The magnetic structures of DyFe4Al8 and HoFe4Al8, which have been reported
to be unusual spin-glass systems, were studied in detail by neutron diffrac
tion, using both unpolarized and polarized beams. In fact these compounds h
ave long-range magnetic order in both the Fe and rare-earth sublattices. Th
e Fe sublattice orders at 175 K with the moments (1.0 mu B) in the ab plane
in a cycloid magnetic structure with a propagation vector along [110]. At
similar to 50 K the rare-earth moment starts to order in DyFe4Al8 and follo
ws the modulation of the Fe sublattice. The ordering of the holmium occurs
at a slightly higher temperature (similar to 80 K) than the dysprosium. At
a lower temperature higher-order harmonics of the modulation develop. The m
agnetic structure of the rare-earth at low temperature is a bunched ellipti
cal cycloid, following the modulation of the Fe sublattice. Although the an
tiferromagnetic coupling of the rare-earth magnetic moments has long-range
order, giving sharp magnetic satellites in the diffraction patterns, a non-
negligible fraction of the 4f moment does not contribute to these peaks but
appears as diffuse scattering beneath the Bra,og peaks. This indicates the
presence of short-range ferromagnetic correlations between neighboring rar
e-earth moments. The magnetic structure of the rare-earth sublattice is ver
y sensitive to a small applied magnetic field, mimicking spin-glass behavio
r in the bulk magnetic properties. The magnetic structure of DyFe4Al8 was s
tudied under an applied magnetic field. A field as low as 0.125 T severely
distorts the magnetic modulation and 0.75 T in the nb plane is sufficient t
o align all the rare-earth moments ferromagnetically. The cycloidal antifer
romagnetic coupling of the Fe moments remains unperturbed up to at least 5
T.