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Sequential Methods for Coupled Geomechanics and Multiphase Flow

Sequential Methods for Coupled Geomechanics and Multiphase Flow

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102 CHAPTER 4. CONVERGENCE OF THE DRAINED AND UNDRAINED SPLITS<br />

Dimensionless distance (z/Lz)<br />

Dimensionless distance (z/Lz)<br />

2<br />

1.8<br />

1.6<br />

1.4<br />

1.2<br />

1<br />

0.8<br />

0.6<br />

0.4<br />

0.2<br />

Undrained (1 iteration)<br />

∆ t d =2.6×10 −2<br />

∆ t d =1.04×10 −2<br />

∆ t d =5.2×10 −3<br />

∆ t d =5.2×10 −4<br />

∆ t d =5.2×10 −5<br />

True solution<br />

0<br />

0 0.2 0.4 0.6 0.8 1<br />

Dimensionless pressure P =(P−P )/∆p<br />

d i i<br />

2<br />

1.8<br />

1.6<br />

1.4<br />

1.2<br />

1<br />

0.8<br />

0.6<br />

0.4<br />

0.2<br />

Undrained (1 iteration)<br />

∆ t d =2.6×10 −2<br />

∆ t d =1.04×10 −2<br />

∆ t d =5.2×10 −3<br />

∆ t d =5.2×10 −4<br />

∆ t d =2.6×10 −4<br />

True solution<br />

0<br />

0 0.005 0.01 0.015 0.02<br />

Dimensionless displacement (u =u/L )<br />

d z<br />

Figure 4.6: Convergence of the undrained split with one iteration <strong>for</strong> Case 4.1: pressure<br />

(top) <strong>and</strong> displacement (bottom).

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