Mossbauer spectroscopy was used to study hyperfine interactions on Fe-57 nu
clei of SrCo1-yFeyO3-z solid solutions (0.2 less than or equal to y less th
an or equal to 0.8). The Fe-57 spectra measured in the paramagnetic tempera
ture range look like a superposition of two quadrupole doublets whose param
eters correspond to high-spin Fe4+ cations ((delta) = 0.1 mm/s; (Delta) = 0
.4 mm/s) in the anion surrounding with coordination number 5 (tetragonal py
ramid) and to Fe3+ cations ((delta) = 0.3 mm/s; (Delta) = 0.4 mm/s) in the
distorted octahedral environment. The relative number and pattern of distri
bution of heterovalent cations (Co4+, Co3+, Fe4+, and Fe3+) in the B-sublat
tice of perovskites were determined. The values of the electronic exchange
constants in the solid solutions obtained through Mossbauer spectroscopy we
re compared with those obtained from thermodynamic calculations. The oxygen
penetration in perovskites was found to depend on their composition and st
ructure.