Equilibrium Temperature Distribution with Mixed Boundary Conditions and using EnsembleProblems
For this tutorial, we consider the following problem:
\[\begin{equation} \begin{aligned} \grad^2 T &= 0 & \vb x \in \Omega, \\ \grad T \vdot \vu n &= 0 & \vb x \in \Gamma_1, \\ T &= 40 & \vb x \in \Gamma_2, \\ k\grad T \vdot \vu n &= h(T_{\infty} - T) & \vb x \in \Gamma_3, \\ T &= 70 & \vb x \in \Gamma_4. \\ \end{aligned} \end{equation}\]
This domain $\Omega$ with boundary $\partial\Omega=\Gamma_1\cup\Gamma_2\cup\Gamma_3\cup\Gamma_4$ is shown below.

Let us start by defining the mesh.
using DelaunayTriangulation, FiniteVolumeMethod, CairoMakie
A, B,
C,
D,
E,
F,
G = (0.0, 0.0),
(0.06, 0.0),
(0.06, 0.03),
(0.05, 0.03),
(0.03, 0.05),
(0.03, 0.06),
(0.0, 0.06)
bn1 = [G, A, B]
bn2 = [B, C]
bn3 = [C, D, E, F]
bn4 = [F, G]
bn = [bn1, bn2, bn3, bn4]
boundary_nodes, points = convert_boundary_points_to_indices(bn)
tri = triangulate(points; boundary_nodes)
refine!(tri; max_area = 1e-4get_area(tri))
triplot(tri)
mesh = FVMGeometry(tri)FVMGeometry with 8171 control volumes, 16007 triangles, and 24177 edgesFor the boundary conditions, the parameters that we use are $k = 3$, $h = 20$, and $T_{\infty} = 20$ for thermal conductivity, heat transfer coefficient, and ambient temperature, respectively.
k = 3.0
h = 20.0
T∞ = 20.0
bc1 = (x, y, t, T, p) -> zero(T) # ∇T⋅n=0
bc2 = (x, y, t, T, p) -> oftype(T, 40.0) # T=40
bc3 = (x, y, t, T, p) -> -p.h * (p.T∞ - T) / p.k # k∇T⋅n=h(T∞-T). The minus is since q = -∇T
bc4 = (x, y, t, T, p) -> oftype(T, 70.0) # T=70
parameters = (nothing, nothing, (h = h, T∞ = T∞, k = k), nothing)
BCs = BoundaryConditions(mesh, (bc1, bc2, bc3, bc4),
(Neumann, Dirichlet, Neumann, Dirichlet);
parameters)BoundaryConditions with 4 boundary conditions with types (Neumann, Dirichlet, Neumann, Dirichlet)Now we can define the actual problem. For the initial condition, which recall is used as an initial guess for steady state problems, let us use an initial condition which ranges from $T=70$ at $y=0.06$ down to $T=40$ at $y=0$.
diffusion_function = (x, y, t, T, p) -> one(T)
f = (x, y) -> 500y + 40
initial_condition = [f(x, y) for (x, y) in DelaunayTriangulation.each_point(tri)]
final_time = Inf
prob = FVMProblem(mesh, BCs;
diffusion_function,
initial_condition,
final_time)FVMProblem with 8171 nodes and time span (0.0, Inf)steady_prob = SteadyFVMProblem(prob)SteadyFVMProblem with 8171 nodesNow we can solve.
using OrdinaryDiffEq, SteadyStateDiffEq
sol = solve(steady_prob, DynamicSS(Rosenbrock23()))retcode: Success
u: 8294-element Vector{Float64}:
70.0
53.10287477155928
40.0
40.0
44.137162557274195
⋮
54.903298517604426
46.931321710843115
51.45239535777522
54.18690061750693
48.423767399647446fig, ax, sc = tricontourf(tri, sol.u, levels = 40:70, axis = (xlabel = "x", ylabel = "y"))
fig
Just the code
An uncommented version of this example is given below. You can view the source code for this file here.
using DelaunayTriangulation, FiniteVolumeMethod, CairoMakie
A, B,
C,
D,
E,
F,
G = (0.0, 0.0),
(0.06, 0.0),
(0.06, 0.03),
(0.05, 0.03),
(0.03, 0.05),
(0.03, 0.06),
(0.0, 0.06)
bn1 = [G, A, B]
bn2 = [B, C]
bn3 = [C, D, E, F]
bn4 = [F, G]
bn = [bn1, bn2, bn3, bn4]
boundary_nodes, points = convert_boundary_points_to_indices(bn)
tri = triangulate(points; boundary_nodes)
refine!(tri; max_area = 1e-4get_area(tri))
triplot(tri)
mesh = FVMGeometry(tri)
k = 3.0
h = 20.0
T∞ = 20.0
bc1 = (x, y, t, T, p) -> zero(T) # ∇T⋅n=0
bc2 = (x, y, t, T, p) -> oftype(T, 40.0) # T=40
bc3 = (x, y, t, T, p) -> -p.h * (p.T∞ - T) / p.k # k∇T⋅n=h(T∞-T). The minus is since q = -∇T
bc4 = (x, y, t, T, p) -> oftype(T, 70.0) # T=70
parameters = (nothing, nothing, (h = h, T∞ = T∞, k = k), nothing)
BCs = BoundaryConditions(mesh, (bc1, bc2, bc3, bc4),
(Neumann, Dirichlet, Neumann, Dirichlet);
parameters)
diffusion_function = (x, y, t, T, p) -> one(T)
f = (x, y) -> 500y + 40
initial_condition = [f(x, y) for (x, y) in DelaunayTriangulation.each_point(tri)]
final_time = Inf
prob = FVMProblem(mesh, BCs;
diffusion_function,
initial_condition,
final_time)
steady_prob = SteadyFVMProblem(prob)
using OrdinaryDiffEq, SteadyStateDiffEq
sol = solve(steady_prob, DynamicSS(Rosenbrock23()))
fig, ax, sc = tricontourf(tri, sol.u, levels = 40:70, axis = (xlabel = "x", ylabel = "y"))
figThis page was generated using Literate.jl.