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Incorporate transmissibility into water flux definition.

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This means that we're computing the correct solution for dt=0.0005 (as
verified by 'sim_simple.m', but we're still failing larger time steps).
This commit is contained in:
Bård Skaflestad 2013-05-05 16:44:51 +02:00
parent 8b12d1506d
commit e31101e80f
1 changed files with 3 additions and 6 deletions
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9
sim_simple.cpp
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@ -403,6 +403,8 @@ int main()
double res_norm = 1e100;
V s1 = /*s0.leftCols<1>()*/0.5*V::Ones(nc,1); // Initial guess.
UpwindSelector<double> upws(grid, ops);
const ADB nkdp = (ADB::constant(transi , block_pattern) *
ADB::constant(ops.ngrad * p1.matrix(), block_pattern));
do {
const std::vector<int>& bp = block_pattern;
ADB s = ADB::variable(0, s1, bp);
@ -411,16 +413,11 @@ int main()
* Eigen::Map<const V>(grid.cell_volumes, nc, 1);
V dtpv = dt/pv;
// std::cout << dtpv;
V ngradp1 = ops.ngrad*p1.matrix();
// std::cout << ngradp1 << std::endl;
std::vector<ADB> pmobc = phaseMobility<ADB>(props, allcells, s.value());
std::vector<ADB> pmobf = upws.select(p1, pmobc);
ADB fw_cell = fluxFunc(pmobc);
ADB fw_face = fluxFunc(pmobf);
// std::cout << fw_face;
ADB flux1 = fw_face*ADB::constant(ngradp1, bp);
ADB flux1 = pmobf[0] * nkdp;
// std::cout << flux1;
V qneg = dtpv*q;
V qpos = dtpv*q;