When a supercritical stream enters a mild-sloped (M) channel section, the type of flow profile would become
Step 1: Recall the classification of flow profiles in gradually varied flow (GVF).
- Flow profiles depend on:
(i) The slope of the channel (mild, steep, horizontal, adverse, critical).
(ii) The depth of flow relative to the normal depth ($y_n$) and critical depth ($y_c$).
- For a mild slope (M), we have:
$y_c < y_n$ (critical depth is smaller than normal depth).
Step 2: Case of supercritical flow entering mild slope.
- Supercritical flow means actual depth of flow $y < y_c$.
- Since $y < y_c < y_n$, the depth is below the critical depth region.
- By GVF profile classification, this corresponds to M$_3$ profile.
Step 3: Verification.
- M$_1$: Depth $> y_n$ (not possible here).
- M$_2$: Depth between $y_c$ and $y_n$ (not possible since $y < y_c$).
- M$_3$: Depth $< y_c$ (true in case of supercritical flow).
\[
\boxed{\text{The flow profile becomes M$_3$.}}
\]
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 $P$?
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:



