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OGS
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OGS
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The implementation uses a monolithic approach, i.e., both processes are assembled within one global system of equations.
The advective term of the heat conduction equation is given by the confined groundwater flow process, i.e., the heat conduction depends on darcy velocity of the groundwater flow process. On the other hand the temperature dependencies of the viscosity and density in the groundwater flow couples the H process to the T process.
Note: This list has been automatically extracted from OGS's benchmark tests (ctests). Therefore it might not be exhaustive, but it should give users a good overview about which properties they can/have to use with this process. Probably most of the properties occurring in this list are mandatory.
The list might contain different property <type>s for some property <name> to illustrate different possibilities the users have.
<type> [case] AqueousLiquid<type> [case] Solid<name> density<type> [case] Constant<name> density<type> [case] Linear<name> density<type> [case] Parameter<name> permeability<type> [case] Constant<name> porosity<type> [case] Constant<name> specific_heat_capacity<type> [case] Constant<name> specific_heat_capacity<type> [case] Parameter<name> storage<type> [case] Constant<name> thermal_conductivity<type> [case] Constant<name> thermal_conductivity<type> [case] Parameter<name> viscosity<type> [case] Constant<name> viscosity<type> [case] Exponential<name> permeability<type> [case] Constant<name> permeability<type> [case] CubicLawPermeability<name> porosity<type> [case] Constant<name> specific_heat_capacity<type> [case] Constant<name> thermal_conductivity<type> [case] EffectiveThermalConductivityPorosityMixing<name> thermal_longitudinal_dispersivity<type> [case] Constant<name> thermal_transversal_dispersivity<type> [case] ConstantNo additional info.
1.12.0