen annealing. Compared to the samples before annealing, PrBaCo2O5+δ and NdBaCo2O5+δ exhibit a distinct MIT, as shown in Fig. S6. This is related to the decrease in symmetry of the REBaCo2O5+δ structure after nitrogen annealing. The TMIT value for PrBaCo2O5+δ is around 290 K, while for NdBaCo2O5+δ, it is approximately 305 K. After nitrogen annealing, the phase transition of SmBaCo2O5+δ and EuBaCo2O5+δ becomes sharper, and the temperature of TMIT for the former increases, as shown in Fig. S8. Fig. S9 presents the ρ–T relationship of REMBaCo2O5+δ (RE = Sm, Eu, Gd, and Tb). Taking TbBaCo2O5+δ as an example, a comparison of this material under different annealing conditions reveals that the phase transition is sharpest for the air-sintered sample. After oxygen annealing, the sharpness of the phase transition decreases, and the post-transition resistance is lower. After nitrogen annealing, the MIT disappears, and the material exhibits insulating behavior throughout the temperature range. Overall, oxygen annealing drives REBaCo2O5+δ towards metallic behavior, while nitrogen annealing promotes its transition to insulating behavior.
Fig. 4(d) demonstrates the temperature dependence of S for REBaCo2O5+δ with light and middle rare-earth elements (RE = Pr, Nd, Sm, and Eu) after nitrogen annealing to reduce their oxygen composition. It can be seen that nitrogen annealing converts the magnitude of S from positive to negative for EuBaCo2O5+δ, indicating the transition in its major carrier type from the hole to the electron. Compared to their air-synthesized counterparts, the magnitude of |S| of all REBaCo2O5+δ increases at 100 K and the temperature dependence of S becomes more sharp, suggesting that after nitrogen annealing, the δ value approaches 0.5,17,24,25 as shown in Fig. S7(b).
ρ)/d(T) − T, and more details are shown in Fig. S10. It can be seen that the TMIT value generally falls within a narrow range of 290–370 K. This differs from 113-type rare-earth nickelates,1 cobaltite RECoO3,2 and A-site ordered oxygen-deficient perovskite REBaFe2O5,35 under which conditions the TMIT value can be regulated within wider temperature ranges via the rRE value. As shown in Fig. 5(a), the TMIT value shows a maximum for REBaCo2O5+δ synthesized in air with RE = Gd, similar to the previous reports.27 For REBaCo2O5+δ with lighter rare-earth compositions (e.g., Sm and Eu), their MITs are more abrupt with the elevated TMIT value upon nitrogen annealing. Similar effects were observed for REBaCo2O5+δ with heavier rare-earth compositions (e.g., Dy and Ho), which indicated that MIT behaviors manifest, but upon annealing at MPa-high oxygen pressures.
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| Fig. 5 (a) Metal-insulator transition temperature (TMIT) of the as-prepared REBaCo2O5+δ sample, of which the solid symbol indicates air-synthesized, the crosses in the box indicate oxygen-annealed and the hollow symbol indicates nitrogen-annealed. (b) Seebeck coefficient of REBaCo2O5+δ at 200 K, of which the solid symbol indicates air-synthesized, the crosses in the box indicate oxygen-annealed and the hollow symbol indicates nitrogen-annealed. (c) Correlation between the oxygen content and the Seebeck coefficient reported in the literature.17,26 (d) Relationship between the oxygen content and the ionic radius of rare-earth elements, where the oxygen content in this work is calculated based on panel (c) and the points from the literature are also marked in the figure.17,24,27–34 | ||
Fig. 5(b) summarizes the S of REBaCo2O5+δ with various RE (e.g., Pr, Nd, Sm, Eu, Gd, Tb, Dy, and Ho) at 100 K. In general, the absolute magnitudes of S are small for air-sintered REBaCo2O5+δ with light and middle rare-earth elements (e.g., Pr–Gd), while much larger ones were observed for REBaCo2O5+δ, e.g., positive S for RE = Tb and Dy, and negative S for RE = Ho. Moreover, the absolute magnitude in the S for EuBaCo2O5+δ was enlarged significantly upon nitrogen anneals (see more details in Fig. S11 and S12). According to the previous reports,17 the magnitude of S can well reflect the oxygen composition (δ) for REBaCo2O5+δ, and the tendency is summarized in Fig. 5(c) for δ–S. Based on the previously reported δ–S tendency, we further estimate the magnitude of δ for the present REBaCo2O5+δ samples. In Fig. 5(d), we further plotted the δ–rRE relationship for REBaCo2O5+δ in this work and also those reported previously. The solid symbols represent those showing abrupt MIT behavior, while those with the absence of MIT are indicated by the hollow symbols. It clearly demonstrates that the occurrence of MIT in REBaCo2O5+δ is more related to an oxygen stoichiometry approaching 5.5 (δ = 0.5), regardless of the rare-earth composition.
Summarizing all the above-mentioned results highlights two prerequisites for the emergence of MIT behavior in REBaCo2O5+δ, from the perspectives of both crystal structure and valence. On the one hand, the ground state of REBaCo2O5+δ exhibits low crystal symmetry (e.g., adopting the Pmmm space group instead of P4/mmm), with its lattice constants changing significantly at TMIT,36,37 which indicates strong spin–orbital–lattice coupling. On the other hand, the oxygen composition should be proper to maintain Co3+ valence states, which is necessary to sustain the high-/low-spin-state transitions for REBaCo2O5+δ (see more details in Fig. S13). The necessity to satisfy both prerequisites limits the tunability of the MIT behavior of the double perovskite system REBaCo2O5+δ in contrast to the 113-type perovskite cobaltite.
Supplementary information (SI) is available. See DOI: https://doi.org/10.1039/d6ra00137h.
Footnote |
| † F. Zhang and Y. Cui contribute equally. |
| This journal is © The Royal Society of Chemistry 2026 |