Water tools
Particle settling velocity and removal in an ideal basin
A particle settles at the speed where drag balances its weight in water. An ideal basin then removes every particle faster than its overflow rate and a proportional share of the slower ones.
How it works
Force balance on a sphere, with the drag coefficient by regime:
Above a Reynolds number of 500 the drag coefficient is 0.44. In an ideal rectangular basin the critical velocity equals the overflow rate, and a slower particle is removed in proportion:
- terminal settling velocity, m/s
- gravity, 9.81 m/s²
- particle and water density, kg/m³
- particle diameter, m
- drag coefficient
- particle Reynolds number
- water viscosity, kg/m·s
- critical settling velocity, m/h
- basin flow, m³/h
- basin surface area, m²
- fraction of a particle class removed
Depth and detention time do not enter. Real suspensions flocculate as they settle and real basins have non-ideal flow, so this is the floor for a discrete suspension. Below about 1 µm Brownian motion dominates and particles do not settle in practical times.
Related reading
These calculators use standard published formulas and are provided for preliminary engineering guidance. Confirm against measured data and vendor projections before design. Model your full water matrix in Nepti or post your project to compare provider proposals.