Flow in varying-area conduits – classification for constant volumetric rate A liquid flows through an expanding tube (increasing cross-section) at a constant volumetric flow rate. How should this flow be classified?
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Asteady uniform flow
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Bsteady non-uniform flow
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Cunsteady uniform flow
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Dunsteady non-uniform flow
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Eperiodic uniform flow
Answer
Correct Answer: steady non-uniform flow
Explanation
Introduction:Correctly labeling flows is essential before applying momentum and energy equations. The two attributes are time variation (steady vs unsteady) and spatial variation along the conduit (uniform vs non-uniform). An expanding tube at constant flow rate provides a classic example to test these definitions.
Given Data / Assumptions:
- Rigid tube with cross-sectional area increasing with downstream distance.
- Volumetric rate Q is constant in time.
- Incompressible liquid; no lateral inflow/outflow.
Concept / Approach:
Steady means properties at a fixed point do not change with time; constant Q satisfies that. Uniform refers to constancy along the flow direction at a given instant. Because area A(x) increases, continuity v(x) = Q / A(x) decreases with x, so velocity is not spatially constant—hence non-uniform. Therefore, the correct classification is steady non-uniform flow.
Step-by-Step Solution:
Apply continuity at each section: v(x) = Q/A(x).Note Q is time-invariant → steady.Observe v varies with x because A changes → non-uniform.Verification / Alternative check:
A diffuser at constant throughput is the canonical steady non-uniform device; velocity and dynamic head decrease downstream while static pressure rises, consistent with Bernoulli plus losses.
Why Other Options Are Wrong:
Steady uniform: Would require constant area or special profile giving constant v; not the case.Unsteady options: Contradict the given constant rate condition.Periodic uniform: No periodic time variation is described.
Common Pitfalls:
Equating constant discharge with uniformity; it guarantees steadiness, not spatial uniformity.
Final Answer:
steady non-uniform flow