Features of the magnetic and charge ordering of the Fe3O2BO3 ludwigite have
been studied using Mossbauer spectroscopy in the range of 4 K < T < 120 K.
From the temperature dependence of the magnetic hyperfine fields (B-hf), a
ssociated to four different iron sites, three magnetic transitions, at 112,
73 and 40 K, can be distinguished in agreement with previous magnetization
measurements. In the temperature region where a weak ferromagnetism appear
s, the B-hf of some Fe sites show two different values related with differe
nt canting angles. (C) 2001 Elsevier Science B.V. All rights reserved.