Boundary layer displacement thickness, denoted ( \delta_1 ) or ( \delta^ ), is the distance by which the outer inviscid flow would need to be shifted away from a wetted wall to account for the flow-rate deficit created by viscosity.* It is defined by
[ \delta_1=\int_0^\infty \left(1-\frac{u(y)}{U}\right),dy ]
where (u(y)) is the local velocity normal to the wall and (U) is the velocity outside the boundary layer. In a wetted flow conduit, it represents the apparent inward growth of the wall caused by slower-moving fluid near the surface, reducing the effective area available to the faster core flow.
Displacement thickness is not the physical height of the boundary layer. It is an equivalent thickness that represents the missing volume flow caused by viscous velocity retardation near a wetted wall.
Why the Boundary Layer Requires an Equivalent Thickness
The velocity deficit near the wall
The no-slip condition makes the fluid velocity zero at a stationary wall. Moving away from the wall, velocity increases continuously until it approaches the outer-flow value.
Because fluid near the wall moves more slowly than the surrounding flow, the actual volume flux is lower than it would be for an ideal, uniform-velocity profile.
Why the conventional boundary layer thickness is limited
A nominal boundary layer thickness is often defined where the velocity reaches 99% of the outer-flow velocity, written as ( \delta_{99} ). However, the velocity approaches the outer value asymptotically, so there is no exact physical edge.
Displacement thickness avoids this ambiguity by integrating the velocity deficit across the entire boundary layer.
How Displacement Thickness Is Defined
Mathematical definition
For a two-dimensional boundary layer, displacement thickness is
[ \delta_1=\int_0^\infty \left(1-\frac{u}{U}\right),dy ]
The integrand measures the local fractional velocity deficit. Integrating it across the wall-normal direction converts that deficit into an equivalent length.
Equivalent flow interpretation
Imagine replacing the real viscous boundary layer with an ideal fluid flowing at the outer velocity (U). To produce the same total flow rate as the real flow, the wall in this idealized system would have to be shifted outward by ( \delta_1 ).
This shifted boundary is why displacement thickness is often described as the apparent displacement of the outer streamlines.
Example for a laminar profile
For the standard approximate laminar profile
[ \frac{u}{U}=\frac{3}{2}\frac{y}{\delta} -\frac{1}{2}\left(\frac{y}{\delta}\right)^3 ]
the displacement thickness is approximately
[ \delta_1=0.375\delta ]
where ( \delta ) is the profile thickness used in that approximation.
For laminar flat-plate flow, the Blasius solution gives
[ \delta_1=1.7208\sqrt{\frac{\nu x}{U_\infty}} ]
This is approximately one-third of the commonly used 99% boundary layer thickness.
What It Represents in Wetted Flow Conduits
Effective reduction in flow area
In a conduit, every wetted wall develops a region of retarded flow. The displacement thickness provides an equivalent measure of how much that wall reduces the area available to the higher-velocity core.
For a conduit with multiple wetted surfaces, the effective blockage depends on the displacement associated with each wall and on how the boundary layers interact.
Modification of the outer flow
The outer flow responds to the boundary layer as though the wall were effectively thicker or had been displaced into the fluid. This changes the local streamlines and can alter the pressure distribution through the conduit.
The effect is especially important where the conduit contracts, expands, curves, or experiences an adverse pressure gradient.
Volume-flow deficit, not direct wall thickness
Displacement thickness measures a deficit in volume flux. It does not directly measure the region containing all viscous effects, nor does it identify the point where the velocity becomes exactly equal to the free-stream velocity.
This distinction matters in pilot-plant experiments because two velocity profiles can have similar nominal thicknesses but different displacement thicknesses and therefore different flow-rate effects.
How It Is Used in Educational Pilot Plants
Interpreting measured velocity profiles
Students can measure (u(y)) at different distances from a wetted surface and calculate the integral of the velocity deficit.
Comparing the measured ( \delta_1 ) with theoretical values tests whether the observed flow agrees with a laminar or other assumed velocity profile.
Estimating flow restriction
The measured displacement thickness can be used to estimate the effective cross-sectional area of the conduit. This helps explain why the actual flow capacity differs from a calculation based only on the nominal geometric dimensions.
Studying boundary layer growth
For laminar flow over a flat surface, displacement thickness grows downstream according to
[ \delta_1 \propto \sqrt{\frac{\nu x}{U_\infty}} ]
Thus, increasing distance from the leading edge or increasing viscosity generally increases the displacement effect, while increasing outer-flow velocity reduces it for a given location.
Separating displacement from momentum effects
Displacement thickness describes the deficit in volume flux. Momentum thickness describes the momentum-flux deficit and is defined as
[ \delta_2=\int_0^\infty \frac{u}{U}\left(1-\frac{u}{U}\right),dy ]
The two quantities should not be treated as interchangeable when interpreting pilot-plant measurements.
Understanding the Trade-offs
It is an equivalent quantity
Displacement thickness is a modeling construct, not a literal layer of fluid with a sharp boundary. It is valuable because it converts a distributed velocity deficit into a simple geometric measure.
Its interpretation becomes less direct when the boundary layer is strongly three-dimensional, separated, or interacting with another wall.
Internal conduits may not have an inviscid outer region
The standard definition assumes a distinguishable outer velocity (U). In a narrow conduit, boundary layers from opposing walls can merge, leaving no clear free-stream region.
In that case, the velocity profile should be analyzed across the complete conduit, and displacement thickness should be interpreted relative to a specified reference velocity or idealized flow model.
Separation changes the interpretation
Under an adverse pressure gradient, the near-wall flow can lose momentum and eventually separate. At separation, the wall shear stress is zero:
[ \tau_w=\mu\left(\frac{\partial u}{\partial y}\right)_w=0 ]
After separation, reversed flow and recirculation can make the usual attached-boundary-layer interpretation of displacement thickness inadequate.
Wall roughness and turbulence matter
Surface roughness, turbulence, entrance effects, and developing internal flow can significantly alter the measured velocity profile. Theoretical laminar correlations should therefore be used as comparison models, not assumed to describe every pilot-plant conduit.
Making the Right Choice for Your Goal
Use displacement thickness as a flow-rate and effective-area measure, while using other boundary-layer parameters when the experiment focuses on momentum loss, wall shear, or energy dissipation.
- If your primary focus is flow-rate reduction: Calculate ( \delta_1 ) by integrating the measured velocity deficit relative to the chosen outer-flow velocity.
- If your primary focus is effective conduit area: Treat each wetted wall's displacement thickness as an apparent inward reduction of the available flow passage, while accounting for interaction between opposing boundary layers.
- If your primary focus is theoretical validation: Compare measured values with laminar correlations such as ( \delta_1=1.7208\sqrt{\nu x/U_\infty} ) only when the flow assumptions are appropriate.
- If your primary focus is separation or pressure loss: Supplement displacement thickness with momentum thickness, wall shear measurements, and pressure-gradient data.
In a wetted conduit, displacement thickness is the clearest equivalent measure of how viscous near-wall retardation reduces the volume flow available to the main stream.
Summary Table:
| Key aspect | Summary |
|---|---|
| Definition | (\delta_1 = \int_0^\infty (1-u/U),dy) |
| Physical meaning | Equivalent wall displacement caused by the velocity deficit near a wetted surface |
| Main effect | Reduces the effective area and volume flow available to the faster core stream |
| Laminar flat-plate relation | (\delta_1 = 1.7208\sqrt{\nu x/U_\infty}) |
| Pilot-plant use | Interpret measured velocity profiles, estimate flow restriction, and validate theory |
| Important limitations | Requires a suitable reference velocity and becomes less direct when layers merge, separate, or become turbulent |
| Related parameter | Momentum thickness evaluates momentum-flux loss rather than volume-flow loss |
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