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Sequential Methods for Coupled Geomechanics and Multiphase Flow

Sequential Methods for Coupled Geomechanics and Multiphase Flow

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4.4. NUMERICAL EXAMPLES 113<br />

P d =P/P i<br />

u x /L x<br />

1.8<br />

1.7<br />

1.6<br />

1.5<br />

1.4<br />

1.3<br />

1.2<br />

1.1<br />

1<br />

0.9<br />

P d at the top layer by Drained<br />

∆ t d =2.06×10 −3 10 iter<br />

∆ t d =2.06×10 −4 1 iter<br />

True solution<br />

0.8<br />

0 0.5 1 1.5<br />

x/Lx<br />

0.9<br />

0.8<br />

0.7<br />

0.6<br />

0.5<br />

0.4<br />

0.3<br />

0.2<br />

0.1<br />

x 10−3<br />

1<br />

u x /L x at the top layer by Drained<br />

∆ t d =2.06×10 −4 1 iter<br />

∆ t d =2.06×10 −3 10 iter<br />

True solution<br />

0<br />

0 0.5 1 1.5<br />

x/Lx<br />

Figure 4.14: Comparison between more iterations <strong>and</strong> refined time step size in the drained<br />

split <strong>for</strong> Case 4.2: pressure (top) <strong>and</strong> displacement (bottom).

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