How it’s calculated
Manning’s equation gives the mean velocity of steady, uniform open-channel flow from the channel’s hydraulic radius (flow area ÷ wetted perimeter), slope and roughness coefficient n. Discharge is velocity × area.
Example (FHWA HDS-4, Example 4.1): a trapezoidal earth channel with B = 2 m, side slopes 1V:2H, S = 0.003, depth 0.5 m and n = 0.02. A = 2(0.5) + 2(0.5)² = 1.5 m², P = 2 + 2(0.5)√5 = 4.24 m, R = 0.354 m. V = (1/0.02)(0.354)^(2/3)(0.003)^(1/2) ≈ 1.37 m/s and Q ≈ 2.06 m³/s (HDS-4 rounds R to 0.35 m and reports 1.36 m/s and 2.0 m³/s).
The calculator works in SI internally, so mixed units are converted exactly; the 1.49 factor applies only if you solve the US-unit form by hand. Results assume uniform flow, where the water surface is parallel to the bed.
Frequently asked questions
What Manning’s n should I use?
Use a value for the lining: about 0.013 for concrete pipe or lined channels, 0.020 for a clean earth canal, and 0.03–0.05 or more for natural streams with stones and vegetation. Roughness dominates the answer, so pick conservatively.
Does a circular pipe carry most when it is full?
No. With Manning’s equation a circular pipe peaks at about 94% depth, because the wetted perimeter grows faster than area near the crown. Design usually uses full-flow capacity.
How do I find normal depth for a given flow?
Adjust the depth until the discharge matches your flow (trial and error, as in HDS-4 Example 4.2).
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Sources
- Introduction to Highway Hydraulics (HDS-4), §4.3 Manning’s Equation and Table B.2 — U.S. Federal Highway Administration
- Guide for Selecting Manning’s Roughness Coefficients for Natural Channels and Flood Plains (WSP 2339) — U.S. Geological Survey
Formulas are taken from the free public references above. Results are provided “as is” for informational and educational purposes only. See our disclaimer.
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