Open Channel Flow Calculator
Calculate uniform SI Manning discharge from a supplied roughness coefficient, flow area, hydraulic radius, and energy slope with explicit coherent-SI inputs, di
Open Channel Flow Calculator
Background.
Open Channel Flow Calculator evaluates uniform SI Manning discharge from a supplied roughness coefficient, flow area, hydraulic radius, and energy slope. The page keeps every model input visible and uses the relationship Q = A R_h^(2/3) S^(1/2) / n. It is designed for a transparent calculation where the quantities have already been measured or selected from an appropriate source. It does not choose a material, operating condition, reference state, or empirical coefficient on the user's behalf.
Enter manning roughness n, flow area, hydraulic radius, energy slope in the units printed beside the fields. These are coherent SI quantities, so the displayed equation can be followed without a hidden unit factor. A result is only comparable with another source when the same quantity definitions, reference conditions, and sign or magnitude convention are used. Record those conditions whenever the number supports engineering, laboratory, or coursework decisions.
The calculator performs arithmetic with Decimal.js and rounds once at the output boundary to twelve significant digits. That protects very small and very large scientific results from early decimal-place rounding. The tests do more than pin one example: they check the dimensional scaling implied by each variable, finite and positive domain guards, several orders of magnitude, and the formula-engine registration used by the live page.
Uniform steady SI Manning model with user-supplied n; gradually/rapidly varied flow, backwater, controls, composite roughness, sediment, freeboard, and code design are outside it. The scope statement appears beside the numerical result because it changes how the answer may be used. A neat number does not remove uncertainty in measurements, material properties, geometry, calibration, or the assumptions used to reduce a real system to one equation.
Use scaling as a quick reasonableness check. If an input appears in the numerator, increasing it should move the result in the same direction; a denominator should move it in the opposite direction; a square-root term changes more slowly. If the page behaves differently from the displayed relationship, stop and review the units. The calculator rejects zero, negative, infinite, and nonnumeric quantities where the equation requires a positive magnitude.
This page is a calculation aid rather than a substitute for measurement standards, a laboratory method, or a discipline-specific design code. Keep more digits than the source data justify only while carrying intermediate work, and round the reported result to the uncertainty of the least certain input. If a source uses centimetre-gram-second units, customary units, gauge values, or a different reference temperature, convert and document those choices before entering the numbers.
This page is a calculation aid rather than a substitute for measurement standards, a laboratory method, or a discipline-specific design code. Keep more digits than the source data justify only while carrying intermediate work, and round the reported result to the uncertainty of the least certain input. If a source uses centimetre-gram-second units, customary units, gauge values, or a different reference temperature, convert and document those choices before entering the numbers.
This page is a calculation aid rather than a substitute for measurement standards, a laboratory method, or a discipline-specific design code. Keep more digits than the source data justify only while carrying intermediate work, and round the reported result to the uncertainty of the least certain input. If a source uses centimetre-gram-second units, customary units, gauge values, or a different reference temperature, convert and document those choices before entering the numbers.
What is open channel flow calculator?
Open Channel Flow Calculator is a transparent implementation of Q = A R_h^(2/3) S^(1/2) / n for uniform SI Manning discharge from a supplied roughness coefficient, flow area, hydraulic radius, and energy slope.
How to use this calculator.
- Confirm that the displayed quantity equation matches the model you intend to use.
- Convert every measurement to the SI unit printed beside its field.
- Enter sourced magnitudes and keep their reference conditions with the result.
- Read the numeric result together with the model-scope output.
- Round the reported value to the uncertainty supported by the inputs.
The formula.
The implementation evaluates Q = A R_h^(2/3) S^(1/2) / n with Decimal.js. Inputs are required to be finite and positive because this page treats them as magnitudes. Arithmetic is not rounded between operations; each numeric output is rounded once to twelve significant digits. The scaling tests independently verify the power of every input in the equation.
A worked example.
Using the displayed default inputs in Q = A R_h^(2/3) S^(1/2) / n gives flowRateM3PerS = 5.13862658133 m³/s. The calculation retains Decimal precision and rounds once at the result boundary.
Frequently asked questions.
What equation does this open channel flow calculator use?
Why must all inputs use the displayed units?
When should I not use this result?
How is the result rounded?
How can I check the answer?
Does the calculator choose reference data?
Can this replace a standard test method?
Why are zero and negative values rejected?
References& sources.
- [1]FHWA HEC-22, Urban Drainage Design Manual, 4th ed.
- [2]USACE EM 1110-2-1601, Hydraulic Design of Flood Control Channels.
- [3]BIPM, The International System of Units (SI Brochure), 9th ed., version 3.01, coherent derived units and quantity equations.
- [4]NIST Special Publication 811, Guide for the Use of the International System of Units, 2008 edition.
- [5]USGS Water-Supply Paper 2339, Guide for Selecting Manning's Roughness Coefficients.
How this page was produced
- Published by
- Quanta Calculator
- Primary sources
- 5 cited below
- Method
- Q = A R_h^(2/3) S^(1/2) / n
- Published
- Last verified
Built with AI assistance and verified by automated tests against the cited sources — every worked example on this page is computed by the same code that runs the calculator. How we build and check calculators.
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