Manning's Equation: Sizing Open Channels and Partially Full Pipes

2026-05-19

Pressurized pipe flow uses Darcy-Weisbach or Hazen-Williams, but the moment water has a free surface — a storm sewer flowing half full, a drainage swale, a concrete-lined channel, a culvert — gravity drives the flow and roughness fights it. Manning's equation is the workhorse civil engineers reach for in this regime, and it's been the standard since 1889 because it's empirical, simple, and accurate enough.

The equation (SI units):

V = (1/n) · R2/3 · S1/2

Where V is mean velocity (m/s), n is Manning's roughness coefficient (dimensionless), R is the hydraulic radius (flow area ÷ wetted perimeter, in meters), and S is the slope of the energy grade line (m/m, often approximated as channel slope). Flow rate Q = V · A.

The key insight: velocity depends on the shape of the wetted cross-section, not just its area. Hydraulic radius R rewards "deep and narrow" over "wide and shallow" because less perimeter means less friction per unit of flow area. A 1 m × 1 m square channel running full has R = 1/4 = 0.25 m. The same area as a 2 m × 0.5 m channel has R = 1/6 ≈ 0.17 m — 30% lower, so it carries roughly 22% less flow at the same slope.

Typical Manning's n values worth memorizing:

Worked example: A 600 mm concrete storm pipe (n = 0.012) at 1% slope, flowing full. R for a full circular pipe = D/4 = 0.15 m. V = (1/0.012) · (0.15)2/3 · (0.01)1/2 = 83.3 · 0.282 · 0.1 = 2.35 m/s. Area = π(0.3)2 = 0.283 m². Q = 0.67 m³/s, or about 600 L/s.

Two practical gotchas:

Engineers don't usually solve Manning's by hand for non-circular partial flow — it's an iterative trig problem. Spreadsheets, nomographs, or tools like HydroCAD and StormCAD do the lookup. But understanding what drives the answer (R and n, both raised to fractional powers) tells you immediately why lining a ditch with concrete can shrink it by half.

See it in action: Check out HP 35s tutorial on Manning Equation for Circular Channel solving flowrate flowing partially full by usefulequations to see this theory applied.
Key Takeaway: Open channel capacity scales with hydraulic radius to the 2/3 power and inversely with roughness, so channel shape and surface matter as much as cross-sectional area.

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