OGS
|
Under the assumptions of the drift-flux model in a geothermal well with a constant cross-sectional area, the transient geo-fluid flow in a two-phase one-component geothermal well can be quantified using one-dimensional formulations of mass, momentum, and energy balance.
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] Gas<name>
density<type>
[tag] WaterDensityIAPWSIF97Region1<name>
enthalpy<type>
[tag] WaterEnthalpyIAPWSIF97Region1<name>
saturation_density<type>
[tag] WaterLiquidDensityIAPWSIF97Region4<name>
saturation_density<type>
[tag] WaterVapourDensityIAPWSIF97Region4<name>
saturation_enthalpy<type>
[tag] WaterLiquidEnthalpyIAPWSIF97Region4<name>
saturation_enthalpy<type>
[tag] WaterVapourEnthalpyIAPWSIF97Region4<name>
saturation_temperature<type>
[tag] WaterSaturationTemperatureIAPWSIF97Region4<name>
temperature<type>
[tag] WaterTemperatureIAPWSIF97Region1<name>
viscosity<type>
[tag] WaterViscosityIAPWSNo additional info.