Large-scale poroelastic fractured reservoirs modeling using the fast multipole displacement discontinuity method

被引:5
作者
Verde, A. [1 ]
Ghassemi, A. [2 ]
机构
[1] Texas A&M Univ, Dept Comp Sci & Engn, College Stn, TX 77843 USA
[2] Univ Oklahoma, Mewbourne Sch Petr & Geol Engn, Norman, OK 73019 USA
关键词
displacement discontinuity method; fast multipole method; geothermal; natural fracture network; shale oil/gas; poroelastic rock; ALGORITHM;
D O I
10.1002/nag.2430
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
An effective approach to modeling the geomechanical behavior of the network and its permeability variation is to use a poroelastic displacement discontinuity method (DDM). However, the approach becomes rather computationally intensive for an extensive system of cracks, particularly when considering coupled diffusion/deformation processes. This is because of additional unknowns and the need for time-marching schemes for the numerical integration. The Fast Multipole Method (FMM) is a technique that can accelerate the solution of large fracture problems with linear complexity with the number of unknowns both in memory and CPU time. Previous works combining DDM and FMM for large-scale problems have accounted only for elastic rocks, neglecting the fluid leak-off from the fractures into the matrix and its influence on pore pressure and stress field. In this work we develop an efficient geomechanical model for large-scale natural fracture networks in poroelastic reservoirs with fracture flow in response to injection and production operations. Accuracy and computational performance of the proposed method with those of conventional poroelastic DDM are compared through several case studies involving up to several tens of thousands of boundary elements. The results show the effectiveness of the FMM approach to successfully evaluate field-scale problems for the design of exploitation strategies in unconventional geothermal and petroleum reservoirs. An example considering faults reveals the impact of reservoir compartmentalization because of sealing faults for both geomechanical and flow variables under elastic and poroelastic rocks. Copyright (C) 2015 John Wiley & Sons, Ltd.
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页码:865 / 886
页数:22
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