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Sequential Methods for Coupled Geomechanics and Multiphase Flow

Sequential Methods for Coupled Geomechanics and Multiphase Flow

Sequential Methods for Coupled Geomechanics and Multiphase Flow

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4.4. NUMERICAL EXAMPLES 107<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 />

−2<br />

−2.5<br />

−3<br />

−3.5<br />

−4<br />

−4.5<br />

−1.5<br />

−2<br />

−2.5<br />

−3<br />

−3.5<br />

−4<br />

−4.5<br />

−5<br />

−5.5<br />

−6<br />

Convergence analysis of pressure<br />

FC<br />

Und (1 iter)<br />

−4 −3 −2<br />

log (∆ t )<br />

10 d<br />

−1 0<br />

Convergence analysis of displacement<br />

FC<br />

Und (1 iter)<br />

−4 −3 −2<br />

log (∆ t )<br />

10 d<br />

−1 0<br />

Figure 4.10: Convergence analysis of pressure (top) <strong>and</strong> displacement (bottom) <strong>for</strong> an<br />

incompressible fluid, where τ = 9.5 × 10 11 ∼ = ∞ <strong>and</strong> cf = 3.5 × 10 −20 Pa −1 ∼ = 0. The<br />

undrained split is not convergent, showing zeroth-order accuracy. But, the fully coupled<br />

method shows first-order accuracy.

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