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$_2$.
\[
\boxed{\text{Profiles near }P:\; \text{M}_2 \text{ (upstream)} \;\text{and}\; \text{S}_2 \text{ (downstream).}}
\]
Consider a five-digit number PQRST that has distinct digits P, Q, R, S, and T, and satisfies the following conditions:
1. \( P<Q \)
2. \( S>P>T \)
3. \( R<T \)
If integers 1 through 5 are used to construct such a number, the value of P is:



