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Free-stream velocity 5.0 m/s
Kinematic viscosity 1.5e-5
Surface roughness 0%
Trip wire position None

Why fluid sticks to surfaces

The no-slip condition is one of the most fundamental facts in fluid mechanics: at a solid surface, the fluid velocity exactly matches the surface velocity. For a stationary wall, the fluid speed is zero at the wall and increases with distance until it reaches the free-stream velocity U∞. The thin region where this transition happens is the boundary layer.

Ludwig Prandtl introduced the boundary layer concept in 1904 in a landmark paper that unified two seemingly incompatible views of fluid flow: inviscid theory (which predicted no drag and worked well far from surfaces) and viscous theory (which was mathematically intractable for general flows). Prandtl showed that viscous effects are confined to a thin layer near the surface, where the velocity gradient is steep. Outside this layer, the flow behaves as if inviscid.

The boundary layer thickness δ grows with distance x from the leading edge. For a laminar boundary layer, δ ∝ √(x), giving the characteristic parabolic growth visible in the simulation. The exact solution is given by the Blasius profile.

Exact solutions in the laminar regime

For steady, incompressible flow over a flat plate with zero pressure gradient, the boundary layer equations admit a similarity solution discovered by Heinrich Blasius (1908). By introducing the similarity variable η = y√(U∞/νx), the partial differential equations reduce to a single ordinary differential equation: f''' + ½ff'' = 0, where the velocity profile is u/U∞ = f'(η).

The Reynolds number Reₓ = U∞x/ν is the ratio of inertial forces to viscous forces at position x along the plate. It determines the boundary layer character. At Reₓ < 5 × 10⁵, the boundary layer is laminar and the Blasius solution applies. The boundary layer thickness is δ ≈ 5x/√Reₓ, and the skin friction coefficient is cṕ = 0.664/√Reₓ.

Above the critical Reynolds number, small perturbations amplify through the Tollmien-Schlichting instability, and the boundary layer transitions to turbulent. Surface roughness and free-stream turbulence can trigger transition earlier. The trip wire in this simulation forces transition at a specific location.

Order gives way to chaos

A laminar boundary layer has smooth, parallel streamlines with a gradual velocity profile. Energy dissipation is relatively low, and the skin friction drag is modest. However, the laminar layer is more susceptible to flow separation in adverse pressure gradients because it lacks the momentum mixing to overcome the pressure rise.

A turbulent boundary layer is characterized by chaotic fluctuations superimposed on the mean flow. The velocity profile is much fuller — the turbulent mixing transports high-momentum fluid from the outer region toward the wall, creating a steeper gradient at the surface and a more uniform profile farther out. This results in higher skin friction but greater resistance to separation.

Golf ball dimples exploit this: by tripping the boundary layer to turbulence, the dimples delay separation behind the ball, reducing pressure drag far more than the slight increase in skin friction drag. The net effect is that a dimpled ball flies roughly twice as far as a smooth one.