diff --git a/doc/doxygen/modules.txt b/doc/doxygen/modules.txt
index b0c15db748d059fc72c9e1d9f0774bf323c8ba4f..13cde77a349278477248a6c9eb00428fd98661d9 100644
--- a/doc/doxygen/modules.txt
+++ b/doc/doxygen/modules.txt
@@ -112,7 +112,7 @@
/*!
* \ingroup PorousmediumflowModels
* \defgroup BoxDFMModel boxdfm
- * \brief \todo
+ * \brief Vertex-centered, continuous-pressure, conforming lower-dimensional discrete-fracture model
* \copydetails ./porousmediumflow/boxdfm/model.hh
*/
/*!
@@ -182,7 +182,7 @@
/* ***************** FreeflowModels ******************/
/*!
* \defgroup FreeflowModels Free Flow Models
- * \brief Single-phase models basing on the Navier-Stokes equation
+ * \brief Single-phase models based on the Navier-Stokes equation
*/
/*!
* \ingroup FreeflowModels
@@ -251,7 +251,7 @@
*/
/*!
* \defgroup Geomechanics Geomechanics Models
- * \brief Models for taking into account solid deformation
+ * \brief Models taking into account solid deformation
*/
/*!
* \ingroup Geomechanics
@@ -460,7 +460,7 @@
/* ***************** Flux ******************/
/*!
* \defgroup Flux Flux
- * \brief All flux related things available in DuMu<sup>x</sup>
+ * \brief Everything flux related in DuMu<sup>x</sup>
*/
/*!
* \ingroup Flux
@@ -495,7 +495,7 @@
/* ***************** Material ******************/
/*!
* \defgroup Material Material and Fluid Framework
- * \brief The DuMu<sup>x</sup> material and fluid framework with constitutive laws and physics
+ * \brief The material and fluid framework with constitutive laws and mixture physics
* \par
* Short description of the most important concepts of the material and fluid framework:
*
@@ -700,15 +700,15 @@
/* ***************** InputOutput ******************/
/*!
* \defgroup InputOutput Input Output
- * \brief Classes and functions dealing with input and output of data and grids
+ * \brief Input and output of data and grids
*/
/* ***************** MultiDomain ******************/
/*!
* \defgroup MultiDomain Multidomain simulations
- * \brief Classes to run problems with multiple domains
+ * \brief Coupling of several regular DuMu<sup>x</sup> problems
*
- * The multi domain module allows to couple regular DuMu<sup>x</sup> problems.
+ * The multi domain module allows coupling regular DuMu<sup>x</sup> problems.
* Several coupling modes are currently available.
*/
/*!
diff --git a/dumux/common/geometry/geometryintersection.hh b/dumux/common/geometry/geometryintersection.hh
index 13f6a4923179dd061b6a049f45e8172a28560c58..cd702ac1c47c8eaff53a9f79b548f2cd0e7ac909 100644
--- a/dumux/common/geometry/geometryintersection.hh
+++ b/dumux/common/geometry/geometryintersection.hh
@@ -1008,7 +1008,7 @@ public:
* \note Algorithm based on the one from "Real-Time Collision Detection" by Christer Ericson,
* published by Morgan Kaufmann Publishers, (c) 2005 Elsevier Inc. (Chapter 5.3.6)
* \param geo1/geo2 The geometries to intersect
- * \param is If the geometries collide, is holds the corner points of
+ * \param intersection If the geometries collide, is holds the corner points of
* the intersection object in global coordinates.
* \note This overload is used when point-like intersections are seeked
*/
@@ -1080,9 +1080,9 @@ public:
* \brief Colliding segment and convex polyhedron
* \note Algorithm based on the one from "Real-Time Collision Detection" by Christer Ericson,
* published by Morgan Kaufmann Publishers, (c) 2005 Elsevier Inc. (Chapter 5.3.6)
- * \param geo1/geo2 The geometries to intersect
* \param is If the geometries collide, is holds the corner points of
* the intersection object in global coordinates.
+ * \param a/b/c/p/q \todo Doc me!
* \note This overload is used when point-like intersections are seeked
*/
template<class P = Policy, std::enable_if_t<P::dimIntersection == 0, int> = 0>
diff --git a/dumux/common/integrate.hh b/dumux/common/integrate.hh
index 7b4fc483881ee2b76ba6391d4adf5862b262cb2c..f458f763655027d37d1d3e093c01d8ad33f482e4 100644
--- a/dumux/common/integrate.hh
+++ b/dumux/common/integrate.hh
@@ -97,7 +97,7 @@ using FieldType = typename FieldTypeImpl<T>::type;
/*!
* \brief Integrate a grid function over a grid view
* \param gg the grid geometry
- * \param f the grid function
+ * \param sol the solution vector
* \param order the order of the quadrature rule
*/
template<class GridGeometry, class SolutionVector,
@@ -127,9 +127,9 @@ auto integrateGridFunction(const GridGeometry& gg,
/*!
* \brief Integrate a function over a grid view
- * \param gv the grid view
- * \param f the first function
- * \param g the second function
+ * \param gg the grid geometry
+ * \param sol1 the first function
+ * \param sol2 the second function
* \param order the order of the quadrature rule
* \note dune functions currently doesn't support composing two functions
*/
diff --git a/dumux/discretization/evalgradients.hh b/dumux/discretization/evalgradients.hh
index 3e930a50a5cf6ed7bff7f19a534bd26adbfa46d2..090a0670b79499c357b05b3162b1e8aa842e4865 100644
--- a/dumux/discretization/evalgradients.hh
+++ b/dumux/discretization/evalgradients.hh
@@ -45,6 +45,7 @@ namespace Dumux {
* \param fvGridGeometry The finite volume grid geometry
* \param elemSol The primary variables at the dofs of the element
* \param globalPos The global position
+ * \param ignoreState If true, the state of primary variables is ignored
*
* \return Dune::FieldVector with as many entries as dimension of
* the PrimaryVariables object (i.e. numEq). Each entry is
diff --git a/dumux/discretization/projection/projector.hh b/dumux/discretization/projection/projector.hh
index fe9160393b0bc205b763590ad6cd5c8c4798f9f9..f9fad6e6a759b1a9e98bc1a321b8cc4d2d6c7432 100644
--- a/dumux/discretization/projection/projector.hh
+++ b/dumux/discretization/projection/projector.hh
@@ -125,6 +125,7 @@ public:
/*!
* \brief Project a solution u into up
* \param u The solution living on the domain space
+ * \param params \todo Doc me!
* \return The projection of u into the target space
*/
template< class BlockType, std::enable_if_t<std::is_convertible<BlockType, ScalarType>::value, int> = 0 >
@@ -162,6 +163,7 @@ public:
/*!
* \brief Project a solution u into up
* \param u The solution living on the domain space
+ * \param params \todo Doc me!
* \return The projection of u into the target space
*/
template< class BlockType, std::enable_if_t<!std::is_convertible<BlockType, ScalarType>::value, int> = 0 >
diff --git a/dumux/freeflow/navierstokes/staggered/staggeredupwindfluxvariables.hh b/dumux/freeflow/navierstokes/staggered/staggeredupwindfluxvariables.hh
index d8485ec10c24ea6b7920385d022f578084e4befb..429aae4516b6f06fa49f21570cf86bc789eb799b 100644
--- a/dumux/freeflow/navierstokes/staggered/staggeredupwindfluxvariables.hh
+++ b/dumux/freeflow/navierstokes/staggered/staggeredupwindfluxvariables.hh
@@ -19,7 +19,7 @@
/*!
* \file
* \ingroup NavierStokesModel
- * \copydoc Dumux::NavierStokesUpwindVariables
+ * \copydoc Dumux::StaggeredUpwindFluxVariables
*/
#ifndef DUMUX_NAVIERSTOKES_STAGGERED_UPWINDVARIABLES_HH
#define DUMUX_NAVIERSTOKES_STAGGERED_UPWINDVARIABLES_HH
diff --git a/dumux/freeflow/rans/oneeq/problem.hh b/dumux/freeflow/rans/oneeq/problem.hh
index ab3ecd1b1b3554eb87952e52dc9e1fa4eca769ef..682f3830d997532590980bac1f2054828caaca83 100644
--- a/dumux/freeflow/rans/oneeq/problem.hh
+++ b/dumux/freeflow/rans/oneeq/problem.hh
@@ -19,7 +19,7 @@
/*!
* \file
* \ingroup OneEqModel
- * \copydoc Dumux::OneEqProblem
+ * \brief One-equation turbulence problem base class.
*/
#ifndef DUMUX_ONEEQ_PROBLEM_HH
#define DUMUX_ONEEQ_PROBLEM_HH
diff --git a/dumux/freeflow/rans/problem.hh b/dumux/freeflow/rans/problem.hh
index 00e6272cdbc287e9f6a8f8e6bd363d428ee898af..5c95e70eb5c44506827d9e399d37d6ff9ff69541 100644
--- a/dumux/freeflow/rans/problem.hh
+++ b/dumux/freeflow/rans/problem.hh
@@ -500,7 +500,7 @@ public:
const Scalar karmanConstant() const
{ return 0.41; }
- //! \brief Returns the \$f \beta_{\omega} \$f constant
+ //! \brief Returns the \f$ \beta_{\omega} \f$ constant
const Scalar betaOmega() const
{
return 0.0708;
diff --git a/dumux/freeflow/rans/twoeq/kepsilon/problem.hh b/dumux/freeflow/rans/twoeq/kepsilon/problem.hh
index 81da26df026baf598242deb99cd0a58ee9efa3be..939fa207ce6b11ea75a3420808a495b0a2e0970e 100644
--- a/dumux/freeflow/rans/twoeq/kepsilon/problem.hh
+++ b/dumux/freeflow/rans/twoeq/kepsilon/problem.hh
@@ -19,7 +19,7 @@
/*!
* \file
* \ingroup KEpsilonModel
- * \copydoc Dumux::KEpsilonProblem
+ * \brief K-epsilon turbulence problem base class.
*/
#ifndef DUMUX_KEPSILON_PROBLEM_HH
#define DUMUX_KEPSILON_PROBLEM_HH
diff --git a/dumux/freeflow/rans/twoeq/komega/problem.hh b/dumux/freeflow/rans/twoeq/komega/problem.hh
index e6acf8e6417854a4e7e48ee18022c179a5318363..9d026e7aeee1aff78cf0591149b568a0182086a8 100644
--- a/dumux/freeflow/rans/twoeq/komega/problem.hh
+++ b/dumux/freeflow/rans/twoeq/komega/problem.hh
@@ -19,7 +19,7 @@
/*!
* \file
* \ingroup KOmegaModel
- * \copydoc Dumux::KOmegaProblem
+ * \brief K-Omega turbulence model problem base class.
*/
#ifndef DUMUX_KOMEGA_PROBLEM_HH
#define DUMUX_KOMEGA_PROBLEM_HH
diff --git a/dumux/freeflow/rans/twoeq/lowrekepsilon/problem.hh b/dumux/freeflow/rans/twoeq/lowrekepsilon/problem.hh
index 92c11329095f0da0b438c1c1ab1c70bd9b1e1d70..29200e009ae94fbe896829ed3c3da2fd0d4d8443 100644
--- a/dumux/freeflow/rans/twoeq/lowrekepsilon/problem.hh
+++ b/dumux/freeflow/rans/twoeq/lowrekepsilon/problem.hh
@@ -19,7 +19,7 @@
/*!
* \file
* \ingroup LowReKEpsilonModel
- * \copydoc Dumux::LowReKEpsilonProblem
+ * \brief Low-Re k-epsilon turbulence problem base class.
*/
#ifndef DUMUX_LOWREKEPSILON_PROBLEM_HH
#define DUMUX_LOWREKEPSILON_PROBLEM_HH
diff --git a/dumux/freeflow/rans/zeroeq/problem.hh b/dumux/freeflow/rans/zeroeq/problem.hh
index 843c4029cbfeab283f3cac7d44d770fd28c03df5..f4594ac4ee8b152a48ea04607aa7e0f0d70f6602 100644
--- a/dumux/freeflow/rans/zeroeq/problem.hh
+++ b/dumux/freeflow/rans/zeroeq/problem.hh
@@ -19,7 +19,7 @@
/*!
* \file
* \ingroup ZeroEqModel
- * \copydoc Dumux::ZeroEqProblem
+ * \brief Zero-equation turbulence problem base class.
*/
#ifndef DUMUX_ZEROEQ_PROBLEM_HH
#define DUMUX_ZEROEQ_PROBLEM_HH
diff --git a/dumux/freeflow/staggeredupwindmethods.hh b/dumux/freeflow/staggeredupwindmethods.hh
index 26754bff295067f88a2bf60bf6df7fa8a623f6cb..592208dba63786a2b0bb17d2536eb0539ed0a8a2 100644
--- a/dumux/freeflow/staggeredupwindmethods.hh
+++ b/dumux/freeflow/staggeredupwindmethods.hh
@@ -38,7 +38,7 @@ enum class TvdApproach
none, uniform, li, hou
};
-//! \biraf Available differencing schemes
+//! \brief Available differencing schemes
enum class DifferencingScheme
{
none, vanleer, vanalbada, minmod, superbee, umist, mclimiter, wahyd
diff --git a/dumux/io/container.hh b/dumux/io/container.hh
index 3c5a04a9157f10a09e6af3ba93c3ecb30b570a06..7799653c783a7de070492bf60931db55b1a2fedb 100644
--- a/dumux/io/container.hh
+++ b/dumux/io/container.hh
@@ -40,6 +40,7 @@ namespace Dumux {
* \brief Writes a container to file
* \param v The container, requires begin() and end() method
* \param filename The filename to write to
+ * \param floatPrecision The total number of digits stored, including decimal
*
* usage: std::vector<double> v(5, 0.0); writeContainerToFile(v, "myvector.txt");
*/
diff --git a/dumux/io/vtk/vtkreader.hh b/dumux/io/vtk/vtkreader.hh
index 8cb862863b1d406361e1db70236ef25a7e2f4728..b69a3d9cc12e0b538e02cbb09208dd87c80f4c40 100644
--- a/dumux/io/vtk/vtkreader.hh
+++ b/dumux/io/vtk/vtkreader.hh
@@ -117,6 +117,7 @@ public:
* \brief Read a grid from a vtk/vtu/vtp file, ignoring cell and point data
* \note use this signature if the factory might be needed outside to interpret the data via the factory's insertion indices
* \param verbose if the output should be verbose
+ * \param factory the (emtpy) grid factory
*/
template<class Grid>
std::unique_ptr<Grid> readGrid(Dune::GridFactory<Grid>& factory, bool verbose = false) const
diff --git a/dumux/material/components/simpleh2o.hh b/dumux/material/components/simpleh2o.hh
index 4c15e8b9efd2a61381e86c33b97710f361efd15b..371b18026a11d7222b738f464d58742b63e95505 100644
--- a/dumux/material/components/simpleh2o.hh
+++ b/dumux/material/components/simpleh2o.hh
@@ -308,11 +308,8 @@ public:
/*!
* \brief Specific isobaric heat capacity of the component \f$\mathrm{[J/(kg*K)]}\f$ as a liquid.
- *
- * \param temperature temperature of component in \f$\mathrm{[K]}\f$
- * \param pressure pressure of component in \f$\mathrm{[Pa]}\f$
- * source: http://webbook.nist.gov/cgi/fluid.cgi?ID=C7732185&Action=Page
- * @ T= 281.15K (8°C) , p=0.1MPa)
+ * source: http://webbook.nist.gov/cgi/fluid.cgi?ID=C7732185&Action=Page
+ * @ T= 281.15K (8°C) , p=0.1MPa)
* \param temperature absolute temperature in \f$\mathrm{[K]}\f$
* \param pressure of the phase in \f$\mathrm{[Pa]}\f$
*/
diff --git a/dumux/material/fluidsystems/brineair.hh b/dumux/material/fluidsystems/brineair.hh
index 89d7908a67a9139e25951d5ae959a783f22095a3..e9f413edf4cf86cf5305e99bd87938a0e47b23f5 100644
--- a/dumux/material/fluidsystems/brineair.hh
+++ b/dumux/material/fluidsystems/brineair.hh
@@ -336,6 +336,7 @@ public:
H2O::init(tempMin, tempMax, nTemp, pressMin, pressMax, nPress);
}
+ using Base::density;
/*!
* \brief Given a phase's composition, temperature, pressure, and
* the partial pressures of all components, return its
@@ -349,7 +350,6 @@ public:
* - cited by: Bachu & Adams (2002)
* "Equations of State for basin geofluids" \cite adams2002
*/
- using Base::density;
template <class FluidState>
static Scalar density(const FluidState &fluidState, int phaseIdx)
{
@@ -386,6 +386,7 @@ public:
DUNE_THROW(Dune::InvalidStateException, "Invalid phase index " << phaseIdx);
}
+ using Base::molarDensity;
/*!
* \brief The molar density \f$\rho_{mol,\alpha}\f$
* of a fluid phase \f$\alpha\f$ in \f$\mathrm{[mol/m^3]}\f$
@@ -395,7 +396,6 @@ public:
*
* \f[\rho_{mol,\alpha} = \frac{\rho_\alpha}{\overline M_\alpha} \;.\f]
*/
- using Base::molarDensity;
template <class FluidState>
static Scalar molarDensity(const FluidState& fluidState, int phaseIdx)
{
@@ -418,6 +418,7 @@ public:
DUNE_THROW(Dune::InvalidStateException, "Invalid phase index " << phaseIdx);
}
+ using Base::viscosity;
/*!
* \brief Calculate the dynamic viscosity of a fluid phase \f$\mathrm{[Pa*s]}\f$
*
@@ -428,7 +429,6 @@ public:
* component is neglected. This contribution is probably not big, but somebody
* would have to find out its influence.
*/
- using Base::viscosity;
template <class FluidState>
static Scalar viscosity(const FluidState& fluidState, int phaseIdx)
{
@@ -440,6 +440,7 @@ public:
return Air::gasViscosity(fluidState.temperature(phaseIdx), fluidState.pressure(phaseIdx));
}
+ using Base::fugacityCoefficient;
/*!
* \brief Returns the fugacity coefficient \f$\mathrm{[-]}\f$ of a component in a
* phase.
@@ -461,7 +462,6 @@ public:
* Henry constant for the solutes and the saturated vapor pressure
* both divided by phase pressure.
*/
- using Base::fugacityCoefficient;
template <class FluidState>
static Scalar fugacityCoefficient(const FluidState& fluidState, int phaseIdx, int compIdx)
{
@@ -505,6 +505,7 @@ public:
DUNE_THROW(Dune::NotImplemented, "Diffusion coefficients");
}
+ using Base::binaryDiffusionCoefficient;
/*!
* \brief Given a phase's composition, temperature and pressure,
* return the binary diffusion coefficient \f$\mathrm{[m^2/s]}\f$ for components
@@ -515,7 +516,6 @@ public:
* \param compIIdx The index of the first component to consider
* \param compJIdx The index of the second component to consider
*/
- using Base::binaryDiffusionCoefficient;
template <class FluidState>
static Scalar binaryDiffusionCoefficient(const FluidState& fluidState,
int phaseIdx,
@@ -563,6 +563,7 @@ public:
DUNE_THROW(Dune::InvalidStateException, "Invalid phase index " << phaseIdx);
}
+ using Base::enthalpy;
/*!
* \brief Given a phase's composition, temperature and pressure,
* return its specific enthalpy \f$\mathrm{[J/kg]}\f$.
@@ -582,7 +583,6 @@ public:
* is neglected. This contribution is probably not big. Somebody would have to
* find out the enthalpy of solution for this system. ...
*/
- using Base::enthalpy;
template <class FluidState>
static Scalar enthalpy(const FluidState& fluidState, int phaseIdx)
{
@@ -637,6 +637,7 @@ public:
DUNE_THROW(Dune::InvalidStateException, "Invalid phase index " << phaseIdx);
}
+ using Base::thermalConductivity;
/*!
* \brief Thermal conductivity of a fluid phase \f$\mathrm{[W/(m K)]}\f$.
* \param fluidState An abitrary fluid state
@@ -646,7 +647,6 @@ public:
* components is neglected. This contribution is probably not big, but somebody
* would have to find out its influence.
*/
- using Base::thermalConductivity;
template <class FluidState>
static Scalar thermalConductivity(const FluidState& fluidState, int phaseIdx)
{
diff --git a/dumux/multidomain/facet/gridmanager.hh b/dumux/multidomain/facet/gridmanager.hh
index 5f7d694f9e0a2054270a148d3eeb1f806cca3287..5e6fa82532ce76d58b0ad04e57963adf07fcd344 100644
--- a/dumux/multidomain/facet/gridmanager.hh
+++ b/dumux/multidomain/facet/gridmanager.hh
@@ -245,8 +245,8 @@ public:
* \param gridFactoryPtr shared pointer to this (id-th) grid factory
* \param embeddedEntityMap map containing the lower-dimensional entities for this grid's elements
* \param adjoinedEntityMap map containing the (d+1)-dimensional elements in which this grid's elements are embedded in
- * \param lowDimGridVertexIndices the hierachy's insertion indices that make up this grid
- * (only necessary for lower-dimensional grids)
+ * \param gridVertexIndices \todo Doc me!
+ * \param numVerticesInHierarchy \todo Doc me!
*/
template<std::size_t id>
void setData( std::shared_ptr<Grid<id>> gridPtr,
diff --git a/dumux/nonlinear/newtonconvergencewriter.hh b/dumux/nonlinear/newtonconvergencewriter.hh
index 6d06350ed547ac3f5c3b8c1e11fe6aa3f37dfb4e..ac5c7cd78337281afb0253a4ea1758e2bf112aab 100644
--- a/dumux/nonlinear/newtonconvergencewriter.hh
+++ b/dumux/nonlinear/newtonconvergencewriter.hh
@@ -62,9 +62,8 @@ class NewtonConvergenceWriter : public ConvergenceWriterInterface<SolutionVector
public:
/*!
* \brief Constructor
- * \param gridView the grid view we are solving on
- * \param size the size of the solution data
- * \param name base name of the vtk output
+ * \param fvGridGeometry The finite-volume grid geometry
+ * \param name Base name of the vtk output
*/
NewtonConvergenceWriter(const FVGridGeometry& fvGridGeometry,
const std::string& name = "newton_convergence")
diff --git a/dumux/porousmediumflow/2p2c/sequential/fvpressure.hh b/dumux/porousmediumflow/2p2c/sequential/fvpressure.hh
index 10d8df265d560c8ad53e001c9b9370e7c640e077..cbe2b1b257e66cf85d789879a16ebd31ba1e5531 100644
--- a/dumux/porousmediumflow/2p2c/sequential/fvpressure.hh
+++ b/dumux/porousmediumflow/2p2c/sequential/fvpressure.hh
@@ -897,7 +897,7 @@ void FVPressure2P2C<TypeTag>::getFluxOnBoundary(Dune::FieldVector<Scalar, 2>& en
* primary variables. In case the method is called after the Transport,
* i.e. at the end / post time step, CellData2p2c.reset() resets the volume
* derivatives for the next time step.
- * \param elementI The element
+ * \param element The element
* \param postTimeStep Flag indicating if we have just completed a time step
*/
template<class TypeTag>
diff --git a/dumux/porousmediumflow/2pnc/model.hh b/dumux/porousmediumflow/2pnc/model.hh
index f7b7ff12d85e3e4cf9df7d26f2e61b8c36359eef..e6cf04b26bf880587e616976ce892191d2e13de0 100644
--- a/dumux/porousmediumflow/2pnc/model.hh
+++ b/dumux/porousmediumflow/2pnc/model.hh
@@ -28,23 +28,23 @@
* The solid phases. The standard multiphase Darcy
* approach is used as the equation for the conservation of momentum:
* \f[
- v_\alpha = - \frac{k_{r\alpha}}{\mu_\alpha} \mbox{\bf K}
- \left(\text{grad}\, p_\alpha - \varrho_{\alpha} \mbox{\bf g} \right)
+ * v_\alpha = - \frac{k_{r\alpha}}{\mu_\alpha} \mbox{\bf K}
+ * \left(\text{grad}\, p_\alpha - \varrho_{\alpha} \mbox{\bf g} \right)
* \f]
*
* By inserting this into the equations for the conservation of the
* components, one gets one transport equation for each component
- * \f{eqnarray}
- && \frac{\partial (\sum_\alpha \varrho_\alpha X_\alpha^\kappa \phi S_\alpha )}
- {\partial t}
- - \sum_\alpha \text{div} \left\{ \varrho_\alpha X_\alpha^\kappa
- \frac{k_{r\alpha}}{\mu_\alpha} \mbox{\bf K}
- (\text{grad}\, p_\alpha - \varrho_{\alpha} \mbox{\bf g}) \right\}
- \nonumber \\ \nonumber \\
- &-& \sum_\alpha \text{div} \left\{{\bf D_{\alpha, pm}^\kappa} \varrho_{\alpha} \text{grad}\, X^\kappa_{\alpha} \right\}
- - \sum_\alpha q_\alpha^\kappa = 0 \qquad \kappa \in \{w, a,\cdots \} \, ,
- \alpha \in \{w, g\}
- \f}
+ * \f{eqnarray*}{
+ * && \frac{\partial (\sum_\alpha \varrho_\alpha X_\alpha^\kappa \phi S_\alpha )}
+ * {\partial t}
+ * - \sum_\alpha \text{div} \left\{ \varrho_\alpha X_\alpha^\kappa
+ * \frac{k_{r\alpha}}{\mu_\alpha} \mbox{\bf K}
+ * (\text{grad}\, p_\alpha - \varrho_{\alpha} \mbox{\bf g}) \right\}
+ * \nonumber \\ \nonumber \\
+ * &-& \sum_\alpha \text{div} \left\{{\bf D_{\alpha, pm}^\kappa} \varrho_{\alpha} \text{grad}\, X^\kappa_{\alpha} \right\}
+ * - \sum_\alpha q_\alpha^\kappa = 0 \qquad \kappa \in \{w, a,\cdots \} \, ,
+ * \alpha \in \{w, g\}
+ * \f}
*
* The solid or mineral phases are assumed to consist of a single component.
* Their mass balance consist only of a storage and a source term:
diff --git a/dumux/porousmediumflow/2pncmin/model.hh b/dumux/porousmediumflow/2pncmin/model.hh
index 98bf40124ffcc6f8e3ff9b97ca0d3ecafa09c34a..f958a723a6ecd63080b24d91a950c79a960ae88d 100644
--- a/dumux/porousmediumflow/2pncmin/model.hh
+++ b/dumux/porousmediumflow/2pncmin/model.hh
@@ -28,23 +28,23 @@
* The solid phases. The standard multiphase Darcy
* approach is used as the equation for the conservation of momentum:
* \f[
- v_\alpha = - \frac{k_{r\alpha}}{\mu_\alpha} \mbox{\bf K}
- \left(\text{grad}\, p_\alpha - \varrho_{\alpha} \mbox{\bf g} \right)
+ * v_\alpha = - \frac{k_{r\alpha}}{\mu_\alpha} \mbox{\bf K}
+ * \left(\text{grad}\, p_\alpha - \varrho_{\alpha} \mbox{\bf g} \right)
* \f]
*
* By inserting this into the equations for the conservation of the
* components, one gets one transport equation for each component
- * \f{eqnarray}
- && \frac{\partial (\sum_\alpha \varrho_\alpha X_\alpha^\kappa \phi S_\alpha )}
- {\partial t}
- - \sum_\alpha \text{div} \left\{ \varrho_\alpha X_\alpha^\kappa
- \frac{k_{r\alpha}}{\mu_\alpha} \mbox{\bf K}
- (\text{grad}\, p_\alpha - \varrho_{\alpha} \mbox{\bf g}) \right\}
- \nonumber \\ \nonumber \\
- &-& \sum_\alpha \text{div} \left\{{\bf D_{\alpha, pm}^\kappa} \varrho_{\alpha} \text{grad}\, X^\kappa_{\alpha} \right\}
- - \sum_\alpha q_\alpha^\kappa = 0 \qquad \kappa \in \{w, a,\cdots \} \, ,
- \alpha \in \{w, g\}
- \f}
+ * \f{eqnarray*}{
+ * && \frac{\partial (\sum_\alpha \varrho_\alpha X_\alpha^\kappa \phi S_\alpha )}
+ * {\partial t}
+ * - \sum_\alpha \text{div} \left\{ \varrho_\alpha X_\alpha^\kappa
+ * \frac{k_{r\alpha}}{\mu_\alpha} \mbox{\bf K}
+ * (\text{grad}\, p_\alpha - \varrho_{\alpha} \mbox{\bf g}) \right\}
+ * \nonumber \\ \nonumber \\
+ * &-& \sum_\alpha \text{div} \left\{{\bf D_{\alpha, pm}^\kappa} \varrho_{\alpha} \text{grad}\, X^\kappa_{\alpha} \right\}
+ * - \sum_\alpha q_\alpha^\kappa = 0 \qquad \kappa \in \{w, a,\cdots \} \, ,
+ * \alpha \in \{w, g\}
+ * \f}
*
* The solid or mineral phases are assumed to consist of a single component.
* Their mass balance consist only of a storage and a source term:
diff --git a/test/freeflow/rans/problem.hh b/test/freeflow/rans/problem.hh
index ddbbdbab1289ec2f2c3b46c4cd8922a4a9833617..0d17ceefee170157b2ccad3f88dfa4dd5e163b2e 100644
--- a/test/freeflow/rans/problem.hh
+++ b/test/freeflow/rans/problem.hh
@@ -252,6 +252,7 @@ public:
* \param element The finite element
* \param fvGeometry The finite-volume geometry
* \param scv The sub control volume
+ * \param pvIdx The primary variable index in the solution vector
*/
template<class Element, class FVElementGeometry, class SubControlVolume>
bool isDirichletCell(const Element& element,
diff --git a/test/freeflow/ransnc/problem.hh b/test/freeflow/ransnc/problem.hh
index 1cef2595a92717a636167d83a30ff3d1b74b857b..13df079f3f7e8387ef349ebc51e80b9f8ae730a2 100644
--- a/test/freeflow/ransnc/problem.hh
+++ b/test/freeflow/ransnc/problem.hh
@@ -264,6 +264,7 @@ public:
* \param element The finite element
* \param fvGeometry The finite-volume geometry
* \param scv The sub control volume
+ * \param pvIdx The primary variable index in the solution vector
*/
template<class Element, class FVElementGeometry, class SubControlVolume>
bool isDirichletCell(const Element& element,
diff --git a/test/porousmediumflow/1p/implicit/convergence/problem.hh b/test/porousmediumflow/1p/implicit/convergence/problem.hh
index f0bfd880a92b570db9e19b0b9e34b1edbb39198b..72b99d09f715f8d8718ca2ae02e3cb89e6a0c971 100644
--- a/test/porousmediumflow/1p/implicit/convergence/problem.hh
+++ b/test/porousmediumflow/1p/implicit/convergence/problem.hh
@@ -181,7 +181,6 @@ public:
/*!
* \brief Returns the temperature \f$\mathrm{[K]}\f$ for an isothermal problem.
- * \param globalPos The center of the finite volume for which it is to be set.
*/
Scalar temperature() const
{ return 283.15; }
diff --git a/test/porousmediumflow/1pnc/implicit/1p2c/nonisothermal/convection/problem.hh b/test/porousmediumflow/1pnc/implicit/1p2c/nonisothermal/convection/problem.hh
index 8475502ad83c2519f6f8c79f56db9242f367706e..641744bedc2b87cafe1b1974c676b218262420d0 100644
--- a/test/porousmediumflow/1pnc/implicit/1p2c/nonisothermal/convection/problem.hh
+++ b/test/porousmediumflow/1pnc/implicit/1p2c/nonisothermal/convection/problem.hh
@@ -300,6 +300,7 @@ public:
* \param element The finite element
* \param fvGeometry The finite-volume geometry
* \param elemVolVars All volume variables for the element
+ * \param elemFluxVarsCache The cache related to flux computation
* \param scvf The sub-control volume face
*
* For this method, the \a values parameter stores the flux