Difficulty: Easy
Correct Answer: V = V0/(1-α)
Explanation:
Introduction:
In flow through porous or fibrous media, engineers distinguish between superficial velocity (based on total cross-sectional area) and interstitial velocity (actual fluid speed within the voids). The relationship depends on the porosity of the medium and is important for estimating residence time and mass-transfer coefficients.
Given Data / Assumptions:
Concept / Approach:
Because only the void fraction carries flow, continuity implies that the actual fluid speed must be higher in the voids than the superficial average by a factor 1/ε. Therefore, V = V0 / ε = V0 / (1 − α). This correction is essential when predicting contact times, Reynolds number in pores, and collection efficiencies that depend on local velocities.
Step-by-Step Solution:
Define ε = 1 − α.Write conservation of volumetric flow: V0 * A_total = V * (ε * A_total).Solve for V: V = V0 / ε = V0 / (1 − α).Interpretation: as α increases (ε decreases), interstitial velocity rises.
Verification / Alternative check:
Dimensional analysis and simple control-volume arguments give the same relationship; empirical measurements of pressure drop also reflect changes with ε via correlations (e.g., Ergun-like forms).
Why Other Options Are Wrong:
Common Pitfalls:
Confusing superficial and interstitial velocities when computing Reynolds number or residence times; always use the correct definition for the phenomenon being modeled.
Final Answer:
V = V0/(1-α)
Discussion & Comments