This paper reviews a profound Mossbauer study on the magnetic properties of
goethites with varying crystallinity and Al-content. It has been found tha
t both the cluster-ordering and the superferromagnetic models reproduce the
temperature dependencies of the average hyperfine fields quite well. Howev
er, the magnetic transition temperatures predicted by the cluster-ordering
model are in better agreement with those measured from thermoscan experimen
ts. On the other hand, it has been found that the hyperfine field of maximu
m probability at low temperatures follows the spin-wave law for antiferroma
gnets. Linear relationships between the saturation hyperfine fields, the in
ter-sublattice exchange interactions, and the Neel temperatures to the Al-c
ontent and crystallinity could be derived. On the other hand, applied-field
Mossbauer spectroscopy seems to suggest that the anisotropy field can diff
erentiate between poor crystallinity and Al-content, and that a certain deg
ree of ferrimagnetism occurs at higher Al-contents.