This prevents spurious factors of 1000 from being introduced in
thermodynamic models. It also generalises the system further with
respect to alternative unit sets.
The legacy fvMeshTopoChangersMovingCone removed, replaced by the more general
mesh mapping approach, see tutorials incompressibleFluid/movingCone and
shockFluid/movingCone.
The specie molecular mass (Wi) and formation enthalpy (hfi) methods now
return dimensioned scalars. This permits their direct inclusion into
dimensioned field expressions. Non-dimensioned methods have been
retained with a "Value" suffix (i.e., WiValue and hfiValue).
All property functions in the low-level templated thermo property
implementations and the high-level virtual interfaces have been made
consistent. All energies and enthalpies are lower case to denote that
they are specific quantities. Molar functions have been removed as these
are no longer used anywhere.
The nearWallDist MeshObject is now deleted on mesh-change rather than updated
which is more efficient for cases with multiple mesh changes, e.g. motion,
stitching and mapping by avoiding unnecessary updates.
As a consequence of this change the wallDist::y() volScalarField reference
should not be cached across mesh changes so the turbulence models now obtain the
y field as required from the new momentumTransportModel::y() function, the
original near-wall distance function is now named momentumTransportModel::yb()
to clarify that it is the wall distance of the boundary cells.
This is consistent with the fluid solvers, and prevents failures
associated with using fields that haven't yet been updated or corrected
following mesh changes
This simple model creates a heat transfer coefficient in proportion with
the corresponding drag model's momentum transfer coefficient. A
user-defined Prandtl number and a harmonic average of the phases'
specific heats are used to specify the constant of proportionality.
This model has no physical basis. It exists primarily for testing
purposes. It has the advantage of being applicable to any interface,
including those representing segregated configurations.
Example usage:
heatTransfer
{
gas_segregatedWith_liquid
{
type Prandtl;
Pr 0.7;
}
}
These classes permit any PtrList of region-associated objects (meshes,
solvers, domainDecompositions, ...) to prefix the region name to the log.
At present these classes are used by decomposePar and reconstructPar
only. The foamMultiRun solver still handles its own prefixing.
The directFieldMapper has been renamed to forwardFieldMapper, and
instances where generalFieldMapper was used instead of a more simple
forward/direct type have been removed.
The patch-specific mapper interfaces, fvPatchFieldMapper and
pointPatchFieldMapper, have been removed as they did not do anything.
Patch mapping constructors and functions now take a basic fieldMapper
reference.
An fvPatchFieldMapper.H header has been provided to aid backwards
compatability so that existing custom boundary conditions continue to
compile.
This lets calling code determine the difference between a polyMesh
topology change and a re-stitch. This prevents unnecessary
post-processing output in a few cases when using NCC; most notably the
generation of cellProc fields by reconstructPar.
Previously this was creating simple processorCyclic fields on the
nonConformalProcessorCyclic patches using a patchType override. The fact
that this worked is an encouraging indication of the system's
robustness, but it is more logical to create a field which directly
corresponds to the underlying patch type.
A number of fixes have been made in order to make non-conformal cyclic
patches compatible with run-time distribution.
A tutorial case, incompressibleVoF/rotatingCube, has been added which
demonstrates simultaneous usage of motion, non-conformal couplings,
adaptive refinement and load-balancing.
Currently in compressibleVoF vDot contains only the compressibility dilatation
effect whereas in multiphaseEuler the effect of sources are also included but
this will be refactored shortly so that the handling of mass sources and
compressibility is consistent between VoF and Euler-Euler solvers.
The previously hard-coded 1e-4 division stabilisation used when linearising vDot
for bounded semi-implicit solution of the phase-fractions is now an optional
user-input with keyword vDotResidualAlpha, e.g. in multiphaseEuler:
solvers
{
"alpha.*"
{
nAlphaCorr 1;
nAlphaSubCycles 2;
vDotResidualAlpha 1e-6;
}
.
.
.
Now both the checkMesh utility and functionObject operate in the same manner
with the same controls, executing the same checkGeometry and checkTopology
functions from the new meshCheck library. The controls have been updated and
made more consistent and flexible, in particular by the addition of optional
user specification for the non-orthogonality and skewness error thresholds:
Application
checkMesh
Description
Checks validity of a mesh.
Usage
\b checkMesh [OPTION]
Options:
- \par noTopology
Skip checking the mesh topology
- \par -allTopology
Check all (including non finite-volume specific) addressing
- \par -allGeometry
Check all (including non finite-volume specific) geometry
- \par -meshQuality
Check against user defined (in \a system/meshQualityDict) quality
settings
- \par -region \<name\>
Specify an alternative mesh region.
- \par -writeSurfaces
Reconstruct cellSets and faceSets of problem faces and write to
postProcessing directory.
- \par -surfaceFormat <format>
Format used to write the cellSets and faceSets surfaces
e.g. vtk or ensight.
- \par -writeSets
Reconstruct pointSets of problem points nd write to
postProcessing directory.
- \par -setFormat <format>
Format used to write the pointSets
e.g. vtk or ensight.
- \par -nonOrthThreshold <threshold value in degrees>
Threshold in degrees for reporting non-orthogonality errors,
default: 70"
- \par -skewThreshold <threshold value>
Threshold for reporting skewness errors, default: 4.
Class
Foam::functionObjects::checkMesh
Description
Executes primitiveMesh::checkMesh(true) every execute time for which the
mesh changed, i.e. moved or changed topology.
Useful to check the correctness of changing and morphing meshes.
Usage
\table
Property | Description | Required | Default value
type | type name: checkMesh | yes |
noTopology | Skip checking the mesh topology | no | false
allTopology | Check all addressing | no | false
allGeometry | Check all geometry | no | false
writeSurfaces | Reconstruct and write problem faces | no | false
surfaceFormat | Format for problem faceSets | no | vtk
writeSets | Reconstruct and write problem points | no | false
setFormat | Format used to write the problem pointSets | no | vtk
nonOrthThreshold | Threshold for non-orthogonality errors | no | 70 deg
skewThreshold | Threshold for reporting skewness errors | no | 4
\endtable
Example of checkMesh specification:
\verbatim
checkMesh
{
type checkMesh;
libs ("libutilityFunctionObjects.so");
executeControl timeStep;
executeInterval 10;
allGeometry true;
allTopology true;
writeSurfaces true;
surfaceFormat vtk;
writeSets true;
setFormat vtk;
}
\endverbatim
or using the standard configuration file:
\verbatim
#includeFunc checkMesh(executeInterval=10, allGeometry=true)
\endverbatim
The fact that these names create sources in their associated transport
equations is clear in context, so the name does not need to contain
'Source'.
Having 'Source' in the name is a historic convention that dates back to
when fvModels and fvConstraints were combined in a single fvOptions
interface. In this interface, disambiguation between sources and
constraints was necessary.
The full set of name changes is as follows:
accelerationSource -> acceleration
actuationDiskSource -> actuationDisk
effectivenessHeatExchangerSource -> effectivenessHeatExchanger
explicitPorositySource -> porosityForce
radialActuationDiskSource -> radialActuationDisk
rotorDiskSource -> rotorDisk
sixDoFAccelerationSource -> sixDoFAcceleration
solidEquilibriumEnergySource -> solidThermalEquilibrium
solidificationMeltingSource -> solidificationMelting
volumeFractionSource -> volumeBlockage
interRegionExplicitPorositySource -> interRegionPorosityForce
VoFSolidificationMeltingSource -> VoFSolidificationMelting
The old names are still available for backwards compatibility.
IsothermalSolidPhaseModel does not update energy and density from pressure
whereas IsothermalPhaseModel does to allow compressible fluid phases to change
volume due to pressure changes.
When an fvModel source introduces fluid into a simulation it should also
create a corresponding source term for all properties transported into
the domain by that injection. The source is, effectively, an alternative
form of inlet boundary, on which all transported properties need an
inlet value specified.
These values are now specified in the property field files. The
following is an example of a 0/U file in which the velocity of fluid
introduced by a fvModel source called "injection1" is set to a fixed
value of (-1 0 0):
dimensions [0 1 -1 0 0 0 0];
internalField uniform (0 0 0);
boundaryField
{
#includeEtc "caseDicts/setConstraintTypes"
wall
{
type noSlip;
}
atmosphere
{
type pressureInletOutletVelocity;
value $internalField;
}
}
// *** NEW ***
sources
{
injection1
{
type uniformFixedValue;
uniformValue (-1 0 0);
}
}
And the following entry in the 0/k file specifies the turbulent kinetic
energy introduced as a fraction of the mean flow kinetic energy:
sources
{
injection1
{
type turbulentIntensityKineticEnergy;
intensity 0.05;
}
}
The specification is directly analogous to boundary conditions. The
conditions are run-time selectable and can be concisely implemented.
They can access each other and be inter-dependent (e.g., the above,
where turbulent kinetic energy depends on velocity). The syntax keeps
field data localised and makes the source model (e.g., massSource,
volumeSource, ...) specification independent from what other models and
fields are present in the simulation. The 'fieldValues' entry previously
required by source models is now no longer required.
If source values need specifying and no source condition has been
supplied in the relevant field file then an error will be generated.
This error is similar to that generated for missing boundary conditions.
This replaces the behaviour where sources such as these would introduce
a value of zero, either silently or with a warning. This is now
considered unacceptable. Zero might be a tolerable default for certain
fields (U, k), but is wholly inappropriate for others (T, epsilon, rho).
This change additionally makes it possible to inject fluid into a
multicomponent solver with a specified temperature. Previously, it was
not possible to do this as there was no means of evaluating the energy
of fluid with the injected composition.
for thermophysical transport within stationary solid phases. This provides a
consistent interface to heat transport within solids for single and now
multiphase solvers so that for example the wallHeatFlux functionObject can now
be used with multiphaseEuler, see tutorials/multiphaseEuler/boilingBed.
Also this development supports anisotropic thermal conductivity within the
stationary solid regions which was not possible previously.
The tutorials/multiphaseEuler/bed and tutorials/multiphaseEuler/boilingBed
tutorial cases have been updated for phaseSolidThermophysicalTransportModel by
changing the thermo type in physicalProperties.solid to heSolidThermo. This
change will need to be made to all multiphaseEuler cases involving stationary
phases.
The interface for fvModels has been modified to improve its application
to "proxy" equations. That is, equations that are not straightforward
statements of conservation laws in OpenFOAM's usual convention.
A standard conservation law typically takes the following form:
fvMatrix<scalar> psiEqn
(
fvm::ddt(alpha, rho, psi)
+ <fluxes>
==
<sources>
);
A proxy equation, on the other hand, may be a derivation or
rearrangement of a law like this, and may be linearised in terms of a
different variable.
The pressure equation is the most common example of a proxy equation. It
represents a statement of the conservation of volume or mass, but it is
a rearrangement of the original continuity equation, and it has been
linearised in terms of a different variable; the pressure. Another
example is that in the pre-predictor of a VoF solver the
phase-continuity equation is constructed, but it is linearised in terms
of volume fraction rather than density.
In these situations, fvModels sources are now applied by calling:
fvModels().sourceProxy(<conserved-fields ...>, <equation-field>)
Where <conserved-fields ...> are (alpha, rho, psi), (rho, psi), just
(psi), or are omitted entirely (for volume continuity), and the
<equation-field> is the field associated with the proxy equation. This
produces a source term identical in value to the following call:
fvModels().source(<conserved-fields ...>)
It is only the linearisation in terms of <equation-field> that differs
between these two calls.
This change permits much greater flexibility in the handling of mass and
volume sources than the previous name-based system did. All the relevant
fields are available, dimensions can be used in the logic to determine
what sources are being constructed, and sources relating to a given
conservation law all share the same function.
This commit adds the functionality for injection-type sources in the
compressibleVoF solver. A following commit will add a volume source
model for use in incompressible solvers.
