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An online generalized multiscale approximation of the multipoint flux mixed finite element method
被引:1
作者:
He, Zhengkang
[1
]
Chen, Jie
[2
]
Chen, Zhangxin
[3
]
Zhang, Tong
[1
]
机构:
[1] Yantai Univ, Sch Math & Informat Sci, Yantai 264005, Peoples R China
[2] Xian Jiaotong Liverpool Univ, Sch Math & Phys, Suzhou 215123, Peoples R China
[3] Univ Calgary, Schulich Sch Engn, Dept Chem & Petr Engn, 2500 Univ Dr NW, Calgary, AB T2N 1N4, Canada
关键词:
Multipoint flux mixed finite element;
methods;
Online generalized multiscale finite;
element methods;
Darcy flow;
Full tensor permeability;
Fractured porous media;
Unstructured grids;
ELLIPTIC PROBLEMS;
MODELING FRACTURES;
FLOW;
INTERFACES;
D O I:
10.1016/j.cam.2023.115498
中图分类号:
O29 [应用数学];
学科分类号:
070104 ;
摘要:
In this paper, we develop an online generalized multiscale approximation of the multi-point flux mixed finite element method (MFMFE) for Darcy flow in highly heterogeneous porous media, which can handle full tensor permeability fields and unstructured grids with local velocity elimination. Here, for illustration of the proposed method, we will mainly consider the situation that the porous medium is filled with fractures, which usually results in unstructured grids, and the extension to the situation that the permeability is represented as a full tensor is straightforward. From the fine-grid discretization by the MFMFE method, we derive the symmetric and positive definite discrete bilinear form for both the matrix and fracture pressure, and thereby obtain the corresponding discrete weak formulation that only related to pressure. In the offline stage, we compute offline basis functions which contain the important local multiscale information of each coarse-grid block to form the initial multiscale space. In the online stage, we construct and add online basis functions to enrich the multiscale space and consequently improve the accuracy of the multiscale solution. Each offline basis function and each online basis function contains multiscale information both for matrix and fracture. We give the theoretical analysis for the convergence of the online enrichment, which shows that more sufficient initial basis functions lead to faster convergence rates. A series of numerical examples that either the permeability is a full tensor or the porous medium is filled with fractures are presented to show the performance of the multiscale method.(c) 2023 Elsevier B.V. All rights reserved.
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