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Sequential Methods for Coupled Geomechanics and Multiphase Flow

Sequential Methods for Coupled Geomechanics and Multiphase Flow

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6.6. NUMERICAL EXAMPLES WITH THE STAGGERED METHOD 205<br />

difference decreases significantly because the fixed-stress split uses updated in<strong>for</strong>mation<br />

from the mechanical problem, capturing the effect of the instantaneous loading. After the<br />

second iteration, the fixed-stress shows the same convergence behavior as the fully coupled<br />

method.<br />

6.6 Numerical Examples with the staggered method<br />

We per<strong>for</strong>m numerical simulation with the staggered method, reusing Case 6.2. The top of<br />

Figure 6.8 shows the results from the drained <strong>and</strong> fixed-strain splits. At early time, the two<br />

splits are stable because the coupling strength is below unity even though they have severe<br />

oscillation. However, the coupling strength increases during simulation because of injection<br />

of the less compressible fluid, namely, water. Then the solutions of the drained <strong>and</strong> fixed<br />

strain splits become unstable because the coupling strength exceeds unity eventually. On<br />

the other h<strong>and</strong>, the undrained <strong>and</strong> fixed-stress splits are stable <strong>for</strong> all time. The bottom of<br />

Figure 6.8 illustrates that the solutions of the undrained <strong>and</strong> fixed-stress splits are stable<br />

with good accuracy with one or two iterations.

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