“…Preliminary refinement of the crystal structures from high-resolution X-ray diffraction (see Figure S10 and Table S2) showed that A 3 V 2 O 8 crystallizes with the palmierite structure (space group R 3̅ m ), which is composed by layers of isolated VO 4 tetrahedral units spaced by empty cationic vacancies. X-ray difference Fourier maps confirmed that V occupies only the 6 c Wyckoff site and that the vacancies are ordered (Figure S11), in contrast with what was seen in some hybrid hexagonal perovskite–palmierite Ba 3 M ′ M ″O 8.5 ( M ′ = Nb; M ″ = Mo, W) materials, where the cation vacancies are disordered. ,,, Previous neutron diffraction studies have shown that materials reported to have the palmierite structure can have more complex oxygen ordering, leading to the formation of hexagonal polytype structures with face- or corner-sharing octahedral units, e.g., Ba 3 Nb 2 O 8 . For this reason, neutron diffraction, which is more sensitive to the oxygen sublattice, was performed on the High-Resolution Powder Diffractometer (HRPD) at the ISIS Neutron and Muon Source at room temperature .…”