The structural and magnetic phase transitions of Fe-I boracite have be
en studied by means of optical examinations of the domain structure an
d by measurements of the spontaneous birefringence using polarized-lig
ht microscopy. These phase transitions have also been characterized by
dielectric and spontaneous polarization studies, realized on ferroela
stic/ferroelectric single-domain states, which were obtained by electr
ic field poling along (100)(cub) and (111)(cub) directions, with simul
taneous visual control of the domain state. In the trigonal 3m1' phase
, an electric field E parallel to(111)(cub) of one polarity produced a
monodomain with the spontaneous polarization P-s and the optical axis
perpendicular to the (111)(cub) plane, while that of the reversed pol
arity gave rise to domains with the three other preferential direction
s of P-s, non-collinear with E, and to a polarization of P-s/3, indica
ting the non-180 degrees-reversibility of P-s along (111)(cub). The ma
gnetic phase transition 3m1' reversible arrow m resulted in anomalies
both in the dielectric permittivity (up to 2 MHz) and in the spontaneo
us polarization at the Curie temperature T-C = 31 K. This suggests an
interaction between the magnetic moment and the electric polarization,
consistent with the ferroelectric/ferroelastic/ferromagnetic coupling
effect previously found for the m phase.