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Sequential Methods for Coupled Geomechanics and Multiphase Flow

Sequential Methods for Coupled Geomechanics and Multiphase Flow

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154 CHAPTER 5. FIXED-STRAIN AND FIXED-STRESS SPLITS<br />

split becomes unstable during iterations (Figures 5.12). No solution by the fixed-strain<br />

split is possible after plasticity. On the other h<strong>and</strong>, the fully coupled <strong>and</strong> fixed-stress split<br />

methods provide stable results well into the plastic regime, as shown in Figure 5.12.<br />

Dimensionless pressure (P/P i )<br />

1<br />

0.9<br />

0.8<br />

0.7<br />

0.6<br />

0.5<br />

0.4<br />

Case 5.4 elastoplasticity (Full iterations )<br />

Fixed strain<br />

Fixed stress<br />

Fully coupled<br />

0.3<br />

0 0.01 0.02 0.03 0.04 0.05<br />

Dimensionless time (pore volume produced)<br />

Figure 5.12: Case 5.4 (2D production problem in elastoplastic regime). Shown is the evolution<br />

of the dimensionless pressure at the observation well against dimensionless time (pore<br />

volume produced). Once the model enters the plastic regime, the fixed-strain split becomes<br />

unstable <strong>and</strong> fails to produce a solution at all.<br />

5.6.2 Convergence<br />

The Terzaghi problem (Case 5.1) - one-dimensional consolidation - is used <strong>for</strong> convergence<br />

analysis. The coupling strength τ is 0.95, <strong>and</strong> other input data are same as Case 5.1. We<br />

determine true solutions of pressure <strong>and</strong> displacement by the fully coupled method with<br />

very small time step sizes.<br />

Figure 5.13 shows the errors between the true <strong>and</strong> numerical solutions using the fixed-<br />

strain, fixed-stress, <strong>and</strong> fully coupled methods with respect to time step size when a fixed<br />

number of iterations is per<strong>for</strong>med. The errors in dimensionless pressure <strong>and</strong> displacement<br />

are measured by the L 2 norm.

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