2019
DOI: 10.1007/s10596-019-9827-z
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Accelerating multiscale simulation of complex geomodels by use of dynamically adapted basis functions

Abstract: A number of different multiscale methods have been developed as a robust alternative to upscaling and as a means for accelerated reservoir simulation of high-resolution geomodels. In their basic setup, multiscale methods use a restriction operator to construct a reduced system of flow equations on a coarser grid, and a prolongation operator to map pressure unknowns from the coarse grid back to the original simulation grid. The prolongation operator consists of basis functions computed numerically by solving lo… Show more

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Cited by 12 publications
(9 citation statements)
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“…Conservation of mass in each block, as defined in Eq. 17, is then enforced by multiplying the saturation by a saturation discrepancy (see Klemetsdal et al 2019b for details). Altogether, this ensures that the mapping is both mass conservative and consistent with the flow model.…”
Section: Dynamic Coarseningmentioning
confidence: 99%
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“…Conservation of mass in each block, as defined in Eq. 17, is then enforced by multiplying the saturation by a saturation discrepancy (see Klemetsdal et al 2019b for details). Altogether, this ensures that the mapping is both mass conservative and consistent with the flow model.…”
Section: Dynamic Coarseningmentioning
confidence: 99%
“…However, careful examination of several numerical examples conducted on real field models indicates that even in cases with strong gravity effects, cells belonging to a connected component only amount to a small fraction of the total number of grid cells. Some of these results are reported in Klemetsdal et al (2019bKlemetsdal et al ( , 2019d. One can also use a nonlinear Gauss-Seidel solver Lie et al 2014) in LRNTS, in which the nodes in a connected component are solved sequentially in a predefined order with variables in all other nodes fixed.…”
Section: Localized Nonlinear Solversmentioning
confidence: 99%
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