Laplace equation solution technique: For three-dimensional potential-flow problems of water (e.g., in a siphon or seepage domain), which method is commonly used to obtain a numerical solution of the Laplacian field?

Difficulty: Easy

Correct Answer: Method of relaxation (iterative numerical solution)

Explanation:


Introduction / Context:
Potential-flow problems in hydraulics—such as steady incompressible flow in siphons, around structures, or in seepage—are governed by Laplace’s equation. Except for simple geometries, closed-form analytical solutions are not available, and numerical approaches are used to solve the Laplacian field.


Given Data / Assumptions:

  • Steady, irrotational, incompressible flow implies the potential satisfies ∇²ϕ = 0.
  • Complex three-dimensional domain (e.g., around/within hydraulic structures).
  • Boundary conditions specified on solid surfaces and inlets/outlets.


Concept / Approach:

The relaxation (successive over-relaxation or Gauss–Seidel-type) method iteratively updates potential values at grid nodes using the discrete Laplace equation until changes fall below a tolerance. It is a classic and robust approach for Laplacian problems where analytic methods are impractical.


Step-by-Step Solution:

Discretize the domain into a computational grid.Apply boundary conditions (Dirichlet/Neumann) at all boundary nodes.Iteratively update each interior node by averaging neighboring nodes (with relaxation factor if used).Repeat sweeps until successive changes are sufficiently small, indicating convergence.


Verification / Alternative check:

Convergence is verified by residual norms or by checking flux balances across boundaries. Benchmark against simpler geometries with known solutions provides confidence.


Why Other Options Are Wrong:

Khosla’s method: specialized analytical charts for seepage under weirs, not general 3D domains.
Unwin’s method: not a standard general solver for 3D Laplace problems.
Pure analytic solution: rarely feasible in complex 3D geometries.
Trial-and-error continuity balancing: non-systematic and not equivalent to solving Laplace’s equation.


Common Pitfalls:

Poor grid resolution, improper boundary conditions, and inadequate stopping criteria can yield inaccurate fields.


Final Answer:

Method of relaxation (iterative numerical solution)

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