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ρ (SI unit: kg/m3) is the fluid density.
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Cp (SI unit: J/(kg·K)) is the fluid heat capacity at constant pressure.
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(ρCp)eff (SI unit: J/(m3·K)) is the effective volumetric heat capacity at constant pressure defined by an averaging model to account for both solid matrix and fluid properties.
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q is the conductive heat flux (SI unit: W/m2).
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u (SI unit: m/s) is the fluid velocity field, either an analytic expression or the velocity field from a Fluid Flow interface. u should be interpreted as the Darcy velocity, that is, the volume flow rate per unit cross sectional area. The average linear velocity (the velocity within the pores) can be calculated as uL = u ⁄ θL, where θL is the fluid’s volume fraction, or equivalently the porosity.
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keff (SI unit: W/(m·K)) is the effective thermal conductivity (a scalar or a tensor if the thermal conductivity is anisotropic), defined by an averaging model to account for both solid matrix and fluid properties.
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Q (SI unit: W/m3) is the heat source (or sink). Add one or several heat sources as separate physics features. See Heat Source node and Viscous Dissipation subnode for example.
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This model input does not override the Reference temperature Tref set in the Physical Model section of the physics interface, and that is used to evaluate the reference enthalpy, and a reference density for incompressible nonisothermal flows.
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The gas constant, with two options for the Gas constant type: Specific gas constant Rs or Mean molar mass Mn. If Mean molar mass is selected the software uses the universal gas constant R = 8.314 J/(mol·K), which is a built-in physical constant, to compute the specific gas constant.
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Either the Heat capacity at constant pressure Cp or Ratio of specific heats γ by selecting the option from the Specify Cp or γ list. For an ideal gas, it is sufficient to specify either Cp or the ratio of specific heats, γ, as these properties are interdependent.
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Vapor mass fraction (the default) to define the ratio of the vapor mass to the total mass.
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Concentration to define the amount of water vapor in the total volume. If selected, a Concentration model input is automatically added in the Model Inputs section.
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Moisture content (also called mixing ratio or humidity ratio) to define the ratio of the water vapor mass to the dry air mass.
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Relative humidity , a quantity defined between 0 and 1, where 0 corresponds to dry air and 1 to a water vapor-saturated air. The Relative humidity, temperature condition and Relative humidity, absolute pressure condition must be specified.
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In this node you specify the volume fraction of solid material θp, whereas in some other nodes (available with other COMSOL add-on modules) the volume fraction of pores (or porosity) εp = 1 − θp is required instead.
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Volume average (default), which computes the effective conductivity of the solid-fluid system as the weighted arithmetic mean of fluid and porous matrix conductivities:
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Reciprocal average, which computes the effective conductivity of the solid-fluid system as the weighted harmonic mean of fluid and porous matrix conductivities:
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Power law, which computes the effective conductivity of the solid-fluid system as the weighted geometric mean of fluid and porous matrix conductivities:
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With certain COMSOL products, the Thermal Dispersion, Viscous Dissipation, Geothermal Heating and Immobile Fluids subnodes are available from the context menu (right-click the parent node) or from the Physics toolbar, Attributes menu.
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When Surface-to-surface radiation is activated, the Opacity (Surface-to-Surface Radiation Interface) subnode is automatically added to the entire selection, with Opaque option selected. The domain selection can’t be edited. To set some part of the domain as transparent, add a new Opacity (Surface-to-Surface Radiation Interface) subnode from the context menu (right-click the parent node) or from the Physics toolbar, Attributes menu.
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Evaporation in Porous Media with Small Evaporation Rates: Application Library path: Heat_Transfer_Module/Phase_Change/evaporation_porous_media_small_rate
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