Froude Number
Froude number formula |
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\( Fr \;=\; \dfrac{ v }{ \sqrt{ g \cdot h_m } } \) (Froude Number) \( v \;=\; Fr \cdot \sqrt{ g \cdot h_m } \) \( g \;=\; \dfrac{ v^2 }{ h_m \cdot Fr^2 }\) \( h_m \;=\; \dfrac{ v^2 }{ g \cdot Fr^2} \) |
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| Symbol | English | Metric |
| \( Fr \) = Froude Number | \(dimensionless\) | \( dimensionless \) |
| \( v \) = Flow Velocity | \(ft\;/\;sec\) | \(m\;/\;s\) |
| \( g \) = Gravitational Acceleration | \(ft\;/\;sec^2\) | \(m\;/\;s^2\) |
| \( h_m \) = Mean Depth | \(ft\) | \(m\) |
Froude number, abbreviated as \(Fr\), a dimensionless number, is use to understand how water (or any fluid with a free surface) moves in open channels, like rivers, canals, spillways, or around ships. In simple terms, it compares the inertial forces (the momentum or push of the flowing water) to the gravitational forces (the pull of gravity that tries to keep the surface level and influences waves). This matters most in situations with a free surface, where the top of the water isn't confined by a pipe or closed conduit, because gravity shapes how surface waves and disturbances behave. The Froude number is calculated as the flow velocity divided by the square root of gravity times a characteristic length (usually the water depth in open channels).
This classification helps engineers design safe and efficient systems. For example, knowing the regime predicts where a hydraulic jump might occur (when fast supercritical flow suddenly slows to subcritical, creating a turbulent rise in water level). It also ensures that small-scale physical models in the lab match real-world behavior through Froude scaling, so tests on rivers, dams, or ship hulls are reliable. Overall, the Froude number is one of the most practical tools for making sense of free-surface flows in everyday hydraulic engineering.

