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Flow in a swale
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Revision as of 17:08, 11 January 2019
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Flow (''Q'') in an open channel, such as a swale, may be calculated using Manning's equation:
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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)}}
Jenny Hill
8,255
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