Searched for: department%3A%22Geoscience%255C%252B%2526%255C%252BEngineering%22
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document
Wang, Y. (author), Hajibeygi, H. (author), Tchelepi, H.A. (author)
The MultiScale Finite Volume (MSFV) method is known to produce non-monotone solutions. The causes of the non-monotone solutions are identified and connected to the local flux across the boundaries of primal coarse cells induced by the basis functions. We propose a monotone MSFV (m-MSFV) method based on a local stencil-fix that guarantees...
journal article 2015
document
Tene, M. (author), Hajibeygi, H. (author), Wang, Y. (author), Tchelepi, H.A. (author)
An adaptive Algebraic Multiscale Solver for Compressible (C-AMS) flow in heterogeneous oil reservoirs is developed. Based on the recently developed AMS [Wang et al., 2014] for incompressible linear flows, the C-AMS extends the algebraic formulation of the multiscale methods for compressible (nonlinear) flows. Several types of basis functions ...
conference paper 2014
document
Wang, Y. (author), Hajibeygi, H. (author), Tchelepi, H.A. (author)
The MultiScale Finite-Volume (MSFV) method is known to produce non-monotone solutions. The causes of the non-monotone solutions are identified and connected to the local flux across the boundaries of primal coarse cells induced by the basis functions. We propose a monotone MSFV (m-MSFV) method based on a local stencil-fix that guarantees...
conference paper 2014
document
Cusini, M. (author), Lukyanov, A. (author), Natvig, J. (author), Hajibeygi, H. (author)
Unconventional Reservoir simulations involve several challenges not only arising from geological heterogeneities, but also from strong nonlinear physical coupling terms. All exiting upscaling and multiscale methods rely on a classical sequential formulation to treat the coupling between the nonlinear flow-transport equations. Unfortunately, the...
conference paper 2014
document
Hajibeygi, H. (author), Tchelepi, H.A. (author)
conference paper 2013
Searched for: department%3A%22Geoscience%255C%252B%2526%255C%252BEngineering%22
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