diff --git a/applications/solvers/multiphase/icoReactingMultiphaseInterFoam/massTransferModels/Lee/Lee.H b/applications/solvers/multiphase/icoReactingMultiphaseInterFoam/massTransferModels/Lee/Lee.H index 5aee11db45..427ad9fae5 100644 --- a/applications/solvers/multiphase/icoReactingMultiphaseInterFoam/massTransferModels/Lee/Lee.H +++ b/applications/solvers/multiphase/icoReactingMultiphaseInterFoam/massTransferModels/Lee/Lee.H @@ -28,14 +28,14 @@ Description Mass tranfer Lee model. Simple model driven by field value difference as: \f[ - mDot = C \rho \alpha (\T - T_{activate})/T_{activate} + \dot{m} = C \rho \alpha (T - T_{activate})/T_{activate} \f] where C is a model constant. if C > 0: \f[ - mDot = C \rho \alpha*(\T - T_{activate})/T_{activate} + \dot{m} = C \rho \alpha (T - T_{activate})/T_{activate} \f] for \f[ T > T_{activate} \f] @@ -46,12 +46,12 @@ Description if C < 0: \f[ - mDot = -C \rho \alpha (T_{activate} - \T)/T_{activate} + \dot{m} = -C \rho \alpha (T_{activate} - T)/T_{activate} \f] for \f[ T < T_{activate} \f] and - \f[ mDot = 0.0 \f] for \f[ T > T_{activate} \f] + \f[ \dot{m} = 0.0 \f] for \f[ T > T_{activate} \f] Based on the reference: -# W. H. Lee. "A Pressure Iteration Scheme for Two-Phase Modeling". diff --git a/applications/solvers/multiphase/icoReactingMultiphaseInterFoam/massTransferModels/kineticGasEvaporation/kineticGasEvaporation.H b/applications/solvers/multiphase/icoReactingMultiphaseInterFoam/massTransferModels/kineticGasEvaporation/kineticGasEvaporation.H index 4dee0ef231..e94fff14a0 100644 --- a/applications/solvers/multiphase/icoReactingMultiphaseInterFoam/massTransferModels/kineticGasEvaporation/kineticGasEvaporation.H +++ b/applications/solvers/multiphase/icoReactingMultiphaseInterFoam/massTransferModels/kineticGasEvaporation/kineticGasEvaporation.H @@ -25,38 +25,37 @@ Class Foam::meltingEvaporationModels::kineticGasEvaporation Description - Considering the Hertz Knudsen formula, which gives the evaporation-condensation flux based on the kinetic theory for flat interface: \f[ - Flux = C sqrt(M/(2 \pi \R T_{activate}))(\p - pSat) + Flux = C \sqrt{\frac{M}{2 \pi R T_{activate}}}(p - p_{sat}) \f] where: \vartable - Flux | mass flux rate [Kg/s/m2] + Flux | mass flux rate [kg/s/m2] M | molecular weight T_{activate} | saturation temperature C | accomodation coefficient R | universal gas constant - pSat | saturation pressure - \p | vapor partial pressure + p_{sat} | saturation pressure + p | vapor partial pressure \endvartable The Clapeyron-Clausius equation relates the pressure to the temperature for the saturation condition: \f[ - dp/dT = - L / (T*(nuv - nul)) + \frac{dp}{dT} = - \frac{L}{T (\nu_v - \nu_l)} \f] where: \vartable L | latent heat - nuv | inverse of the vapor density - nul | inverse of the liquid density + \nu_v | inverse of the vapor density + \nu_l | inverse of the liquid density \endvartable @@ -64,10 +63,10 @@ Description \f[ Flux = - 2 C/(2 - C) - sqrt(M/(2 \pi \R T_{activate})) + 2 \frac{C}{2 - C} + \sqrt{\frac{M}{2 \pi R T_{activate}}} L (\rho_{v}*\rho_{l}/(\rho_{l} - \rho_{v})) - (\T - T_{activate})/T_{activate} + (T - T_{activate})/T_{activate} \f] This assumes liquid and vapour are in equilibrium, then the accomodation @@ -75,7 +74,7 @@ Description Hertz-Knudsen-Schrage. Based on the reference: - - Van P. Carey, “Liquid-Vapor Phase Change Phenomena”, ISBN 0-89116836, + - Van P. Carey, Liquid-Vapor Phase Change Phenomena, ISBN 0-89116836, 1992, pp. 112-121. diff --git a/src/meshTools/sets/cellSources/regionToCell/regionToCell.H b/src/meshTools/sets/cellSources/regionToCell/regionToCell.H index dd699df550..93ae8e6df6 100644 --- a/src/meshTools/sets/cellSources/regionToCell/regionToCell.H +++ b/src/meshTools/sets/cellSources/regionToCell/regionToCell.H @@ -28,6 +28,7 @@ Description A topoSetCellSource to select cells belonging to a topological connected region (that contains given points) +Usage In dictionary input: \verbatim // optional name of cellSet delimiting search @@ -41,7 +42,7 @@ Description insidePoints ((1 2 3)); \endverbatim - \heading Dictionary parameters + Dictionary parameters: \table Property | Description | Required | Default insidePoints | Points inside regions | yes | @@ -68,7 +69,7 @@ namespace Foam class regionSplit; /*---------------------------------------------------------------------------*\ - Class regionToCell Declaration + Class regionToCell Declaration \*---------------------------------------------------------------------------*/ class regionToCell @@ -151,7 +152,6 @@ public: const topoSetSource::setAction action, topoSet& set ) const; - }; diff --git a/src/sampling/sampledSurface/writers/boundaryData/boundaryDataSurfaceWriter.H b/src/sampling/sampledSurface/writers/boundaryData/boundaryDataSurfaceWriter.H index b1b01e76a1..d155cd0048 100644 --- a/src/sampling/sampledSurface/writers/boundaryData/boundaryDataSurfaceWriter.H +++ b/src/sampling/sampledSurface/writers/boundaryData/boundaryDataSurfaceWriter.H @@ -70,14 +70,14 @@ Description The \c rootdir normally corresponds to something like \c postProcessing/\ - \subheading Geometry + where the geometry is written as: \verbatim rootdir `-- surfaceName `-- "points" \endverbatim - \subheading Fields + and field data: \verbatim rootdir `-- surfaceName