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).
\[
\boxed{\text{The flow profile becomes M$_3$.}}
\]