Shields parameter#
Also known as: Shields number.
Named after: Albert Frank Shields (1908-1974).
$$\theta \stackrel{\text{def}}{=} \frac{\tau}{(\rho_s - \rho_f) g L} \sim \frac{\text{bed shear stress}}{\text{submerged particle weight}}$$
Description#
Measures bed shear stress relative to submerged particle weight. It indicates whether grains on a bed remain stable or begin to move.
Quantities#
| Name | Symbol | SI units | Dimension |
|---|---|---|---|
| shear stress | \(\tau\) | \(\mathrm{Pa}\) | \(\text L^{-1}\,\text M\,\text T^{-2}\) |
| solid-fluid density difference | \(\rho_s - \rho_f\) | \(\mathrm{kg}\,\mathrm{m}^{-3}\) | \(\text L^{-3}\,\text M\) |
| gravitational acceleration | \(g\) | \(\mathrm{m}\,\mathrm{s}^{-2}\) | \(\text L\,\text T^{-2}\) |
| characteristic length | \(L\) | \(\mathrm{m}\) | \(\text L\) |
Regimes#
Sediment transport
| Range | Regime | Description |
|---|---|---|
| 0 – 0.03 | stable bed | Bed shear is below the typical threshold for sustained grain motion. |
| 0.03 – 0.06 | incipient motion | Grains are near the onset of motion; transport depends sensitively on particle Reynolds number, packing, and turbulence. |
| 0.06 – ∞ | mobile bed | Bed shear is high enough for sustained sediment motion and bed-load transport. |