The magnetic properties of double perovskite oxide Sr2FeWO6 have been repor
ted. The magnetic susceptibility and Mossbauer effect of Fe-57 show that th
is compound is an antiferromagnet with T-N = 37 K. The Mossbauer parameters
below similar to 20 K are the center shift of + 1.2 mm/s relative to metal
lic iron, the quadrupole splitting of 1.9 mm/s and the hyperfine field of s
imilar to 110 kOe. The quadrupole splitting has a strong temperature depend
ence. From these data, we conclude that Fe in Sr2FeWO6 is in the Fe2+ high-
spin state, while the hyperfine held seems to be quite small. (C) 2000 Else
vier Science B.V. All rights reserved.