In this work, recent studies of surface magnetism, as observed by x-ray sca
ttering techniques, are described. The experiments were concerned with uran
ium dioxide crystals for which x-ray resonance effects enhance the small ma
gnetic signal from the surface. The main result is that, in contrast to the
bulk which exhibits a discontinuous magnetic ordering transition, both the
(001) and (111) surface layers order continuously. This is reminiscent of
the general phenomenon of surface wetting, but had not been previously obse
rved for magnetic materials. Magnetic reflectivity studies show further tha
t the near-surface magnetic layers are more disordered than layers deep in
the bulk, even at low temperatures.