Published online by Cambridge University Press: 23 May 2018
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 $\unicode[STIX]{x1D707}(I)$-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
$\sqrt{\unicode[STIX]{x1D708}t}$, where
$\unicode[STIX]{x1D708}$ is the kinematic viscosity. For a dense granular viscoplastic 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
$\sqrt{\unicode[STIX]{x1D708}_{g}t}$ analogous to a Newtonian fluid where
$\unicode[STIX]{x1D708}_{g}$ is an equivalent granular kinematic viscosity depending not only on the intrinsic properties of the granular medium, such as grain diameter
$d$, density
$\unicode[STIX]{x1D70C}$ and friction coefficients, but also on the applied pressure
$p_{w}$ at the moving wall and the solid fraction
$\unicode[STIX]{x1D719}$ (constant). In addition, the
$\unicode[STIX]{x1D707}(I)$-rheology indicates that this growth continues until reaching the steady-state boundary layer thickness
$\unicode[STIX]{x1D6FF}_{s}=\unicode[STIX]{x1D6FD}_{w}(p_{w}/\unicode[STIX]{x1D719}\unicode[STIX]{x1D70C}g)$, independent of the grain size, at approximately a finite time proportional to
$\unicode[STIX]{x1D6FD}_{w}^{2}(p_{w}/\unicode[STIX]{x1D70C}gd)^{3/2}\sqrt{d/g}$, where
$g$ is the acceleration due to gravity and
$\unicode[STIX]{x1D6FD}_{w}=(\unicode[STIX]{x1D70F}_{w}-\unicode[STIX]{x1D70F}_{s})/\unicode[STIX]{x1D70F}_{s}$ is the relative surplus of the steady-state wall shear stress
$\unicode[STIX]{x1D70F}_{w}$ over the critical wall shear stress
$\unicode[STIX]{x1D70F}_{s}$ (yield stress) that is needed to bring the granular medium into motion. For the case of Stokes’ first problem when the wall shear stress
$\unicode[STIX]{x1D70F}_{w}$ is imposed externally, the
$\unicode[STIX]{x1D707}(I)$-rheology suggests that the wall velocity simply grows as
$\sqrt{t}$ before saturating to a constant value whereby the internal resistance of the granular medium balances out the applied stresses. In contrast, for the case with an externally imposed wall speed
$u_{w}$, the dense granular medium near the wall initially maintains a shear stress very close to
$\unicode[STIX]{x1D70F}_{d}$ which is the maximum internal resistance via grain–grain contact friction within the context of the
$\unicode[STIX]{x1D707}(I)$-rheology. Then the wall shear stress
$\unicode[STIX]{x1D70F}_{w}$ decreases as
$1/\sqrt{t}$ until ultimately saturating to a constant value so that it gives precisely the same steady-state solution as for the imposed shear-stress case. Thereby, the steady-state wall velocity, wall shear stress and the applied wall pressure are related as
$u_{w}\sim (g\unicode[STIX]{x1D6FF}_{s}^{2}/\unicode[STIX]{x1D708}_{g})f(\unicode[STIX]{x1D6FD}_{w})$ where
$f(\unicode[STIX]{x1D6FD}_{w})$ is either
$O(1)$ if
$\unicode[STIX]{x1D70F}_{w}\sim \unicode[STIX]{x1D70F}_{s}$ or logarithmically large as
$\unicode[STIX]{x1D70F}_{w}$ approaches
$\unicode[STIX]{x1D70F}_{d}$.