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Sequential Methods for Coupled Geomechanics and Multiphase Flow

Sequential Methods for Coupled Geomechanics and Multiphase Flow

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66 CHAPTER 3. STABILITY OF THE DRAINED AND UNDRAINED SPLITS<br />

Dimensionless pressure (P/P i )<br />

Dimensionless pressure (P/P i )<br />

0.8<br />

0.75<br />

0.7<br />

0.65<br />

Case 3.2, τ=0.95<br />

Drained ∆ t d =4.4 × 10 −5<br />

Drained ∆ t d =4.4 × 10 −2<br />

0.6<br />

0 0.2 0.4 0.6 0.8 1<br />

Dimensionless time (pore volume produced)<br />

0.8<br />

0.75<br />

0.7<br />

0.65<br />

Case 3.2, τ=1.05<br />

Drained ∆ t d =4.4 × 10 −5<br />

Drained ∆ t d =4.4 × 10 −2<br />

0.6<br />

0 0.2 0.4 0.6 0.8 1<br />

Dimensionless time (pore volume produced)<br />

Figure 3.11: Case 3.2 (1D injection–production problem). Results are shown <strong>for</strong> the drained<br />

split with two different coupling strengths: τ = 0.95 (top), <strong>and</strong> τ = 1.05 (bottom) <strong>and</strong> two<br />

very different time step sizes. The stability of the drained split is independent of the time<br />

step size. The drained split is stable if τ < 1 <strong>and</strong> unstable if τ > 1, regardless of the time<br />

step size.

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