  The classical Stokes' problem describing the fluid motion due to a steadily
moving infinite wall is revisited in the context of dense granular flows of
mono-dispersed beads using the recently proposed $\mu(I)$--rheology. In
Newtonian fluids, molecular diffusion brings about a self-similar velocity
profile and the boundary layer in which the fluid motion takes place increases
indefinitely with time $t$ as $\sqrt{\nu t}$, where $\nu$ is the kinematic
viscosity. For a dense granular visco-plastic liquid, it is shown that the
local shear stress, when properly rescaled, exhibits self-similar behaviour at
short-time scales and it then rapidly evolves towards a steady-state solution.
The resulting shear layer increases in thickness as $\sqrt{\nu_g t}$ analogous
to a Newtonian fluid where $\nu_g$ is an equivalent granular kinematic
viscosity depending not only on the intrinsic properties of the granular media
such as grain diameter $d$, density $\rho$ and friction coefficients but also
on the applied pressure $p_w$ at the moving wall and the solid fraction $\phi$
(constant). In addition, the $\mu(I)$--rheology indicates that this growth
continues until reaching the steady-state boundary layer thickness $\delta_s =
\beta_w (p_w/\phi \rho g )$, independent of the grain size, at about a finite
time proportional to $\beta_w^2 (p_w/\rho g d)^{3/2} \sqrt{d/g}$, where $g$ is
the acceleration due to gravity and $\beta_w = (\tau_w - \tau_s)/\tau_s$ is the
relative surplus of the steady-state wall shear-stress $\tau_w$ over the
critical wall shear stress $\tau_s$ (yield stress) that is needed to bring the
granular media into motion... (see article for a complete abstract).
