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M1 profile upstream of a free outfall

Short answer

M1 is a backwater curve on a mild slope with depth above normal depth, increasing downstream, asymptotic to normal depth upstream and horizontal downstream. For the free outfall the profile is M2; the depth 2 km upstream of the fall is about 2.14 m.

What is M1 Profile? A rectangular canal is 10 m wide and carries a flow of 50 m³/s. The bottom and sides of the canal are concrete-lined, the longitudinal bottom slope is 0.0006 and the canal ends in a free outfall. If the flow depth is critical at a distance of 4yc4y_c upstream of the fall, what is the depth of flow 2 km upstream of the fall? Use either direct integration method (Bresse's method) taking three steps or Standard step method.

M1 profile

On a mild slope (yn>ycy_n > y_c), the M1 profile is the backwater curve in zone 1, where y>yn>ycy > y_n > y_c. Its depth increases downstream. It is asymptotic to the normal depth line upstream and approaches a horizontal water surface downstream. It occurs upstream of dams, weirs and reservoirs. (The profile in the numerical part, upstream of a free outfall, is the drawdown curve M2, because the depth falls from yny_n to ycy_c.)

Numerical part

Given: b=10 mb = 10\ \text{m}, Q=50 m3/sQ = 50\ \text{m}^3/\text{s}, S0=0.0006S_0 = 0.0006, free outfall. Concrete lining: n=0.014n = 0.014 assumed.

Depths (q=5 m2/sq = 5\ \text{m}^2/\text{s}):

yc=(529.81)1/3=1.366 m,yn=2.169 m (Manning, R=A/P)y_c = \left(\frac{5^2}{9.81}\right)^{1/3} = 1.366\ \text{m},\qquad y_n = 2.169\ \text{m}\ (\text{Manning, } R = A/P)

Since yn>ycy_n > y_c the slope is mild, and the profile is M2. The depth is ycy_c at 4yc=5.464y_c = 5.46 m upstream of the fall, which is the control section. The point asked about is 2000 m upstream of the fall, i.e. 2000−5.46=1994.5 m2000 - 5.46 = 1994.5\ \text{m} upstream of the control.

Bresse's method (three depth steps)

x=ynS0[u−(1−(ycyn)3)ϕ(u)],u=yynx = \frac{y_n}{S_0}\left[u - \left(1 - \left(\frac{y_c}{y_n}\right)^3\right)\phi(u)\right],\quad u = \frac{y}{y_n} ϕ(u)=16ln⁡u2+u+1(u−1)2+13tan⁡−12u+13\phi(u) = \frac{1}{6}\ln\frac{u^2 + u + 1}{(u-1)^2} + \frac{1}{\sqrt3}\tan^{-1}\frac{2u + 1}{\sqrt3}

ynS0=3614.5 m\dfrac{y_n}{S_0} = 3614.5\ \text{m} and 1−(yc/yn)3=1−0.62983=0.75021 - (y_c/y_n)^3 = 1 - 0.6298^3 = 0.7502.

Three equal depth steps from ycy_c upwards (trial for the end depth):

yy (m)uuϕ(u)\phi(u)xx from control (m)
1.3660.62980.97830
1.6230.74831.1560-53.5
1.8800.86681.4131-322.5
2.1370.98522.1877-1994.5

The last row is the depth at which the distance equals 1994.5 m upstream. A fine numerical integration gives 2.135 m, which confirms it.

Answer: Depth of flow 2 km upstream of the fall ≈2.14 m\approx 2.14\ \text{m} (very close to yn=2.17y_n = 2.17 m).

✓ Answer checked by Claude Opus 5.5 (high effort)

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