Open Channel Flow Calculator

Calculate rectangular open-channel velocity, discharge, and hydraulic radius with Manning's equation.

Calculate rectangular channel flow
Use consistent SI dimensions, channel slope, and a Manning roughness coefficient.

About open channel flow

Open channel flow has a free surface exposed to atmospheric pressure, as found in rivers, canals, roadside ditches, culverts that are not full, and wastewater channels. Gravity supplies the driving force. Manning's equation is one of the most widely used empirical relationships for estimating steady uniform flow. In SI units, mean velocity equals one divided by the Manning roughness coefficient, multiplied by hydraulic radius raised to the two-thirds power and by the square root of energy slope. Discharge is mean velocity multiplied by flow area. This calculator models a rectangular channel. Its cross-sectional flow area is bottom width times water depth. Its wetted perimeter is the bottom width plus twice the depth, because those are the boundaries in contact with water. Hydraulic radius is area divided by wetted perimeter; it is not simply half the depth or an actual geometric radius. Channel slope is entered as a dimensionless rise-over-run ratio, so a one-percent fall is 0.01. Under uniform-flow assumptions, the energy grade-line slope is approximated by the channel-bed slope. The Manning coefficient represents resistance caused by surface material, vegetation, irregularity, alignment, obstructions, and other conditions. Smooth finished concrete can have a relatively low coefficient, while natural streams with stones and brush have larger values. Because velocity is inversely proportional to this coefficient, selecting an unrealistically small value can substantially overpredict capacity. Published reference ranges help with preliminary work, but field calibration and engineering judgment are important. Seasonal vegetation, sediment, damage, and changing depth can alter effective roughness. Manning's formula assumes steady, uniform, gravity-driven flow and a sufficiently long prismatic reach. It does not capture rapidly varied flow near gates, weirs, drops, bends, transitions, or hydraulic jumps. It also does not test whether the assumed depth is normal depth or whether flow is subcritical or supercritical. Use the calculator for transparent estimates, classroom exercises, drainage screening, and comparisons between rectangular designs. Final flood-control, roadway, and public-safety designs should include surveyed geometry, appropriate design storms and boundary conditions, freeboard, sediment considerations, and review under applicable hydraulic standards.

Open channel flow examples

Rectangular examples use SI Manning coefficients and uniform-flow assumptions.

Channel inputsCalculated resultApplication
Width 2 m; depth 1 m; slope 0.01; n 0.013Velocity 4.846 m/s; discharge 9.692 m³/sA smooth, relatively steep rectangular channel.
Width 3 m; depth 0.5 m; slope 0.002; n 0.015Velocity 1.550 m/s; discharge 2.325 m³/sA shallower channel on a mild grade.
Width 1 m; depth 0.4 m; slope 0.005; n 0.025Velocity about 1.04 m/sRoughness reduces velocity and capacity.

How to calculate open channel flow

  1. Enter the rectangular channel's inside bottom width and water depth in metres.
  2. Enter bed slope as a decimal rise-over-run ratio.
  3. Choose and enter a representative Manning roughness coefficient.
  4. Select Calculate Flow to obtain velocity, discharge, and hydraulic radius.

Open channel flow FAQ

What does a slope of 0.01 mean?

It means the channel falls one unit vertically for every one hundred units horizontally. This is a one-percent slope, entered as a decimal rather than as 1.

How do I choose Manning's n?

Use published ranges for the channel material and condition, then account for vegetation and irregularity. Important designs should calibrate roughness against observed levels or flows where possible.

What is hydraulic radius?

Hydraulic radius is flow area divided by wetted perimeter. It measures hydraulic efficiency and is not generally the same as water depth.

Can this calculate a trapezoidal channel?

This version specifically uses rectangular geometry. A trapezoidal section has a different area and wetted perimeter, so its side slopes must be included in another model.

Does the result determine flood safety?

No, it estimates one steady uniform-flow condition. Flood design also requires inflow hydrology, backwater effects, transitions, debris, freeboard, and applicable safety criteria.