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Manning Equation Calculator

Calculate open-channel flow rate and velocity for rectangular, trapezoidal, and circular cross-sections

Reviewed by Christopher FloiedUpdated

This free online manning equation calculator provides instant results with no signup required. All calculations run directly in your browser — your data is never sent to a server. Supports both metric (SI) and imperial units with built-in unit selection dropdowns on every input field, so you can work in whatever units your problem provides. Designed for engineering students and professionals working through coursework, design projects, or quick reference calculations.

Manning Equation Calculator

Q = (1/n) · A · R^(2/3) · S^(1/2)  ·  V = Q/A

e.g. 0.001 = 1 m drop per 1000 m length

Results — Rectangular 2.000m × 1.000m

Flow Rate Q

3.0648 m³/s

3064.78 L/s

Mean Velocity V

1.5324 m/s

Cross-section Area A

2.0000

Hydraulic Radius R

0.5000 m

Wetted Perimeter P

4.0000 m

Formula

Q = (1/0.0132.0000·0.5000^(2/3)·√0.001

= 3.0648 m³/s

How to Use This Calculator

1

Enter your input values

Fill in all required input fields for the Manning Equation Calculator. Most fields include unit selectors so you can work in your preferred unit system — metric or imperial, whichever matches your problem.

2

Review your inputs

Double-check that all values are correct and that you have selected the right units for each field. Incorrect units are the most common source of calculation errors and can produce results that are off by factors of 2, 10, or more.

3

Read the results

The Manning Equation Calculator instantly computes the output and displays results with units clearly labeled. All calculations happen in your browser — no loading time and no data sent to a server.

4

Explore parameter sensitivity

Try adjusting individual input values to see how the output changes. This is a quick and effective way to develop intuition about how different parameters influence the result and to identify which inputs have the largest effect.

Formula Reference

Manning Equation Calculator Formula

See calculator inputs for the governing equation

Variables: All variables and their units are labeled in the calculator interface above. Input fields accept values in multiple unit systems — select your preferred unit from the dropdown next to each field.

When to Use This Calculator

  • Use the Manning Equation Calculator when solving homework or exam problems that require quick numerical verification of your hand calculations — instant feedback helps identify arithmetic errors before they propagate.
  • Use it during the early design phase to rapidly iterate on parameters and narrow down feasible configurations before committing time to detailed finite element simulations or full design packages.
  • Use it when reviewing a colleague's calculation or checking a vendor's data sheet for plausibility — a quick sanity check can prevent costly downstream errors.
  • Use it to generate reference data for a technical report or presentation without manual computation, ensuring consistent, reproducible numbers throughout the document.
  • Use it in the field when a quick estimate is needed and a full engineering software package is not available.

About This Calculator

The Manning Equation Calculator is a precision engineering calculation tool designed for students, engineers, and technical professionals. Calculate open-channel flow rate and velocity for rectangular, trapezoidal, and circular cross-sections All calculations are performed using established engineering formulas from the relevant scientific literature and standards. Inputs support both metric (SI) and imperial unit systems, with unit conversion handled automatically — simply select your preferred unit from the dropdown next to each field. Results are computed instantly in the browser without sending data to a server, ensuring both speed and privacy. This calculator is intended as a supplementary tool for learning and design exploration; always verify results against authoritative references for safety-critical applications.

The Theory Behind It

The Manning equation (also called Manning-Strickler) computes velocity in open-channel flow under gravity: V = (1/n)·R_h^(2/3)·S^(1/2), where V is velocity (m/s), n is Manning's roughness coefficient (s/m^(1/3)), R_h is hydraulic radius (area divided by wetted perimeter), and S is the channel slope (dimensionless). The flow rate is Q = V·A, where A is the cross-sectional area of flow. In US customary units, the formula includes a factor of 1.486: V (ft/s) = (1.486/n)·R_h^(2/3)·S^(1/2) with R_h in feet. Manning's n is an empirical coefficient characterizing the channel surface and vegetation. Typical values: smooth concrete 0.011-0.015, corrugated metal 0.022-0.024, earth channel (clean) 0.022-0.025, earth channel (vegetation) 0.030-0.050, natural streams 0.030-0.050, heavy vegetation or meandering 0.075-0.15. The equation applies to uniform flow (constant velocity, depth, and cross-section) in open channels with free surface exposed to atmosphere. Non-uniform flow requires additional analysis with the energy equation and backwater calculations. The Manning equation is the workhorse of open channel hydraulics, used for rivers, streams, canals, drainage ditches, storm sewers partly full, and wastewater collection. It is simpler and more practical than the theoretically-superior Darcy-Weisbach for open channels because n values are empirically tabulated for channel types.

Real-World Applications

  • Storm sewer and drainage design: size pipes and channels for storm water runoff using Manning's equation for partly-full conditions. Typical n = 0.013 for concrete, 0.024 for corrugated metal pipe.
  • Irrigation canal design: compute required cross-section and slope for irrigation channels carrying specified flow rates. Vegetated or lined channels have different n values.
  • Natural stream flow analysis: estimate flow in natural streams from measured slope, cross-section, and estimated roughness (typical n = 0.030-0.075 for natural channels).
  • Wastewater gravity sewer design: partly-full flow in circular sewer pipes uses Manning's equation with geometrical formulas for A and R_h as functions of depth of flow.
  • Open-channel flow meters: weirs and flumes (Parshall, rectangular, V-notch) are designed using Manning's equation combined with specific flow-over-weir formulas.

Frequently Asked Questions

What is Manning's equation?

V = (1/n)·R_h^(2/3)·S^(1/2) for SI units (or V = (1.486/n)·R_h^(2/3)·S^(1/2) for US units with R_h in feet). This empirical equation predicts open-channel flow velocity from channel geometry and roughness. Q = V·A for the volumetric flow rate. Manning's n is an empirical roughness coefficient tabulated for various channel types.

What is the hydraulic radius?

R_h = A/P, where A is the cross-sectional area of flow and P is the wetted perimeter (the length of the boundary in contact with the fluid). For a circular pipe flowing full, R_h = D/4. For a rectangular channel of width b and depth y, R_h = by/(b+2y). R_h is the fundamental length scale in open channel flow and appears in all friction equations.

What's a typical Manning's n value?

Smooth concrete: 0.011-0.015. Corrugated metal: 0.022-0.024. Clean earth channel: 0.022-0.025. Earth with grass: 0.030-0.035. Rocky channel with weeds: 0.040-0.050. Natural stream with gravel bed: 0.030-0.050. Heavy vegetation or braided channel: 0.075-0.15. Choose n based on the dominant roughness source; composite roughness for multi-section channels uses area-weighted averaging or more sophisticated methods.

Does Manning's equation work for pipes flowing full?

Yes, the equation is commonly used for sewer and drainage pipes flowing partly or fully. For a circular pipe flowing full, R_h = D/4, A = πD²/4. Manning's equation is simpler than Darcy-Weisbach for these applications because n is directly tabulated for pipe types. However, for pressure flow in pipes, Darcy-Weisbach with Reynolds-dependent friction factor is more accurate for high Re.

What's the slope S in Manning's equation?

S is the channel bed slope for uniform flow, measured as dimensionless rise over run. A 1% slope (S = 0.01) means the channel drops 1 meter per 100 meters of length. For uniform flow (constant depth, velocity, cross-section), the energy slope equals the bed slope. For non-uniform flow, the energy slope differs from the bed slope and requires more detailed analysis with the energy equation.

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References & Further Reading