Samples of pure (Ca 2 FeAlO 5 ) and lightly doped (Ca 2 Fe 0.95 Al 0.95 Mg 0.05 Si 0.05 O 5 ) brownmillerite have been synthesized. Synchrotron X-ray and neutron diffraction data have been collected so that the structures can be re®ned using, simultaneously, both diffraction data sets and known compositional information; this overcomes the problem of under-determinacy resulting from multioccupation of the tetrahedrally and octahedrally coordinated sites in the structure. For the pure form, a 2.7:1 iron/aluminium preference for octahedral/ tetrahedral (respectively) occupation is obtained. This trend is re¯ected also in the doped brownmillerite, though, because of the low level of Mg doping, the occupancy of Mg is only resolved through the additional use of Mg EXAFS (extended X-ray absorption ®ne structure) data, which shows that Mg displays a distinct octahedral site preference rather than a disordered occupation between the octahedral/tetrahedral sites. The consequences of Mg doping are then examined using time-resolved multi-angle energy-dispersive powder X-ray diffraction studies of the mineral undergoing hydration; this shows that the pure form is more active than the doped form.