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$_2$.
\[
\boxed{\text{Profiles near }P:\; \text{M}_2 \text{ (upstream)} \;\text{and}\; \text{S}_2 \text{ (downstream).}}
\]
In levelling between two points A and B on the opposite banks of a river, the readings are taken by setting the instrument both at A and B, as shown in the table. If the RL of A is 150.000 m, the RL of B (in m) is ....... (rounded off to 3 decimal places). 
A one-way, single lane road has traffic that consists of 30% trucks and 70% cars. The speed of trucks (in km/h) is a uniform random variable on the interval (30, 60), and the speed of cars (in km/h) is a uniform random variable on the interval (40, 80). The speed limit on the road is 50 km/h. The percentage of vehicles that exceed the speed limit is ........ (rounded off to 1 decimal place). 