Original close-packed structure and magnetic properties of the Pb4Mn9O20 manganite

The crystal structure of the Pb4Mn9O20 compound (previously known as “Pb0.43MnO2.18”) was solved from powder X-ray diffraction, electron diffraction, and high resolution electron microscopy data (S.G. Pnma, a=13.8888(2) Å, b=11.2665(2) Å, c=9.9867(1) Å, RI=0.016, RP=0.047). The structure is based on a 6H (cch)2 close packing of pure oxygen “h”-type (O16) layers alternating with mixed “c”-type (Pb4O12) layers. The Mn atoms occupy octahedral interstices formed by the oxygen atoms of the close-packed layers. The MnO6 octahedra share edges within the layers, whereas the octahedra in neighboring layers are linked through corner sharing. The relationship with the closely related Pb3Mn7O15 structure is discussed. Magnetization measurements reveal a peculiar magnetic behavior with a phase transition at 52 K, a small net magnetization below the transition temperature, and a tendency towards spin freezing.

The crystal structure of Pb4Mn9O20 is based on a 6H (cch)2 close packing of “h”-type (O16) layers alternating with “c”-type (Pb4O12) layers. The Mn atoms occupy octahedral interstices. The MnO6 octahedra share edges within the layers and corners across the layers. Magnetization measurements reveal a tendency towards spin freezing.Figure optionsDownload as PowerPoint slide