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examples/p4est_2d_dgsem/elixir_navierstokes_viscous_shock_newton_krylov.jl
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| Original file line number | Diff line number | Diff line change |
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| @@ -0,0 +1,183 @@ | ||
| using Trixi | ||
|
|
||
| using OrdinaryDiffEqSDIRK | ||
| using LinearSolve # For Jacobian-free Newton-Krylov (GMRES) solver | ||
| using ADTypes # For automatic differentiation via finite differences | ||
|
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||
| # This is the classic 1D viscous shock wave problem with analytical solution | ||
| # for a special value of the Prandtl number. | ||
| # The original references are: | ||
| # | ||
| # - R. Becker (1922) | ||
| # Stoßwelle und Detonation. | ||
| # [DOI: 10.1007/BF01329605](https://doi.org/10.1007/BF01329605) | ||
| # | ||
| # English translations: | ||
| # Impact waves and detonation. Part I. | ||
| # https://ntrs.nasa.gov/api/citations/19930090862/downloads/19930090862.pdf | ||
| # Impact waves and detonation. Part II. | ||
| # https://ntrs.nasa.gov/api/citations/19930090863/downloads/19930090863.pdf | ||
| # | ||
| # - M. Morduchow, P. A. Libby (1949) | ||
| # On a Complete Solution of the One-Dimensional Flow Equations | ||
| # of a Viscous, Head-Conducting, Compressible Gas | ||
| # [DOI: 10.2514/8.11882](https://doi.org/10.2514/8.11882) | ||
| # | ||
| # | ||
| # The particular problem considered here is described in | ||
| # - L. G. Margolin, J. M. Reisner, P. M. Jordan (2017) | ||
| # Entropy in self-similar shock profiles | ||
| # [DOI: 10.1016/j.ijnonlinmec.2017.07.003](https://doi.org/10.1016/j.ijnonlinmec.2017.07.003) | ||
|
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||
| ### Fixed parameters ### | ||
|
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| # Special value for which nonlinear solver can be omitted | ||
| # Corresponds essentially to fixing the Mach number | ||
| alpha = 0.5 | ||
| # We want kappa = cp * mu = mu_bar to ensure constant enthalpy | ||
| prandtl_number() = 3 / 4 | ||
|
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||
| ### Free choices: ### | ||
| gamma() = 5 / 3 | ||
|
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| # In Margolin et al., the Navier-Stokes equations are given for an | ||
| # isotropic stress tensor τ, i.e., ∇ ⋅ τ = μ Δu | ||
| mu_isotropic() = 0.15 | ||
| mu_bar() = mu_isotropic() / (gamma() - 1) # Re-scaled viscosity | ||
|
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| rho_0() = 1 | ||
| v() = 1 # Shock speed | ||
|
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| domain_length = 4.0 | ||
|
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| ### Derived quantities ### | ||
|
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| Ma() = 2 / sqrt(3 - gamma()) # Mach number for alpha = 0.5 | ||
| c_0() = v() / Ma() # Speed of sound ahead of the shock | ||
|
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| # From constant enthalpy condition | ||
| p_0() = c_0()^2 * rho_0() / gamma() | ||
|
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| l() = mu_bar() / (rho_0() * v()) * 2 * gamma() / (gamma() + 1) # Appropriate length scale | ||
|
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| """ | ||
| initial_condition_viscous_shock(x, t, equations) | ||
|
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| Classic 1D viscous shock wave problem with analytical solution | ||
| for a special value of the Prandtl number. | ||
| The version implemented here is described in | ||
| - L. G. Margolin, J. M. Reisner, P. M. Jordan (2017) | ||
| Entropy in self-similar shock profiles | ||
| [DOI: 10.1016/j.ijnonlinmec.2017.07.003](https://doi.org/10.1016/j.ijnonlinmec.2017.07.003) | ||
| """ | ||
| function initial_condition_viscous_shock(x, t, equations) | ||
| y = x[1] - v() * t # Translated coordinate | ||
|
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||
| # Coordinate transformation. See eq. (33) in Margolin et al. (2017) | ||
| chi = 2 * exp(y / (2 * l())) | ||
|
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| w = 1 + 1 / (2 * chi^2) * (1 - sqrt(1 + 2 * chi^2)) | ||
|
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| rho = rho_0() / w | ||
| u = v() * (1 - w) | ||
| p = p_0() * 1 / w * (1 + (gamma() - 1) / 2 * Ma()^2 * (1 - w^2)) | ||
|
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| return prim2cons(SVector(rho, u, 0, p), equations) | ||
| end | ||
| initial_condition = initial_condition_viscous_shock | ||
|
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| ############################################################################### | ||
| # semidiscretization of the ideal compressible Navier-Stokes equations | ||
|
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| equations = CompressibleEulerEquations2D(gamma()) | ||
|
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| # Trixi implements the stress tensor in deviatoric form, thus we need to | ||
| # convert the "isotropic viscosity" to the "deviatoric viscosity" | ||
| mu_deviatoric() = mu_bar() * 3 / 4 | ||
| equations_parabolic = CompressibleNavierStokesDiffusion2D(equations, mu = mu_deviatoric(), | ||
| Prandtl = prandtl_number(), | ||
| gradient_variables = GradientVariablesEntropy()) | ||
|
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| solver = DGSEM(polydeg = 3, surface_flux = flux_hlle) | ||
|
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| coordinates_min = (-domain_length / 2, -domain_length / 2) | ||
| coordinates_max = (domain_length / 2, domain_length / 2) | ||
|
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| trees_per_dimension = (12, 3) | ||
| mesh = P4estMesh(trees_per_dimension, | ||
| polydeg = 3, initial_refinement_level = 0, | ||
| coordinates_min = coordinates_min, coordinates_max = coordinates_max, | ||
| periodicity = (false, true)) | ||
|
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| ### Inviscid boundary conditions ### | ||
|
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| # Prescribe pure influx based on initial conditions | ||
| function boundary_condition_inflow(u_inner, normal_direction::AbstractVector, x, t, | ||
| surface_flux_function, | ||
| equations::CompressibleEulerEquations2D) | ||
| u_cons = initial_condition_viscous_shock(x, t, equations) | ||
| flux = Trixi.flux(u_cons, normal_direction, equations) | ||
|
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| return flux | ||
| end | ||
|
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| boundary_conditions = Dict(:x_neg => boundary_condition_inflow, | ||
| :x_pos => boundary_condition_do_nothing) | ||
|
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| ### Viscous boundary conditions ### | ||
| # For the viscous BCs, we use the known analytical solution | ||
| velocity_bc = NoSlip() do x, t, equations_parabolic | ||
| Trixi.velocity(initial_condition_viscous_shock(x, | ||
| t, | ||
| equations_parabolic), | ||
| equations_parabolic) | ||
| end | ||
|
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| heat_bc = Isothermal() do x, t, equations_parabolic | ||
| Trixi.temperature(initial_condition_viscous_shock(x, | ||
| t, | ||
| equations_parabolic), | ||
| equations_parabolic) | ||
| end | ||
|
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| boundary_condition_parabolic = BoundaryConditionNavierStokesWall(velocity_bc, heat_bc) | ||
|
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| boundary_conditions_parabolic = Dict(:x_neg => boundary_condition_parabolic, | ||
| :x_pos => boundary_condition_parabolic) | ||
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| semi = SemidiscretizationHyperbolicParabolic(mesh, (equations, equations_parabolic), | ||
| initial_condition, solver; | ||
| boundary_conditions = (boundary_conditions, | ||
| boundary_conditions_parabolic)) | ||
|
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| ############################################################################### | ||
| # ODE solvers, callbacks etc. | ||
|
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| tspan = (0.0, 1.0) | ||
| ode = semidiscretize(semi, tspan) | ||
|
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| summary_callback = SummaryCallback() | ||
| alive_callback = AliveCallback(alive_interval = 1) | ||
| analysis_callback = AnalysisCallback(semi, interval = 100) | ||
|
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| callbacks = CallbackSet(summary_callback, alive_callback, analysis_callback) | ||
|
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| ############################################################################### | ||
| # run the simulation | ||
|
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| # Tolerances for GMRES residual, see https://jso.dev/Krylov.jl/stable/solvers/unsymmetric/#Krylov.gmres | ||
| atol_lin_solve = 1e-5 | ||
| rtol_lin_solve = 1e-5 | ||
|
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| # Jacobian-free Newton-Krylov (GMRES) solver | ||
| linsolve = KrylovJL_GMRES(atol = atol_lin_solve, rtol = rtol_lin_solve) | ||
|
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| # Use (diagonally) implicit Runge-Kutta, see | ||
| # https://docs.sciml.ai/DiffEqDocs/stable/tutorials/advanced_ode_example/#Using-Jacobian-Free-Newton-Krylov | ||
| ode_alg = Kvaerno4(autodiff = AutoFiniteDiff(), linsolve = linsolve) | ||
|
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| atol_ode_solve = 1e-4 | ||
| rtol_ode_solve = 1e-4 | ||
| sol = solve(ode, ode_alg; | ||
| abstol = atol_ode_solve, reltol = rtol_ode_solve, | ||
| ode_default_options()..., callback = callbacks); |
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71 changes: 71 additions & 0 deletions
71
examples/tree_1d_dgsem/elixir_diffusion_ldg_newton_krylov.jl
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| Original file line number | Diff line number | Diff line change |
|---|---|---|
| @@ -0,0 +1,71 @@ | ||
| using Trixi | ||
|
|
||
| using OrdinaryDiffEqSDIRK | ||
| using LinearSolve # For Jacobian-free Newton-Krylov (GMRES) solver | ||
| using ADTypes # For automatic differentiation via finite differences | ||
|
|
||
| ############################################################################### | ||
| # semidiscretization of the linear (advection) diffusion equation | ||
|
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| advection_velocity = 0.0 # Note: This renders the equation mathematically purely parabolic | ||
| equations = LinearScalarAdvectionEquation1D(advection_velocity) | ||
| diffusivity() = 0.5 | ||
| equations_parabolic = LaplaceDiffusion1D(diffusivity(), equations) | ||
|
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| # surface flux does not matter for pure diffusion problem | ||
| solver = DGSEM(polydeg = 3, surface_flux = flux_central) | ||
|
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| coordinates_min = -convert(Float64, pi) | ||
| coordinates_max = convert(Float64, pi) | ||
|
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| mesh = TreeMesh(coordinates_min, coordinates_max, | ||
| initial_refinement_level = 4, | ||
| n_cells_max = 30_000) | ||
|
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| function initial_condition_pure_diffusion_1d_convergence_test(x, t, | ||
| equation) | ||
| nu = diffusivity() | ||
| c = 0 | ||
| A = 1 | ||
| omega = 1 | ||
| scalar = c + A * sin(omega * sum(x)) * exp(-nu * omega^2 * t) | ||
| return SVector(scalar) | ||
| end | ||
| initial_condition = initial_condition_pure_diffusion_1d_convergence_test | ||
|
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| solver_parabolic = ViscousFormulationLocalDG() | ||
| semi = SemidiscretizationHyperbolicParabolic(mesh, (equations, equations_parabolic), | ||
| initial_condition, | ||
| solver; solver_parabolic) | ||
|
|
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| ############################################################################### | ||
| # ODE solvers, callbacks etc. | ||
|
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| tspan = (0.0, 2.0) | ||
| ode = semidiscretize(semi, tspan) | ||
|
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| summary_callback = SummaryCallback() | ||
| analysis_callback = AnalysisCallback(semi, interval = 10) | ||
| alive_callback = AliveCallback(alive_interval = 1) | ||
|
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| callbacks = CallbackSet(summary_callback, analysis_callback, alive_callback) | ||
|
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| ############################################################################### | ||
| # run the simulation | ||
|
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| # Tolerances for GMRES residual, see https://jso.dev/Krylov.jl/stable/solvers/unsymmetric/#Krylov.gmres | ||
| atol_lin_solve = 1e-6 | ||
| rtol_lin_solve = 1e-5 | ||
|
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| # Jacobian-free Newton-Krylov (GMRES) solver | ||
| linsolve = KrylovJL_GMRES(atol = atol_lin_solve, rtol = rtol_lin_solve) | ||
|
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| # Use (diagonally) implicit Runge-Kutta, see | ||
| # https://docs.sciml.ai/DiffEqDocs/stable/tutorials/advanced_ode_example/#Using-Jacobian-Free-Newton-Krylov | ||
| ode_alg = KenCarp47(autodiff = AutoFiniteDiff(), linsolve = linsolve) | ||
|
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| atol_ode_solve = 1e-5 | ||
| rtol_ode_solve = 1e-4 | ||
| sol = solve(ode, ode_alg; | ||
| abstol = atol_ode_solve, reltol = rtol_ode_solve, | ||
| ode_default_options()..., callback = callbacks); |
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