Math 2.0

Fluid mechanics Incompressible viscous flow Example

Stokes' first and second problems

Builds on Navier–Stokes equationsNo-slip conditionBoundary layer

Example

Let a viscous fluid of kinematic viscosity ν>0\nu > 0 fill the half-space y>0y > 0 above a flat plate y=0y = 0. Look for flows u=(w(y,t),0,0)u = (w(y, t), 0, 0) with constant pressure. Such a field is divergence-free, and (u⋅∇)u=w ∂xu=0(u \cdot \nabla) u = w \, \partial_x u = 0. So the Navier–Stokes equations reduce to the heat equation ∂tw=ν ∂y2w\partial_t w = \nu \, \partial_y^2 w.

  1. First problem (impulsively started plate): the fluid is at rest for t<0t < 0, and for t>0t > 0 the plate moves with constant speed UU. The solution is w(y,t)=Uerfc⁡(y2νt),w(y, t) = U \operatorname{erfc}\Big( \frac{y}{2 \sqrt{\nu t}} \Big), where erfc⁡(s)=2π∫s∞e−σ2dσ\operatorname{erfc}(s) = \frac{2}{\sqrt{\pi}} \int_s^\infty e^{-\sigma^2} d\sigma.
  2. Second problem (oscillating plate): the plate moves with velocity Ucos⁡(ωt)U \cos(\omega t), with ω>0\omega > 0. The time-periodic solution that stays bounded as y→∞y \to \infty is w(y,t)=Ue−kycos⁡(ωt−ky),k=ω2ν.w(y, t) = U e^{-k y} \cos(\omega t - k y), \qquad k = \sqrt{\frac{\omega}{2 \nu}}.

Check of 2: ww is the real part of W=Ueiωt−(1+i)kyW = U e^{i \omega t - (1 + i) k y}. Then ∂tW=iωW\partial_t W = i \omega W and ν ∂y2W=ν(1+i)2k2W=2iνk2W=iωW\nu \, \partial_y^2 W = \nu (1 + i)^2 k^2 W = 2 i \nu k^2 W = i \omega W. At y=0y = 0, w=Ucos⁡(ωt)w = U \cos(\omega t), so the no-slip condition holds. Check of 1: erfc⁡(y/(2νt))\operatorname{erfc}(y / (2 \sqrt{\nu t})) is the standard similarity solution of the heat equation. It equals 11 at y=0y = 0 and tends to 00 as y→∞y \to \infty or t→0+t \to 0^+.

Remarks

In the first problem the plate's motion spreads into the fluid over a distance of order νt\sqrt{\nu t}. In the second problem the motion is confined to a layer of thickness of order 2ν/ω\sqrt{2 \nu / \omega}, the Stokes layer, and the phase lags behind the plate as yy grows. Both are exact solutions of the full Navier–Stokes equations, and both are basic models of a boundary layer. The first problem is also called the Rayleigh problem.

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To understand this page from the ground up, read these 4 pages in order. The foundations come first.

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  1. Boundary layer concept
  2. Navier–Stokes equations concept
  3. No-slip condition concept
  4. Stokes' first and second problems example

Further reading

  1. Web https://en.wikipedia.org/wiki/Stokes_problem
About this page
Tag5S45NEQ2KZ
URIm2://5S45NEQ2KZ
Kindexample
WritingW0 stub
MSC76D05, 76D10
IllustratesNavier–Stokes equations
UsesNavier–Stokes equations, No-slip condition, Boundary layer
Changed3 November 2026

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