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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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5.6. NUMERICAL EXAMPLES 159<br />

Figure 5.16: Two test cases to investigate the effect of different η’s. Case 5.5: consolidation<br />

problem with constrained boundary (left picture). Case 5.6: consolidation problem with<br />

unconstrained boundary (right picture).<br />

For Case 5.5, the dimension of the domain is 3 m×14 m with 3×7 grid blocks under the<br />

plane strain mechanical condition. The domain is homogeneous. Grid spacings, ∆x <strong>and</strong> ∆z<br />

are 1 m <strong>and</strong> 2 m, respectively. The domain has an overburden ¯σ = 2×2.125 MPa on the top,<br />

no horizontal displacement boundary on both sides, <strong>and</strong> no vertical or horizontal displace-<br />

ment at the bottom. The bulk density of the porous medium is ρb = 2400 kg m −1 . Initial<br />

fluid pressure is Pi = 2.125 MPa. The fluid density <strong>and</strong> viscosity are ρf,0 = 1000 kg m −1<br />

<strong>and</strong> µ = 1.0 cp, respectively. Permeability is kp = 50 md, <strong>and</strong> porosity is φ0 = 0.3. Young’s<br />

modulus is E = 500 MPa, <strong>and</strong> Poisson’s ratio is ν = 0.0. The Biot coefficient is b = 1.0.<br />

The observation well is located at (2,5). We have a drainage boundary <strong>for</strong> flow on the top,<br />

where the boundary fluid pressure is Pbc = 2.125 MPa. No-flow boundary conditions are<br />

applied to both sides <strong>and</strong> the bottom. Gravity is neglected.

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