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Sequential Methods for Coupled Geomechanics and Multiphase Flow

Sequential Methods for Coupled Geomechanics and Multiphase Flow

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1.3. STABILITY OF SEQUENTIAL SCHEMES 5<br />

coupled flow–mechanics simulation, it is desirable to develop sequential solution methods<br />

that can be competitive with the fully coupled approach. <strong>Sequential</strong>, or staggered, solution<br />

schemes offer wide flexibility <strong>and</strong> are highly desirable from a software engineering perspec-<br />

tive. Moreover, sequential schemes allow <strong>for</strong> using specialized numerical methods <strong>for</strong> each of<br />

the mechanics <strong>and</strong> flow problems (Felippa <strong>and</strong> Park, 1980). In a sequential solution frame-<br />

work, one uses separate software modules <strong>for</strong> mechanics <strong>and</strong> flow. Communication between<br />

the modules takes place using a clear, well-defined interface (Felippa <strong>and</strong> Park, 1980; Gai,<br />

2004; Samier <strong>and</strong> Gennaro, 2007). In such a setting, the robustness <strong>and</strong> efficiency of each<br />

simulator (module) — flow <strong>and</strong> geomechanics — are available <strong>for</strong> the coupled problem. For<br />

a sequential simulation framework to be competitive in engineering practice, it must be ro-<br />

bust across a wide range of problems <strong>and</strong> have stability <strong>and</strong> convergence properties that are<br />

similar to those enjoyed by the fully coupled method. This thesis deals with the challenge of<br />

meeting such requirements with focus on the numerical stability <strong>and</strong> convergence behaviors<br />

of sequential-implicit solution strategies.<br />

1.3 Stability of <strong>Sequential</strong> Schemes<br />

Significant ef<strong>for</strong>ts to find stable <strong>and</strong> efficient sequential methods <strong>for</strong> coupled poromechanics<br />

(or the analogous thermo-mechanics problem) have been pursued in the geotechnical <strong>and</strong><br />

computational mechanics communities (Park, 1983; Farhat et al., 1991; Armero <strong>and</strong> Simo,<br />

1992, 1993; Huang <strong>and</strong> Zienkiewicz, 1998; Armero, 1999; Soares, 2008). Most of the methods<br />

developed assume that the mechanical subproblem is solved first. Two sequential schemes<br />

are relevant here. One is called the drained split (the isothermal split in the thermo-elastic<br />

<strong>and</strong> thermo-plastic problems (Armero <strong>and</strong> Simo, 1992, 1993)), <strong>and</strong> the other one is the<br />

undrained split (Zienkiewicz et al., 1988; Armero, 1999; Jha <strong>and</strong> Juanes, 2007) (the adiabatic<br />

split in the thermo-elastic <strong>and</strong> thermo-plastic problems (Armero <strong>and</strong> Simo, 1992, 1993)).<br />

The drained split simply freezes the pressure during the mechanical step, thus allowing <strong>for</strong><br />

flow to take place. Then, the computed strain <strong>and</strong> stress fields are used when solving the<br />

flow problem. Despite its simplicity, the drained split is, at best, conditionally stable. The

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