The fixedDmdt phase change boundary condition has been removed as this
is not a physical model and was only ever needed for testing.
The phase change wall function interface has been simplified and made a
mix-in, rather than a derivation from a fixed value patch field. This
reduces forwarding and mapping code and permits wall functions to derive
from patch fields other than fixed value.
Minor style and consisteny improvements have been made to the wall
boiling wall function.
used in the incompressibleMultiphaseMixture and compressibleMultiphaseMixture
respectively which are used in multiphaseInterFoam and
compressibleMultiphaseInterFoam respectively.
Also the PtrDictionary of phases has been replaced by PtrListDictionary of
phases and iterations over the linked-list replaced by forAll loops which is
easier to use and consistent with the multiphaseEuler solver module.
Tests have shown that the alphaDByAf phase-pressure diffusion coefficient
provides better stability without the optional (1 - phase) prefactor without
introducing excessive smearing of the solution.
None of the current thermophysicalTransportModels solve transport equations in
order to evaluate the thermophysical transport properties so it makes more sense
that the evaluation occurs at the beginning of the time-step rather than at the
end where conservative fluxes are available for transport solution. To enable
this the correct() functions have been renamed predict() and called in the
prePredictor() step of foamRun and foamMultiRun and at the beginning of the
time-step in the legacy solvers. A particular advantage of this approach is
that complex data cached in the thermophysicalTransportModels can now be deleted
following mesh topology changes and recreated in the predict() call which is
more efficient than attempting to register and map the data.
An empty correct() function is included in addition to the new predict()
function in thermophysicalTransportModel to support scalar flux transport
closure in the future if needed.
Additionally the two transport model corrector function calls in foamRun and
foamMultiRun have been combined into a single postCorrector() call to allow
greater flexibility in transport property prediction and correction in the
modular solvers.
Simplifies the setting of the scheme for the phase pressure, e.g. choosing localMax
interpolationSchemes
{
default linear;
pPrime localMax;
}
improves stability and reduces chequerboarding in the solution at higher Courant
numbers.
In order that the phase-fractions sum to 1 it is necessary that the same
diffusivity is used for ALL phases in the implicitPhasePressure option. This is
guaranteed by the new alphaDByAf function which returns a single
surfaceScalarField diffusivity to be used when forming the Laplacian term in the
implicit phase-fraction diffusion correction equation in phaseSystemSolve.
The phase-pressure and turbulent dispersion interface terms are summed over all
phases and interfaces in alphaDByAf to form a single diffusivity.
The timeName() function simply returns the dimensionedScalar::name() which holds
the user-time name of the current time and now that timeName() is no longer
virtual the dimensionedScalar::name() can be called directly. The timeName()
function implementation is maintained for backward-compatibility.
Given that the number of solid solver modules is currently 1 and unlikely to
exceed 3 it is not very useful to maintain solid and fluid sub-directories and
easier to see the correspondence between the solver modules and tutorial cases
without.
