Difficulty: Easy
Correct Answer: ∇²φ = 0
Explanation:
Introduction / Context:
Potential flow theory is frequently applied to seepage and groundwater problems via analogies. In an incompressible, irrotational field, the scalar velocity potential provides a convenient description of the flow, governed by Laplace’s equation.
Given Data / Assumptions:
Concept / Approach:
For incompressible flow, continuity gives ∇·V = 0. If V = ∇φ (irrotational), then ∇·(∇φ) = ∇²φ = 0, the Laplace equation. This harmonic condition underpins flow nets and electrical analogs used in geotechnical seepage analysis.
Step-by-Step Solution:
Verification / Alternative check:
Seepage through earth dams and under sheet piles is solved using Laplace’s equation for hydraulic head or potential with appropriate boundary conditions.
Why Other Options Are Wrong:
(b) is continuity but not the Laplacian for φ; (c) is irrotationality but not the governing equation for φ; (e) is not isotropic Laplace equation; (d) is false because a correct equation exists.
Common Pitfalls:
Confusing conditions on V with the equation for φ; overlooking boundary condition specification importance.
Final Answer:
∇²φ = 0
Discussion & Comments