Added computeTransportSource() function. Handling bdy fluxes in spu_2p.

This commit is contained in:
Atgeirr Flø Rasmussen 2012-03-12 13:00:48 +01:00
parent 38aaa867bb
commit 03200bbf37
2 changed files with 64 additions and 0 deletions

View File

@ -141,6 +141,48 @@ namespace Opm
}
}
/// Compute two-phase transport source terms from face fluxes,
/// and pressure equation source terms. This puts boundary flows
/// into the source terms for the transport equation.
/// \param[in] grid The grid used.
/// \param[in] src Pressure eq. source terms. The sign convention is:
/// (+) positive total inflow (positive velocity divergence)
/// (-) negative total outflow
/// \param[in] faceflux Signed face fluxes, typically the result from a flow solver.
/// \param[in] inflow_frac Fraction of inflow that consists of first phase.
/// Example: if only water is injected, inflow_frac == 1.0.
/// Note: it is not possible (with this method) to use different fractions
/// for different inflow sources, be they source terms of boundary flows.
/// \param[out] transport_src The transport source terms. They are to be interpreted depending on sign:
/// (+) positive inflow of first phase (water)
/// (-) negative total outflow of both phases
void computeTransportSource(const UnstructuredGrid& grid,
const std::vector<double>& src,
const std::vector<double>& faceflux,
const double inflow_frac,
std::vector<double>& transport_src)
{
int nc = grid.number_of_cells;
transport_src.resize(nc);
for (int c = 0; c < nc; ++c) {
transport_src[c] = 0.0;
transport_src[c] += src[c] > 0.0 ? inflow_frac*src[c] : src[c];
for (int hf = grid.cell_facepos[c]; hf < grid.cell_facepos[c + 1]; ++hf) {
int f = grid.cell_faces[hf];
const int* f2c = &grid.face_cells[2*f];
double bdy_influx = 0.0;
if (f2c[0] == c && f2c[1] == -1) {
bdy_influx = -faceflux[f];
} else if (f2c[0] == -1 && f2c[1] == c) {
bdy_influx = faceflux[f];
}
if (bdy_influx != 0.0) {
transport_src[c] += bdy_influx > 0.0 ? inflow_frac*bdy_influx : bdy_influx;
}
}
}
}
/// @brief Estimates a scalar cell velocity from face fluxes.
/// @param[in] grid a grid
/// @param[in] face_flux signed per-face fluxes

View File

@ -73,6 +73,27 @@ namespace Opm
std::vector<double>& totmob,
std::vector<double>& omega);
/// Compute two-phase transport source terms from face fluxes,
/// and pressure equation source terms. This puts boundary flows
/// into the source terms for the transport equation.
/// \param[in] grid The grid used.
/// \param[in] src Pressure eq. source terms. The sign convention is:
/// (+) positive total inflow (positive velocity divergence)
/// (-) negative total outflow
/// \param[in] faceflux Signed face fluxes, typically the result from a flow solver.
/// \param[in] inflow_frac Fraction of inflow that consists of first phase.
/// Example: if only water is injected, inflow_frac == 1.0.
/// Note: it is not possible (with this method) to use different fractions
/// for different inflow sources, be they source terms of boundary flows.
/// \param[out] transport_src The transport source terms. They are to be interpreted depending on sign:
/// (+) positive inflow of first phase (water)
/// (-) negative total outflow of both phases
void computeTransportSource(const UnstructuredGrid& grid,
const std::vector<double>& src,
const std::vector<double>& faceflux,
const double inflow_frac,
std::vector<double>& transport_src);
/// @brief Estimates a scalar cell velocity from face fluxes.
/// @param[in] grid a grid
/// @param[in] face_flux signed per-face fluxes
@ -91,6 +112,7 @@ namespace Opm
void toBothSat(const std::vector<double>& sw,
std::vector<double>& sboth);
} // namespace Opm
#endif // OPM_MISCUTILITIES_HEADER_INCLUDED