A very wide rectangular channel carries a discharge $Q=70~\mathrm{m^3/s}$ per meter width. Its bed slope changes from $S_0=0.0001$ to $S_0=0.0009$ at a point $P$ (not to scale). The Manning's roughness coefficient is $n=0.01$. What water-surface profile(s) exist(s) near the point $P$?
Step 1: Critical depth for a very wide rectangular channel.
For unit width, critical depth is
\[
y_c=\left(\frac{q^2}{g}\right)^{1/3}, q=Q=70~\mathrm{m^2/s}.
\]
\[
y_c=\left(\frac{70^2}{9.81}\right)^{1/3}\approx 7.93~\mathrm{m}.
\]
Step 2: Normal depth on each reach (Manning, very wide).
For a very wide rectangle, $A=y$, $R\approx y$, and
\[
q=\frac{1}{n}\,y^{5/3}\,S_0^{1/2}\;\Rightarrow\;
y_n=\left(q\,n\,S_0^{-1/2}\right)^{3/5}.
\]
Upstream ( $S_0=0.0001$ ):
\[
y_{n1}=\left(\frac{70\cdot 0.01}{\sqrt{0.0001}}\right)^{3/5}\approx 12.80~\mathrm{m}.
\]
Downstream ( $S_0=0.0009$ ):
\[
y_{n2}=\left(\frac{70\cdot 0.01}{\sqrt{0.0009}}\right)^{3/5}\approx 6.62~\mathrm{m}.
\]
Step 3: Classify slopes.
- Upstream: $y_{n1}>y_c$ $\Rightarrow$ mild slope (M).
- Downstream: $y_{n2}<y_c$ $\Rightarrow$ steep slope (S).
Step 4: Profiles near $P$.
Approaching the steeper reach, depth must decrease from $y_{n1}$ toward the control; on a mild slope such a drawdown with $y_c<y<y_n$ is profile M$_2$.
Immediately downstream on the steep slope, the flow adjusts from near-critical toward $y_{n2}(<y_c)$; the curve with $y_n<y<y_c$ is profile S$_2$.
\[
\boxed{\text{Profiles near }P:\; \text{M}_2 \text{ (upstream)} \;\text{and}\; \text{S}_2 \text{ (downstream).}}
\]
The critical flow condition in a channel is given by [Note: $\alpha$ – kinetic energy correction factor; $Q$ – discharge; $A_c$ – cross-sectional area of flow at critical flow condition; $T_c$ – top width of flow at critical flow condition; $g$ – acceleration due to gravity]
The pressure in a pipe at X is to be measured by an open manometer as shown in the figure. Fluid A is oil with a specific gravity of 0.8 and Fluid B is mercury with a specific gravity of 13.6. The absolute pressure at X is kN/m\(^2\). (round off to one decimal place).}
[Assume Density of water = 1000 kg/m³, gravity = 9.81 m/s², atmospheric pressure = 101.3 kN/m².]
A hydraulic jump occurs in a 1.0 m wide horizontal, frictionless, rectangular channel, with a pre-jump depth of $0.2$ m and a post-jump depth of $1.0$ m. Take g=10 m/s^2. The values of the specific force at the pre-jump and post-jump sections are the same and are equal to (in m$^3$, rounded off to two decimal places)
The Rational Method formula for estimating peak runoff is given as \(Q = \frac{CiA}{360}\). For the result \(Q\) to be in cubic meters per second (\(m^3/s\)), what must be the units of rainfall intensity (\(i\)) and catchment area (\(A\))?
| Point | Staff Readings Back side | Staff Readings Fore side | Remarks |
|---|---|---|---|
| P | -2.050 | - | 200.000 |
| Q | 1.050 | 0.95 | Change Point |
| R | - | -1.655 | - |