INGENIA

HYD-01

Manning discharge

Uniform-flow discharge Q = (1/n) A R^{2/3} S^{1/2} (SI).

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Open channelManning 1890ISO 748

Governing equation

Q=1nAR2/3S1/2,R=A/PQ=\dfrac{1}{n}A R^{2/3} S^{1/2},\quad R=A/P

where

n
Manning n (s/m^{1/3})
b
Width (m)
y
Depth (m)
S
Bed slope ()
R
Hydraulic radius (m)
Q
Discharge (m³/s)
V
Velocity (m/s)

Lecture brief

Historical brief

Open-channel and pipe flow were written by Chezy, Manning, Darcy and Weisbach in the nineteenth century, then Bakhmeteff and Bélanger on the hydraulic jump. The sheets compute conveyance, head loss and gradually varied profiles. This sheet (HYD-01 — Manning discharge) is the form associated with Manning 1890 · ISO 748. Working symbols: nn, bb, yy, SS \rightarrow RR, QQ, VV. Manning recast Chézy's C as R^{1/6}/n. The formula is empirical yet the open-channel standard for uniform flow.

Purpose

Purpose: compute RR, QQ, VV from nn, bb, yy, SS in Hydraulics via Q=1nAR2/3S1/2,R=A/PQ=\dfrac{1}{n}A R^{2/3} S^{1/2},\quad R=A/P Uniform-flow discharge Q = (1/n) A R^{2/3} S^{1/2} (SI). Use it when a real hydraulics question must be answered in SI before a code check.

Live realistic example

In symbols

Live case. Given n=0.030s/m1/3n = 0.030\,\mathrm{s/m^1/3}, b=8.000mb = 8.000\,\mathrm{m}, y=1.500my = 1.500\,\mathrm{m}, S=0.001S = 0.001\,\mathrm{—}, the governing relation Q=1nAR2/3S1/2,R=A/PQ=\dfrac{1}{n}A R^{2/3} S^{1/2},\quad R=A/P yields R=1.091mR = 1.091\,\mathrm{m}, Q=13.405m3/sQ = 13.405\,\mathrm{m^{3}/s}, V=1.117m/sV = 1.117\,\mathrm{m/s}. Wide rectangle: A = b y, P = b+2y, R = A/P. SI n. Move a slider: the numbers are this situation, not a canned story.

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Inputs

Outputs

  • Hydraulic radius R1.091 m
  • Discharge Q13.405 m³/s
  • Velocity V1.117 m/s
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HYD-01 · pipe
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Narration of this film

Wide rectangle: A = b y, P = b+2y, R = A/P. SI n.

Manning recast Chézy's C as R^{1/6}/n. The formula is empirical yet the open-channel standard for uniform flow.

Reading speed

Watch on YouTube