The sedimentation rate of a particle is its theoretical downward rate in clear, stagnant water. Particles will only settle if :
- In a longitudinal flow, the ratio of the length of the reservoir to the height of the reservoir is greater than the ratio of the water velocity to the sedimentation velocity.
- In a vertical upward flow, the upward water velocity is lower than the sedimentation limit velocity.
The settling follows what is known as Stokes’ law. It shows that the speed at which a particle falls is proportional to the square of its size. It also depends on the difference in density between the particle and the liquid.
Therefore, the increase in particle diameter significantly increases sedimentation. This is why flocculation is a widely used technique in water treatment, whether in sanitation or for the production of drinking water.
There are physical forces that also play a role in settling such as viscosity and particle size.