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Sequential Methods for Coupled Geomechanics and Multiphase Flow

Sequential Methods for Coupled Geomechanics and Multiphase Flow

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5.6. NUMERICAL EXAMPLES 155<br />

log ||e ||<br />

10 Pd<br />

log ||e ||<br />

10 ud<br />

0.5<br />

0<br />

−0.5<br />

−1<br />

−1.5<br />

Case 5.1. Convergence analysis<br />

−2<br />

−2.5<br />

FC<br />

FSS (1 iter)<br />

FSN (3 iter)<br />

FSN (2 iter)<br />

FSN (1 iter)<br />

−3<br />

−4.5 −4 −3.5 −3 −2.5 −2 −1.5 −1<br />

log (∆ t )<br />

10 d<br />

−2<br />

−2.5<br />

−3<br />

−3.5<br />

−4<br />

Case 5.1. Convergence analysis<br />

FC<br />

FSS (1 iter)<br />

−4.5<br />

FSN (3 iter)<br />

FSN (2 iter)<br />

FSN (1 iter)<br />

−5<br />

−4 −3.5 −3 −2.5 −2 −1.5 −1<br />

log (∆ t )<br />

10 d<br />

Figure 5.13: Convergence analysis of Case 5.1 on pressure (top) <strong>and</strong> displacement (bottom).<br />

∆td = 4cv∆t/Lz 2 . FC, FSS, <strong>and</strong> FSN indicate the fully coupled, fixed-stress, <strong>and</strong> fixedstrain<br />

split methods, respectively. The fixed-strain split shows zeroth-order accuracy. But,<br />

the fixed-stress split yields first-order accuracy.

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