Difficulty: Easy
Correct Answer: False
Explanation:
Introduction:
Understanding velocity distribution across a cross-section is crucial for accurate discharge measurement and sediment transport analysis. Real flows exhibit shear near boundaries, creating non-uniform profiles.
Given Data / Assumptions:
Concept / Approach:
Viscous and turbulent shear cause velocity to vary from near zero at the bed and banks to a maximum just below the free surface. Hence, only an average (mean) velocity is uniform in the sense of a single representative value; point velocities differ across the section.
Step-by-Step Solution:
Recall boundary condition: velocity approaches zero at solid boundaries.Recognize free-surface shear is small; thus peak velocity occurs slightly below the surface.Therefore the statement of uniform velocity across the section is false.
Verification / Alternative check:
Velocity-area method uses a velocity distribution (via current meters or ADCP) precisely because velocities vary spatially; this confirms non-uniformity.
Why Other Options Are Wrong:
Choosing “True” would neglect shear and turbulence—contrary to basic fluid mechanics.
Common Pitfalls:
Assuming plug flow because textbooks draw simplified diagrams; confusing time-steady flow with spatially uniform profiles.
Final Answer:
False
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