Addendum to: Communications Chemistry https://doi.org/10.1038/s42004-025-01843-1, published online 13 December 2025
After formal acceptance of our manuscript, we became aware of a previous study whose research topics and results partially overlap with our work1,2. The present Addendum is devoted to clarifying nomenclature confusion and numerical consistency of calculation results related to ε/κ-Ga2O3, and the connections between the findings presented in our publication and those reported by the authors of the referenced study.
Nomenclature and structural relationship between ε-Ga2O3 and κ-Ga2O3
The confusion around the ε and κ phases stems from the historical evolution of structural characterization and nomenclature in the Ga2O3 field, which we clarify based on widely accepted crystallographic studies.
Historical nomenclature and structural correction
Prior to 2017, ε-Ga2O3 was initially assigned to a hexagonal crystal system with the space group P63mc due to its pseudo-hexagonal diffraction characteristics in conventional XRD measurements3,4,5. However, theoretical studies consistently predicted that ε-Ga2O3 belongs to the orthorhombic crystal structure6. In 2017, Cora et al. resolved this ambiguity using high-resolution transmission electron microscopy (HRTEM), demonstrating that the so-called ε-Ga2O3 has an intrinsic orthorhombic crystal structure with the non-centrosymmetric space group Pna217. The exact same structure defined as κ-Ga2O3. The macroscopically observed hexagonal symmetry of ε-Ga2O3 thin films arises entirely from 120° in-plane rotational twinning of orthorhombic κ-Ga2O3 domains, rather than an intrinsic hexagonal lattice8. Therefore, the term κ-Ga2O3 in our work refers to orthorhombic κ-Ga2O3, as characterized by microstructural analysis.
Intrinsic structural unity
In both experimental and theoretical research, ε-Ga2O3 and κ-Ga2O3 are universally referred to as the ε/κ phase system, as they share an identical orthorhombic Pna21 crystal structure unit cell, with 4 crystallographically inequivalent Ga sites and 6 inequivalent O sites9. This is the only structurally stable lattice model for first-principles calculations of this polymorph, as multi-domain twinned ε-Ga2O3 cannot be accurately modeled via conventional periodic supercell calculations.
The only meaningful distinction between the two terms in the field lies in their microstructural morphology. ε-Ga2O3 typically refers to the experimentally common multi-domain, pseudo-hexagonal thin films, composed of three orthorhombic κ-Ga2O3 domains rotated by 120° relative to each other. In addition, κ-Ga2O3 specifically refers to the single-domain, intrinsic orthorhombic phase, which is the ideal lattice model for all first-principles calculations of this polymorph’s intrinsic physical and defect properties. In short, the ε and κ phases share the exact same intrinsic crystal structure at the unit cell, and the two nomenclatures describe the same polymorph from macroscopic morphological and microscopic crystallographic perspectives, respectively. Consequently, numerous researchers refer to orthorhombic Ga2O3 as either ε-Ga2O3 or κ-Ga2O310,11. This is the fundamental reason for the consistency in the physical trends of oxygen vacancy defects between the two studies1,2.
Connections of the close numerical values between the two works
The close numerical values of the charge transition levels (CTLs) and formation energies of oxygen vacancies between Ref. 1 on ε-Ga₂O₃ and our work in Ref. 2 on κ-Ga2O3 constitute a scientifically rational result. Since the two studies are based on the same Pna21 orthorhombic unit cell (the only stable lattice model for this polymorph), the formation energy and CTLs of oxygen vacancies, as intrinsic point defects, are fundamentally determined by the local atomic coordination, electronic structure, and bonding characteristics of the lattice. The high consistency in the overall trend and numerical range of defect properties between the two works is direct evidence of the reproducibility of the physical laws of oxygen vacancies in the ε/κ-Ga2O3 system, which is a core feature of credible first-principles research in condensed matter physics.
Our work is completely independent in calculation methodology. Ref. 1 employed the PBE0-TC-LRC hybrid functional with a 480-atom supercell for ε-Ga2O3 calculations. In contrast, our work used the HSE06 hybrid functional (the most widely used functional for Ga2O3 defect calculations in the field) and a 160-atom fully relaxed orthorhombic κ-Ga2O3 supercell. The differences in exchange-correlation functional selection, supercell size, and k-point sampling scheme determine that all numerical results in our work are independent calculation outputs. Although the trends in transition levels are in close concordance with the published results, minor numerical differences between the two works (e.g., the (+2/0) CTL of VO6 is 1.84 eV relative to the calculated CBM in the ref. 1 on ε-phase work, while we obtained 2.05 eV for the same site; the (+2/0) CTL of VO1 is 0.95 eV relative to the calculated CBM in the ref. 1 on work vs. 1.01 eV in ours) further verify the independence of our calculations by different functional. In summary, the close numerical values between the two works are a testament to the universality of the physical laws of oxygen vacancies in the ε/κ-Ga2O3 system, while our work provides independent calculation results and novel physical mechanism insights for this polymorph.
We acknowledge the contributions of Kaewmeechai et al. to the study of oxygen vacancies in Ga2O3 polymorphs; their systematic investigation of α-, β-, and ε-Ga2O3 provides a valuable reference for understanding the universal characteristics of VO in Ga2O3 materials, and our work complements the research gap in κ-Ga2O3, enriching the academic community’s understanding of defect behaviors in metastable Ga2O3 phases1,2.
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Feng, W., Fang, P., Zhang, Y. et al. Addendum: The role of oxygen vacancies in the electronic and optical properties of κ-Ga2O3. Commun Chem 9, 182 (2026). https://doi.org/10.1038/s42004-026-02045-z
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DOI: https://doi.org/10.1038/s42004-026-02045-z