A polycrystalline sample of nominal composition SrMn0.7Fe0.3O3-delta w
as prepared by standard ceramic techniques and investigated at room te
mperature by iodometry, Fe-57 Mossbauer spectroscopy and neutron powde
r diffraction. The former two techniques established;delta = 0.11 +/-
0.01. Neutron diffraction showed that the sample was biphasic. The maj
or component [98.3 (5)% by mass] was a 10H perovskite [space group P6(
3)/mmc; a = 5.45035(5), c = 22.3735(2) Angstrom], with the Sr-O layers
adopting a cccchcccch stacking sequence. A full structural refinement
showed the composition to be SrMn0.72Fe0.28O2.87. The minor phase was
a pseudo-cubic perovskite. The Mossbauer data suggest that the oxygen
vacancies in the major phase are predominantly found in the coordinat
ion shell of Fe3+ cations. The sample did not show long-range magnetic
order at room temperature.