Froude number classification in open-channel flow: when is the flow subcritical (tranquil)?

Difficulty: Easy

Correct Answer: less than 1.0

Explanation:


Introduction / Context:
The Froude number Fr is a key dimensionless parameter in open-channel hydraulics used to classify flow regimes. Correctly identifying subcritical, critical, and supercritical states guides design decisions for channels, spillways, and energy dissipation structures.


Given Data / Assumptions:

  • Prismatic channel with steady, uniform flow conceptually.
  • Hydraulic depth D_h = A/T (area over top width) used for wide channels; for rectangular sections, D_h ≈ flow depth y.
  • Froude number defined as Fr = V / √(g * D_h).


Concept / Approach:

Flow classification is based on the relative importance of inertia to gravity waves. When Fr < 1, surface gravity waves can propagate upstream, and the flow is subcritical (tranquil). At Fr = 1, flow is at the critical state. When Fr > 1, the flow is supercritical (rapid), dominated by inertia; disturbances cannot move upstream.


Step-by-Step Solution:

Compute Fr = V / √(g * D_h).Compare Fr to unity: Fr < 1 indicates subcritical; Fr = 1 indicates critical; Fr > 1 indicates supercritical.Infer engineering implications: hydraulic jumps occur when supercritical transitions to subcritical, requiring energy dissipation considerations.


Verification / Alternative check:

For a wide rectangular channel, substitute D_h ≈ y. Example: if V = 0.8 m/s and y = 1.0 m, g = 9.81 m/s^2, then Fr ≈ 0.8 / 3.13 ≈ 0.26 < 1, confirming subcritical flow.


Why Other Options Are Wrong:

(b) Fr = 1.0 defines the critical condition, not subcritical. (c) Fr > 1.0 is supercritical. (d) and (e) are inconsistent with the standard definition and would misclassify many flows.


Common Pitfalls:

Using geometric depth instead of hydraulic depth in irregular sections; ignoring that local accelerations can change Fr along a transition.


Final Answer:

less than 1.0

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