Not intended for real-world applications.
Approx. Depth for Q: -- m
Velocity (at that depth): -- m/s
Hydraulic Radius (R): -- m
Flow Area (A): -- m²
This tool calculates the swale flow characteristics for a trapezoidal channel using Manning’s Equation:
where v is velocity (m/s), n is Manning’s roughness coefficient, R is hydraulic radius (m), and S is the channel slope (dimensionless).
The flow area (A) and wetted perimeter (P) of a trapezoidal channel are:
The hydraulic radius is R = A / P. By evaluating velocity (and therefore flow Q = A·v) for incremental depths, we can plot a non-linear velocity vs. depth curve.
Adjust the sliders for flow rate (Q), channel slope (S), Manning's n, bottom width (b), and side slope (z) to see real-time updates of the velocity–depth relationship.