Archimedes number#

Named after: Archimedes (c. 287-c. 212 BCE).

$$\text{Ar} \stackrel{\text{def}}{=} \frac{g L^{3} \rho (\rho_s - \rho_f)}{\mu^{2}} \sim \frac{\text{buoyancy}}{\text{viscous resistance}}$$

Description#

Measures buoyant forcing on a particle or bubble relative to viscous resistance. It indicates the settling or rising regime set by density contrast.

Quantities#

NameSymbolSI unitsDimension
gravitational acceleration\(g\)\(\mathrm{m}\,\mathrm{s}^{-2}\)\(\text L\,\text T^{-2}\)
characteristic length\(L\)\(\mathrm{m}\)\(\text L\)
mass density\(\rho\)\(\mathrm{kg}\,\mathrm{m}^{-3}\)\(\text L^{-3}\,\text M\)
solid-fluid density difference\(\rho_s - \rho_f\)\(\mathrm{kg}\,\mathrm{m}^{-3}\)\(\text L^{-3}\,\text M\)
dynamic viscosity\(\mu\)\(\mathrm{Pa}\,\mathrm{s}\)\(\text L^{-1}\,\text M\,\text T^{-1}\)

Regimes#

Particle settling

viscous settlingtransitional settlinginertial settling011000
RangeRegimeDescription
0 – 1viscous settlingViscous resistance dominates buoyant motion. Particles or bubbles settle slowly in creeping flow.
1 – 1000transitional settlingBuoyancy, viscosity, and inertia are all important. Wake effects and shape sensitivity may appear.
1000 – ∞inertial settlingBuoyant forcing is large compared with viscous resistance. Inertial wakes and unsteady paths become important.