Difficulty: Easy
Correct Answer: rate of discharge (flow rate) in the open channel
Explanation:
Introduction:
Critical depth meters (such as flumes that force Froude number to unity at a throat) convert a difficult-to-measure discharge into an easily measured depth at a calibrated section. This question asks you to identify the primary hydraulic quantity obtained by using such a device.
Given Data / Assumptions:
Concept / Approach:
At critical flow, specific energy is minimized, and for a given control geometry the depth at the throat (or at a gauge point) is a unique function of the discharge. Therefore, by measuring depth at that location, one infers the flow rate Q using a calibration curve or formula. Instruments like the Parshall flume and Venturi flume are examples of critical-depth meters used worldwide for flow gauging in irrigation canals and wastewater channels.
Step-by-Step Solution:
Verification / Alternative check:
Manufacturer calibration tables and standard hydraulics texts provide Q–h relationships for flumes; field use confirms accurate discharge measurement over wide ranges when submergence criteria are met.
Why Other Options Are Wrong:
Velocity only or depth only: The device’s purpose is to infer Q from depth under controlled conditions, not to report velocity or depth in isolation.Hydraulic jump detection and slope measurement are different diagnostic tasks.
Common Pitfalls:
Using the meter under submerged conditions without correction factors; submergence invalidates the simple Q–h relation for many flumes.
Final Answer:
rate of discharge (flow rate) in the open channel
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