diff --git a/Project.toml b/Project.toml index 4d6eb29..68e77f8 100644 --- a/Project.toml +++ b/Project.toml @@ -26,7 +26,7 @@ WriteVTK = "64499a7a-5c06-52f2-abe2-ccb03c286192" [compat] CUDA = "4 - 5" CairoMakie = "0.8 - 0.20" -GeophysicalModelGenerator = "0.3 - 0.6" +GeophysicalModelGenerator = "0.7" GeoParams = "0.5" Interpolations = "0.13 - 0.15" JLD2 = "0.4" diff --git a/README.md b/README.md index ea9c396..21c8d86 100644 --- a/README.md +++ b/README.md @@ -10,10 +10,14 @@ This easy to use and versatile package simulates the thermal evolution of magmat Below we give a number of example scripts that show how it can be used to simulate a number of scenarios. ## Contents +- [MagmaThermoKinematics.jl](#magmathermokinematicsjl) + - [Contents](#contents) - [100-lines 2D example](#100-lines-2d-example) - [100-lines 3D example](#100-lines-3d-example) - [Dependencies](#dependencies) - [Installation](#installation) + - [Ongoing development](#ongoing-development) + - [Related work](#related-work) ## 100-lines 2D example A simple example that simulates the emplacement of dikes within the crust over a period of 10'000 years is shown below. @@ -41,7 +45,7 @@ Num = Numeric_params(verbose=false) # No MatParam = ( SetMaterialParams(Name="Rock", Phase=1, Density = ConstantDensity(ρ=2800kg/m^3), - HeatCapacity = ConstantHeatCapacity(cp=1050J/kg/K), + HeatCapacity = ConstantHeatCapacity(Cp=1050J/kg/K), Conductivity = ConstantConductivity(k=1.5Watt/K/m), LatentHeat = ConstantLatentHeat(Q_L=350e3J/kg), Melting = MeltingParam_Caricchi()), @@ -166,7 +170,7 @@ using WriteVTK MatParam = ( SetMaterialParams(Name="Rock", Phase=1, Density = ConstantDensity(ρ=2800kg/m^3), - HeatCapacity = ConstantHeatCapacity(cp=1050J/kg/K), + HeatCapacity = ConstantHeatCapacity(Cp=1050J/kg/K), Conductivity = ConstantConductivity(k=1.5Watt/K/m), LatentHeat = ConstantLatentHeat(Q_L=350e3J/kg), Melting = MeltingParam_Caricchi()), diff --git a/examples/Example2D.jl b/examples/Example2D.jl index 85dee14..f38aabc 100644 --- a/examples/Example2D.jl +++ b/examples/Example2D.jl @@ -18,7 +18,7 @@ using Plots MatParam = ( SetMaterialParams(Name="Rock", Phase=1, Density = ConstantDensity(ρ=2800kg/m^3), - HeatCapacity = ConstantHeatCapacity(cp=1050J/kg/K), + HeatCapacity = ConstantHeatCapacity(Cp=1050J/kg/K), Conductivity = ConstantConductivity(k=1.5Watt/K/m), LatentHeat = ConstantLatentHeat(Q_L=350e3J/kg), Melting = MeltingParam_Caricchi()), diff --git a/examples/Example2D_ZASSy.jl b/examples/Example2D_ZASSy.jl index 2d32c69..905074d 100644 --- a/examples/Example2D_ZASSy.jl +++ b/examples/Example2D_ZASSy.jl @@ -2,11 +2,11 @@ # It includes comparisons with 2D simulations done by the Geneva (Gregor Weber, Luca Caricchi) & UCLA (Oscar Lovera) Tracers_SimParams # # -const USE_GPU=true; +const USE_GPU=false; using MagmaThermoKinematics if USE_GPU environment!(:gpu, Float64, 2) # initialize parallel stencil in 2D - CUDA.device!(1) # select the GPU you use (starts @ zero) + # CUDA.device!(1) # select the GPU you use (starts @ zero) else environment!(:cpu, Float64, 2) # initialize parallel stencil in 2D end @@ -446,7 +446,7 @@ if 1==0 # Conductivity = ConstantConductivity(k=3.3Watt/K/m), # in case we use constant k Conductivity = T_Conductivity_Whittington_parameterised(), # T-dependent k #Conductivity = T_Conductivity_Whittington(), # T-dependent k - HeatCapacity = ConstantHeatCapacity(cp=1000J/kg/K), + HeatCapacity = ConstantHeatCapacity(Cp=1000J/kg/K), Melting = SmoothMelting(MeltingParam_4thOrder())), # Marxer & Ulmer melting # Melting = MeltingParam_Caricchi()), # Caricchi melting @@ -665,7 +665,7 @@ if 1==1 Conductivity = T_Conductivity_Whittington(), # T-dependent k HeatCapacity = T_HeatCapacity_Whittington(), # T-dependent cp # Conductivity = ConstantConductivity(k=3.3Watt/K/m), # in case we use constant k - # HeatCapacity = ConstantHeatCapacity(cp=1000J/kg/K), + # HeatCapacity = ConstantHeatCapacity(Cp=1000J/kg/K), Melting = MeltingParam_Assimilation() # Quadratic parameterization as in Tierney et al. #Melting = MeltingParam_Caricchi() ), @@ -676,7 +676,7 @@ if 1==1 Conductivity = T_Conductivity_Whittington(), # T-dependent k HeatCapacity = T_HeatCapacity_Whittington(), # T-dependent cp #Conductivity = ConstantConductivity(k=3.3Watt/K/m), # in case we use constant k - #HeatCapacity = ConstantHeatCapacity(cp=1000J/kg/K), + #HeatCapacity = ConstantHeatCapacity(Cp=1000J/kg/K), Melting = SmoothMelting(MeltingParam_Quadratic(T_s=(700+273.15)K, T_l=(1100+273.15)K)) #Melting = MeltingParam_Caricchi() ) diff --git a/examples/Example3D.jl b/examples/Example3D.jl index 9297acc..b3e045c 100644 --- a/examples/Example3D.jl +++ b/examples/Example3D.jl @@ -19,7 +19,7 @@ using WriteVTK MatParam = ( SetMaterialParams(Name="Rock", Phase=1, Density = ConstantDensity(ρ=2800kg/m^3), - HeatCapacity = ConstantHeatCapacity(cp=1050J/kg/K), + HeatCapacity = ConstantHeatCapacity(Cp=1050J/kg/K), Conductivity = ConstantConductivity(k=1.5Watt/K/m), LatentHeat = ConstantLatentHeat(Q_L=350e3J/kg), Melting = MeltingParam_Caricchi()), diff --git a/examples/Example3D_v2.jl b/examples/Example3D_v2.jl index 3d6b1fa..4fd8f60 100644 --- a/examples/Example3D_v2.jl +++ b/examples/Example3D_v2.jl @@ -19,7 +19,7 @@ using WriteVTK MatParam = ( SetMaterialParams(Name="Rock", Phase=1, Density = ConstantDensity(ρ=2800kg/m^3), - HeatCapacity = ConstantHeatCapacity(cp=1050J/kg/K), + HeatCapacity = ConstantHeatCapacity(Cp=1050J/kg/K), Conductivity = ConstantConductivity(k=1.5Watt/K/m), LatentHeat = ConstantLatentHeat(Q_L=350e3J/kg), Melting = MeltingParam_Caricchi()), diff --git a/examples/MTK_GMG_2D_example1.jl b/examples/MTK_GMG_2D_example1.jl index 669c200..7a42059 100644 --- a/examples/MTK_GMG_2D_example1.jl +++ b/examples/MTK_GMG_2D_example1.jl @@ -69,7 +69,7 @@ function MTK_GMG.MTK_initialize!(Arrays::NamedTuple, Grid::GridData, Num::Numeri # open pvd file if requested if Num.Output_VTK name = joinpath(Num.SimName,Num.SimName*".pvd") - Num.pvd = Movie_Paraview(name=name, Initialize=true); + Num.pvd = movie_paraview(name=name, Initialize=true); end return nothing diff --git a/examples/MTK_GMG_2D_example2.jl b/examples/MTK_GMG_2D_example2.jl index 7d03655..59cb646 100644 --- a/examples/MTK_GMG_2D_example2.jl +++ b/examples/MTK_GMG_2D_example2.jl @@ -1,10 +1,4 @@ -# This is a second example that shows how to use MTK in combination with the GeophysicalModelGenerator -# Compared to example 1, we show a few more features: -# - How to define a custom structure with temporal values & use it in the code -# - How to generate a model setup using GMG -# - How to overwrite some of the default functions to customize the simulation -# - How to create paraview files - +# Unzen setup const USE_GPU=false; using MagmaThermoKinematics if USE_GPU @@ -18,33 +12,34 @@ using Plots using Random using GeophysicalModelGenerator -# Test setup -println("Example 2 of the MTK - GMG integration") - +# Model setup println(" --- Generating Setup --- ") # Topography and project it. # NOTE: The first time you do this, please set this to true, which will download the topography data from the internet and save it in a file if false - using GMT, Statistics - Topo = ImportTopo(lon = [130.0, 130.5], lat=[32.55, 32.90], file="@earth_relief_03s.grd") - proj = ProjectionPoint(; Lat=mean(Topo.lat.val), Lon=mean(Topo.lon.val)) - Topo_cart = Convert2CartData(Topo, proj) - save_GMG("examples/Topo_cart", Topo_cart) + using GMT, Statistics + Topo = ImportTopo(lon = [130.0, 130.5], lat=[32.55, 32.90], file="@earth_relief_03s.grd") + proj = ProjectionPoint(; Lat=mean(Topo.lat.val), Lon=mean(Topo.lon.val)) + Topo_cart = Convert2CartData(Topo, proj) + Xt,Yt,Zt = xyz_grid(-23:.1:23,-19:.1:19,0) + Topo_cart = ProjectCartData(CartData(Xt,Yt,Zt,(Zt=Zt,)), Topo, proj) + + save_GMG("Topo_cart", Topo_cart) end Topo_cart = load_GMG("Topo_cart") # Create 3D grid of the region -X,Y,Z = XYZGrid(-23:.1:23,-19:.1:19,-20:.1:5) +X,Y,Z = xyz_grid(-23:.1:23,-19:.1:19,-20:.1:5) Data_set3D = CartData(X,Y,Z,(Phases=zeros(Int64,size(X)),Temp=zeros(size(X)))); # 3D dataset # Create 2D cross-section Nx = 135*6; # resolution in x Nz = 135*4; Data_2D = CrossSection(Data_set3D, Start=(-20,4), End=(20,4), dims=(Nx, Nz)) -Data_2D = AddField(Data_2D,"FlatCrossSection", FlattenCrossSection(Data_2D)) -Data_2D = AddField(Data_2D,"Phases", Int64.(Data_2D.fields.Phases)) +Data_2D = addfield(Data_2D,"FlatCrossSection", FlattenCrossSection(Data_2D)) +Data_2D = addfield(Data_2D,"Phases", Int64.(Data_2D.fields.Phases)) # Intersect with topography Below = BelowSurface(Data_2D, Topo_cart) @@ -63,7 +58,6 @@ x_c, z_c, r = -10, -15, 2.5 Volume = 4/3*pi*r^3 # equivalent 3D volume of the anomaly [km^3] @views Data_2D.fields.Temp[(Data_2D.x.val .- x_c).^2 .+ (Data_2D.z.val .- z_c).^2 .< r^2] .= 800.0 - println(" --- Performing MTK models --- ") # Overwrite some of the default functions @@ -167,24 +161,24 @@ MatParam = (SetMaterialParams(Name="Air", Phase=0, Density = ConstantDensity(ρ=2700kg/m^3), LatentHeat = ConstantLatentHeat(Q_L=0.0J/kg), Conductivity = ConstantConductivity(k=3Watt/K/m), # in case we use constant k - HeatCapacity = ConstantHeatCapacity(cp=1000J/kg/K), + HeatCapacity = ConstantHeatCapacity(Cp=1000J/kg/K), Melting = SmoothMelting(MeltingParam_4thOrder())), # Marxer & Ulmer melting SetMaterialParams(Name="Crust", Phase=1, Density = ConstantDensity(ρ=2700kg/m^3), LatentHeat = ConstantLatentHeat(Q_L=3.13e5J/kg), Conductivity = T_Conductivity_Whittington_parameterised(), # T-dependent k - HeatCapacity = ConstantHeatCapacity(cp=1000J/kg/K), + HeatCapacity = ConstantHeatCapacity(Cp=1000J/kg/K), Melting = SmoothMelting(MeltingParam_4thOrder())), # Marxer & Ulmer melting SetMaterialParams(Name="Mantle", Phase=2, Density = ConstantDensity(ρ=2700kg/m^3), LatentHeat = ConstantLatentHeat(Q_L=3.13e5J/kg), Conductivity = T_Conductivity_Whittington_parameterised(), # T-dependent k - HeatCapacity = ConstantHeatCapacity(cp=1000J/kg/K)), + HeatCapacity = ConstantHeatCapacity(Cp=1000J/kg/K)), SetMaterialParams(Name="Dikes", Phase=3, Density = ConstantDensity(ρ=2700kg/m^3), LatentHeat = ConstantLatentHeat(Q_L=3.13e5J/kg), Conductivity = T_Conductivity_Whittington_parameterised(), # T-dependent k - HeatCapacity = ConstantHeatCapacity(cp=1000J/kg/K), + HeatCapacity = ConstantHeatCapacity(Cp=1000J/kg/K), Melting = SmoothMelting(MeltingParam_4thOrder())) # Marxer & Ulmer melting ) diff --git a/src/MTK_GMG.jl b/src/MTK_GMG.jl index 6f0c26a..85d0179 100644 --- a/src/MTK_GMG.jl +++ b/src/MTK_GMG.jl @@ -138,7 +138,7 @@ function MTK_initialize!(Arrays::NamedTuple, Grid::GridData, Num::NumericalParam # Open pvd file if requested if Num.Output_VTK name = joinpath(Num.SimName,Num.SimName*".pvd") - Num.pvd = Movie_Paraview(name=name, Initialize=true); + Num.pvd = movie_paraview(name=name, Initialize=true); end return nothing @@ -201,7 +201,7 @@ function MTK_initialize!(Arrays::NamedTuple, Grid::GridData, Num::NumericalParam # open pvd file if requested if Num.Output_VTK name = joinpath(Num.SimName,Num.SimName*".pvd") - Num.pvd = Movie_Paraview(name=name, Initialize=true); + Num.pvd = movie_paraview(name=name, Initialize=true); end return nothing @@ -215,7 +215,7 @@ Finalize model run """ function MTK_finalize!(Arrays::NamedTuple, Grid::GridData, Num::NumericalParameters, Tracers::StructArray, Dikes::DikeParameters, CartData_input::Union{Nothing,CartData}) if Num.Output_VTK & !isnothing(Num.pvd) - Movie_Paraview(pvd=Num.pvd, Finalize=true) + movie_paraview(pvd=Num.pvd, Finalize=true) end return nothing @@ -270,9 +270,9 @@ function MTK_save_output(Grid::GridData, Arrays::NamedTuple, Tracers::StructArra Data_set3D = CartData_input else if length(Grid.coord1D)==3 - X,Y,Z = XYZGrid(Grid.coord1D...) + X,Y,Z = xyz_grid(Grid.coord1D...) elseif length(Grid.coord1D)==2 - X,Y,Z = XYZGrid(Grid.coord1D[1], 0, Grid.coord1D[2]) + X,Y,Z = xyz_grid(Grid.coord1D[1], 0, Grid.coord1D[2]) end Data_set3D = CartData(X/1e3,Y/1e3,Z/1e3, (Z=Z,)) end @@ -282,7 +282,7 @@ function MTK_save_output(Grid::GridData, Arrays::NamedTuple, Tracers::StructArra Data_set3D = add_data_CartData(Data_set3D, "MeltFraction", Array(Arrays.ϕ)); # Save output to CartData - Num.pvd = Write_Paraview(Data_set3D, name, pvd=Num.pvd,time=Num.time/SecYear/1e3); + Num.pvd = write_paraview(Data_set3D, name, pvd=Num.pvd,time=Num.time/SecYear/1e3); end end return nothing @@ -304,7 +304,7 @@ function add_data_CartData(d::CartData, name::String, data::Array) else a = data end - d = AddField(d, name, a) + d = addfield(d, name, a) return d end diff --git a/src/MTK_GMG_2D.jl b/src/MTK_GMG_2D.jl index c2864f5..ec6c963 100644 --- a/src/MTK_GMG_2D.jl +++ b/src/MTK_GMG_2D.jl @@ -53,7 +53,7 @@ There are a few functions that you can overwrite in your user code to customize if !isnothing(CartData_input) if !hasfield(typeof(CartData_input.fields),:FlatCrossSection) - error("You should add a Field :FlatCrossSection to your data structure with Data_Cross = AddField(Data_Cross,\"FlatCrossSection\", FlattenCrossSection(Data_Cross))") + error("You should add a Field :FlatCrossSection to your data structure with Data_Cross = addfield(Data_Cross,\"FlatCrossSection\", FlattenCrossSection(Data_Cross))") end Num = MTK_GMG.Setup_Model_CartData(CartData_input, Num, Mat_tup) diff --git a/test/test_MTK_GMG_2D.jl b/test/test_MTK_GMG_2D.jl index 3a0abf2..c90bdc6 100644 --- a/test/test_MTK_GMG_2D.jl +++ b/test/test_MTK_GMG_2D.jl @@ -58,7 +58,7 @@ MatParam = (SetMaterialParams(Name="Rock & partial melt", Phase=1, # Conductivity = ConstantConductivity(k=3.3Watt/K/m), # in case we use constant k Conductivity = T_Conductivity_Whittington_parameterised(), # T-dependent k #Conductivity = T_Conductivity_Whittington(), # T-dependent k - HeatCapacity = ConstantHeatCapacity(cp=1000J/kg/K), + HeatCapacity = ConstantHeatCapacity(Cp=1000J/kg/K), Melting = SmoothMelting(MeltingParam_4thOrder())), # Marxer & Ulmer melting # Melting = MeltingParam_Caricchi()), # Caricchi melting # add more parameters here, in case you have >1 phase in the model @@ -75,15 +75,15 @@ Grid, Arrays, Tracers, Dikes, time_props = MTK_GeoParams_2D(MatParam, Num, Dike_ Topo_cart = load_GMG("../examples/Topo_cart") # Note: Laacher seee is around [10,20] # Create 3D grid of the region -X,Y,Z = XYZGrid(-23:.1:23,-19:.1:19,-20:.1:5) +X,Y,Z = xyz_grid(-23:.1:23,-19:.1:19,-20:.1:5) Data_set3D = CartData(X,Y,Z,(Phases=zeros(Int64,size(X)),Temp=zeros(size(X)))); # 3D dataset # Create 2D cross-section Nx = Num.Nx; # resolution in x Nz = Num.Nz; Data_2D = CrossSection(Data_set3D, Start=(-20,4), End=(20,4), dims=(Nx, Nz)) -Data_2D = AddField(Data_2D,"FlatCrossSection", FlattenCrossSection(Data_2D)) -Data_2D = AddField(Data_2D,"Phases", Int64.(Data_2D.fields.Phases)) +Data_2D = addfield(Data_2D,"FlatCrossSection", FlattenCrossSection(Data_2D)) +Data_2D = addfield(Data_2D,"Phases", Int64.(Data_2D.fields.Phases)) # Intersect with topography Below = BelowSurface(Data_2D, Topo_cart) @@ -141,7 +141,7 @@ MatParam = (SetMaterialParams(Name="Air", Phase=0, Density = ConstantDensity(ρ=2700kg/m^3), LatentHeat = ConstantLatentHeat(Q_L=0.0J/kg), Conductivity = ConstantConductivity(k=3Watt/K/m), # in case we use constant k - HeatCapacity = ConstantHeatCapacity(cp=1000J/kg/K), + HeatCapacity = ConstantHeatCapacity(Cp=1000J/kg/K), Melting = SmoothMelting(MeltingParam_4thOrder())), # Marxer & Ulmer melting SetMaterialParams(Name="Crust", Phase=1, @@ -149,14 +149,14 @@ MatParam = (SetMaterialParams(Name="Air", Phase=0, LatentHeat = ConstantLatentHeat(Q_L=3.13e5J/kg), Conductivity = T_Conductivity_Whittington_parameterised(), # T-dependent k #Conductivity = T_Conductivity_Whittington(), # T-dependent k - HeatCapacity = ConstantHeatCapacity(cp=1000J/kg/K), + HeatCapacity = ConstantHeatCapacity(Cp=1000J/kg/K), Melting = SmoothMelting(MeltingParam_4thOrder())), # Marxer & Ulmer melting SetMaterialParams(Name="Mantle", Phase=2, Density = ConstantDensity(ρ=2700kg/m^3), LatentHeat = ConstantLatentHeat(Q_L=3.13e5J/kg), Conductivity = T_Conductivity_Whittington_parameterised(), # T-dependent k - HeatCapacity = ConstantHeatCapacity(cp=1000J/kg/K)), + HeatCapacity = ConstantHeatCapacity(Cp=1000J/kg/K)), SetMaterialParams(Name="Dikes", Phase=3, Density = ConstantDensity(ρ=2700kg/m^3), @@ -164,7 +164,7 @@ MatParam = (SetMaterialParams(Name="Air", Phase=0, # Conductivity = ConstantConductivity(k=3.3Watt/K/m), # in case we use constant k Conductivity = T_Conductivity_Whittington_parameterised(), # T-dependent k #Conductivity = T_Conductivity_Whittington(), # T-dependent k - HeatCapacity = ConstantHeatCapacity(cp=1000J/kg/K), + HeatCapacity = ConstantHeatCapacity(Cp=1000J/kg/K), Melting = SmoothMelting(MeltingParam_4thOrder())) # Marxer & Ulmer melting ) diff --git a/test/test_MTK_GMG_3D.jl b/test/test_MTK_GMG_3D.jl index c66d5a4..b17b849 100644 --- a/test/test_MTK_GMG_3D.jl +++ b/test/test_MTK_GMG_3D.jl @@ -66,7 +66,7 @@ MatParam = (SetMaterialParams(Name="Rock & partial melt", Phase=1, # Conductivity = ConstantConductivity(k=3.3Watt/K/m), # in case we use constant k Conductivity = T_Conductivity_Whittington_parameterised(), # T-dependent k #Conductivity = T_Conductivity_Whittington(), # T-dependent k - HeatCapacity = ConstantHeatCapacity(cp=1000J/kg/K), + HeatCapacity = ConstantHeatCapacity(Cp=1000J/kg/K), Melting = SmoothMelting(MeltingParam_4thOrder())), # Marxer & Ulmer melting # Melting = MeltingParam_Caricchi()), # Caricchi melting # add more parameters here, in case you have >1 phase in the model @@ -84,7 +84,7 @@ Topo_cart = load_GMG("../examples/Topo_cart") # Note: Laacher seee is arou # Create 3D grid of the region Nx,Ny,Nz = 100,100,100 -X,Y,Z = XYZGrid(range(-23,23, length=Nx),range(-19,19, length=Ny),range(-20,5, length=Nz)) +X,Y,Z = xyz_grid(range(-23,23, length=Nx),range(-19,19, length=Ny),range(-20,5, length=Nz)) Data_3D = CartData(X,Y,Z,(Phases=zeros(Int64,size(X)),Temp=zeros(size(X)))); # 3D dataset # Intersect with topography @@ -131,7 +131,7 @@ MatParam = (SetMaterialParams(Name="Air", Phase=0, Density = ConstantDensity(ρ=2700kg/m^3), LatentHeat = ConstantLatentHeat(Q_L=0.0J/kg), Conductivity = ConstantConductivity(k=3Watt/K/m), # in case we use constant k - HeatCapacity = ConstantHeatCapacity(cp=1000J/kg/K), + HeatCapacity = ConstantHeatCapacity(Cp=1000J/kg/K), Melting = SmoothMelting(MeltingParam_4thOrder())), # Marxer & Ulmer melting SetMaterialParams(Name="Crust", Phase=1, @@ -139,14 +139,14 @@ MatParam = (SetMaterialParams(Name="Air", Phase=0, LatentHeat = ConstantLatentHeat(Q_L=3.13e5J/kg), Conductivity = T_Conductivity_Whittington_parameterised(), # T-dependent k #Conductivity = T_Conductivity_Whittington(), # T-dependent k - HeatCapacity = ConstantHeatCapacity(cp=1000J/kg/K), + HeatCapacity = ConstantHeatCapacity(Cp=1000J/kg/K), Melting = SmoothMelting(MeltingParam_4thOrder())), # Marxer & Ulmer melting SetMaterialParams(Name="Mantle", Phase=2, Density = ConstantDensity(ρ=2700kg/m^3), LatentHeat = ConstantLatentHeat(Q_L=3.13e5J/kg), Conductivity = T_Conductivity_Whittington_parameterised(), # T-dependent k - HeatCapacity = ConstantHeatCapacity(cp=1000J/kg/K)), + HeatCapacity = ConstantHeatCapacity(Cp=1000J/kg/K)), SetMaterialParams(Name="Dikes", Phase=3, Density = ConstantDensity(ρ=2700kg/m^3), @@ -154,7 +154,7 @@ MatParam = (SetMaterialParams(Name="Air", Phase=0, # Conductivity = ConstantConductivity(k=3.3Watt/K/m), # in case we use constant k Conductivity = T_Conductivity_Whittington_parameterised(), # T-dependent k #Conductivity = T_Conductivity_Whittington(), # T-dependent k - HeatCapacity = ConstantHeatCapacity(cp=1000J/kg/K), + HeatCapacity = ConstantHeatCapacity(Cp=1000J/kg/K), Melting = SmoothMelting(MeltingParam_4thOrder())) # Marxer & Ulmer melting ) diff --git a/test/test_ZASSY.jl b/test/test_ZASSY.jl index 9501255..616e558 100644 --- a/test/test_ZASSY.jl +++ b/test/test_ZASSY.jl @@ -355,7 +355,7 @@ if 1==1 # Conductivity = ConstantConductivity(k=3.3Watt/K/m), # in case we use constant k Conductivity = T_Conductivity_Whittington_parameterised(), # T-dependent k #Conductivity = T_Conductivity_Whittington(), # T-dependent k - HeatCapacity = ConstantHeatCapacity(cp=1000J/kg/K), + HeatCapacity = ConstantHeatCapacity(Cp=1000J/kg/K), Melting = SmoothMelting(MeltingParam_4thOrder())), # Marxer & Ulmer melting # Melting = MeltingParam_Caricchi()), # Caricchi melting # add more parameters here, in case you have >1 phase in the model