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Incorporate transmissibility into water flux definition.
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).
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@ -403,6 +403,8 @@ int main()
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double res_norm = 1e100;
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V s1 = /*s0.leftCols<1>()*/0.5*V::Ones(nc,1); // Initial guess.
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UpwindSelector<double> upws(grid, ops);
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const ADB nkdp = (ADB::constant(transi , block_pattern) *
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ADB::constant(ops.ngrad * p1.matrix(), block_pattern));
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do {
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const std::vector<int>& bp = block_pattern;
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ADB s = ADB::variable(0, s1, bp);
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@ -411,16 +413,11 @@ int main()
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* Eigen::Map<const V>(grid.cell_volumes, nc, 1);
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V dtpv = dt/pv;
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// std::cout << dtpv;
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V ngradp1 = ops.ngrad*p1.matrix();
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// std::cout << ngradp1 << std::endl;
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std::vector<ADB> pmobc = phaseMobility<ADB>(props, allcells, s.value());
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std::vector<ADB> pmobf = upws.select(p1, pmobc);
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ADB fw_cell = fluxFunc(pmobc);
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ADB fw_face = fluxFunc(pmobf);
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// std::cout << fw_face;
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ADB flux1 = fw_face*ADB::constant(ngradp1, bp);
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ADB flux1 = pmobf[0] * nkdp;
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// std::cout << flux1;
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V qneg = dtpv*q;
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V qpos = dtpv*q;
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