Difficulty: Easy
Correct Answer: Q = Cd * a * sqrt(2 * g * h)
Explanation:
Introduction:
Flow through small sharp-edged orifices is estimated using Torricelli's theorem corrected by a discharge coefficient Cd to account for contraction and viscous effects.
Given Data / Assumptions:
Concept / Approach:
Ideal velocity from Torricelli: V_ideal = sqrt(2 * g * h). Ideal discharge would be a * V_ideal. Real discharge requires multiplying by Cd. Hence Q = Cd * a * sqrt(2 * g * h).
Step-by-Step Solution:
Verification / Alternative check:
Dimensional check confirms units of Q are volume per unit time. Empirical values of Cd for sharp-edged orifices (about 0.60 to 0.65) support the corrected formula.
Why Other Options Are Wrong:
Cd * a * (2 * g * h): Missing the square root; dimensionally incorrect.Cd / a * sqrt(2 * g * h): Inverts area, giving wrong dimensions.a * sqrt(2 * g * h) / Cd: Dividing by Cd overestimates flow; Cd < 1.Cd * h * sqrt(2 * g * a): Mixes variables improperly; dimensionally wrong.
Common Pitfalls:
Forgetting the square root on 2 * g * h or using head to the wrong datum. Also confusing Cd with coefficients of contraction or velocity individually.
Final Answer:
Q = Cd * a * sqrt(2 * g * h)
Discussion & Comments