Difference between revisions of "Flow in a swale"
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Jenny Hill (talk | contribs) (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)