Answer:
Q = 14.578 m³/s
Step-by-step explanation:
Given
We use the Manning Equation as follows
Q = (1/n)*A*(∛R²)*(√S)
where
- Q = volumetric water flow rate passing through the stretch of channel (m³/s for S.I.)
- A = cross-sectional area of flow perpendicular to the flow direction, (m² for S.I.)
- S = bottom slope of channel, m/m (dimensionless) = 2.5% = 0.025
- n = Manning roughness coefficient (empirical constant), dimensionless = 0.023
- R = hydraulic radius = A/P (m for S.I.) where :
- A = cross-sectional area of flow as defined above,
- P = wetted perimeter of cross-sectional flow area (m for S.I.)
we get A as follows
A = (B*h)/2
where
B = 5 m (the top width of the flowing channel)
h = (B/2)*(m) = (5 m/2)*(1/2) = 1.25 m (the deep)
A = (5 m*1.25 m/2) = 3.125 m²
then we find P
P = 2*√((B/2)²+h²) ⇒ P = 2*√((2.5 m)²+(1.25 m)²) = 5.59 m
⇒ R = A/P ⇒ R = 3.125 m²/5.59 m = 0.559 m
Substituting values into the Manning equation gives:
Q = (1/0.023)*(3.125 m²)*(∛(0.559 m)²)*(√0.025)
⇒ Q = 14.578 m³/s