Difficulty: Easy
Correct Answer: tranquil flow
Explanation:
Introduction:
In open-channel hydraulics, flow is categorized by comparing the actual depth with the critical depth and, equivalently, by the Froude number Fr = V / sqrt(g * y_h). Recognizing subcritical (tranquil) versus supercritical (torrential) flow determines how disturbances propagate and which equations or control sections to use.
Given Data / Assumptions:
Concept / Approach:
Critical depth is defined where specific energy is minimum for a given discharge. When actual depth is larger than the critical depth, gravitational potential effects dominate inertial effects, yielding a low Froude number (Fr < 1) and tranquil behavior. Surface waves can travel upstream in subcritical flow, which is important for control and measurement.
Step-by-Step Solution:
Verification / Alternative check:
On a mild channel slope with given discharge, backwater curves (M-profiles) occur when depth exceeds normal or approaches subcritical conditions, consistent with tranquil flow characteristics (slow, deep, gravity-dominated).
Why Other Options Are Wrong:
Torrential flow: Another name for supercritical, requires Fr > 1 and depth less than critical. Critical flow: Occurs only at exactly the critical depth (Fr = 1). Supercritical flow and rapid flow: Both indicate depth less than critical with high velocity.
Common Pitfalls:
Confusing the terms tranquil and torrential; mixing pipe flow criteria (Reynolds number) with open-channel criteria (Froude number); assuming high depth always implies high discharge without considering section shape and specific energy.
Final Answer:
tranquil flow
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