Résumé
Metal-ordered rock-salt oxides (e.g., AMO2, A2MO3, A3MO4) exhibit diverse functionalities arising from cation ordering, yet their structural evolution is difficult to predict due to the lack of systematic design principles. For A2MO3 compounds, although two-dimensional (2D) honeycomb structures have been widely explored, the three-dimensional (3D) hyperhoneycomb phase is still rare, despite its appeal as a battery cathode and as a Kitaev spin-liquid candidate. Here, we report pressure-induced phase transitions of Li2SnO3, from the ambient-pressure honeycomb phase to a hyperhoneycomb phase at 3 GPa, and subsequently to a Li2PbO3-type phase at 8 GPa. By integrating analyses of octahedral connectivity and Madelung energy, together with machine-learning-assisted molecular dynamics simulations, we established the thermodynamic landscape governing these transitions. Specifically, the hyperhoneycomb structure becomes competitive with the honeycomb structure under pressure and is stabilized by elevated temperatures, whereas the Li2PbO3-type structure stabilizes only at high pressures. This framework rationalizes the entire sequence of observed pressure-induced phase transitions. Furthermore, the hyperhoneycomb phase is accessible across the entire solid solution of Li2(Sn1–xRux)O3, although Ru-rich compositions require higher pressure. Remarkably, the phase-pure hyperhoneycomb x = 0.75 exhibits complete electrochemical lithium deintercalation. Given the prevalence of 2D oxides under ambient conditions, designing hyperhoneycomb phases via pressure highlights a hidden yet attractive chemical space of 3D polymorphs, offering new chemical landscapes and exotic functionalities.