In gradually varied flow, the flow profile is determined by
- AThe Froude number only
- BThe slope of the channel, flow depth and flow typeCorrect
- CThe discharge and Manning’s coefficient
- DThe type of sediment in the flow
Solution
Concept
Gradually Varied Flow Profiles
Formula
Yes, the dynamic equation for gradually varied flow is given by: dy/dx = (S0 - Sf) / (1 - Fr2) Where: - dy/dx = slope of the water surface relative to the channel bed - S0 = channel bed slope - Sf = friction slope - Fr = Froude number
Step-by-step solution
1. Identify the bed slope (S0) and friction slope (Sf) of the channel. 2. Determine the Froude number (Fr) to identify whether the flow is subcritical (Fr \< 1) or supercritical (Fr \> 1). 3. Evaluate the sign of dy/dx = (S0 - Sf) / (1 - Fr²) to determine if the water surface profile rises or falls along the flow direction.
Explanation
In gradually varied flow, the shape of the water surface profile depends on the bed slope of the channel (mild, steep, critical, horizontal, or adverse), the actual depth of water relative to normal and critical depths, and the type of flow regime (subcritical or supercritical). Together, these factors define the specific flow profile (such as M1, M2, S1, etc.).
Shortcut
Remember the acronym S-D-T(Slope, Depth, Type): - Slope of the channel (mild, steep, critical, etc.) - Depth of flow (actual depth relative to normal and critical depths) - Type of flow regime (subcritical or supercritical)
Common mistake
Many students mistakenly choose Option A (The Froude number only) because the Froude number plays a critical role in determining subcritical vs. supercritical flow, overlooking that the overall surface profile classification also requires knowing the channel bed slope and actual flow depth relative to normal/critical depths.
Correct answer: B) The slope of the channel, flow depth and flow type