Abstract

The quaternary ferrite Ba 12Fe 28Ti 15O 84 has monoclinic symmetry, space group C2 m , a = 9.988(7), b = 17.298(9), c = 19.17(2) Å, β = 99.33(6)°, Z = 2. The crystal structure was refined to R w = 0.048 for 2283 independent reflections collected on a Philips PW1100 diffractometer using Ag Kα radiation. The structure is based on a close packed array of Ba + O atoms with a 24-layer stacking sequence ( cchcccch) 3 along c∗ and with metal atoms occupying both octahedral and tetrahedral interstices. The iron and titanium atoms are substantially ordered into blocks of cubic stacked layers centered at z = 0 and 1 2 , respectively. The titanium rich segments have a structure closely related to cubic BaTiO 3 while the iron rich blocks have features in common with the spinel structure. The two blocks are joined via a transition layer containing both titanium- and iron-rich octahedra.

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