Skip to main content

Slope break 0.01 to 0.0064: profile and length

Short answer

The downstream profile is S3 (supercritical, depth rising). Computed by the direct step method, its length to 99% of the new normal depth is about 370 m.

A rectangular channel 10 m wide is laid with a break in its bottom slope from 0.01 to 0.0064. If it carries 125 m³/s, determine the nature of the surface profile and compute its length. Take n = 0.015.

Given: b=10b = 10 m, Q=125 m3/sQ = 125\ \text{m}^3/\text{s} (q=12.5 m2/sq = 12.5\ \text{m}^2/\text{s}), n=0.015n = 0.015, slope changes from S01=0.01S_{01} = 0.01 to S02=0.0064S_{02} = 0.0064.

Depths

yc=(12.529.81)1/3=2.516 my_c = \left(\frac{12.5^2}{9.81}\right)^{1/3} = 2.516\ \text{m}

By Manning's equation (trial, R=A/PR = A/P):

ReachS0S_0yny_n (m)Class
10.01001.633steep
20.00641.896steep

Both slopes are steep, and the flow is supercritical throughout. The flow arrives at the break with y=1.633y = 1.633 m, which is below the new normal depth 1.896 m, so on the downstream reach y<yn2<ycy < y_{n2} < y_c. The profile is S3 (rising depth, asymptotic to yn2y_{n2}). No jump occurs.

Length of S3 profile. The curve reaches yn2y_{n2} only at infinity, so its length is computed up to 0.99 yn2=1.8770.99\,y_{n2} = 1.877 m, using the direct step method with 4 equal steps and S0=0.0064S_0 = 0.0064.

E=y+V22g,Sf=n2V2R4/3,Δx=E2−E1S0−SˉfE = y + \frac{V^2}{2g},\quad S_f = \frac{n^2V^2}{R^{4/3}},\quad \Delta x = \frac{E_2 - E_1}{S_0 - \bar S_f}
yy (m)RR (m)VV (m/s)EE (m)SfS_fSˉf\bar S_fΔx\Delta x (m)
1.63261.2317.6564.62040.01000
1.69371.2657.3804.46990.008960.0094848.9
1.75471.2997.1244.34120.008060.0085161.1
1.81581.3326.8844.23120.007280.0076786.9
1.87681.3656.6604.13770.006590.00693175.0
L=48.9+61.1+86.9+175.0≈372 mL = 48.9 + 61.1 + 86.9 + 175.0 \approx 372\ \text{m}

A finer calculation gives about 407 m.

Answer: S3 profile on the downstream slope; length about 370 m (to within 1% of the new normal depth).

✓ Answer checked by Claude Opus 5.5 (high effort)

All Hydraulics chapter 8 questions →