  When a granular bed is sheared by a fluid that flows above a critical limit,
it undergoes a complex motion that varies along time: it can contain fluid-
(bedload) and solid-like (creep) regions, being prone to strain hardening and,
in case of polydispersity, segregation. In this paper, we investigate
experimentally the short- and long-time evolution of a bidisperse bed sheared
by a viscous liquid. Different from previous experiments, the density ratio
between grains and fluid is 2.7, close to values found in rivers and oceans. We
show the existence of diffusive, advective and constrained regions, that most
of segregation occurs during the very first stages of the flow, and that bed
hardening becomes stronger while bedload and creep weaken along time. We obtain
the segregation rates, their evolution along time, their variation with the
applied shearing, and the time evolution of creeping and bedload. Finally, we
propose characteristic times for the segregation of large particles and bed
hardening. Our results shed light on the complex motion of sheared beds
existing in nature, such as river beds and creeping lands.
