Froude number classification in open-channel flow: when is the flow subcritical (tranquil)?
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Aless than 1.0
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Bequal to 1.0
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Cgreater than 1.0
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Dnone
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Ebetween 1.0 and 2.0 only
Answer
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