Worked examples — Boundary layer thickness, displacement thickness, momentum thickness
This page is a drill floor. The parent note built the three thicknesses , , from first principles. Here we throw every kind of input at those formulas so no exam question can surprise you.
Before we start, one reminder of the three tools, in plain words:
Recall The three definitions (know these cold)
- ::: distance from wall where speed reaches of the free-stream .
- ::: thickness of the "missing slab" of mass flow.
- ::: thickness of the "missing slab" of momentum.
Here is the fluid speed at height above the wall, is the free-stream speed, is kinematic viscosity, and everything obeys the No-slip condition ( at ).
The scenario matrix
Every question about these thicknesses lands in one of these boxes. We will hit every box with a worked example.
| Cell | Case class | What makes it tricky | Hit by |
|---|---|---|---|
| A | Linear profile | simplest polynomial, warm-up | Ex 1 |
| B | Polynomial (cubic) profile | matching slope + curvature at edge | Ex 2 |
| C | Trigonometric (sine) profile | integrating | Ex 3 |
| D | Degenerate: plug/uniform flow ( everywhere) | zero deficit — do the limits break? | Ex 4 |
| E | Degenerate: stagnant limit () | maximal deficit, sanity ceiling | Ex 4 |
| F | Profile defined only to (finite cutoff) | the trap | Ex 5 |
| G | Real-world word problem (numbers, units) | Reynolds number, mm-scale answer | Ex 6 |
| H | Downstream growth / scaling with | how all scale | Ex 7 |
| I | Exam twist: given and , back out | reverse the Blasius solution shape factor | Ex 8 |
| J | Sign/limiting sanity: ordering | why the inequality can never flip | Ex 9 |
A recurring trick: for a profile that only depends on the shape, write (a pure number from to ). Then and every thickness comes out as (a pure number) × . That pure number is all that changes between profiles.
The figure below plots the three model profiles we use (linear, cubic, sine) on the same axes, so you can see why they give different thicknesses. The horizontal axis is , the vertical axis is . Look at how each curve leaves the wall (bottom-left) and reaches (the dashed navy line) at the top. The shaded magenta band between the linear curve and is exactly the deficit that integrates — a curve that hugs the dashed line more closely (like the orange sine) leaves a thinner band, hence a smaller .

Keep this picture in mind: the further a profile sits from the dashed line, the fatter its deficit, the bigger its .
Example 1 — Linear profile (Cell A)
Forecast: guess before computing — will be bigger or smaller than ? (The velocity is below across the whole layer, but the deficit shrinks linearly to zero...)
- Switch to . So , , limits . Why this step? It strips out so the integral is just a number. This is the red magenta line in the figure above.
- Displacement: Why this step? is the fractional deficit — the shaded band in the figure.
- Momentum: Why this step? The extra factor weights the deficit by how much mass is actually there.
- Shape factor: (Recall is defined in the box above.)
Verify: ✓ (ordering holds). Units: every term is , a length ✓. Forecast check: exactly — the linear deficit averages to .
Example 2 — Cubic profile (Cell B)
Forecast: this profile is steeper at the wall (bigger slope at ) than the linear one — it is the violet curve in the figure. Will its be above or below ?
-
Displacement: . Why this step? Just integrate term by term; each power gives .
-
Momentum — expand the integrand first. Multiply out : Distribute term by term: Collect like powers (the two terms add to ): Why this step? Momentum needs ; you cannot integrate the product without expanding it into powers first.
-
Integrate each power using , then put every term over the common denominator :
term value Sum of the last column: . Hence Why this step? The table forces every fraction onto one denominator () so no term is mis-scaled — the safe way to add many fractions.
-
Shape factor:
Verify: is much closer to the true Blasius solution value than the linear profile's — as expected, the more realistic curved profile predicts drag better. Ordering: ✓.
Example 3 — Sine profile (Cell C)
Forecast: the sine bulges above the linear line for most of the layer (it rises fast then flattens) — the orange curve in the figure, hugging the dashed line. So its deficit is smaller — expect .
- Displacement: Why this step? . We use a trig tool here (not polynomials) because the profile itself is trig — the antiderivative of is a known clean function.
- Momentum: . Using and : Why this step? We used the half-angle identity to integrate — that's why we reach for it, because you can't integrate directly.
- Shape factor:
Verify: , again close to Blasius ✓. Forecast confirmed: ✓.
Example 4 — Degenerate limits: plug flow and stagnant flow (Cells D, E)
Forecast: with no slowdown, the deficit is zero — both thicknesses should vanish. With maximal slowdown, the deficit should approach its ceiling: the whole layer .
- (a) Plug flow: everywhere, so Why this step? If nothing is slowed, no mass and no momentum are "missing." This is the sanity floor.
- (b) Power-law : Why this step? One clean integral covers a whole family of profiles.
- Take : Why this step? As , the fluid is near-zero for almost all then jumps to — the deficit fills the whole layer.
Verify: For (linear) this gives , matching Example 1 ✓. The limit is the theoretical ceiling: can never exceed because . Plug flow gives , the floor ✓.
Example 5 — The "" trap (Cell F)
Forecast: the piece from to contributes... what?
- Split the integral at (i.e. ): Why this step? The profile is defined piecewise, so split where the pieces meet.
- Beyond , , so and the second integral is . Why this step? This is the whole resolution — the tail contributes nothing. That's why and agree for any profile that reaches at .
- Compute the finite part with , so :
Verify: so ✓. Value ✓. Sanity: this parabola sits above the linear line, smaller deficit than , and indeed ✓.
Example 6 — Real-world word problem (Cell G)
Forecast: boundary layers on everyday objects are surprisingly thin — guess in mm.
- Reynolds number: Why this step? tells us the flow is laminar (well below the transition band) and it drives the growth law.
- Boundary layer thickness (Blasius solution growth law): Why this step? is the fraction of occupied by slowed fluid.
- Choose a profile model. We only measured , not the full velocity field . To get and we must assume a profile shape; the simplest is the linear one from Example 1, which gave the fixed ratios and . Why this step? and are integrals of — without knowing the profile they are undefined, so a model profile is mandatory. The linear model is the crudest estimate but shows the correct scale.
- Displacement & momentum from those ratios:
- Shape factor — for the linear profile it is a pure number independent of the physical size: Why this step? depends only on the profile shape, not on , so it equals the Example 1 value .
Verify: Units: dimensionless ✓ for . — thin, as forecast ✓. Ordering ✓, and matches Example 1 ✓.
Example 7 — Downstream scaling (Cell H)
Forecast: more wall means more slowed fluid — all three grow. But by how much? Linearly with ? Or slower?
- Growth law: with , so and Why this step? Substitute into the law — the in the numerator partly cancels the downstairs.
- Since and are fixed fractions of (for a self-similar laminar profile), they also scale as . Why this step? Self-similarity means the profile shape is unchanged with ; only stretches, so stays constant while all three lengths grow together.
- Factor for 4× distance: . All three double.
Verify: . That is exactly ✓. The layer thickens like , not linearly — a key laminar fact behind Skin friction drag.
Example 8 — Exam twist: reverse the shape factor (Cell I)
Forecast: rising means grows relative to — the profile is getting "emptier" near the wall. What physical event does that precede?
- Definition of shape factor: Why this step? Rearranging the single definition (see the definition box) is all we need — no integrals.
- (a)
- (b) Rising signals impending Boundary layer separation — the near-wall fluid is slowing so much it is about to reverse. New Why this step? Same formula; larger (with fixed) means smaller — the momentum-carrying capacity has collapsed near the wall.
Verify: ✓. And ✓. Both reproduce the measured .
Example 9 — Why can never flip (Cell J)
Forecast: compare the two integrands term-by-term — one always sits below the other. Why?
- Write both integrands: has ; has . Why this step? Same factor appears in both; only the extra differs. Comparing them reduces the whole ordering to comparing this one extra factor against .
- The extra multiplier is : since , we have . Multiplying a non-negative quantity by something in can only shrink it (or leave it unchanged): Why this step? This is the core of the whole ordering — the momentum deficit carries the extra mass factor , and a mass fraction never exceeds .
- Integrate both sides over . Integration preserves the sign, so Why this step? If everywhere and both are integrable, then .
- Strictness. Equality in step 2 needs (or ) at every height. A real profile climbs strictly from to , so it is not at those extremes across the whole layer — hence the inequality is strict: .
- Top end. Likewise , since wherever . Chaining gives the full guarantee: This single argument is why every earlier example obeyed the ordering — it is not a coincidence, it follows from alone.
Verify: Check every earlier example: linear ✓, cubic ✓, sine ✓, parabola ✓ — all obey exactly as the proof demands.