Difference between revisions of "Flow in a swale"

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(Created page with "Flow (''Q'') in an open channel, such as a swale, may be calculated using Manning's equation: <math>Q=VA=\frac{R^{\frac{2}{3}}S^{\frac{1}{2}}}{n}</math> Where: <math>R=\frac{A...")
 
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Flow (''Q'') in an open channel, such as a swale, may be calculated using Manning's equation:
Flow (''Q'') in an open channel, such as a [[swale]], may be calculated using Manning's equation:
<math>Q=VA=\frac{R^{\frac{2}{3}}S^{\frac{1}{2}}}{n}</math>
<math>Q=VA=\frac{R^{\frac{2}{3}}S^{\frac{1}{2}}}{n}</math>
Where:
Where:
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*''P'' = the wetted perimeter of the swale (m)
*''P'' = the wetted perimeter of the swale (m)
*''S'' = the longitudinal slope (m/m)
*''S'' = the longitudinal slope (m/m)
*''n'' = Manning's coefficient (dimensionless)}}
*''n'' = [[Manning's coefficient]] (dimensionless)}}

Revision as of 17:08, 11 January 2019

Flow (Q) in an open channel, such as a swale, may be calculated using Manning's equation: Where:

Where:

  • Q = the flow in the swale (m3/s)
  • A = the cross sectional area of the swale (m2)
  • P = the wetted perimeter of the swale (m)
  • S = the longitudinal slope (m/m)
  • n = Manning's coefficient (dimensionless)