Hydrodynamic Film Pressure⚠ unverified
Mechanical / Lubrication · Approximate hydrodynamic film pressure
Parameters
| Input | Symbol | Unit | Default | Description |
|---|---|---|---|---|
| mu | μ | Pa*s | 0.05 | Dynamic viscosity |
| U | U | m/s | 10.0 | Sliding velocity |
| L | L | m | 0.1 | Bearing length |
| h | h | m | 0.0001 | Film thickness |
| Output | Symbol | Unit | Description |
|---|---|---|---|
| p | p | Pa | Film pressure |
The science & history
Understanding the Parameters
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Viscosity $\mu$ and velocity $U$ — their product is the drag that entrains oil into the gap. More viscous oil or faster motion pumps more oil into the converging wedge, building more pressure — so film pressure rises with both. This is why a bearing generates no supporting pressure at rest ($U = 0$).
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Length $L$ — the distance over which pressure builds up along the film; a longer wedge integrates more pressure rise.
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Film thickness $h$ — enters as $1/h^2$, the dominant sensitivity. Halving the film quadruples the pressure. This steep dependence is self-stabilising: if the load pushes the surfaces closer, the film pressure shoots up to push them back apart — the automatic load-balancing that makes hydrodynamic bearings work.
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Order-of-magnitude only — this is a scaling estimate, not the true pressure distribution (which is parabolic-ish and set by the full Reynolds equation with a definite peak and a cavitation region). Use it for a quick sanity check of magnitude, not for design.
Derivation (Approaching a Proof)
The pressure comes from Reynolds' lubrication equation, itself a thin-film reduction of the Navier–Stokes equations. In a thin film the flow is dominated by viscosity, and the pressure gradient balances the viscous shear. In one dimension the Reynolds equation is
$$\frac{\mathrm{d}}{\mathrm{d}x}\!\left(\frac{h^3}{12\mu}\frac{\mathrm{d}p}{\mathrm{d}x}\right) = \frac{U}{2}\frac{\mathrm{d}h}{\mathrm{d}x}.$$
The left side is the pressure-driven (Poiseuille) flow; the right side is the shear-driven (Couette) flow that the converging wedge ($\mathrm{d}h/\mathrm{d}x < 0$) must divert into pressure. Scaling by characteristic values — pressure $p$ over length $L$, film $h$, speed $U$ — the balance gives
$$\frac{h^3}{\mu}\frac{p}{L^2} \sim U\,\frac{h}{L} \;\Longrightarrow\; p \sim \frac{\mu U L}{h^2}.$$
The $1/h^2$ arises because the pressure flow scales with $h^3$ while the driving shear flow scales with $h$, so their ratio (the pressure) scales with $1/h^2$. Physically: a converging gap forces the entrained oil to "escape" against viscous resistance, and the thinner the gap the harder that escape, the higher the pressure. Integrating the true Reynolds equation over a wedge gives the exact distribution and load; this scaling captures the essential magnitude and the crucial thin-film sensitivity.
Dimensional check. $\dfrac{\mu U L}{h^2} = \dfrac{(\text{Pa}\cdot\text{s})(\text{m/s})\,\text{m}}{\text{m}^2} = \text{Pa}$. ✓
History and Development
Osborne Reynolds derived the lubrication equation in 1886 to explain Beauchamp Tower's experimental discovery (1883) that a lubricated railway journal bearing developed large oil-film pressures on its own. It is one of the foundational results of tribology — the reason hydrodynamic bearings support enormous loads with no wear — and underlies the Sommerfeld Number, Minimum Film Thickness, and all journal/thrust/ slider bearing design.
Related Concepts: Sommerfeld Number, Minimum Film Thickness, Petroff Friction, Elastohydrodynamic Film, Journal Bearing Load Capacity, Reynolds Number
Notes: Order-of-magnitude scaling from the Reynolds equation — not the true distribution (which peaks and cavitates). $1/h^2$ sensitivity gives self-stabilising load support. Full design uses the Reynolds equation / Raimondi–Boyd charts.