A space-time multigrid method for poroelasticity equations with random hydraulic conductivity

• Published in: Numerical heat transfer. Part B, Fundamentals Fundamentals, 2024-09, Vol.85 (9), p.1226-1235
• Main Authors: Franco, Sebastião Romero, Pinto, Marcio Augusto Villela
• Format: Article
• Language: English
• Subjects: Algorithms; Biot's model; fixed-stress; Hydraulic conductivity; Hydraulics; MSC 65F10; MSC 65M06; MSC 65M22; MSC 65M55; Multigrid methods; PACS 02.60.Cb; PACS 02.70.Bf; PACS 47.56.+r; PACS 91.60.Np; Poroelasticity; random coefficients; Solvers; Spacetime; standard coarsening; Stress relaxation; Thermodynamics
• ISSN: 1040-7790; 1521-0626
• DOI: 10.1080/10407790.2023.2262746

In this work, we propose a space-time multigrid method for solving a finite difference discretization of the linear Biot's model in two space dimensions considering random hydraulic conductivity. This method is an extension of the one developed by Franco et al. [ 1 ] and which was applied to the heat equation. Particularly for the poroelasticity problem, we need to use the Tri-Diagonal Matrix Algorithm (TDMA) for systems of equations with multiple variables (block TDMA) solver on the planes xt and yt with zebra-type wise-manner (the domain is divided into planes and solve each odd plane first and then each even plane independently [ 2 ]). On the planes xy, the F-cycle multigrid with fixed-stress smoother is improved by red-black relaxation. A fixed-stress smoother is compound solver, where the mechanical and flow parts are addressed by two distinctive solvers and symmetric Gauss-Seidel iteration. This is the basis of the proposed method which does not converge only with the standard line-in-time red-black solver [ 1 ]. This combination allows the code parallelization. The use of standard coarsening associated with line or plane smoothers in the strong coupling direction allows an application in real world problems and, in particular, the random hydraulic conductivity case. This would not be possible using the standard space-time method with semicoarsening in the strong coupling direction. The spatial and temporal approximations of the problem are performed, respectively, by using Central Difference Scheme (CDS) and implicit Euler methods. The robustness and excellent performance of the multigrid method, even with random hydraulic conductivity, are illustrated with numerical experiments through the average convergence factor.