06.08.2013 Views

Sequential Methods for Coupled Geomechanics and Multiphase Flow

Sequential Methods for Coupled Geomechanics and Multiphase Flow

Sequential Methods for Coupled Geomechanics and Multiphase Flow

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

144 CHAPTER 5. FIXED-STRAIN AND FIXED-STRESS 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 5.2, τ=0.95<br />

Fixed strain ∆ t d =4.4 × 10 −5<br />

Fixed strain ∆ 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 5.2, τ=1.05<br />

Fixed strain ∆ t d =4.4 × 10 −5<br />

Fixed strain ∆ 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 5.4: Case 5.2 (1D injection–production problem). Results are shown <strong>for</strong> the fixedstrain<br />

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

<strong>and</strong> two very different time step sizes. The stability of the fixed-strain split is independent<br />

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

of time step size.

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!