Validation of the multiscale mixed finite-element method

被引:13
作者
Pal, Mayur [1 ]
Lamine, Sadok [2 ]
Lie, Knut-Andreas [3 ]
Krogstad, Stein [3 ]
机构
[1] Maersk Oil & Gas, Copenhagen, Denmark
[2] Shell Int, Rijswijk, Netherlands
[3] SINTEF ICT, N-0314 Oslo, Norway
关键词
multiscale methods; mimetic methods; basis functions; geological modeling; reservoir simulation; upscaling; fractures; barriers; BLACK-OIL MODEL; POROUS-MEDIA; VOLUME METHOD; MISCIBLE DISPLACEMENT; QUADRILATERAL GRIDS; POLYHEDRAL MESHES; ELLIPTIC PROBLEMS; FLOW; SIMULATION; DISCRETIZATION;
D O I
10.1002/fld.3978
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
Subsurface reservoirs generally have a complex description in terms of both geometry and geology. This poses a continuing challenge in modeling and simulation of petroleum reservoirs owing to variations of static and dynamic properties at different length scales. Multiscale methods constitute a promising approach that enables efficient simulation of geological models while retaining a level of detail in heterogeneity that would not be possible via conventional upscaling methods. Multiscale methods developed to solve coupled flow equations for reservoir simulation are based on a hierarchical strategy in which the pressure equation is solved on a coarsened grid and the transport equation is solved on the fine grid, and the two equations are treated as a decoupled system. In particular, the multiscale mixed finite-element (MsMFE) method attempts to capture subgrid geological heterogeneity directly into the coarse-scale equations via a set of numerically computed basis functions. These basis functions are able to capture the predominant multiscale information and are coupled through a global formulation to provide good approximation of the subsurface flow solution. In the literature, the general formulation of the MsMFE method for incompressible two-phase and compressible three-phase flow has mainly addressed problems with idealized flow physics. In this paper, we first outline a recent formulation that accounts for compressibility, gravity, and spatially dependent rock-fluid parameters. Then, we validate the method by evaluating its computational efficiency and accuracy on a series of representative benchmark tests that have a high degree of realism with respect to flow physics, heterogeneity in the petrophysical models, and geometry/topology of the corner-point grids. In particular, the MsMFE method is validated and compared against an industry-standard fine-scale solver. The fine-scale flux, pressure, and saturation fields computed by the multiscale simulation show a noteworthy improvement in resolution and accuracy compared with coarse-scale models. Copyright (c) 2014 John Wiley & Sons, Ltd.
引用
收藏
页码:206 / 223
页数:18
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