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Sequential Methods for Coupled Geomechanics and Multiphase Flow

Sequential Methods for Coupled Geomechanics and Multiphase Flow

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58 CHAPTER 3. STABILITY OF THE DRAINED AND UNDRAINED SPLITS<br />

3.7 Numerical Examples<br />

We use five test cases to compare the various coupling strategies.<br />

Case 3.1 The Terzaghi problem in a 1D linear poroelastic medium (the left picture in<br />

Figure 3.7). The driving mechanical <strong>for</strong>ce is provided by the overburden.<br />

Case 3.2 Injection <strong>and</strong> production in a 1D poroelastic medium. The driving <strong>for</strong>ce is due to<br />

injection <strong>and</strong> production (the right picture in Figure 3.7).<br />

Case 3.3 The M<strong>and</strong>el problem in a 2D elastic medium. The driving <strong>for</strong>ce is provided by<br />

the side burden (the left picture in Figure 3.8).<br />

Case 3.4 Injection <strong>and</strong> production in a 1D poro-elasto-plastic medium with isotropic hard-<br />

ening. The driving <strong>for</strong>ce is due to injection <strong>and</strong> production (the right picture in<br />

Figure 3.7).<br />

Case 3.5 Fluid production in 2D with elasto-plastic behavior described by the modified<br />

Cam-clay model. The compaction of the reservoir occurs due to production (the right<br />

picture in Figure 3.8).<br />

The numerical results are based on one iteration per time step (i.e., staggered method)<br />

unless noted explicitly otherwise.<br />

3.7.1 Numerical results <strong>for</strong> elasticity<br />

Case 3.1—The Terzaghi problem<br />

We have drainage boundaries <strong>for</strong> flow at the top <strong>and</strong> bottom, where the boundary fluid<br />

pressure is Pbc = 2.125 MPa. The overburden is ¯σ = 2 × 2.125 MPa at the top, <strong>and</strong> a no-<br />

displacement boundary condition is applied to the bottom. The domain has 20 grid blocks.<br />

The length of the domain is Lz = 40 m with grid spacing ∆z = 2 m. The bulk density of<br />

the porous medium is ρb = 2400 kg m −1 . Initial fluid pressure is Pi = 2.125 MPa. Fluid<br />

density <strong>and</strong> viscosity are ρf,0 = 1000 kg m −1 <strong>and</strong> µ = 1.0 cp, respectively. Permeability is

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