The structure of, and transitions between, liquids, crystals and glass
es have commonly been studied with the hard-sphere model(1-5), in whic
h the atoms are modelled as spheres that interact only through an infi
nite repulsion on contact. Suspensions of uniform colloidal polymer pa
rticles are good approximations to hard spheres(6-11), and so provide
an experimental model system for investigating hard-sphere phases. The
y display a crystallization transition driven by entropy alone. Becaus
e the particles are much larger than atoms, and the crystals are weakl
y bound, gravity plays a significant role in the formation and structu
re of these colloidal crystals. Here we report the results of microgra
vity experiments performed on the Space Shuttle Columbia to elucidate
the effects of gravity on colloidal crystallization. Whereas in normal
gravity colloidal crystals grown just above the volume fraction at me
lting show a mixture of random stacking of hexagonally close-packed pl
anes (r.h.c.p.) and face-centred cubic (f.c.c.) packing if allowed tim
e to settle(7,8), those in microgravity exhibit the r.h.c.p. structure
alone, suggesting that the f.c.c. component may be induced by gravity
-induced stresses. We also see dendritic growth instabilities that are
not evident in normal gravity, presumably because they are disrupted
by shear-induced stresses as the crystals settle under gravity. Finall
y, glassy samples at high volume fraction which fail to crystallize af
ter more than a year on Earth crystallize fully in less than two weeks
in microgravity. Clearly gravity masks or alters some of the intrinsi
c aspects of colloidal crystallization.