Consider steady flow of a Newtonian fluid in incompressible flow with constant dynamic viscosity between parallel plates at and . The bottom plate is stationary and obeys the Navier slip boundary condition with slip length . The top plate moves at velocity and obeys the no-slip boundary condition. There is no streamwise pressure gradient or body force. The Couette flow solution is
Here is the constant shear stress magnitude. The lower wall's Navier slip boundary condition holds exactly because . At the top, is exactly the prescribed no-slip boundary condition; no finite upper-wall slip length is imposed in this example.
For a numerical example, stipulate , , and . The bottom velocity is and the shear stress is , compared with when both plates obey the no-slip boundary condition. The extrapolated profile reaches zero at .
Figure 1.
Couette profiles reveal slip length by extrapolation beneath the lower wall
. The bottom wall is stationary with slip length ; the upper wall at moves at velocity with a no-slip boundary condition. Solid lines show Couette flow for , and . Dashed continuations inside the shaded solid reach zero at . Increasing slip length reduces the shear rate required for the same upper-wall velocity. Details.
For fixed , and , recovers . As , throughout the gap and : the moving upper wall selects the limiting uniform velocity, while the lower wall approaches a stress-free boundary condition. The dynamic viscosity stays positive; the disappearing shear stress comes from the disappearing velocity gradient.
A short derivation uses unidirectional flow: the convective acceleration vanishes and the Navier-Stokes equation reduces to . Write . The bottom condition gives and the top condition gives .
Linearize about a relaxed state with constant mass density . In the unforced momentum conservation equation , the component of the pressure gradient is zero for a freely evolving unidirectional flow independent of . A prescribed external pressure gradient would add a forcing term.
For , incompressibility is automatic and the only nonzero entries of the rate-of-strain tensor are . Products of stress and velocity gradient are quadratic in the small amplitude. The constitutive equation consequently becomes to first order. With , its shear component and the component of momentum conservation are
The diagonal stress components have only homogeneous relaxation at this order and vanish if initially relaxed. In particular, does not enter this linear response.
For this steady unidirectional flow, the convective acceleration vanishes because depends only on . The axial Navier-Stokes equation reduces to , with . The no-slip boundary conditions therefore give
This is a superposition of Couette flow and pressure-driven Poiseuille flow.
For the unidirectional flow , incompressibility gives . Hence , and the convective acceleration vanishes. The transverse components of the Navier-Stokes equation give , while the axial component gives
A steady-flow assumption is implicit in the question. Neither unidirectional flow nor a time-independent pressure gradient alone eliminates : a decaying transient can be superposed on the final pipe profile. The native PDF does not explicitly say steady flow in this part. For the intended steady flow, , and therefore
Taking the pipe walls to be stationary, the no-slip boundary condition is
The no-penetration boundary condition is already satisfied by the assumed velocity field. This is the Poisson equation defining rectangular duct flow.
Rectangular duct flow 2026-10-25
Rectangular duct flow is steady flow of a Newtonian fluid down a straight rectangular pipe under a constant axial pressure gradient . For stationary walls and unidirectional flow, incompressibility eliminates axial dependence and the Navier-Stokes equation becomes a two-dimensional Poisson equation with zero Dirichlet boundary conditions. Subtracting a plane Poiseuille flow profile leaves a harmonic function that repairs the side-wall values using separation of variables. Uniqueness follows from Green's first identity: the difference of two solutions has zero boundary values and zero integral of the squared gradient, and hence vanishes.