2014
DOI: 10.1002/nme.4682
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An offline–online homogenization strategy to solve quasilinear two‐scale problems at the cost of one‐scale problems

Abstract: SUMMARYInspired by recent analyses of the finite element heterogeneous multiscale method and the reduced basis technique for nonlinear problems, we present a simple and concise finite element algorithm for the reliable and efficient resolution of elliptic or parabolic multiscale problems of nonmonotone type. Solutions of appropriate cell problems on sampling domains are selected by a greedy algorithm in an offline stage and assembled in a reduced basis (RB). This RB is then used in an online stage to solve two… Show more

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Cited by 16 publications
(19 citation statements)
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“…For other approaches to decrease the computational burden in linear and quasi-linear elliptic multiscale PDEs see e.g. [6][7][8].…”
Section: The Heterogeneous Multiscale Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…For other approaches to decrease the computational burden in linear and quasi-linear elliptic multiscale PDEs see e.g. [6][7][8].…”
Section: The Heterogeneous Multiscale Methodsmentioning
confidence: 99%
“…where û is given in (8). For an analysis of the FEM version of the HMM for elliptic problems we refer the reader to [9], see also [10] for a fully discrete analysis.…”
Section: The Heterogeneous Multiscale Methodsmentioning
confidence: 99%
“…Following [5] we propose a linearized scheme. The idea is to decouple the micro-solutions in (99) and to consider…”
Section: A Linearized Methodsmentioning
confidence: 99%
“…We next mention classical estimates for FEM with numerical quadrature that are needed in the analysis below [23,Thms 4,5]. Assuming (Q1) and appropriate regularity of the homogenised solution u 0 we have for all v H , w H ∈ S 0 (Ω , T H ) (where µ = 0 or 1),…”
Section: Lemmamentioning
confidence: 99%
“…As mentioned in §5a, for this type of nonlinear problem, we have cell problems defined in ( with κ = (x, s). The offline settings and outputs can be seen in table 5, where the parameter range of s is estimated by an offline procedure proposed in [62]. Online stage.…”
Section: (C) Richards Equation In An Unsaturated Soil Domainmentioning
confidence: 99%