Surface overflow rate (basin 30 m x 10 m)–
Time for floc to settle the full depth–
Time water spends in the basin–
This floc–
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Ideal settling basin theory

Imagine a particle entering at the surface. It has to fall the full depth while the water carries it the length of the basin. Settling time = depth / settling velocity, and the water's time in the basin = volume / flow. Set them equal and depth cancels: a particle is captured if its settling velocity is at least flow / surface area. That ratio is the surface overflow rate.

This is the classic ideal basin model, simplified: real basins have currents, wind and temperature effects, so designers add safety margin. Operators often quote overflow rate in gallons per day per square foot; 1 m/h is about 590 gpd/ft².

Try it: hold the floc settling velocity at 1.5 m/h and raise the plant flow from 400 to 900 m³/h. The overflow rate climbs past 1.5 m/h, the readout flips to 'Partly carried over the weir', and the brown floc particles start riding over the far end.

Depth buys time, not capture

Making the basin deeper increases how long water stays, which helps with storage and smoothing out surges, but in the ideal model it does not change which particles are caught. Better coagulation, which makes faster sinking floc, or more surface area are what improve capture.

Sources

How to cite this model

Avid Solutions International. (2026, November 11). How a treatment plant settles out dirt [Interactive 3D model]. Avid Field Lab. https://avidsolutionsintl.com/explore/water-treatment-clarifier

Last updated November 11, 2026

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