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Slope break and distance to depth 0.4 m

Short answer

Both slopes are mild (y_n1=2.437 m, y_n2=1.504 m > y_c=0.997 m); upstream M2 drawdown, downstream uniform flow. The depth 0.4 m is below critical and cannot occur. The M2 profile from the break upstream to 2.388 m depth extends about 5.1 km, computed with three direct steps.

A wide rectangular channel has an average bed slope of 0.0002 and discharge per unit width of 3.12 m³/s/m. Assume a Manning's value n = 0.02. If a break in slope occurs and the slope becomes 0.001, classify the flow profiles in both the slopes and use direct step method (3 steps only) to determine the distance downstream of the slope change at which the water surface level reaches 0.4 m.

Given: wide rectangular channel, q=3.12 m2/sq = 3.12\ \text{m}^2/\text{s}, n=0.02n = 0.02, S01=0.0002S_{01} = 0.0002, S02=0.001S_{02} = 0.001. Wide channel: R≈yR \approx y.

Critical and normal depths

yc=(3.1229.81)1/3=0.997 my_c = \left(\frac{3.12^2}{9.81}\right)^{1/3} = 0.997\ \text{m} yn1=(0.02×3.120.0002)3/5=2.437 m,yn2=(0.02×3.120.001)3/5=1.504 my_{n1} = \left(\frac{0.02 \times 3.12}{\sqrt{0.0002}}\right)^{3/5} = 2.437\ \text{m},\qquad y_{n2} = \left(\frac{0.02 \times 3.12}{\sqrt{0.001}}\right)^{3/5} = 1.504\ \text{m}

Both yn1y_{n1} and yn2y_{n2} exceed ycy_c, so both slopes are mild, the second being steeper. Flow is subcritical throughout, so the control is downstream.

Classification

  • Downstream slope (S02S_{02}): uniform flow at yn2=1.504y_{n2} = 1.504 m.
  • Upstream slope (S01S_{01}): the depth must fall from yn1=2.437y_{n1} = 2.437 m (far upstream) to yn2=1.504y_{n2} = 1.504 m at the break. This lies between yny_n and ycy_c, so the profile is an M2 (drawdown) curve.

Reading of the 0.4 m depth. A depth of 0.4 m is below yc=0.997y_c = 0.997 m, which cannot occur on a mild slope for this discharge (it would be an M3 curve and needs a gate or other supercritical control). The calculation below is therefore done for the actual M2 curve: the distance upstream of the break at which the depth has recovered to 0.98 yn1=2.3880.98\,y_{n1} = 2.388 m.

Direct step (3 steps, S0=0.0002S_0 = 0.0002)

E=y+V22g,Sf=n2q2y10/3,Δx=E2−E1S0−SˉfE = y + \frac{V^2}{2g},\quad S_f = \frac{n^2 q^2}{y^{10/3}},\quad \Delta x = \frac{E_2 - E_1}{S_0 - \bar S_f}
yy (m)VV (m/s)EE (m)SfS_fSˉf\bar S_fS0−SˉfS_0 - \bar S_fΔx\Delta x (m)
1.50352.0751.72300.001000
1.79831.7351.95180.0005510.000775-0.000575-397.6
2.09321.4912.20640.0003320.000441-0.000241-1055.6
2.38801.3072.47500.0002140.000273-0.0000729-3682.9

The negative sign means the distances are measured upstream of the slope change.

∑Δx=−397.6−1055.6−3682.9=−5136 m\sum \Delta x = -397.6 - 1055.6 - 3682.9 = -5136\ \text{m}

Answer: Both reaches are mild (M2 profile on the flatter upstream slope, uniform flow on the steeper one). The depth rises from 1.50 m at the break to 2.39 m at about 5.1 km upstream. A depth of 0.4 m is below critical depth (0.997 m) and cannot occur in this flow without a control.

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